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DSHW-2024-007988
Revised August 2018 Division of Waste Management and Radiation Control Solid Waste Management Program Mailing AddressOffice Location Phone (801) 536-0200 P.O. Box 144880 195 North 1950 West Fax (801) 536-0222 Salt Lake City, Utah 84114-4880 Salt Lake City, Utah 84116 www.deq.utah.gov APPLICATION FOR A PERMIT TO OPERATE A CLASS II LANDFILL Please read the instructions that are found in the document, INSTRUCTIONS FOR APPLICATION FOR A PERMIT TO OPERATE A CLASS II LANDFILL. This application form shall be used for all Class II solid waste disposal facility permits and modifications. Part I, GENERAL INFORMATION, must accompany a permit application. Part II, APPLICATION CHECKLIST, is provided to assist applicants and, if included with the application, will assist review. Part II is provided to assist in preparation and review of a permit application; it is not required by rule. The text of the rule governs all permit application contents and should be consulted when questions arise. Please note the version date of this form found on the lower right of the page; if you have received this form more than six months after this date it is recommended you contact our office at (801) 536-0200 to determine if this form is still current. When completed, please return this form and support documents, forms, drawings, and maps to: Douglas J. Hansen, Director Division of Waste Management and Radiation Control Utah Department of Environmental Quality PO Box 144880 Salt Lake City, Utah 84114-4880 Utah Class II Landfill Permit Application Form Part I General Information APPLICANT: PLEASE COMPLETE ALL SECTIONS. I. Landfill Type Class II II. Application Type New Application Renewal Application Facility Expansion Modification For Renewal Applications, Facility Expansion Applications and Modifications Enter Current Permit Number III. Facility Name and Location Name of Facility Wayne County-Long Hollow Class II Landfill Site Address (street or directions to site) County Wayne City Loa Zip Code 84747 Telephone 435-836-2731 Township 28 Range 2 Section(s) 21 & 22 Quarter/Quarter Section Quarter Section 1/4 Main Gate Latitude degrees 38 minutes 21 seconds 30 Longitude degrees 111 minutes 41 seconds 16 IV. Facility Owner(s) Information Name of Facility Owner Wayne County Address (mailing) PO Box 189 City Loa State UT Zip Code Telephone 435-836-2731 V. Facility Operator(s) Information Name of Facility Operator Scott Chesnut Address (mailing) PO Box 189 City Loa State UT Zip Code 84747 Telephone 435-491-2771 VI. Property Owner(s) Information Name of Property Owner Wayne County Address (mailing) PO Box 189 City Loa State UT Zip Code 84747 Telephone 435-836-2731 VII. Contact Information Owner Contact Felicia Snow Title Address (mailing) PO Box 189 City Loa State UT Zip Code 84747 Telephone 435-836-2731 Email Address felicia@wayne.utah.gov Alternative Telephone (cell or other) Operator Contact Scott Chesnut Title Address (mailing) PO Box 189 City Loa State UT Zip Code 84747 Telephone 435-491-2771 Email Address nutsonline@hotmail.com Alternative Telephone (cell or other) Property Owner Contact Wayne County-Felicia Snow Title Address (mailing) PO Box 189 City Loa State UT Zip Code 84747 Telephone 435-836-2731 Email Address felicia@wayne.utah.gov Alternative Telephone (cell or other) Utah Class II Landfill Permit Application Form Part I General Information (continued) VIII. Waste Types (check all that apply) IX. Facility Area All non-hazardous solid waste OR the following specific waste types: Waste Type Combined Disposal Unit Monofill Unit Municipal Waste Construction & Demolition Industrial Incinerator Ash Animals Asbestos Other Facility Area............................................................ 199 acres Disposal Area......................................................... 60 acres Design Capacity Years...................................................... 55 Cubic Yards............................................ 606667 Tons....................................................... 273000 X. Fee and Application Documents Indicate Documents Attached To This Application Application Fee: Amount $ Facility Map or Maps Facility Legal Description Plan of Operation Waste Description Ground Water Report Closure Design Cost Estimates Financial Assurance I HEREBY CERTIFY THAT THIS INFORMATION AND ALL ATTACHED PAGES ARE CORRECT AND COMPLETE. Signature of Authorized Owner Representative Dennis Blackburn Name typed or printed Title County Commisioner Date 7/19/24 Address PO Box 189, Loa, UT 84747 Email Address Alternative Telephone (cell or other) 435-896-2765 Signature of Authorized Land Owner Representative (if applicable) Dennis Blackburn Name typed or printed Title County Commisioner Date 7/19/24 Address PO Box 189, Loa, UT 84747 Email Address Alternative Telephone (cell or other) 435-896-2765 Signature of Authorized Operator Representative (if applicable) Scott Chesnut Name typed or printed Title Opperator Date 7/19/24 Address PO Box 189, Loa, UT 84747 Email Address Alternative Telephone (cell or other) 435-896-2765 Important Note: The following checklist is for the permit application and addresses only the requirements of the Division of Waste Management and Radiation Control. Other federal, state, or local agencies may have requirements that the facility must meet. The applicant is responsible to be informed of, and meet, any applicable requirements. Examples of these requirements may include obtaining a conditional use permit, a business license, or a storm water permit. The applicant is reminded that obtaining a permit under the Solid Waste Permitting and Management Rules does not exempt the facility from these other requirements. Please take note of the heading of each section for the facilities that the section applies to. An application for a permit to construct and operate a landfill is the documentation that the landfill will be located, designed, constructed, operated, and closed in compliance with the requirements of Utah Administrative Code R315-301 through 320 (Utah Solid Waste Permitting and Management Rules) and Utah Code Annotated 19-6- 101 through 126 (Utah Solid and Hazardous Waste Act). The application should be written to be understandable by regulatory agencies, landfill operators, and the general public. The application should also be written so that the landfill operator, after reading it, will be able to operate the landfill according to the requirements with a minimum of additional training. Copies of the Solid Waste Permitting and Management Rules, the Utah Solid and Hazardous Waste Act, along with many other useful guidance documents can be obtained by contacting the Division of Waste Management and Radiation Control at 801-536-0200. Most of these documents are available on the Division’s web page at Utah Class II Landfill Permit Application Checklist Page 4 of 5 https://deq.utah.gov/division-waste-management-radiation-control. Guidance documents can be found at the solid waste section portion of the web page. Part II Application Checklist I. Facility General Information Description of Item Location In Document Ia. General Information for All Facilities Completed Part I General information form above General description of the facility (R315-310-3(1)(b)) 1.3 p 6 Legal description of property (R315-310-3(1)€) 1.3 p 5 Proof of ownership, lease agreement, or other mechanism (R315-310-3(1)€) Exhibit 3 Area served by the facility including population (R315-310-3(1)(d)) 1.4 p 6 A demonstration that the landfill is not a commercial facility 1.4 p 6 Waste type and anticipated daily volume (R315-310-3(1)(d)) 1.4 p 6 Ib. Information Required for All New Or Laterally Expanding Facilities Intended schedule of construction (R315-302-2(2)(a)) 2.3 p 8 Name and address of all property owners within 1000 feet of the facility boundary (R315-310-3(2)(i)) Exhibit 1 Documentation that a notice of intent to apply for a permit has been sent to all property owners listed above (R315-310-3(2)(ii)) N/A Name of the local government with jurisdiction over the facility site (R315-310- 3(2)(iii)) 1.2 p 5 Ic. Location Standards for All New And Expanding Facilities Documentation that the facility has met the historical survey requirement of R315-302-1(2)(f) 4.1 p15 Land use compatibility (R315-302-1(2)(a)) 3.8 p 14 Maps showing the existing land use, topography, residences, parks, monuments, recreation areas or wilderness areas within 1000 feet of the site boundary Exhibit 1A Certifications that no ecologically or scientifically significant areas or endangered species are present in site area N/A List of airports within five miles of facility and distance to each N/A Geology (R315-302-1(2)(b)) 3.1 p 12 Geologic maps showing significant geologic features, faults, and unstable areas Exhibit 12 Maps showing site soils Exhibit 6 Surface water (R315-302-1(2)€) 3.6 p 13 Magnitude of 24 hour 25 year and 100 year storm events Average annual rainfall Utah Class II Landfill Permit Application Checklist Page 5 of 5 I. Facility General Information Description of Item Location In Document Maximum elevation of flood waters proximate to the facility 4.1 Maximum elevation of flood water from 100 year flood for waters proximate to the facility 4.1 Wetlands (R315-302-1(2)(d)) N/A Ground water (R315-302-1(2)€) N/A Id. Plan of Operations for All Facilities (R315-310-3(1)€ and R315- 302-2(2)) Forms and other information as required in R3315-302-2(3) including a description of on-site waste handling procedures and an example of the form that will be used to record the weights or volumes of waste received (R315-302-2(2)(b) And R315-310-3(1)(f)) 1.5 p 6 Schedule for conducting inspections and monitoring, and examples of the forms that will be used to record the results of the inspections and monitoring (R315- 302-2(2)€, R315-302-2(5)(a), and R315-310-3(1)(g)) * 1.6 p 6 Contingency plans in the event of a fire or explosion (R315-302-2(2)(d)) 2.13 p 10 Corrective action programs to be initiated if ground water is contaminated (R315- 302-2(2)€) 2.12 p 10 Contingency plans for other releases, e.g. explosive gases* or failure of run-off collection system (R315-302-2(2)(f)) 2.12 p 8 Plan to control fugitive dust generated from roads, construction, general operations, and covering the waste (R315-302-2(2)(g)) 2.15 p 11 Plan for litter control and collection (R315-302-2(2)(h)) 2.16 p 11 Description of maintenance of installed equipment (R315-302-2(2)(i)) 2.17 p 11 Procedures for excluding the receipt of prohibited hazardous or PCB containing wastes (R315-302-2(2)(j)) 2.18 p 11 Procedures for controlling disease vectors (R315-302-2(2)(k)) 2.19 p 12 A plan for alternative waste handling (R315-302-2(2)(l)) 2.20 p 12 A general training plan for site operations (R315-302-2(2)(o)) 2.21 p 12 Any recycling programs planned at the facility (R315-303-4(6)) 2.22 p 12 Closure and post-closure care Plan (R315-302-2(2)(m)) 5.1 p 17 Procedures for the handling of special wastes (R315-315) 2.11 p 10 Plans and operation procedures to minimize liquids (R315-303-3(1)) 2.23 p 12 Plans and procedures to address the requirements of R315-303-3(7)€ through (i) and R315-303-4 Section 2 Approved traffic impact study from the agency with jurisdiction over the roads, including the safety, operation, and condition of roadways serving the proposed facility [Utah Solid and Hazardous Waste Act 19-6-108(9)(g)]. N/A For a facility owned or operated by a local government, disclosure of costs for establishing and operating the facility [Utah Solid and Hazardous Waste Act 19-6- 108(9)(h)]. Section 2 Utah Class II Landfill Permit Application Checklist Page 6 of 5 I. Facility General Information Description of Item Location In Document Any other site-specific information pertaining to the plan of operation required by the Director (R315-302-2(2)(p)) II Facility Technical Information Description of Item Location In Document Iia. Maps for All Facilities Topographic map drawn to the required scale with contours showing the boundaries of the landfill unit, gas monitoring points, and the borrow and fill areas (R315-310-4(2)(a)(i)) Exhibit 1A Most recent U.S. Geological Survey topographic map, 7-1/2 minute series, showing the waste facility boundary; the property boundary; surface drainage channels; any existing utilities and structures within one-fourth mile of the site; and the direction of the prevailing winds (R315-310-4(2)(a)(ii)) Exhibit 2 Iib. Geohydrological Assessment for All Facilities (R315-310- 4(2)(b)) Local and regional geology and hydrology including faults, unstable slopes and subsidence areas on site (R315-310-4(2)(b)(i)) Exhibit 12 Evaluation of bedrock and soil types and properties including permeability rates (R315-310-4(2)(b)(ii)) Exhibit 6 Depth to ground water (R315-310-4(2)(b)(iii)) Exhibit 6 Quantity, location, and construction of any private or public wells on-site or within 2,000 feet of the facility boundary (R315-310-4(2)(b)(v)) Exhibit 7 Tabulation of all water rights for ground water and surface water on-site and within 2,000 feet of the facility boundary (R315-310-4(2)(b)(vi)) Exhibit 7 Identification and description of all surface waters on-site and within one mile of the facility boundary (R315-310-4(2)(b)(vii)) Exhibit 7 For an existing facility, identification of impacts upon the ground water and surface water from leachate discharges (R315-310-4(2)(b)(viii)) NA Calculation of site water balance (R315-310-4(2)(b)(ix)) Exhibit 7 Iic. Engineering Report – Plans, Specifications, And Calculations for All Facilities Documentation that the facility will meet all of the performance standards of R315- 303-2 4.0 Engineering reports required to meet the location standards of R315-302-1 including documentation of any demonstration or exemption made for any location standard (R315-310-4(2)€(i)) 4.0 Anticipated facility life and the basis for calculating the facility’s life (R315-310- 4(2)€(ii)) 4.3 p 15 Unit design to include cover design; fill methods; and elevation of final cover including plans and drawings signed and sealed by a professional engineer registered in the State of Utah, when required (R315-303-3(3), R315-303-3(6) and (7)(a), R315-310-3(1)(b) and R315-310-4(2)(c)(iii)) 4.0 Utah Class II Landfill Permit Application Checklist Page 7 of 5 II Facility Technical Information Description of Item Location In Document Equipment requirements and availability (R315-310-4(2)€(iii)) 4.6 p 16 Identification of borrow sources for daily and final cover and for soil liners (R315- 310-4(2)€(iv)) 4.7 p 16 Run-On and run-off diversion designs (R315-303-3(1)€, (d) and €) 4.10 p 17 Landfill gas monitoring and control plan that meets the requirements of Subsection R315-303-3(5) (R315-310-4(2)€(vii)) 4.9 p 16 Slope stability analysis for static and under the anticipated seismic event for the facility (R315-310-4(2)(b)(i) and R315-302-1(2)(b)(ii)) N/A Design and location of run-on and run-off control systems (R315-310-4(2)€(viii)) 4.0 Iid. Closure Plan for All Facilities (R315-310-3(1)(h)) Closure Plan (R315-302-3(2) and (3)) 5.1 p 17 Closure schedule (R315-310-4(2)(d)(i)) 5.2 p 17 Design of final cover (R315-310-4(2)€(iii)) 5.3 p 17 Capacity of site in volume and tonnage (R315-310-4(2)(d)(ii)) 5.4 p 18 Final inspection by regulatory agencies (R315-310-4(2)(d)(iii)) 5.6 p 19 Iie. Post-Closure Care Plan for All Facilities (R315-310-3(1)(h)) Post-Closure Plan (R315-302-3(5) and (6)) 5.1 p 17 Site monitoring of landfill gases*, and surface water, if required (R315-310- 4(2)€(i)) 5.7 p 20 Changes to record of title, land use, and zoning restrictions (R315-310-4(2)€(v)) 5.8 p 20 Maintenance activities to maintain cover and run-on/run-off control systems (R315-310-4(2)€(iii)) 5.9 p 20 List the name, address, and telephone number of the person or office to contact about the facility during the post-closure care period (R315-310-4(2)€(vi)) 5.10 p 20 Iif. Financial Assurance for All Facilities (R315-310-3(1)(j)) Identification of closure costs including cost calculations (R315-310-4(2)(d)(iv)) 6.3 p 21 Identification of post-closure care costs including cost calculations (R315-310- 4(2)€(iv)) 6.3 p 21 Identification of the financial assurance mechanism that meets the requirements of Rule R315-309 and the date that the mechanism will become effective (R315- 309-1(1)) 6.2 p 21 Revised 1/12/22 U:\SW General Folders\SW-Form\Permit forms\2015-16_Forms\2018_ClassIIApplication&Checklist.docx *A Class II landfill may be able to receive an exemption to gas monitoring by demonstrating through modeling, climatic conditions, and waste acceptance rates that the requirements of R315-303-3(5)(d) of the Utah Administrative Code are met. UTAH CLASS II LANDFILL PERMIT APPLICATION REPORT LONG HOLLOW LANDFILL August 2024 PREPARED BY: Brennan Rees, PE Kelly Chappell, PE 225 North 100 East Richfield, UT 84701 pg. 2 1 Contents 1 Contents ................................................................................................................................................ 2 1.0 APPLICATION ..................................................................................................................................... 5 1.1 INTRODUCTION ............................................................................................................................. 5 1.2 RESPONSIBLE PARTIES .................................................................................................................. 5 1.3 GENERAL DESCRIPTION ................................................................................................................. 5 1.4 WASTE TYPES/AREAS TO BE SERVED ............................................................................................ 6 1.5 REQUIRED FORMS ......................................................................................................................... 6 1.6 INSPECTIONS ................................................................................................................................. 6 1.7 FINANCIAL ASSURANCE................................................................................................................. 8 2 PLAN OF OPERATION ............................................................................................................................ 8 2.1 INTRODUCTION ............................................................................................................................. 8 2.2 HOURS OF OPERATION ................................................................................................................. 8 2.3 SCHEDULE OF CONSTRUCTION ..................................................................................................... 8 2.4 HANDLING PROCEDURES .............................................................................................................. 8 2.5 CONSTRUCTION/DEMOLITION WASTES ....................................................................................... 9 2.6 YARD WASTES ............................................................................................................................... 9 2.7 DEAD ANIMALS ............................................................................................................................. 9 2.8 HOUSEHOLD AND COMMERCIAL WASTE ................................................................................... 10 2.9 INDUSTRIAL WASTES ................................................................................................................... 10 2.10 TIRES ............................................................................................................................................ 10 2.11 SPECIAL WASTE ........................................................................................................................... 10 2.12 CORRECTIVE ACTION FOR CONTAMINATED GROUND WATER .................................................. 10 2.13 CONTINGENCY PLAN FOR OTHER RELEASES ............................................................................... 10 2.14 FIRE/EXPLOSION CONTINGENCY PLAN ....................................................................................... 10 2.15 DUST CONTROL / AIR QUALITY ................................................................................................... 11 2.16 LITTER CONTROL ......................................................................................................................... 11 2.17 EQUIPMENT MAINTENANCE ....................................................................................................... 11 2.18 PROHIBITEDHAZARDOUS/PCB WASTE EXCLUSION PROGRAM .................................................. 11 2.19 DISEASE VECTOR CONTROL......................................................................................................... 12 2.20 ALTERNATIVE WASTE HANDLING ............................................................................................... 12 2.21 TRAINING AND SAFETY ............................................................................................................... 12 pg. 3 2.22 RECYCLING .................................................................................................................................. 12 2.23 PROCEDURE TO MINIMIZE LIQUID.............................................................................................. 12 3 GEOHYDROLOGICAL ASSESSMENT ..................................................................................................... 12 3.1 GEOLOGY ..................................................................................................................................... 12 3.2 HYDROLOGY ................................................................................................................................ 13 3.3 ON SITE SOIL PROPERTIES ........................................................................................................... 13 3.4 GROUNDWATER .......................................................................................................................... 13 3.5 WELLS AND WATER RIGHTS ........................................................................................................ 13 3.6 SURFACE WATERS ....................................................................................................................... 13 3.7 WATER BALANCE / MONITORING ............................................................................................... 13 3.8 IMPACTS TO WATER RESOURCES ............................................................................................... 14 4 PRELIMINARY ENGINEERING REPORT ................................................................................................. 15 4.1 SITING CRITERIA .......................................................................................................................... 15 4.2 SOLID WASTE MANAGEMENT COMPLIANCE .............................................................................. 15 4.3 FACILITY LIFE ............................................................................................................................... 15 4.4 LINER DESIGN .............................................................................................................................. 15 4.5 CELL DESIGN AND OPERATION ................................................................................................... 15 4.6 EQUIPMENT AVAILABILITY .......................................................................................................... 16 4.7 BORROW SOURCES ..................................................................................................................... 16 4.8 LEACHATE COLLECTION TREATMENT AND DISPOSAL ................................................................ 16 4.9 LANDFILL GAS CONTROL AND MONITORING ............................................................................. 16 4.10 RUN-ON/RUN-OFF CONTROL ...................................................................................................... 17 5 CLOSURE / POST CLOSURE PLAN ........................................................................................................ 17 5.1 CLOSURE/POST CLOSURE PLAN .................................................................................................. 17 5.2 CLOSURE SCHEDULE .................................................................................................................... 17 5.3 FINAL COVER, SEEDING, CONTOURING ...................................................................................... 17 5.4 SITE CAPACITY ............................................................................................................................. 18 5.5 CLOSURE TIMING AND NOTIFICATION ....................................................................................... 19 5.6 FINAL INSPECTION ...................................................................................................................... 19 5.7 SITE MONITORING ...................................................................................................................... 20 5.8 LAND TRANSFERS AND USES ....................................................................................................... 20 5.9 POST CLOSURE MAINTENANCE ................................................................................................... 20 5.10 RESPONSIBLE PARTIES ................................................................................................................ 20 pg. 4 6 FINANCIAL ASSURANCE PLAN ............................................................................................................. 21 6.1 INTRODUCTION ........................................................................................................................... 21 6.2 MECHANISMS .............................................................................................................................. 21 6.3 COST ESTIMATE ........................................................................................................................... 21 7 EXHIBITS .............................................................................................................................................. 22 EXHIBITS Exhibit 1: General Vicinity Map Exhibit #1A Boundary Topo Survey (BTS) Exhibit 2: USGS TOPO Map Exhibit 3: Property Patent Exhibit 4a: Record Volume Form Exhibit 4b: Hazardous and PCB Waste Inventory Exhibit 5: Quarterly Inspection Log Exhibit 6: Onsite Soil Data Exhibit 7: Water Rights Map Exhibit 8: HELP Model Results Exhibit 9: Cell Progression Map Exhibit 10: Typical Cell Design Detail Exhibit 11: SHPO Letter Exhibit 12: Geological Map pg. 5 1.0 APPLICATION 1.1 INTRODUCTION This report serves as the renewal application for the Long Hollow Sanitary Landfill located approximately 4 miles Southwest of Loa, Utah in what is known as Long Hollow. Additionally, an expansion of this landfill of approximately 62 acres is also proposed. The purpose of this report is to comply with R-315- 301 through 319 Administrative Rules of the Utah Solid and Hazardous Waste Control Board, Utah Department of Environmental Quality. The landfill is currently located on a 199-acre site. Present operations cover 73 acres. Future expansion, aligned with the site development plan, includes a request for an additional 45 acres to the north and 17 acres to the east, designated as a Class II facility. The landfill currently serves the citizens of Wayne County. 1.2 RESPONSIBLE PARTIES The applicant, property owner, and responsible party for the site operation is: Wayne County Wayne County Courthouse 18 South Main Loa, Utah 84747 Attn: Scott Chesnut Phone:(435)836-2731 Technical questions and comments regarding the application can be directed to: Kelly Chappell, PE or Brennan Rees, PE Ensign Engineering & Land Surveying 225 North 100 East Richfield, UT 84701 Wayne County will notify the Executive Secretary of any changes in responsible party status at least 30 days prior to their effective date. 1.3 GENERAL DESCRIPTION The site is legally described as: THE EAST 1/2 OF THE EAST 1/2 OF THE SOUTHEAST 1/4 SECTION 21, THE EAST 1/2 OF THE SOUTHEAST 1/4 OF THE NORTHEAST 1/4 SECTION 21, THE WEST 1/2 OF THE SOUTHWEST 1/4 SECTION 22, THE SOUTHWEST 1/4 OF THE NORTHWEST 1/4 SECTION 22, AND THE WEST 1/2 OF THE SOUTHEAST 1/4 OF THE SOUTHWEST 1/4 OF SECTION 22, TOWNSHIP 28 SOUTH, RANGE 2 EAST, SALT LAKE BASE AND MERIDIAN. CONTAINING 200.099 ACRES MORE OR LESS (AS SURVEYED ACREAGE) pg. 6 The existing landfill main gate is located at Latitude 38.358662° North and Longitude -111.687593° West. Exhibit 1 depicts a site map and location of the Long Hollow Class II Landfill site. Exhibit 2 contains a USGS 7 1/2 minute map of the site. Exhibit 3 contains the patent for the property. 1.4 WASTE TYPES/AREAS TO BE SERVED The Long Hollow Landfill is expected to receive at least 60-90 tons of waste per week and is considered a Class II facility. The proposed Class II Landfill will accept the following types of waste for disposal or recycling; · household waste (excluding bulk liquids) · non-hazardous industrial waste · commercial waste · dead animals · white goods and scrap metal · tires · yard waste · construction/demolition waste · non-hazardous sludge containing no free liquids · car bodies · non-friable asbestos The service area consists of the entire county including Torrey, Grover, Teasdale, Hanksville, Caineville, Bicknell, Lyman, Fremont, and Loa and the surrounding areas within Wayne County (est. population 2,450). In order to maintain it's municipal, non-profit status, the Long Hollow Sanitary Landfill only accepts waste generated outside the service area if an appropriate interlocal agreement or memorandum of understanding has been executed with the governmental solid waste manager where the waste is generated. 1.5 REQUIRED FORMS The daily record form used to record weights of volumes of waste received required by Subsection R315-302-2(3)(a)(i) is included as Exhibit 4a. The form for recording inspections for hazardous and PCB wastes is included as Exhibit 4b. 1.6 INSPECTIONS The owner or operator will inspect the facility to prevent malfunctions, deterioration, operational errors, and discharges that may result in the release of wastes to the environment or pose a threat to human health. An example of inspection types and frequencies is shown in the table below: Table 1-1 Inspection Types and Frequency Inspection Type Frequency Description Access Road Condition and Maintenance Quarterly Inspections to ensure roads are safe and passable. pg. 7 Fence Inspection and Maintenance Monthly Inspections to maintain the integrity of the landfill’s fencing. Daily Cover Inspection Daily during operation Inspections to ensure proper covering of waste. Post-Closure Final Cover Inspection Monthly Inspections to verify the condition of the final cover post-closure. Drainage Channels Condition Quarterly Inspections to ensure proper drainage and prevent erosion. Landfill Equipment Maintenance As per manufacturer's recommendations Maintenance performed according to manufacturers' recommendations. Gas Monitoring Quarterly Monitoring for landfill gases using a methane detection meter capable of measuring methane at levels below the Lower Explosive Limit (LEL). Documentation: The owner or operator will conduct these inspections based on the frequency outlined in the table and will complete the inspection log included as Exhibit 5. The inspection log will be maintained for a minimum of three years from the date of inspection. Any issues detected during inspections will be documented and addressed promptly. Annual Reporting: An annual report detailing facility activities for the previous year will be prepared and submitted by March 1. The report will include: · Name and address of the facility. · Calendar year covered by the report. · Annual quantity of solid waste received. · Updates on financial assurance mechanisms. · Results of groundwater and gas monitoring. · Details of completed training programs. Access for Inspection: The Executive Secretary or any duly authorized officer, employee, or representative of the Board may, at any reasonable time the facility is open and upon presentation of acceptable credentials, enter the facility for inspection purposes. Certified copies of all sampling, monitoring, and testing records, including photographic, video, and electronic data, and all data communications and results of the inspection, shall be furnished to the owner and operator within 30 days of the inspection. A written summary of the inspection, containing a list of any deficiencies and recommended actions, will be furnished to the owner and operator as soon as practicable. Additionally, the inspector may discuss potential problems and make preliminary recommendations prior to leaving the facility. pg. 8 1.7 FINANCIAL ASSURANCE A detailed financial assurance plan as required by R315-309 is included in other sections of this document. The County has established an escrow account for financial assurance sufficient to assure adequate closure, post-closure care, and corrective action, if required. 2 PLAN OF OPERATION 2.1 INTRODUCTION This Plan of Operation has been prepared by Wayne County to reflect the operation of the Long Hollow Class II Landfill in compliance with the Utah Division of Solid and Hazardous Waste Administrative Rules, R315-302-2(2). 2.2 HOURS OF OPERATION The landfill operator is onsite during all hours the facility is open to the public. The schedule for operation of the Long Hollow Class II Landfill is as follows: Monday: 1 pm - 5 pm Wednesday: 1 pm - 5 pm Friday: 1 pm - 5 pm Saturday: 1 pm - 5 pm 2.3 SCHEDULE OF CONSTRUCTION The Long Hollow Landfill initially completed its construction in 1995, which included the development of the first Class II cell. Over the years, the landfill has continued to meet the solid waste disposal needs of Wayne County. Initial Construction: · 1995: Initial construction of the first Class II cell and associated infrastructure. Expansion and Additional Cells: · Subsequent Years: As the initial Class II cells reached its capacity, additional Class II cells were constructed to the south of the original site. · Current Status: The landfill now includes several Class II cells, with the most recent cell opened to the south to accommodate ongoing and future waste disposal needs. Future Construction Plans: · The Long Hollow Landfill is projected to continue meeting the solid waste disposal requirements for the area for the foreseeable future. · Planning for additional cells will be conducted as needed, with each new cell designed to provide approximately 10-years of capacity, similar to the initial cells. 2.4 HANDLING PROCEDURES All waste placed in the Long Hollow Class II facility will be on the days scheduled. All incoming vehicles are stopped at the gate by the landfill attendant. Commercial and private haul vehicle load weights are pg. 9 estimated based on type and volume of waste. The date, vehicle type, and waste type are recorded on the "Record Volume Form" for every incoming load. A copy of the form is included as Exhibit 4. A receipt is issued for every incoming load. Daily totals are recorded on the "Daily Operating Record" attached as Exhibit 5. Equipment dedicated to the Long Hollow Class II facility for waste and soil handling and general site operations include: · Cat D8 Dozer · Cat 938 loader · Cat 320 Excavator · Cat 316 Compactor · Case 580 backhoe · 3 crew trucks, 5 garbage trucks, 2 dump trucks, water truck, and belly dump Additional equipment is available on an as needed basis from the Wayne County Road Department. Minor vehicle maintenance is performed onsite by the landfill operator. Major repairs are performed either at the Wayne County Road Department facilities or by a contractor. 2.5 CONSTRUCTION/DEMOLITION WASTES UAC 315-301-2(16) defines construction/demolition (C&D) waste as waste from building materials, packaging, rubble resulting from construction, remodeling, repair, and demolition operations on pavements, houses, commercial buildings, and other structures. Typical C&D waste includes bricks, concrete or other masonry materials, soil, rock, untreated lumber, rebar, and tree stumps. All construction/demolition waste is inspected by the landfill attendant, recorded and deposited in the designated cell, and covered with soil as often as is necessary to reduce the potential for fires and vector harborage. 2.6 YARD WASTES Yard waste is vegetative matter generated from landscaping, lawn maintenance, and land clearing operations and may include tree and brush trimmings, grass clippings, and other discarded material from yards, gardens and parks. Yard waste does not include garbage, paper, plastic, sludge, septage, or manure. Loads containing only stumps, branches, tree clippings, and/or grass clippings are directed to the designated yard waste stockpile. After the appropriate permits are obtained from the local fire marshal, all yard waste is burned in accordance with Utah Air Quality requirements. 2.7 DEAD ANIMALS The Long Hollow Class II Landfill accepts dead animals for disposal in a separate monofill within the landfill property. All received dead animals are completely covered with a minimum of six inches of soil by the end of the work day. pg. 10 2.8 HOUSEHOLD AND COMMERCIAL WASTE Most of the waste generated in the County is picked up and hauled to the Landfill by Wayne County Landfill personnel. Incoming waste from commercial and private haulers is discharged at or near the active disposal face. Landfill personnel move discharged loads from the unloading area to the active face. The waste is spread in layers not exceeding two feet in thickness, and compacted. Waste is covered daily with six inches of soil. Wind fences are also placed around the working face of the household/commercial waste cell for litter control. 2.9 INDUSTRIAL WASTES The Long Hollow Landfill does not currently accept industrial waste. However, the facility will accept non-hazardous solid waste generated by industrial sources, provided sufficient documentation is submitted to verify the non-hazardous nature of the material. 2.10 TIRES Tires are currently stockpiled in a designated area until a sufficient amount is accumulated. At that time, the State of Utah is contacted and arrangements are made for tire pickup through the State funded tire recycling program. Operating Records contain the date, volume, and tonnage for materials removed from the landfill. 2.11 SPECIAL WASTE The Long Hollow Landfill includes a designated area specifically for the disposal of special waste in accordance with Utah State Code R315-315. Sludges, if they contain no free liquids, may be placed in the landfill working face and covered with other solid waste or other suitable cover material. 2.12 CORRECTIVE ACTION FOR CONTAMINATED GROUND WATER This section describes corrective actions to be taken by owners and operators to regain compliance with protection levels for the Long Hollow Sanitary Landfill in the event concentration limits are exceeded in a down gradient well as a result of landfill operations. No monitoring wells are proposed for the Long Hollow Landfill. However, if the concentrations of parameters in down gradient wells exceed the concentration limits as a result of landfill operations and as substantiated by confirmatory analyses, owners and operators of the Long Hollow Landfill will implement a corrective action program as outlined in R315-308. 2.13 CONTINGENCY PLAN FOR OTHER RELEASES This section describes corrective actions to be taken by the Long Hollow Sanitary Landfill to regain compliance with the protection levels of the permit in the event releases are discovered and acceptable concentration limits are exceeded. When the concentration of parameters exceeds acceptable limits as substantiated by confirmatory analyses, owners and operators of the Long Hollow Sanitary Landfill will implement a corrective action program approved by the Executive Secretary. 2.14 FIRE/EXPLOSION CONTINGENCY PLAN In the event of a fire or explosion, incoming waste is diverted to the alternate onsite storage area. The waste will be stored until the existing disposal cell can be open or another cell is constructed. Waste will not be stored more than 30 days. Upon resolution of the unexpected event, the materials will be transported to its final destination and treated as incoming waste. pg. 11 Fires and/or explosions at the Long Hollow Class II Landfill are managed and controlled by the landfill operator with equipment available at the site. However, local fire departments are available and will respond to and provide assistance if requested by the landfill operator. The outline for procedures to follow in case of fire or explosion is: 1. Secure Affected Area 2. Divert Incoming Waste 3. Isolate Fire/Explosion 4. Suppress Incident, if Possible 5. Request Additional Assistance as Needed 6. Report & Record Necessary Information 2.15 DUST CONTROL / AIR QUALITY Fugitive dust is not anticipated to reach unacceptable levels at the Long Hollow Sanitary Landfill. If fugitive dust exceeds acceptable levels, actions will be implemented to reduce dust. These actions may include watering access roads, developing wind breaks, altering management scenarios, or other appropriate measures. 2.16 LITTER CONTROL Litter is controlled through use of best management practices. Active areas and working faces are limited; waste is covered shortly after deposition; and blowing trash is confined as much as practical. In addition, litter control fencing may be established along the perimeter of the active area. However, if high winds occasionally occur at the landfill, unacceptable litter escaping the perimeter of the landfill will be periodically picked up by hand. 2.17 EQUIPMENT MAINTENANCE Active collection systems for leachate and/or explosive gases are not proposed for the Long Hollow Sanitary Landfill. Therefore, no maintenance will be required for these items. Maintenance of equipment used in day-to-day operations will be performed by landfill employees or contracted mechanics in accordance with manufacturers recommendations and industry practices. 2.18 PROHIBITEDHAZARDOUS/PCB WASTE EXCLUSION PROGRAM According to UAC R315-303-3(7), an owner or operator shall not knowingly dispose, treat, store, or handle hazardous waste or waste containing PCBs. The following section describes load inspection, training, and handling procedures employed at the Long Hollow Class II facility. All incoming loads are visually inspected by the landfill attendant at or near the active disposal area. Private haul vehicles are also inspected at the gate for the presence of prohibited materials. In addition, a minimum of 1% of all incoming loads are randomly inspected to prevent the disposal of prohibited waste. Random inspection procedures consist of spreading the waste load in a designated area. The landfill operator will then examine the waste and record the findings on the random inspection form pg. 12 contained in Exhibit 4b. The landfill operator is trained to identify regulated hazardous or PCB wastes. The landfill does not accept noncontainerized liquids or liquids in containers larger than 5 gallons. 2.19 DISEASE VECTOR CONTROL The Long Hollow Class II Landfill has limited vector problems. Appropriate cover eliminates the possibility of disease and vector problems within the dead animal area. The cover consists of a 6-inch minimum layer of earthen material. Rodents and other vermin are not permitted to burrow or nest in the active area or recyclable area of the landfill. Trapping or extinction methods are implemented to protect the integrity of the disease vector control program. 2.20 ALTERNATIVE WASTE HANDLING Alternative waste handling procedures for periods when the landfill is not in operation will be similar to procedures for fires and explosions. Waste will be deposited in the emergency disposal site and covered with an approved alternate daily cover. Procedures will continue in this manner until operations at the landfill can return to normal. In the event of equipment breakdown that cannot be repaired in a reasonable time frame, equipment will be borrowed from contributing entities or leased from local distributors. 2.21 TRAINING AND SAFETY The landfill operator has received the proper training enabling him to identify hazardous and exclude hazardous wastes. Safety procedures conform to OSHA guidelines and landfill employees are encouraged to participate in additional landfill management, waste screening, safety and first aid workshops. 2.22 RECYCLING No viable recycling markets currently exist for solid waste disposal at the Long Hollow Sanitary Landfill. 2.23 PROCEDURE TO MINIMIZE LIQUID The landfill will minimize liquids by prohibiting containerized liquids or waste containing free liquids in containers larger than five gallons, non-containerized liquids, and /or sludges' containing free liquids. No waste treatment plant sludge, digested wastewater treatment plant sludge, or septage containing free liquids will be disposed in portions of the landfill containing other solid waste. Water treatment plant sludge, digested wastewater treatment plant sludge, or septage containing no free liquids will be placed at or near the bottom of the landfill working face and covered with other solid waste or other suitable cover material. 3 GEOHYDROLOGICAL ASSESSMENT 3.1 GEOLOGY The project site is situated in the high desert of southwestern Utah, approximately 3.5 miles southwest of Loa. The elevation of the site is approximately 7678 ft. The general soil description is gravely loam. Site-specific geology indicates that the area is predominantly characterized by Millmeadow, which consists of very gravelly loam for the top 8 inches, transitioning to extremely cobbly sandy loam and pg. 13 large boulders or bedrock at varying depths beyond 19 inches. There IS A MAPPED FAULT ON THE EASTERN PROPERTY BOUNDARY. This fault is not known to be active. There is no evidence of unstable slopes, or subsidence areas within the boundaries of the project site. 3.2 HYDROLOGY The climate in the area is mainly dry semi-arid and continental, with well-defined seasons and a wide daily range in temperature. The average length of the frost-free period is from May to October, which can vary considerably each year. Average annual precipitation in the Loa area is approximately 8 to 12 inches. The largest amount of precipitation occurs in the months of September and October, with the least precipitation in February, June, and December. 3.3 ON SITE SOIL PROPERTIES In order to determine on-site soil properties, a field soils classification was performed by Ensign Engineering. Test holes were dug up to a depth of 10 feet. Data from the investigation shows that the soil consists of very gravelly loam at the surface, transitioning to extremely cobbly sandy loam with large cobbles and boulders encountered at depths beyond 19 inches. All samples were classified by the tester at the time of the test. Additional data concerning on-site soils can be found in Exhibit 6. 3.4 GROUNDWATER No groundwater was encountered during the investigative process. Water levels per the wells in the area (closest well is 3.0 miles away), have water levels at approximately 60 to 100 feet or more in depth. 3.5 WELLS AND WATER RIGHTS Based on the Utah Division of Water Rights, no wells were identified within 15,000 feet of the Long Hollow Landfill. There are several wells located west and southeast of Loa Town, however they are located more than three miles from the landfill. Due to the semi-limited precipitation in the area, and existing drainage patterns, the landfill is considered to be hydraulically isolated. Exhibit 7 is a map provided by the Division of Drinking Water showing no wells within 2000 feet of the Landfill. Information is not available regarding background and surface water quality assessments in the area. 3.6 SURFACE WATERS No perennial streams, rivers, or permanent surface waters exist within proximity of the landfill. The closest perennial surface water is Spring Creek located approximately 3.5 miles east of the landfill. Any drainage on site would occur only during large storm events, and would drain to the northeast. Due to the soil characteristics around the landfill, most runoff would infiltrate into the ground before reaching any surface waters except during very large events. 3.7 WATER BALANCE / MONITORING A HELP Model simulation of the Long Hollow Landfill indicates leachate will not develop within 10 ft. of the bottom of the waste during the life of the permit (50 years). Precipitation data was used from the primary station of Fishlake as well as Hanksville Rain Station, and Monticello Stations. The soil in the area is gravely loam. The soil used was loam which used a total porosity of 0.463 vol/vol and a wilting point of 0.116 vol/vol. The model results showed that the max amount of leakage through the bottom layer was 0.020376 inches, which results in 0.01% of the total volume of precipitation on site. In the model, there was little change in volume of water in the bottom five layers, which shows that leakage through those layers and the bottom layer which is de minimus and not a threat to the groundwater in pg. 14 the area. No groundwater monitoring would be required for this landfill. Exhibit 8 show HELP model results. Groundwater monitoring has not been implemented at the Long Hollow landfill and is not anticipated during the life of the permit. Existing depth to groundwater, limited precipitation and extensive evapotranspiration render groundwater monitoring impractical. In addition, on site groundwater monitoring wells could serve as a conduit for contamination. 3.8 IMPACTS TO WATER RESOURCES As a small, arid facility the Long Hollow Landfill is exempt from groundwater monitoring requirements. The landfill receives less than 20 tons of waste per day. It receives less than 25 inches of precipitation per year and is located more than 100 ft. above existing groundwater aquifers. Based on Utah State regulations, these characteristics indicate groundwater monitoring requirements are not necessary. In addition, there is no potential for migration of hazardous constituents from the facility to the groundwater during the active life of the facility and during the post closure period. This conclusion is supported by three separate analyses: 1) onsite geologic and hydrologic conditions, 2) water balance and leachate production modeling, and 3) operational practices which minimize the amount of water that can come in contact with the waste. Each analysis makes its own strong argument for suspending groundwater monitoring requirements. In addition to favorable soil conditions and depths to groundwater which minimize the potential for liquid migration, local climatic conditions prevent the production of significant amounts of leachate. Average annual precipitation is only 7.67 inches per year and the lack of significant moisture passing beyond the vegetative zone is evidenced by the sparsely grown surface plants which are limited by minimum amounts of moisture. Water balance and leachate production modeling also demonstrate a de minimus potential for hazardous constituents reaching groundwater resources. Regional HELP model analysis and site-specific HELP model analysis described above indicates numerous worst-case conditions would be required for leachate to be produced in sufficient quantities to result in the migration of any liquid to the groundwater. Worst case scenarios were used, so actual conditions should result in a greater level of confidence and a lower production of leachate than identified by the model. Operational practices will also reduce the amount of water that could possibly come in contact with the waste. Surface waters will be diverted to protect landfill cells from run on water for storms greater than the 25-year event. The size and progression of the units will result in cells being brought to final elevation and closed in the minimum amount of time possible, reducing the amount of water entering the waste. Contouring operations will reduce ponding and promote drainage away from active areas; use of alternate daily covers may prevent the infiltration of limited precipitation into the waste. The limited working face will require the removal of any snow from the active area, so incoming waste can be deposited. All of these measures result in the reduction of an extremely limited source of moisture. Considering onsite geologic and hydrologic conditions, water balance and leachate production modelling and operational practices which reduce the amount of water contacting the waste, groundwater monitoring and vadose zone monitoring are not justified. In fact, installation of monitoring wells may provide a more viable conduit for groundwater contamination. The Executive Secretary is requested to pg. 15 exempt the Long Hollow Sanitary Landfill from groundwater monitoring requirements in accordance with Subsection R315-303-3.(3)(e)of the Solid Waste Rules. 4 PRELIMINARY ENGINEERING REPORT 4.1 SITING CRITERIA The proposed Long Hollow Sanitary Landfill complies with siting criteria currently mandated by regulation and recognized by the State of Utah Solid and Hazardous Waste Committee. Specifically, no airport is located within 10,000 feet of the proposed landfill. The site is free from unstable areas and is not located within a 100-year floodplain or in any wetland. In addition to federal mandated criteria, the site is compatible with existing land uses for long term landfill operation and is in a remote area free from dwellings and other incompatible structures such as churches, schools, hospitals, etc. Cultural resources within the landfill will be mitigated in accordance with State Historic Preservation Officer (SHPO) requirements. SHPO has been contacted and their response is pending. 4.2 SOLID WASTE MANAGEMENT COMPLIANCE The Wayne County Solid Waste Management Plan required by Senate Bill 255 identifies the need for re- permitting and or development of landfills capable of long-term service in the planning area. The plan further supports continuation of the landfill. The Long Hollow Sanitary Landfill is in complete compliance with the County's Solid Waste Management Plan. 4.3 FACILITY LIFE The anticipated facility life for the Long Hollow Landfill cannot be accurately estimated. Based on the overall size of the property, relatively low waste volumes. and current efficiencies, facility life is estimated far in excess of the permit but is considered 10 years for this permit renewal process. 4.4 LINER DESIGN Current volumes of solid waste disposed, as measured by scales serviced by the Long Hollow Landfill, are well below 20 tons per day, and the facility is eligible for the small landfill design exemptions. The landfill meets all the requirements of the small landfill exemption as explained in R315-303-3 i.e. the average precipitation is less than 25 inches per year, with no evidence of groundwater contamination, and no reasonable alterative. These exemptions include liner design and groundwater monitoring. When average annual volumes exceed 20 tons per day, the Long Hollow Sanitary Landfill may have to design disposal cells with liners, leachate collection and groundwater monitoring. Final cover on the facility will be an Evapotransformation (ET) Cover. This ET cover initially consists of at least 12 inches of native material from the approved source covered with at least 24 inches of additional soil to protect from frost damage. Managers of the landfill may (with approval of the Executive Secretary) install synthetic liners, covers, or other alternate systems if the are deemed to meet the code requirements. 4.5 CELL DESIGN AND OPERATION The Long Hollow Sanitary Landfill is designed to minimize active areas and to reach final elevation as soon as practical in order to minimize infiltration and leachate generation. The cells are designed to accommodate from two to five years of waste and to expand in an orderly fashion. Cells may be excavated as much as 40 feet deep and may extend approximately 50 feet in height. Bottom widths will range from 40 feet to 100 feet. Length and height of the cells will vary with volumes pg. 16 of waste, season of the year. and soil stockpile needs: but initial excavation will approximate 100 feet. Current proposals contemplate providing a minimum of 1 year excess excavated area for growth and unexpected problems. Excavated interior side slopes will originally be 4:1 and may be steepened to 2:1 immediately before receiving waste to expand capacity and augment covering. operations. Near the close of each working day waste will be spread, compacted, and covered with 6 inches of native soil or an alternate daily cover. When daily waste volumes are too small to permit efficient use of landfill space, solid waste will be stockpiled at the working face and covered with an alternate daily cover (a synthetic blanket designed to prevent infiltration). The 40-foot cell height described earlier is a nominal dimension and does not consider final slopes to promote drainage or additional covering requirements. Cells are anticipated to follow existing contours and to consist of solid waste compacted in lifts ranging from 7 feet to 12 feet and covered with 6 inches to 12 inches of daily or intermediate cover material. Exhibit 9 is an illustration of the proposed cell progression. Exhibit 10 is a conceptual design of a typical cell. 4.6 EQUIPMENT AVAILABILITY Minimum equipment requirements at the Long Hollow Sanitary Landfill are limited to a track-type loader for daily operations and periodic use of additional equipment (dozer, scraper, grader, compactor, etc.) for specific covering, stockpiling, contouring and compacting operations. The facility will have equipment mobilized to the site as needed and will utilize other equipment from the Wayne County Road Department pool as needed. Overtime, adequate equipment will be acquired to guarantee the needs of the landfill will be met in a timely manner. 4.7 BORROW SOURCES The Long Hollow Sanitary Landfill will generally utilize onsite borrow materials for daily cover, final cover, and soil liners. Current estimates indicate adequate material is available within the landfill limits. Existing cell location utilizes excavated on site material and provides for ongoing borrow operations. Onsite soils will be augmented with existing offsite borrow sources as needed. These borrow sources include local clays that have been used during the operation of the existing facility and will continue to be used to their greatest utility. 4.8 LEACHATE COLLECTION TREATMENT AND DISPOSAL The Long Hollow Sanitary Landfill is a natural attenuation facility located in an arid region with favorable soil conditions. No leachate collection and disposal will occur at the facility. 4.9 LANDFILL GAS CONTROL AND MONITORING Due to the arid nature of the climate at the Long Hollow Sanitary Landfill and the nature of the waste accepted at the facility, landfill gas concentrations are not anticipated to reach significant levels. The relatively open area of the proposed facility is designed to accommodate dissipation of any landfill gases prior to reaching the property boundary. Monitoring for landfill gases will be conducted as part of the quarterly inspections performed by landfill managers. Concentration will be measured in the existing structures. Results will be recorded on quarterly inspection forms. Should unacceptable levels of landfill gases be detected, contingency plans described in other areas of this permit will be implemented. If gas levels exceed 25% of the lower explosive limit in structures or the pg. 17 100% of the lower explosive limit at property boundaries, immediate action will be taken to protect human health, and the Executive Secretary will be contacted within 24 hours. Additional state regulation, including operating record notations within seven days and implementation of a remediation plan within sixty days, will be completed. 4.10 RUN-ON/RUN-OFF CONTROL The County will control the run on and runoff resulting from storms smaller than the 25- year event from contacting solid waste and leaving the landfill. This will be accomplished through a series of best management practices. Any potential surface drainages will be diverted around cells. Daily, intermediate and final cover material will be excavated from the uphill side of active areas and will be accumulated at the interface between the natural ground and the waste cell. Doing this will create excavated areas and berms to prevent any surface waters from contacting the waste. Runoff will he controlled through ditches, berms, roads, culverts, and other passive systems as needed. 5 CLOSURE / POST CLOSURE PLAN 5.1 CLOSURE/POST CLOSURE PLAN Closure of active portions of the Long Hollow Sanitary Landfill contemplates controlling, minimizing, and eliminating threats to human health and the environment from post closure escape of solid waste constituents, contaminated runoff or waste composition products to the ground, groundwater, surface water, and the atmosphere. When an area of the landfill exceeding 10,000 square yards reaches final elevation, it will be covered within 60 days with 12 inches of intermediate cover and graded to promote drainage. The surface shall be free from ponding and shall minimize infiltration. Not more than 6 months after completion of the intermediate cover, the area will be covered with a minimum of 18 inches of material having a hydraulic conductivity of less, than 1 x 10" cm/sec or an alternate final cover approved by the Executive Secretary. The impermeable barrier will be covered with 6 inches of native soil or 6 inches of material capable of supporting, vegetative growth. The final slope shall not exceed 33% nor be less than 2%. Post closure care of inactive sections of the landfill will consist of maintaining the integrity of the final and vegetative covers. Any areas subject to erosion will also be corrected; and appropriate measures will be implemented to identify and eliminate the source. Groundwater monitoring, leachate collection, and gas collection are not proposed for the Long Hollow Sanitary Landfill. Therefore, closure and post closure activities associated with these functions will not be performed. 5.2 CLOSURE SCHEDULE Closure operations at the Long Hollow Sanitary Landfill will be performed on an ongoing basis. Adequate capacity exists at the landfill to continue operation for many years. A final closing date cannot be determined at this time. Ongoing closure operations will generally be performed from May through October, the normal frost-free construction period, or as weather permits. No area larger than 2 acres that has achieved final elevation will remain open longer than 6 months. 5.3 FINAL COVER, SEEDING, CONTOURING Closure operations will consist of leveling, contouring, and placement of appropriate covers and seeding as necessary to reduce infiltration and preserve the integrity of the completed areas of the landfill. pg. 18 Areas of the landfill reaching final elevation will be closed within 6 months. Closure operations will include leveling and contouring using intermediate cover to reduce infiltration and ponding. Excess material may be stripped and utilized in other operations or left in place. After grading operations promoting drainage are complete, a geosynthetic clay liner or 18 inches of material with a permeability of 1 x 10” cm/sec or less will be installed. Geosynthetic clay liners and other compatible covering systems may be used when permeability characteristics are equal to or better than earthen materials. Alternate designs meeting the performance standard of impermeable material may be used if approved by the Executive Secretary prior to placement. Upon completion of the impermeable cover, closed areas will be seeded. The seed mixture shall be developed after consultation with BLM range specialists and verifying availability of local seed markets. Recently closed sections of the landfill will be evaluated as part of the quarterly inspection process during the first year and then placed on post closure status. 5.4 SITE CAPACITY The site capacity for the entire Long Hollow Sanitary Landfill cannot be accurately estimated due to various factors affecting its future use and development. However, based on current operations and available land, the following assumptions can be made: The landfill is currently located on a 199-acre site. Present operations cover 73 acres. Future expansion, aligned with the site development plan, includes a request for an additional 45 acres to the north and 17 acres to the east, designated as a Class II facility. The landfill currently serves the citizens of Wayne County. · Remaining Land: It is estimated that 62 acres of the original 199.64 acres are proposed and requested for future landfill operations. · Trench Style Operation: o Dimensions: 40 ft. bottom width, 300 ft. length, 220 ft top width, 480 ft. length 3:1 side slopes, with a depth of 30 ft. o Lifts: Three 8.5-foot lifts of waste with a 1.5-foot intermediate cover. o Waste Density: An average density of 900 lbs. per cubic yard. Using these assumptions, the estimated waste volumes can be calculated as follows: · Site Area Used: 62 acres (2,700,720 square feet) · Trench Volume Calculation: o Each trench has a volume of: Cross Sectional Area: × 220 + 40 × 30 = 3,900 . . Depth: 30 ft pg. 19 Volume per trench: 3,900 sq. ft. × 300 ft = 1,170,000 cubic feet · Total Volume for 14 trenches: Total volume = 1,170,000 cu.ft × 14 trenches = 16,380,000 cu.ft.÷ 27 (). .= 606,667 ().*+. · Waste Volume Calculation: o Applying 900 lbs. per cubic yard: Total waste in tons = 606,0667 cu.yd. × 900 lbs.per cu.yd. ÷ 1 23 2000 45 = 273,000 tons Therefore, the estimated site capacity, using the remaining 62-acres, is approximately 606,667 cubic yards or 273,000 tons of waste. 5.5 CLOSURE TIMING AND NOTIFICATION Closure activities at the Long Hollow Sanitary Landfill will be performed on an ongoing basis. The Executive Secretary will be notified of closure progress by reviewing quarterly and annual reports and by contacting Division of Solid and Hazardous Waste inspectors who have visited the site. Considering the ongoing nature of closure operations and the justification for performing closure operations as a cell reaches final elevation, alternate notification procedures may not be feasible. In addition to the ongoing notification indicated above, the Executive Secretary will be notified in writing prior to initiation of final cover operations and the final cover design and the construction quality assurance/quality control (QA/QC) plan will be submitted to the Executive Secretary for review and approval. The QA/QC plan for closure will include tests for permeability and depth. Permeability tests, where required, will be performed at the rate of a test per 3000 cubic yards of material and will randomly selected throughout the working area. Permeability tests may include in field or laboratory tests, nuclear density extrapolations, or other industry wide procedures and practices. Depth tests will utilize standard cross section survey methods and will be performed at a rate equal to or greater than tests performed for permeability. Closure as-builts and certification of closure according to the plan identified above will be signed by a registered professional engineer and forwarded to the Executive Secretary within 90 days of completion. 5.6 FINAL INSPECTION The Long Hollow Landfill is anticipated to operate well beyond the life of this permit. At least 60 days prior to any closure, the Division of Solid and Hazardous Waste will be contacted, and a final inspection will be scheduled. The Executive Secretary will be informed of incremental closures of individual cells through routine state inspections, annual reports, and renewal applications. In addition, a QA/QC plan will be submitted for approval prior to any closure operations. Within 90 days of unit and/or facility closure, as built plans signed by a professional engineer shall be forwarded to the Executive Secretary. Landfill owners and operators shall allow the Executive Secretary of the Utah Solid and Hazardous Waste Control Board or an authorized representative, including representatives from the local District Health Department, upon representation of credentials, to enter during operating hours and/or inspect at reasonable times any facilities, equipment, practices or operations regulated or required under this permit. pg. 20 A record of the inspection may be made by photographic, videotape, electronic or other reasonable means. A copy of any such record shall be provided to the owner and the operator within a reasonable time. 5.7 SITE MONITORING No permanent monitoring devices are proposed for the Long Hollow Sanitary Landfill. Landfill gas in closed sections will be monitored as described for active cells in the Preliminary Engineering Report section of this document. No groundwater monitoring wells, lysimeters, vadose zone equipment or other monitors are planned for this facility. Surface waters in closed portions of the landfill will be evaluated as part of the annual inspection. Monitoring will be limited to identifying situations which promote infiltration. 5.8 LAND TRANSFERS AND USES Plats and a statement of fact concerning the location of any disposal site shall be recorded as part of the record of title with the County Recorder not later than 60 days after certification of closure. Upon recording, proof of the record of filing will be submitted to the Executive Secretary. 5.9 POST CLOSURE MAINTENANCE Post-closure care of inactive sections of the landfill will consist of maintaining the integrity of the final and vegetative covers. Any areas subject to erosion will be corrected and appropriate measures will be implemented to identify and eliminate the source. No active or technical devices are proposed for use at the Long Hollow Sanitary Landfill. Best management practices will be implemented to minimize infiltration and assure the integrity of the run-on/run-off system. Evaluation of the system will be made during the quarterly inspections and corrective measures, if any, will be implemented. Run-on and run- off from events smaller than the 25-year storm will be controlled by way of ditches, berms and use of machinery to ensure proper run-off. No leachate collection devices are proposed for the facility. Closed portions of the landfill will be inspected as part of the quarterly reviews performed by the landfill operator. Closed areas will also be inspected as part of the in-depth annual inspection. Any deficiencies will be repaired as soon as practical. For those failures which jeopardize the environmental integrity of the facility or permit the uncontrolled infiltration of significant amounts of moisture, corrective measures will be initiated immediately. No alternate land use for closed sections has been developed to date. Closed cells will remain under the jurisdiction of the landfill manager. If alternate land use plans are developed, they will be addressed during the permit renewal process or a separate permit modification may be processed. 5.10 RESPONSIBLE PARTIES The applicant, property owner, and responsible party for the post closure care period is: Wayne County Wayne County Courthouse 18 South Main Loa, Utah 84747 Attn: Scott Chesnut Phone: (435) 836-2731 pg. 21 It should be noted Wayne County is continually upgrading solid waste management services. Future agreements, potential special service district creation, the extended life of the landfill, and alternate ownership/operation scenarios may require modification of this section of the permit. In addition, the County may contract site operations with private entities. The County will notify the Executive Secretary of any changes in responsible party status at least 30 days prior to their effective date. Other changes to the information listed above will be provided in annual reports and permit renewal documents. 6 FINANCIAL ASSURANCE PLAN 6.1 INTRODUCTION This section of the permit describes compliance with Subsection R315-309, Financial Assurance of the Administrative Rules for Solid Waste Permitting and Management. Cost estimates consider the most expensive option during the period and are based on a third-party performing closure and post closure care. 6.2 MECHANISMS The mechanism used at the Long Hollow Sanitary Landfill is a dedicated escrow/capital improvement account. The account is established with the State Treasurer's Office, and the Utah State Treasurer serves as the escrow agent. A detailed set of procedures has been established by the Treasurer's office. Funds in excess of the estimate listed below may be used for capital improvements, to offset rate increases, operational expenses and other items deemed necessary by landfill managers. The Long Hollow landfill may alter the mechanism to include insurance, surety bonds, trust funds, or other options as they become feasible with Executive Secretary approval. 6.3 COST ESTIMATE Closure and post-closure cost estimates were developed considering the largest area of the disposal facility requiring final cover during the operating period and using projections for a third party to perform the work. Estimates were developed using Utah State guidance, historical costs, project records and standardized rates for Wayne County. A cost estimate summary identifying major closure and post- closure components is included below. Items that are identified in the rules but are not applicable to the Long Hollow Landfill have not been listed. pg. 22 7 EXHIBITS Exhibit #1: General Vicinity Map Exhibit #1A Boundary Topo Survey (BTS) Exhibit #2: USGS TOPO Map Exhibit #3: Property Patent Exhibit #4a-4b: Record Volume Form and Hazardous and PCB Waste Inventory Exhibit #5: Quarterly Inspection Log Exhibit #6: Onsite Soil Data Exhibit #7: Water Rights Map Exhibit #8: HELP Model Results Exhibit #9: Cell Progression Map Exhibit #10: Typical Cell Design Detail Exhibit #11: SHPO Letter Exhibit #12: Geological Map ITEM DESCRIPTION UNIT QUANTITY UNIT COST TOTAL 1. Closure Costs 100 Soil Placement (Topsoil) CY 7,000 10.00$ 70,000.00$ 101 Soil Placement (18" compacted) CY 9,000 12.00$ 108,000.00$ 102 Seeding Acre 5 200.00$ 1,000.00$ 103 Correctional Plans and Specifications EA 1 10,000.00$ 10,000.00$ 104 Grading LS 1 15,000.00$ 15,000.00$ 105 Contigency LS 1 20,000.00$ 20,000.00$ 224,000.00$ 2. Post-Closure Costs 200 Engineering/Project Management/Admin LS 1 25,000.00$ 25,000.00$ 201 Cover Maintenance LS 1 5,000.00$ 5,000.00$ 202 General Maintenance LS 1 5,000.00$ 5,000.00$ 35,000.00$ 259,000.00$ Subtotal GRAND TOTAL Subtotal SITLA 2031 South Industrial Park Road Richfield, Utah 84701 BLM 150 E 900 N, Richfield, UT 84701 PRIVATE LONG HOLLOW LANDFILL SITLA 2031 South Industrial Park Road Richfield, Utah 84701 SITLA 2031 South Industrial Park Road Richfield, Utah 84701 BLM 150 E 900 N, Richfield, UT 84701 BLM 150 E 900 N, Richfield, UT 84701 HORIZONTAL GRAPHIC SCALE 0 ( IN FEET ) HORZ: 1 inch = ft.200 200 100 200 400 LOCATED IN THE EAST HALF OF SECTION 22 AND THE WEST HALF OF SECTION 21, TOWNSHIP 28 SOUTH, RANGE 2 EAST, SALT LAKE BASE AND MERIDIAN WAYNE COUNTY, UTAH ENSIGN ENG. LAND SURV. SECTION CORNER-BRASS CAP MONUMENT SET RIVET SET ENSIGN REBAR AND CAP BUILDING PRIMARY ADJACENT RIGHT OF WAY RIGHT OF WAY CENTERLINE PROPERTY LINE ADJACENT PROPERTY LINE DEED LINE GRAVEL DRIVE FENCE LEGEND X DESIGNED BY PROJECT NUMBER FOR: PROJECT MANAGER PRINT DATE PHONE: CONTACT: WWW.ENSIGNENG.COM RICHFIELD 225 N 100 E Richfield, UT 84701 Phone: 435.896.2983 SANDY Phone: 801.255.0529 LAYTON Phone: 801.547.1100 TOOELE Phone: 435.843.3590 CEDAR CITY Phone: 435.865.1453 13336 LO N G H O L L O W L A N D F I L L LO A L A N D F I L L R D . LO A , U T A H WAYNE COUNTY CLIENT'S ADDRESS CLIENT CITY STATE ZIP CLIENT CONTACT 801.000.0000 K. CHAPPELL B.REES 2024-07-25 EXHIBIT-1 VICINITY MAP CALL BLUESTAKES @ 811 AT LEAST 48 HOURS PRIOR TO THE COMMENCEMENT OF ANY CONSTRUCTION.Know what's below. before you dig.Call R FOUND REBAR AND ALUMINUM CAP (LS 6295) FOUND REBAR AND ALUMINUM CAP (LS 6295) FOUND REBAR AND ALUMINUM CAP (LS 6295) FOUND REBAR AND ALUMINUM CAP (LS 6295) FOUND REBAR AND ALUMINUM CAP (LS 6295) FOUND REBAR AND ALUMINUM CAP (LS 6295) S 0 ° 1 8 ' 3 9 " W 2 6 4 1 . 1 7 ' S 0 ° 1 8 ' 3 9 " W 2 6 4 1 . 9 7 ' N 89°49'40" W 2647.02'S 89°51'50" E 2636.80' FOUND REBAR AND ALUMINUM CAP (LS 6295) BLM BLMBLM BLM BLM BLM X X X X X X X X X X X X OH P OH P OH P OH P OH P OH P OH P OH P N 0 ° 1 7 ' 3 3 " E 5 2 8 2 . 9 9 ' BA S I S O F B E A R I N G EXISTING BUILDINGS 7655 7660 7665 767 0 7675 7680 76 8 5 769 0 769 5 7700 77 0 5 77 1 0 77 1 5 77 2 0 772 5 77 3 0 77 3 5 77 4 0 7 7 4 5 77 5 0 7 7 5 5 776 0 776 5 7 6 1 0 7 6 1 5 7 6 2 0 7 6 2 5 7 6 3 0 7 6 3 5 7640 7 6 4 5 76 5 0 7 6 5 5 7 6 6 0 75 9 0 7 5 9 5 7 6 0 0 76 0 5 76 1 0 76 1 5 76 1 5 7 6 1 5 76 2 0 76 2 5 76 3 0 76 3 5 76 4 0 7 6 4 5 7 6 1 0 7615 76 2 0 76 2 5 7630 7635 764 0 76 4 5 765 0 7 6 5 5 7 6 6 0 7 6 6 5 7 6 7 0 76 7 5 7680 7 6 8 5 7690 7 6 9 5 7 7 0 0 7615 7620 7625 7630 7635 7640 76 4 5 7650 7655 7660 76 6 5 76 7 0 7675 7 6 8 0 7 6 8 5 76 9 0 7 6 9 5 7690 7695 7700 77 0 5 7645 7650 7655 76 6 0 766 5 7670 7675 7680 7685 7690 7695 7700 7705 7710 7715 772 0 772 5 773 0 763 5 76 3 5 7 6 4 0 7640 76 4 5 7645 7650 76 2 0 7 6 2 0 762 5 76 2 5 7 6 3 0 763 0 76 3 5 7 6 3 5 76 4 0 7 6 4 0 766 5 7 6 7 0 7 6 7 5 7680 7685 7690 7695 7680 7680 7685 7690 7 6 8 5 7 6 9 0 7690769 5 77 0 0 7 7 0 5 7 7 0 0 77 0 5 77 1 0 77 1 5 7 7 2 0 7 7 2 5 7 7 3 0 77 3 5 7730 7 7 3 5 7715 7705 76 9 0 7 6 9 5 7 7 0 0 769 0 7 6 9 5 7700 7655 766 0 76 6 5 76 7 0 7 6 7 5 7680 76 1 0 7 6 3 0 7 6 4 0 76 4 5 7 6 5 0 76 5 5 7 6 1 5 759 0 759 5 760 0 7605 7610 7615 7620 7625 7630 7635 7640 7645 7650 7715 7720 772 5 77 3 0 77 3 5 77 0 5 7 7 1 0 FOUND REBAR N 89°49'26" W 1322.33' S 89°52'27" E 2637.95' BLM BLM BLM N 89°49'26" W 3965.42' S 89°52'27" E 2637.64' S 0 ° 1 7 ' 3 3 " W 2 6 4 1 . 5 0 ' S 0 ° 1 7 ' 3 3 " W 2 6 4 1 . 4 9 ' BLM XX X X X X X X X X X X X X X X X X X X X X X X X X X X X X X X X X X X X X X X X X X X X SITE LOA LONG HOLLOW RD. MAIN ST. HORIZONTAL GRAPHIC SCALE 0 ( IN FEET ) HORZ: 1 inch = ft.200 200 100 200 400 LOCATED IN SECTION 21 AND SECTION 22, TOWNSHIP 28 SOUTH, RANGE 2 EAST, SALT LAKE BASE AND MERIDIAN WAYNE COUNTY, UTAH DESIGNED BY PROJECT NUMBER FOR: PROJECT MANAGER PRINT DATE PHONE: CONTACT: WWW.ENSIGNENG.COM RICHFIELD 225 N 100 E Richfield, UT 84701 Phone: 435.896.2983 SANDY Phone: 801.255.0529 LAYTON Phone: 801.547.1100 TOOELE Phone: 435.843.3590 CEDAR CITY Phone: 435.865.1453 13336 1 OF 1 WA Y N E C O U N T Y L A N D F I L L BO U N D A R Y A N D T O P O G R A P H I C S U R V E Y LO N G H O L L O W R O A D WA Y N E C O U N T Y U T A H BOUNDARY AND TOPOGRPHIC SURVEY WAYNE COUNTY 18 S MAIN ST. LOA, UT 84747 - 435-836-1300 KLC DDS 2024-08-01 SOUTHWEST CORNER OF SECTION 22, T.28 S., R.2 E., S.L.B. & M. FOUND 1915 U.S.G.L.O. BRASS CAP BENCHMARK SOUTHWEST CORNER OF SECTION 22, TOWNSHIP 28 SOUTH, RANGE 2 EAST SALT LAKE BASE AND MERIDIAN ELEV = 7712.87' SOUTH QUARTER CORNER OF SECTION 22, T. 28 S., R.2 E., S.L.B. & M. (CALCULATED) NORTHWEST CORNER OF SECTION 22, T.28 S., R.2 E., S.L.B. & M. FOUND 1915 U.S.G.L.O. BRASS CAP NORTH QUARTER CORNER OF SECTION 22, T.28 S., R.2 E., S.L.B. & M. (CALCULATED) SOUTH QUARTER CORNER OF SECTION 21, T.28 S., R.2 E., S.L.B. & M. (CALCULATED) NOT TO SCALE VICINITY MAP ENSIGN ENG. LAND SURV. LEGEND DEED DESCRIPTION THE EAST 1/2 OF THE EAST 1/2 OF THE SOUTHEAST 1/4 SECTION 21, THE EAST 1/2 OF THE SOUTHEAST 1/4 OF THE NORTHEAST 1/4 SECTION 21, THE WEST 1/2 OF THE SOUTHWEST 1/4 SECTION 22, THE SOUTHWEST 1/4 OF THE NORTHWEST 1/4 SECTION 22, AND THE WEST 1/2 OF THE SOUTHEAST 1/4 OF THE SOUTHWEST 1/4 OF SECTION 22, TOWNSHIP 28 SOUTH, RANGE 2 EAST, SALT LAKE BASE AND MERIDIAN. CONTAINING 200.099 ACRES MORE OR LESS (AS SURVEYED ACREAGE) NOTES 1. THE PURPOSE OF THIS SURVEY WAS TO LOCATE THE BOUNDARY OF THE HEREON SHOWN AND DESCRIBED PARCEL OF LAND. 2. THE BASIS OF BEARING USED WAS N00°17'33"E BETWEEN THE SOUTHWEST CORNER AND THE NORTHWEST CORNER OF SECTION 22, T.28 S., R.2 E., S.L.B. & M. 3. THE BOUNDARY INFORMATION SHOWN HEREON WAS TAKEN FROM THE JONES AND DEMILLE ENGINEERING PROPERTY SURVEY FOR WAYNE COUNTY LANDFILL DATED 11/17/94 AS FOUND IN THE OFFICE OF THE WAYNE COUNTY RECORDER, FILE NUMBER 85. THE JONES AND DEMILLE ENGINEERING SURVEY WAS ROTATED CLOCKWISE 00°04'33" TO MATCH THE BASIS OF BEARING OF THIS SURVEY. 4. THE CONTOURS WERE OBTAINED USING A DRONE FLIGHT. X SECTION CORNER AS NOTED MONUMENT EXISTING REBAR AND CAP AS NOTED SET ENSIGN REBAR AND CAP SURVEYED BOUNDARY LINE SECTION LINE QUARTER SECTION LINE SIXTEENTH SECTION LINE EXISTING FENCE EXISTING EDGE OF ASPHALT EXISTING BUILDING EXISTING OVERHEAD POWERLINE EXISTING CENTERLINE GRAVEL / DIRT ROAD EDGE OF GRAVEL ROAD OHP WEST QUARTER CORNER OF SECTION 21, T.28 S., R.2 E., S.L.B. & M. (CALCULATED) EAST QUARTER CORNER OF SECTION 22, T.28 S., R.2 E., S.L.B. & M. (CALCULATED) SURVEYORS CERTIFICATE I, TREVOR R. GADD, A PROFESSIONAL LAND SURVEYOR AS PRESCRIBED BY THE LAWS OF THE STATE OF UTAH, HOLDING CERTIFICATE #343639, CERTIFY THAT THE SURVEY SHOWN HEREON WAS MADE UNDER MY DIRECTION. I FURTHER CERTIFY THAT THIS PLAT CORRECTLY SHOWS THE DIMENSIONS OF THE PROPERTY SURVEYED. TREVOR ROY GADD No. 343639 P ROF E S S I O N A L L A ND S U R V E Y O R S TATE O F U T A H 08/01/2024 ―│―│―│―│―│ ―│―│ ―│ ―│ ―│―│―│―│ ―│―│―│―│ ―│―│―│―│ ―│―│―│ ―│―│―│ ―│―│―│ ―│―│―│ ―│―│―│―│ ―│―│―│―│ ―│―│―│―│ ―│―│―│―│ ―│―│―│―│ ―│―│―│―│ ―│―│―│―│ ―│―│―│―│ ―│―│―│ ―│―│―│ ―│―│ ―│―│ ―│―│―│ ―│―│―│ ―│―│ ―│―│ ―│―│ ―│―│ ―│ ―│ ―│―│ ―│―│ ―│ ―│ ―│ ―│―│―│―│―│―│ ―│―│―│―│―│―│ ―│―│―│―│―│―│ ―│―│―│―│―│―│ ―│―│―│―│―│―│ ―│―│―│―│―│―│ ―│―│―│―│―│―│ ―│―│―│―│―│―│ ―│―│―│―│―│―│ ―│―│―│―│―│―│ ―│―│―│―│―│―│ ―│―│―│―│―│―│ ―│―│―│―│―│―│ ―│―│―│―│―│―│ ―│―│―│―│―│―│ ―│―│―│―│―│―│ ―│―│―│―│―│―│ ―│―│―│―│―│―│ ―│―│―│―│―│―│ ―│―│―│―│―│―│ ―│―│―│―│―│―│ ―│―│―│―│―│―│ ―│―│―│―│―│―│ ―│―│―│―│―│―│―│ ―│―│―│―│―│―│―│ ―│―│―│―│―│―│―│ ―│―│―│―│―│―│―│ ―│―│―│―│―│―│―│ ―│―│―│―│―│―│―│ ―│―│―│―│―│―│―│ ―│―│―│―│―│―│―│ ―│―│―│―│―│―│―│ ―│―│―│―│―│―│―│ ―│―│―│―│―│―│―│ ―│―│―│―│―│―│―│ ―│―│―│―│―│―│ ―│―│―│―│―│―│ ―│―│―│―│―│―│ ―│―│―│―│―│―│ ―│―│―│―│―│―│ ―│―│―│―│―│―│ ―│―│―│―│―│―│ ―│―│―│―│―│―│ ―│―│―│―│―│―│ ―│―│―│―│―│―│ ―│―│―│―│―│―│ ―│―│―│―│―│―│ ―│―│―│―│―│―│―│ ―│―│―│―│―│―│―│ ―│―│―│―│―│―│―│ ―│―│―│―│―│―│―│ ―│―│―│―│―│―│―│ ―│―│―│―│―│―│―│ ―│―│―│―│―│―│―│ ―│―│―│―│―│―│―│ ―│―│―│―│―│―│―│ ―│―│―│―│―│―│―│ ―│―│―│―│―│―│―│ ―│―│―│―│―│―│―│ ―│―│―│―│―│―│―│ ―│―│―│―│―│―│―│ ―│―│―│―│―│―│―│ ―│―│―│―│―│―│―│ ―│―│―│―│―│―│―│ ―│―│―│―│―│―│―│ ―│―│―│―│―│―│―│ ―│―│―│―│―│―│―│ ―│―│―│―│―│―│―│ ―│―│―│―│―│―│―│ ―│―│―│―│―│―│―│ ―│―│―│―│―│―│―│ ―│―│―│―│―│―│―│ ―│―│―│―│―│―│―│ ―│―│―│―│―│―│―│ ―│―│―│―│―│―│―│ ―│―│―│―│―│―│―│ ―│―│―│―│―│―│―│ ―│―│―│―│―│―│―│ ―│―│―│―│―│―│―│ ―│―│―│―│―│―│―│ ―│―│―│―│―│―│―│ ―│―│―│―│―│―│―│ ―│―│―│―│―│―│―│ ―│―│―│―│―│―│―│ ―│―│―│―│―│―│―│ ―│―│―│―│―│―│―│ ―│―│―│―│―│―│―│ ―│―│―│―│―│―│―│ ―│―│―│―│―│―│―│ ―│―│―│―│―│―│―│ ~~~~~~~~~~~~~~~~ ~~~~~~~~~~~~ ~~~~~~~~~~~~ ~~~~~~~~~~~~ ~~~~~~~~~ ~~~~~~~~~~~~~~~~ ~~~~~~~~~ T29S R2E T28S R2E T29SR1E T29S R3E T28S R3ET28S R1E 17 29 49 1 18 38 25 31 5 18 1415 10 18 20 13 12 8 17 41 22 33 14 23 42 19 11 19 27 27 35 32 36 3025 12 30 21 13 50 4 2 35 26 31 15 24 36 13 2422 29 13 24 1 9 25 34 16 3432 28 28 19 16 20 31 30 23 24 3 36 7 33 6 26 36 21 25 39 35 36 37 38 39 40 41 42 43 44 45 46 34 4247 000mN 35 36 37 38 39 40 41 42 43 44 45 46 4234000mN 47 36 37 38 39 40 41 42 43 4435 445 000mE 36 37 38 39 40 41 42 43 44435000mE 45 38.2500° 38.3750° -111.7500°-111.6250°38.3750° 38.2500°-111.6250°-111.7500° 77 0 0 7800 7400 7600 8500 8400 830 0 8200 8100 81 0 0 80 0 0 8000 8200 8200 8100 7900 7900 7800 7800 7800 82 0 0 8100 8000 850 0 8 2 0 0 8100 8200 8300 8100 83 0 0 8200 81 0 0 8200 8 4 0 0 8400 8 5 0 0 85 0 0 8400 8 5 0 0 85 0 0 8 5 0 0 8 5 0 0 85 0 0 8500 83 0 0 84 0 0 8300 8300 8200 8300 830 0 8300 8300 8300 8100 8100 8200 8200 8200 8200 8200 8100 81 0 0 81 0 0 81 0 0 8 1 0 0 7900 790 0 8000 8 0 0 0 7 8 0 0 7900 7900 7700 7800 7800 7700 7800 7600 77 0 0 76 0 07700 7700 7600 7 6 0 0 7 5 0 0 7500 7400 7400 7100 7 1 0 0 8400 Bull RoostReservoir MoroniReservoir CameronReservoir WoodysReservoir Rock PointReservoir Long HollowReservoir Flat TopReservoir BEHIN D B I G R O C K S R D BIG R O CKS R D L O N G H O L L O W R D T V T O W E R R D L A N D F I L L R D BIG ROCE RD J A CKSON'SGRAVEL PIT R D S p ringCr Sage Flat Terza Flat Bull Roost BullheadBench Awapa Plateau Blackb u r n H o l l o w R a b b i t V a l l e y W i l d c a t H o l l o w Tommy Hollow Sage Flat Draw Big H o l l o w L o n g H o l l o w Post Hollow Balsam Hollow C y c l o n e D r a w Big Flat Top Moroni Peak LittleFlat Top ElsiesNipple × Ù GN MN 0°26´8 MILS 10°38´189 MILS UTM GRID AND 2021 MAGNETIC NORTHDECLINATION AT CENTER OF SHEET VH Grid Zone Designation12S U.S. National Grid100,000 - m Square ID U.S. DEPARTMENT OF THE INTERIOR U.S. GEOLOGICAL SURVEY SCALE 1:24 000 CONTOUR INTERVAL 20 FEETNORTH AMERICAN VERTICAL DATUM OF 1988 1000 500 0 METERS 1000 2000 21KILOMETERS00.51 1 0.5 0 MILES 1 1000 0 1000 2000 3000 4000 5000 6000 7000 8000 9000 10000 FEET CONTOUR SMOOTHNESS = Medium North American Datum of 1983 (NAD83)World Geodetic System of 1984 (WGS84). Projection and1 000-meter grid:Universal Transverse Mercator, Zone 12S Produced by the United States Geological Survey Data is provided by The National Map (TNM), is the best available at the time of mapgeneration, and includes data content from supporting themes of Elevation,Hydrography, Geographic Names, Boundaries, Transportation, Structures, Land Cover,and Orthoimagery. Refer to associated Federal Geographic Data Committee (FGDC)Metadata for additional source data information. This map is not a legal document. Boundaries may be generalized for this map scale.Private lands within government reservations may not be shown. Obtain permissionbefore entering private lands. Temporal changes may have occurred since these datawere collected and some data may no longer represent actual surface conditions. Learn About The National Map: https://nationalmap.gov QUADRANGLE LOCATION UTAH ADJOINING QUADRANGLES MORONI PEAK QUADRANGLEUTAH - WAYNE COUNTY7.5-MINUTE TOPO Bicknell AbesKnoll MoroniPeak FlossieKnoll JakesKnoll GovernmentPoint Loa Lyman SmoothKnoll MORONI PEAK, UT 2024 Expressway Local Connector ROAD CLASSIFICATION Ramp 4WD Secondary Hwy Local Road Interstate Route State RouteUS RouteWX./ Long Hollow Landfill Hanksville Class IV Landfill Record Volume Form Date Vehicle C = CAR P = PICKUP T = TRUCK Waste Type Estimated Amount EXHIBIT 2: RECORD VOLUME FORM HANKSVILLE CLASS II LANDFILL RECORD VOLUME FORM EXHIBIT #4 WAYNE COUNTY LANDFILL QUARTERLY INSPECTION FORM Performed by_ Date I. Structures and Roads 1. 2. 3. 4. 5. 6. Buildings Fences Gates Road leading to facility Inside perimeter road Gas monitor levels . Overall Condition Satisfactory Needs Work* O a a a a a a o a a .*Specify recommended repairs and/or list actions taken: II. Operations 1. 2. 3. 4. 5. Litter and weed control Excavations Daily Final cover cover Waste Piles A. B. C. D. E. F. Appliances Construction/Demolition Tires Inert waste Car bodies Yard waste 6. Recyclables/Furniture storage area 'Specify recommended repairs and/or list actions taken: • a a a o a a a a a a a a a a o o o ••-"It 7: Quarterly Inspection Form J EXHIBIT #5 Location: Long Hollow Landfill TP-1 Date: 7/23/2024 Name: Kelly Chappell Gravel Cobbles & Stones Gray % Red % 0-6" Loam Medium 15 5 Granular 0 0 6-36" Loam Medium 25 10 Granular 0 0 36-50" Sandy Loam Medium 30 10 Granular 0 0 50-60" Loam Medium 20 5 Platy 0 0 60-94" Soft Rock Medium 25 15 Granular 0 0 Depth: Record depth of layer in inches Soil Texture: Determine the soil texture using the USDA textural triangle (i.e., soil loam, clay loam) Sand Size: If the soil texture is sand, loamy sand, or sandy loam, determine the size of the sand grains Coarse Fragments: Estimate the percent of gravel by volume Gravel = 0.1" to 3" in diameter Cobble = 3" to 10" in diameter Stone = greater than 10" in diameter Soil Structure: Mottles: Indicate whether or not mottles exist in the layer, along with the color (red or grey) and % Few: less than 2% of the exposed surface is occupied by mottles Common: from 2% to 20% of the exposed surface is occupied by mottles Many: more than 20% of the exposed surface is occupied by mottles Depth (in)Soil Texture (USDA) Sand Size Coarse Fragments % by Volume Soil Structure Determine the dominant structure in the layer (granular, blocky, prismatic, or platy). If the soil is classified as sand using the USDA textural triangle, list the structure as single grain. If no structure exists, list the structure as massive. Comments Mottles Location: Long Hollow Landfill TP-2 Date: 7/23/2024 Name: Kelly Chappell Gravel Cobbles & Stones Gray % Red % 0-6" Loam Fine 5 5 Granular 0 0 6-48" Loam Medium 10 10 Granular 0 0 48-50" Loam Medium 30 10 Granular 0 0 50-60" Loam Fine 20 20 Granular 0 0 60-70" Loam Fine 15 20 Granular 0 0 70-180" Loam Fine 15 20 Granular 0 0 Depth: Record depth of layer in inches Soil Texture: Determine the soil texture using the USDA textural triangle (i.e., soil loam, clay loam) Sand Size: If the soil texture is sand, loamy sand, or sandy loam, determine the size of the sand grains Coarse Fragments: Estimate the percent of gravel by volume Gravel = 0.1" to 3" in diameter Cobble = 3" to 10" in diameter Stone = greater than 10" in diameter Soil Structure: Mottles: Indicate whether or not mottles exist in the layer, along with the color (red or grey) and % Few: less than 2% of the exposed surface is occupied by mottles Common: from 2% to 20% of the exposed surface is occupied by mottles Many: more than 20% of the exposed surface is occupied by mottles Depth (in)Soil Texture (USDA) Sand Size Coarse Fragments % by Volume Soil Structure Comments Determine the dominant structure in the layer (granular, blocky, prismatic, or platy). If the soil is classified as sand using the USDA textural triangle, list the structure as single grain. If no structure exists, list the structure as massive. Roots/Top Soil Mottles Location: Long Hollow Landfill TP-3 Date: 7/23/2024 Name: Kelly Chappell Gravel Cobbles & Stones Gray % Red % 0-6" Loam Fine 5 5 Granular 0 0 6-36" Loam Medium 10 10 Granular 0 0 36-54" Loam Medium 30 10 Granular 0 0 54-60" Loam Fine 20 20 Granular 0 0 60-80" Loam Fine 15 20 Granular 0 0 80-180" Loam Fine 15 20 Granular 0 0 Depth: Record depth of layer in inches Soil Texture: Determine the soil texture using the USDA textural triangle (i.e., soil loam, clay loam) Sand Size: If the soil texture is sand, loamy sand, or sandy loam, determine the size of the sand grains Coarse Fragments: Estimate the percent of gravel by volume Gravel = 0.1" to 3" in diameter Cobble = 3" to 10" in diameter Stone = greater than 10" in diameter Soil Structure: Mottles: Indicate whether or not mottles exist in the layer, along with the color (red or grey) and % Few: less than 2% of the exposed surface is occupied by mottles Common: from 2% to 20% of the exposed surface is occupied by mottles Many: more than 20% of the exposed surface is occupied by mottles Determine the dominant structure in the layer (granular, blocky, prismatic, or platy). If the soil is classified as sand using the USDA textural triangle, list the structure as single grain. If no structure exists, list the structure as massive. Comments Roots/Top Soil Depth (in)Soil Texture (USDA) Sand Size Coarse Fragments % by Volume Soil Structure Mottles United States Department of Agriculture A product of the National Cooperative Soil Survey, a joint effort of the United States Department of Agriculture and other Federal agencies, State agencies including the Agricultural Experiment Stations, and local participants Custom Soil Resource Report for Loa-Marysvale Area, Utah, Parts of Piute, Wayne, and Garfield Counties Natural Resources Conservation Service July 29, 2024 Preface Soil surveys contain information that affects land use planning in survey areas. They highlight soil limitations that affect various land uses and provide information about the properties of the soils in the survey areas. Soil surveys are designed for many different users, including farmers, ranchers, foresters, agronomists, urban planners, community officials, engineers, developers, builders, and home buyers. Also, conservationists, teachers, students, and specialists in recreation, waste disposal, and pollution control can use the surveys to help them understand, protect, or enhance the environment. Various land use regulations of Federal, State, and local governments may impose special restrictions on land use or land treatment. Soil surveys identify soil properties that are used in making various land use or land treatment decisions. The information is intended to help the land users identify and reduce the effects of soil limitations on various land uses. The landowner or user is responsible for identifying and complying with existing laws and regulations. Although soil survey information can be used for general farm, local, and wider area planning, onsite investigation is needed to supplement this information in some cases. Examples include soil quality assessments (http://www.nrcs.usda.gov/wps/ portal/nrcs/main/soils/health/) and certain conservation and engineering applications. For more detailed information, contact your local USDA Service Center (https://offices.sc.egov.usda.gov/locator/app?agency=nrcs) or your NRCS State Soil Scientist (http://www.nrcs.usda.gov/wps/portal/nrcs/detail/soils/contactus/? cid=nrcs142p2_053951). Great differences in soil properties can occur within short distances. Some soils are seasonally wet or subject to flooding. Some are too unstable to be used as a foundation for buildings or roads. Clayey or wet soils are poorly suited to use as septic tank absorption fields. A high water table makes a soil poorly suited to basements or underground installations. The National Cooperative Soil Survey is a joint effort of the United States Department of Agriculture and other Federal agencies, State agencies including the Agricultural Experiment Stations, and local agencies. The Natural Resources Conservation Service (NRCS) has leadership for the Federal part of the National Cooperative Soil Survey. Information about soils is updated periodically. Updated information is available through the NRCS Web Soil Survey, the site for official soil survey information. The U.S. Department of Agriculture (USDA) prohibits discrimination in all its programs and activities on the basis of race, color, national origin, age, disability, and where applicable, sex, marital status, familial status, parental status, religion, sexual orientation, genetic information, political beliefs, reprisal, or because all or a part of an individual's income is derived from any public assistance program. (Not all prohibited bases apply to all programs.) Persons with disabilities who require 2 alternative means for communication of program information (Braille, large print, audiotape, etc.) should contact USDA's TARGET Center at (202) 720-2600 (voice and TDD). To file a complaint of discrimination, write to USDA, Director, Office of Civil Rights, 1400 Independence Avenue, S.W., Washington, D.C. 20250-9410 or call (800) 795-3272 (voice) or (202) 720-6382 (TDD). USDA is an equal opportunity provider and employer. 3 Contents Preface....................................................................................................................2 How Soil Surveys Are Made..................................................................................5 Soil Map..................................................................................................................8 Soil Map................................................................................................................9 Legend................................................................................................................10 Map Unit Legend................................................................................................12 Map Unit Descriptions........................................................................................12 Loa-Marysvale Area, Utah, Parts of Piute, Wayne, and Garfield Counties.....14 Sd1—Millmeadow, extremely stony-Woody-Awapa, rubbly association, 3 to 40 percent slopes...........................................................................14 References............................................................................................................18 4 How Soil Surveys Are Made Soil surveys are made to provide information about the soils and miscellaneous areas in a specific area. They include a description of the soils and miscellaneous areas and their location on the landscape and tables that show soil properties and limitations affecting various uses. Soil scientists observed the steepness, length, and shape of the slopes; the general pattern of drainage; the kinds of crops and native plants; and the kinds of bedrock. They observed and described many soil profiles. A soil profile is the sequence of natural layers, or horizons, in a soil. The profile extends from the surface down into the unconsolidated material in which the soil formed or from the surface down to bedrock. The unconsolidated material is devoid of roots and other living organisms and has not been changed by other biological activity. Currently, soils are mapped according to the boundaries of major land resource areas (MLRAs). MLRAs are geographically associated land resource units that share common characteristics related to physiography, geology, climate, water resources, soils, biological resources, and land uses (USDA, 2006). Soil survey areas typically consist of parts of one or more MLRA. The soils and miscellaneous areas in a survey area occur in an orderly pattern that is related to the geology, landforms, relief, climate, and natural vegetation of the area. Each kind of soil and miscellaneous area is associated with a particular kind of landform or with a segment of the landform. By observing the soils and miscellaneous areas in the survey area and relating their position to specific segments of the landform, a soil scientist develops a concept, or model, of how they were formed. Thus, during mapping, this model enables the soil scientist to predict with a considerable degree of accuracy the kind of soil or miscellaneous area at a specific location on the landscape. Commonly, individual soils on the landscape merge into one another as their characteristics gradually change. To construct an accurate soil map, however, soil scientists must determine the boundaries between the soils. They can observe only a limited number of soil profiles. Nevertheless, these observations, supplemented by an understanding of the soil-vegetation-landscape relationship, are sufficient to verify predictions of the kinds of soil in an area and to determine the boundaries. Soil scientists recorded the characteristics of the soil profiles that they studied. They noted soil color, texture, size and shape of soil aggregates, kind and amount of rock fragments, distribution of plant roots, reaction, and other features that enable them to identify soils. After describing the soils in the survey area and determining their properties, the soil scientists assigned the soils to taxonomic classes (units). Taxonomic classes are concepts. Each taxonomic class has a set of soil characteristics with precisely defined limits. The classes are used as a basis for comparison to classify soils systematically. Soil taxonomy, the system of taxonomic classification used in the United States, is based mainly on the kind and character of soil properties and the arrangement of horizons within the profile. After the soil 5 scientists classified and named the soils in the survey area, they compared the individual soils with similar soils in the same taxonomic class in other areas so that they could confirm data and assemble additional data based on experience and research. The objective of soil mapping is not to delineate pure map unit components; the objective is to separate the landscape into landforms or landform segments that have similar use and management requirements. Each map unit is defined by a unique combination of soil components and/or miscellaneous areas in predictable proportions. Some components may be highly contrasting to the other components of the map unit. The presence of minor components in a map unit in no way diminishes the usefulness or accuracy of the data. The delineation of such landforms and landform segments on the map provides sufficient information for the development of resource plans. If intensive use of small areas is planned, onsite investigation is needed to define and locate the soils and miscellaneous areas. Soil scientists make many field observations in the process of producing a soil map. The frequency of observation is dependent upon several factors, including scale of mapping, intensity of mapping, design of map units, complexity of the landscape, and experience of the soil scientist. Observations are made to test and refine the soil-landscape model and predictions and to verify the classification of the soils at specific locations. Once the soil-landscape model is refined, a significantly smaller number of measurements of individual soil properties are made and recorded. These measurements may include field measurements, such as those for color, depth to bedrock, and texture, and laboratory measurements, such as those for content of sand, silt, clay, salt, and other components. Properties of each soil typically vary from one point to another across the landscape. Observations for map unit components are aggregated to develop ranges of characteristics for the components. The aggregated values are presented. Direct measurements do not exist for every property presented for every map unit component. Values for some properties are estimated from combinations of other properties. While a soil survey is in progress, samples of some of the soils in the area generally are collected for laboratory analyses and for engineering tests. Soil scientists interpret the data from these analyses and tests as well as the field-observed characteristics and the soil properties to determine the expected behavior of the soils under different uses. Interpretations for all of the soils are field tested through observation of the soils in different uses and under different levels of management. Some interpretations are modified to fit local conditions, and some new interpretations are developed to meet local needs. Data are assembled from other sources, such as research information, production records, and field experience of specialists. For example, data on crop yields under defined levels of management are assembled from farm records and from field or plot experiments on the same kinds of soil. Predictions about soil behavior are based not only on soil properties but also on such variables as climate and biological activity. Soil conditions are predictable over long periods of time, but they are not predictable from year to year. For example, soil scientists can predict with a fairly high degree of accuracy that a given soil will have a high water table within certain depths in most years, but they cannot predict that a high water table will always be at a specific level in the soil on a specific date. After soil scientists located and identified the significant natural bodies of soil in the survey area, they drew the boundaries of these bodies on aerial photographs and Custom Soil Resource Report 6 identified each as a specific map unit. Aerial photographs show trees, buildings, fields, roads, and rivers, all of which help in locating boundaries accurately. Custom Soil Resource Report 7 Soil Map The soil map section includes the soil map for the defined area of interest, a list of soil map units on the map and extent of each map unit, and cartographic symbols displayed on the map. Also presented are various metadata about data used to produce the map, and a description of each soil map unit. 8 9 Custom Soil Resource Report Soil Map 42 4 5 2 0 0 42 4 5 3 0 0 42 4 5 4 0 0 42 4 5 5 0 0 42 4 5 6 0 0 42 4 5 7 0 0 42 4 5 8 0 0 42 4 5 9 0 0 42 4 6 0 0 0 42 4 6 1 0 0 42 4 6 2 0 0 42 4 6 3 0 0 42 4 6 4 0 0 42 4 6 5 0 0 42 4 6 6 0 0 42 4 5 2 0 0 42 4 5 3 0 0 42 4 5 4 0 0 42 4 5 5 0 0 42 4 5 6 0 0 42 4 5 7 0 0 42 4 5 8 0 0 42 4 5 9 0 0 42 4 6 0 0 0 42 4 6 1 0 0 42 4 6 2 0 0 42 4 6 3 0 0 42 4 6 4 0 0 42 4 6 5 0 0 42 4 6 6 0 0 439500 439600 439700 439800 439900 440000 440100 440200 440300 440400 440500 439500 439600 439700 439800 439900 440000 440100 440200 440300 440400 440500 38° 21' 58'' N 11 1 ° 4 1 ' 3 5 ' ' W 38° 21' 58'' N 11 1 ° 4 0 ' 4 9 ' ' W 38° 21' 9'' N 11 1 ° 4 1 ' 3 5 ' ' W 38° 21' 9'' N 11 1 ° 4 0 ' 4 9 ' ' W N Map projection: Web Mercator Corner coordinates: WGS84 Edge tics: UTM Zone 12N WGS84 0 350 700 1400 2100 Feet 0 100 200 400 600 Meters Map Scale: 1:7,250 if printed on A portrait (8.5" x 11") sheet. Soil Map may not be valid at this scale. MAP LEGEND MAP INFORMATION Area of Interest (AOI) Area of Interest (AOI) Soils Soil Map Unit Polygons Soil Map Unit Lines Soil Map Unit Points Special Point Features Blowout Borrow Pit Clay Spot Closed Depression Gravel Pit Gravelly Spot Landfill Lava Flow Marsh or swamp Mine or Quarry Miscellaneous Water Perennial Water Rock Outcrop Saline Spot Sandy Spot Severely Eroded Spot Sinkhole Slide or Slip Sodic Spot Spoil Area Stony Spot Very Stony Spot Wet Spot Other Special Line Features Water Features Streams and Canals Transportation Rails Interstate Highways US Routes Major Roads Local Roads Background Aerial Photography The soil surveys that comprise your AOI were mapped at 1:24,000. Warning: Soil Map may not be valid at this scale. Enlargement of maps beyond the scale of mapping can cause misunderstanding of the detail of mapping and accuracy of soil line placement. The maps do not show the small areas of contrasting soils that could have been shown at a more detailed scale. Please rely on the bar scale on each map sheet for map measurements. Source of Map: Natural Resources Conservation Service Web Soil Survey URL: Coordinate System: Web Mercator (EPSG:3857) Maps from the Web Soil Survey are based on the Web Mercator projection, which preserves direction and shape but distorts distance and area. A projection that preserves area, such as the Albers equal-area conic projection, should be used if more accurate calculations of distance or area are required. This product is generated from the USDA-NRCS certified data as of the version date(s) listed below. Soil Survey Area: Loa-Marysvale Area, Utah, Parts of Piute, Wayne, and Garfield Counties Survey Area Data: Version 7, Sep 8, 2023 Soil map units are labeled (as space allows) for map scales 1:50,000 or larger. Date(s) aerial images were photographed: Jul 9, 2021—Aug 27, 2021 The orthophoto or other base map on which the soil lines were compiled and digitized probably differs from the background Custom Soil Resource Report 10 MAP LEGEND MAP INFORMATION imagery displayed on these maps. As a result, some minor shifting of map unit boundaries may be evident. Custom Soil Resource Report 11 Map Unit Legend Map Unit Symbol Map Unit Name Acres in AOI Percent of AOI Sd1 Millmeadow, extremely stony- Woody-Awapa, rubbly association, 3 to 40 percent slopes 205.2 100.0% Totals for Area of Interest 205.2 100.0% Map Unit Descriptions The map units delineated on the detailed soil maps in a soil survey represent the soils or miscellaneous areas in the survey area. The map unit descriptions, along with the maps, can be used to determine the composition and properties of a unit. A map unit delineation on a soil map represents an area dominated by one or more major kinds of soil or miscellaneous areas. A map unit is identified and named according to the taxonomic classification of the dominant soils. Within a taxonomic class there are precisely defined limits for the properties of the soils. On the landscape, however, the soils are natural phenomena, and they have the characteristic variability of all natural phenomena. Thus, the range of some observed properties may extend beyond the limits defined for a taxonomic class. Areas of soils of a single taxonomic class rarely, if ever, can be mapped without including areas of other taxonomic classes. Consequently, every map unit is made up of the soils or miscellaneous areas for which it is named and some minor components that belong to taxonomic classes other than those of the major soils. Most minor soils have properties similar to those of the dominant soil or soils in the map unit, and thus they do not affect use and management. These are called noncontrasting, or similar, components. They may or may not be mentioned in a particular map unit description. Other minor components, however, have properties and behavioral characteristics divergent enough to affect use or to require different management. These are called contrasting, or dissimilar, components. They generally are in small areas and could not be mapped separately because of the scale used. Some small areas of strongly contrasting soils or miscellaneous areas are identified by a special symbol on the maps. If included in the database for a given area, the contrasting minor components are identified in the map unit descriptions along with some characteristics of each. A few areas of minor components may not have been observed, and consequently they are not mentioned in the descriptions, especially where the pattern was so complex that it was impractical to make enough observations to identify all the soils and miscellaneous areas on the landscape. The presence of minor components in a map unit in no way diminishes the usefulness or accuracy of the data. The objective of mapping is not to delineate pure taxonomic classes but rather to separate the landscape into landforms or landform segments that have similar use and management requirements. The delineation of such segments on the map provides sufficient information for the development of resource plans. If intensive use of small areas is planned, however, Custom Soil Resource Report 12 onsite investigation is needed to define and locate the soils and miscellaneous areas. An identifying symbol precedes the map unit name in the map unit descriptions. Each description includes general facts about the unit and gives important soil properties and qualities. Soils that have profiles that are almost alike make up a soil series. Except for differences in texture of the surface layer, all the soils of a series have major horizons that are similar in composition, thickness, and arrangement. Soils of one series can differ in texture of the surface layer, slope, stoniness, salinity, degree of erosion, and other characteristics that affect their use. On the basis of such differences, a soil series is divided into soil phases. Most of the areas shown on the detailed soil maps are phases of soil series. The name of a soil phase commonly indicates a feature that affects use or management. For example, Alpha silt loam, 0 to 2 percent slopes, is a phase of the Alpha series. Some map units are made up of two or more major soils or miscellaneous areas. These map units are complexes, associations, or undifferentiated groups. A complex consists of two or more soils or miscellaneous areas in such an intricate pattern or in such small areas that they cannot be shown separately on the maps. The pattern and proportion of the soils or miscellaneous areas are somewhat similar in all areas. Alpha-Beta complex, 0 to 6 percent slopes, is an example. An association is made up of two or more geographically associated soils or miscellaneous areas that are shown as one unit on the maps. Because of present or anticipated uses of the map units in the survey area, it was not considered practical or necessary to map the soils or miscellaneous areas separately. The pattern and relative proportion of the soils or miscellaneous areas are somewhat similar. Alpha-Beta association, 0 to 2 percent slopes, is an example. An undifferentiated group is made up of two or more soils or miscellaneous areas that could be mapped individually but are mapped as one unit because similar interpretations can be made for use and management. The pattern and proportion of the soils or miscellaneous areas in a mapped area are not uniform. An area can be made up of only one of the major soils or miscellaneous areas, or it can be made up of all of them. Alpha and Beta soils, 0 to 2 percent slopes, is an example. Some surveys include miscellaneous areas. Such areas have little or no soil material and support little or no vegetation. Rock outcrop is an example. Custom Soil Resource Report 13 Loa-Marysvale Area, Utah, Parts of Piute, Wayne, and Garfield Counties Sd1—Millmeadow, extremely stony-Woody-Awapa, rubbly association, 3 to 40 percent slopes Map Unit Setting National map unit symbol: 2q89c Elevation: 6,910 to 8,600 feet Mean annual precipitation: 8 to 12 inches Mean annual air temperature: 39 to 45 degrees F Frost-free period: 70 to 100 days Farmland classification: Not prime farmland Map Unit Composition Millmeadow, extremely stony, and similar soils:40 percent Woody and similar soils:30 percent Awapa, rubbly, and similar soils:15 percent Minor components:15 percent Estimates are based on observations, descriptions, and transects of the mapunit. Description of Millmeadow, Extremely Stony Setting Landform:Hills Landform position (two-dimensional):Backslope, shoulder, summit Landform position (three-dimensional):Side slope Down-slope shape:Convex Across-slope shape:Convex Parent material:Colluvium and/or slope alluvium derived from andesite, dacite, basalt and tuff Typical profile A - 0 to 8 inches: very gravelly loam Bt - 8 to 12 inches: very gravelly loam Bk1 - 12 to 16 inches: very gravelly loam Bk2 - 16 to 19 inches: extremely cobbly sandy loam Bkm - 19 to 19 inches: cemented material R - 19 to 60 inches: bedrock Properties and qualities Slope:5 to 25 percent Surface area covered with cobbles, stones or boulders:5.0 percent Depth to restrictive feature:10 to 20 inches to petrocalcic; 10 to 20 inches to lithic bedrock Drainage class:Well drained Runoff class: Medium Capacity of the most limiting layer to transmit water (Ksat):Very low to moderately low (0.00 to 0.07 in/hr) Depth to water table:More than 80 inches Frequency of flooding:None Frequency of ponding:None Calcium carbonate, maximum content:50 percent Gypsum, maximum content:2 percent Maximum salinity:Nonsaline to very slightly saline (0.0 to 2.0 mmhos/cm) Sodium adsorption ratio, maximum:5.0 Custom Soil Resource Report 14 Available water supply, 0 to 60 inches: Very low (about 1.7 inches) Interpretive groups Land capability classification (irrigated): None specified Land capability classification (nonirrigated): 7s Hydrologic Soil Group: D Ecological site: R047XB236UT - Semidesert Shallow Loam (black sagebrush) Hydric soil rating: No Description of Woody Setting Landform:Hills Landform position (two-dimensional):Toeslope Landform position (three-dimensional):Base slope Down-slope shape:Concave Across-slope shape:Concave Parent material:Colluvium and/or slope alluvium derived from andesite, dacite, basalt and tuff Typical profile A1 - 0 to 9 inches: gravelly loam A2 - 9 to 13 inches: gravelly loam Bw - 13 to 24 inches: gravelly loam Bk - 24 to 36 inches: gravelly sandy clay loam 2CBk - 36 to 72 inches: extremely gravelly sandy loam Properties and qualities Slope:3 to 12 percent Depth to restrictive feature:More than 80 inches Drainage class:Well drained Runoff class: Medium Capacity of the most limiting layer to transmit water (Ksat):Moderately high to high (0.71 to 2.13 in/hr) Depth to water table:More than 80 inches Frequency of flooding:None Frequency of ponding:None Calcium carbonate, maximum content:15 percent Gypsum, maximum content:2 percent Maximum salinity:Nonsaline to slightly saline (0.0 to 4.0 mmhos/cm) Sodium adsorption ratio, maximum:5.0 Available water supply, 0 to 60 inches: Low (about 5.7 inches) Interpretive groups Land capability classification (irrigated): 4e Land capability classification (nonirrigated): 7c Hydrologic Soil Group: B Ecological site: R047XB222UT - Semidesert Loam (Wyoming big sagebrush) Hydric soil rating: No Description of Awapa, Rubbly Setting Landform:Hills Landform position (two-dimensional):Backslope Landform position (three-dimensional):Side slope Down-slope shape:Convex Custom Soil Resource Report 15 Across-slope shape:Convex Parent material:Colluvium and/or slope alluvium derived from andesite, dacite, basalt and tuff Typical profile A - 0 to 9 inches: extremely cobbly loam Bk1 - 9 to 18 inches: very gravelly loam Bk2 - 18 to 33 inches: extremely gravelly loam CBk - 33 to 79 inches: extremely gravelly sandy loam Properties and qualities Slope:25 to 40 percent Surface area covered with cobbles, stones or boulders:30.0 percent Depth to restrictive feature:More than 80 inches Drainage class:Well drained Runoff class: High Capacity of the most limiting layer to transmit water (Ksat):Moderately high to high (0.71 to 2.13 in/hr) Depth to water table:More than 80 inches Frequency of flooding:None Frequency of ponding:None Calcium carbonate, maximum content:15 percent Gypsum, maximum content:2 percent Maximum salinity:Nonsaline to slightly saline (0.0 to 4.0 mmhos/cm) Sodium adsorption ratio, maximum:10.0 Available water supply, 0 to 60 inches: Very low (about 2.6 inches) Interpretive groups Land capability classification (irrigated): None specified Land capability classification (nonirrigated): 7s Hydrologic Soil Group: B Ecological site: R047XB252UT - Semidesert Stony Loam (black sagebrush) Hydric soil rating: No Minor Components Rock outcrop Percent of map unit:10 percent Landform:Ledges, escarpments, erosion remnants, cliffs Down-slope shape:Linear, convex Across-slope shape:Linear, convex Hydric soil rating: No Secondledge Percent of map unit:3 percent Landform:Hills Landform position (two-dimensional):Backslope, shoulder, summit Landform position (three-dimensional):Side slope Down-slope shape:Convex Across-slope shape:Convex Ecological site:R047XB326UT - Upland Shallow Loam (pinyon/Utah juniper) Hydric soil rating: No Fluvents Percent of map unit:2 percent Landform:Drainageways Landform position (three-dimensional):Base slope Custom Soil Resource Report 16 Down-slope shape:Linear Across-slope shape:Concave Ecological site:R047XB220UT - Semidesert Loam (basin big sagebrush) Hydric soil rating: No Custom Soil Resource Report 17 References American Association of State Highway and Transportation Officials (AASHTO). 2004. Standard specifications for transportation materials and methods of sampling and testing. 24th edition. American Society for Testing and Materials (ASTM). 2005. Standard classification of soils for engineering purposes. ASTM Standard D2487-00. Cowardin, L.M., V. Carter, F.C. Golet, and E.T. LaRoe. 1979. Classification of wetlands and deep-water habitats of the United States. U.S. Fish and Wildlife Service FWS/OBS-79/31. Federal Register. July 13, 1994. Changes in hydric soils of the United States. Federal Register. September 18, 2002. Hydric soils of the United States. Hurt, G.W., and L.M. Vasilas, editors. Version 6.0, 2006. Field indicators of hydric soils in the United States. National Research Council. 1995. Wetlands: Characteristics and boundaries. Soil Survey Division Staff. 1993. Soil survey manual. Soil Conservation Service. U.S. Department of Agriculture Handbook 18. http://www.nrcs.usda.gov/wps/portal/ nrcs/detail/national/soils/?cid=nrcs142p2_054262 Soil Survey Staff. 1999. Soil taxonomy: A basic system of soil classification for making and interpreting soil surveys. 2nd edition. Natural Resources Conservation Service, U.S. Department of Agriculture Handbook 436. http:// www.nrcs.usda.gov/wps/portal/nrcs/detail/national/soils/?cid=nrcs142p2_053577 Soil Survey Staff. 2010. Keys to soil taxonomy. 11th edition. U.S. Department of Agriculture, Natural Resources Conservation Service. http:// www.nrcs.usda.gov/wps/portal/nrcs/detail/national/soils/?cid=nrcs142p2_053580 Tiner, R.W., Jr. 1985. Wetlands of Delaware. U.S. Fish and Wildlife Service and Delaware Department of Natural Resources and Environmental Control, Wetlands Section. United States Army Corps of Engineers, Environmental Laboratory. 1987. Corps of Engineers wetlands delineation manual. Waterways Experiment Station Technical Report Y-87-1. United States Department of Agriculture, Natural Resources Conservation Service. National forestry manual. http://www.nrcs.usda.gov/wps/portal/nrcs/detail/soils/ home/?cid=nrcs142p2_053374 United States Department of Agriculture, Natural Resources Conservation Service. National range and pasture handbook. http://www.nrcs.usda.gov/wps/portal/nrcs/ detail/national/landuse/rangepasture/?cid=stelprdb1043084 18 United States Department of Agriculture, Natural Resources Conservation Service. National soil survey handbook, title 430-VI. http://www.nrcs.usda.gov/wps/portal/ nrcs/detail/soils/scientists/?cid=nrcs142p2_054242 United States Department of Agriculture, Natural Resources Conservation Service. 2006. Land resource regions and major land resource areas of the United States, the Caribbean, and the Pacific Basin. U.S. Department of Agriculture Handbook 296. http://www.nrcs.usda.gov/wps/portal/nrcs/detail/national/soils/? cid=nrcs142p2_053624 United States Department of Agriculture, Soil Conservation Service. 1961. Land capability classification. U.S. Department of Agriculture Handbook 210. http:// www.nrcs.usda.gov/Internet/FSE_DOCUMENTS/nrcs142p2_052290.pdf Custom Soil Resource Report 19 An o icial website Division ofWater Rights 0 0.1 0.2mi 7/25/24, 1:36 PM Map https://maps.waterrights.utah.gov/EsriMap/map.asp?layersToAdd=wellsearch 1/1 ----------------------------------------------------------------------------------------------------------------------- HYDROLOGIC EVALUATION OF LANDFILL PERFORMANCE HELP MODEL VERSION 4.0 BETA (2018) DEVELOPED BY USEPA NATIONAL RISK MANAGEMENT RESEARCH LABORATORY ----------------------------------------------------------------------------------------------------------------------- Title: Long Valley Landfill Simulated On: 7/19/2024 11:04 ----------------------------------------------------------------------------------------------------------------------- Layer 1 Type 1 - Vertical Percolation Layer (Cover Soil) L - Loam Material Texture Number 8 Thickness =3 inches Porosity =0.463 vol/vol Field Capacity =0.232 vol/vol Wilting Point =0.116 vol/vol Initial Soil Water Content =0.178 vol/vol Effective Sat. Hyd. Conductivity =3.70E-04 cm/sec Layer 2 Type 3 - Barrier Soil Liner CL - Clay Loam (Moderate) Material Texture Number 25 Thickness =18 inches Porosity =0.437 vol/vol Field Capacity =0.373 vol/vol Wilting Point =0.266 vol/vol Initial Soil Water Content =0.437 vol/vol Effective Sat. Hyd. Conductivity =3.60E-06 cm/sec Layer 3 Type 1 - Vertical Percolation Layer L - Loam Material Texture Number 8 Thickness =6 inches Porosity =0.463 vol/vol Field Capacity =0.232 vol/vol Wilting Point =0.116 vol/vol Initial Soil Water Content =0.232 vol/vol Effective Sat. Hyd. Conductivity =3.70E-04 cm/sec Layer 4 Type 1 - Vertical Percolation Layer L - Loam Page 1 of 128 Material Texture Number 8 Thickness =120 inches Porosity =0.463 vol/vol Field Capacity =0.232 vol/vol Wilting Point =0.116 vol/vol Initial Soil Water Content =0.2618 vol/vol Effective Sat. Hyd. Conductivity =3.70E-04 cm/sec Layer 5 Type 1 - Vertical Percolation Layer L - Loam Material Texture Number 8 Thickness =12 inches Porosity =0.463 vol/vol Field Capacity =0.232 vol/vol Wilting Point =0.116 vol/vol Initial Soil Water Content =0.2644 vol/vol Effective Sat. Hyd. Conductivity =3.70E-04 cm/sec Layer 6 Type 1 - Vertical Percolation Layer L - Loam Material Texture Number 8 Thickness =120 inches Porosity =0.463 vol/vol Field Capacity =0.232 vol/vol Wilting Point =0.116 vol/vol Initial Soil Water Content =0.2356 vol/vol Effective Sat. Hyd. Conductivity =3.70E-04 cm/sec Layer 7 Type 1 - Vertical Percolation Layer L - Loam Material Texture Number 8 Thickness =12 inches Porosity =0.463 vol/vol Field Capacity =0.232 vol/vol Wilting Point =0.116 vol/vol Initial Soil Water Content =0.2356 vol/vol Effective Sat. Hyd. Conductivity =3.70E-04 cm/sec Layer 8 Type 1 - Vertical Percolation Layer L - Loam Page 2 of 128 Material Texture Number 8 Thickness =120 inches Porosity =0.463 vol/vol Field Capacity =0.232 vol/vol Wilting Point =0.116 vol/vol Initial Soil Water Content =0.2324 vol/vol Effective Sat. Hyd. Conductivity =3.70E-04 cm/sec Layer 9 Type 1 - Vertical Percolation Layer L - Loam Material Texture Number 8 Thickness =120 inches Porosity =0.463 vol/vol Field Capacity =0.232 vol/vol Wilting Point =0.116 vol/vol Initial Soil Water Content =0.232 vol/vol Effective Sat. Hyd. Conductivity =3.70E-04 cm/sec Layer 10 Type 1 - Vertical Percolation Layer L - Loam Material Texture Number 8 Thickness =120 inches Porosity =0.463 vol/vol Field Capacity =0.232 vol/vol Wilting Point =0.116 vol/vol Initial Soil Water Content =0.232 vol/vol Effective Sat. Hyd. Conductivity =3.70E-04 cm/sec Layer 11 Type 1 - Vertical Percolation Layer L - Loam Material Texture Number 8 Thickness =120 inches Porosity =0.463 vol/vol Field Capacity =0.232 vol/vol Wilting Point =0.116 vol/vol Initial Soil Water Content =0.232 vol/vol Effective Sat. Hyd. Conductivity =3.70E-04 cm/sec Layer 12 Type 1 - Vertical Percolation Layer L - Loam Page 3 of 128 Material Texture Number 8 Thickness =120 inches Porosity =0.463 vol/vol Field Capacity =0.232 vol/vol Wilting Point =0.116 vol/vol Initial Soil Water Content =0.2321 vol/vol Effective Sat. Hyd. Conductivity =3.70E-04 cm/sec ----------------------------------------------------------------------------------------------------------------------- Note:Initial moisture content of the layers and snow water were computed as nearly steady-state values by HELP. General Design and Evaporative Zone Data SCS Runoff Curve Number =84.3 Fraction of Area Allowing Runoff =100 % Area projected on a horizontal plane =70 acres Evaporative Zone Depth =3 inches Initial Water in Evaporative Zone =0.534 inches Upper Limit of Evaporative Storage =1.389 inches Lower Limit of Evaporative Storage =0.348 inches Initial Snow Water =0 inches Initial Water in Layer Materials =214.75 inches Total Initial Water =214.75 inches Total Subsurface Inflow =0 inches/year --------------------------------------------------------- Note: SCS Runoff Curve Number was calculated by HELP. Evapotranspiration and Weather Data Station Latitude =38.41 Degrees Maximum Leaf Area Index =3 Start of Growing Season (Julian Date)=138 days End of Growing Season (Julian Date)=276 days Average Wind Speed =6 mph Average 1st Quarter Relative Humidity =65 % Average 2nd Quarter Relative Humidity =40 % Average 3rd Quarter Relative Humidity =36 % Average 4th Quarter Relative Humidity =75 % --------------------------------------------------------- Note: Evapotranspiration data was obtained for , Utah Normal Mean Monthly Precipitation (inches) Jan/Jul Feb/Aug Mar/Sep Apr/Oct May/Nov Jun/Dec Page 4 of 128 1.2090909 1.3636364 1.4636364 1.2454545 1.4181818 0.3 2.0909091 1.6545455 1.5090909 1.1363636 1.3 1.7272727 --------------------------------------------------------- Note:Precipitation was simulated using NOAA data for the following weather stations: FISH LAKE UTAH, UT US, HANKSVILLE, UT US, MONTICELLO 24 NW, UT US Normal Mean Monthly Temperature (Degrees Fahrenheit) Jan/Jul Feb/Aug Mar/Sep Apr/Oct May/Nov Jun/Dec 23.2 25.5 33.7 40.1 47.4 58.8 63.8 61.7 54.3 42.7 32.8 23.5 --------------------------------------------------------- Note:Temperature was simulated using NOAA data for the following weather stations: FISH LAKE UTAH, UT US, HANKSVILLE, UT US, MONTICELLO 24 NW, UT US Solar radiation was simulated based on HELP V4 weather simulation for: Lat/Long: 38.41/-111.64 Page 5 of 128 Daily Output for Year 1 Column key:Head #1: drainage from Layer 2 Title:Long Valley Landfill Simulated On:Leak #1: leakage thru Layer 2 Leak #2: leakage thru Layer 12 Day Rain Runoff ET Evap. Zone Water Head #1 Drain #1 Leak #1 Head #2 Drain #2 Leak #2 Air Soil (inches)(inches)(inches)(in/in)(inches)(inches)(inches)(inches)(inches)(inches) 1 * * 0.00 0.000 0.000 0.1780 0.0000 0.0000 0.00E+00 0.0000 0.0000 5.60E-04 2 * * 0.10 0.000 0.029 0.1780 0.0000 0.0000 0.00E+00 0.0000 0.0000 8.59E-04 3 * * 0.00 0.000 0.022 0.1780 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.13E-03 4 * * 0.00 0.000 0.017 0.1780 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.38E-03 5 * * 0.00 0.000 0.015 0.1780 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.60E-03 6 * * 0.00 0.000 0.011 0.1780 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.79E-03 7 * * 0.00 0.000 0.006 0.1780 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.83E-03 8 * * 0.00 0.000 0.000 0.1780 0.0000 0.0000 0.00E+00 0.0000 0.0000 2.48E-03 9 * * 0.00 0.000 0.000 0.1780 0.0000 0.0000 0.00E+00 0.0000 0.0000 3.54E-03 10 * * 0.00 0.000 0.000 0.1780 0.0000 0.0000 0.00E+00 0.0000 0.0000 3.40E-03 11 * * 0.00 0.000 0.000 0.1780 0.0000 0.0000 0.00E+00 0.0000 0.0000 3.27E-03 12 * 0.00 0.000 0.000 0.1780 0.0000 0.0000 0.00E+00 0.0000 0.0000 3.14E-03 13 * 0.00 0.000 0.000 0.1780 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.21E-03 14 * 0.00 0.000 0.000 0.1780 0.0000 0.0000 0.00E+00 0.0000 0.0000 7.57E-04 15 * * 0.10 0.000 0.029 0.1780 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.48E-03 16 * 0.00 0.000 0.035 0.1780 0.0000 0.0000 0.00E+00 0.0000 0.0000 7.87E-04 17 * 0.00 0.000 0.036 0.1780 0.0000 0.0000 0.00E+00 0.0000 0.0000 3.67E-04 18 * 0.00 0.000 0.000 0.1780 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 19 * 0.30 0.059 0.007 0.2562 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 20 0.00 0.000 0.036 0.2234 0.1772 0.0000 6.24E-02 0.0000 0.0000 0.00E+00 21 0.00 0.000 0.013 0.1887 0.1858 0.0000 9.12E-02 0.0000 0.0000 1.01E-03 22 0.00 0.000 0.013 0.1845 0.0002 0.0000 1.14E-04 0.0000 0.0000 8.03E-04 23 0.00 0.000 0.013 0.1803 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.21E-03 24 * 0.00 0.000 0.012 0.1762 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.97E-04 25 0.00 0.000 0.012 0.1720 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.08E-03 26 0.00 0.000 0.012 0.1679 0.0000 0.0000 0.00E+00 0.0000 0.0000 9.45E-04 27 0.00 0.000 0.012 0.1639 0.0000 0.0000 0.00E+00 0.0000 0.0000 4.99E-05 7/19/2024 11:05 Freezing Status* Page 6 of 128 28 0.00 0.000 0.012 0.1599 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.05E-03 29 0.00 0.000 0.012 0.1559 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 30 0.00 0.000 0.012 0.1519 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 31 0.10 0.000 0.018 0.1792 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 32 0.00 0.000 0.012 0.1753 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 33 0.00 0.000 0.012 0.1715 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 34 0.00 0.000 0.012 0.1676 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 35 * 0.10 0.000 0.046 0.1742 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 36 0.00 0.000 0.041 0.1719 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 37 * 0.00 0.000 0.011 0.1682 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 38 * 0.00 0.000 0.011 0.1644 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 39 * 0.00 0.000 0.011 0.1607 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 40 * 0.00 0.000 0.011 0.1570 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 41 0.00 0.000 0.011 0.1533 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 42 0.00 0.000 0.011 0.1497 0.0000 0.0000 0.00E+00 0.0000 0.0000 9.27E-04 43 0.00 0.000 0.011 0.1461 0.0000 0.0000 0.00E+00 0.0000 0.0000 6.93E-04 44 0.00 0.000 0.010 0.1428 0.0000 0.0000 0.00E+00 0.0000 0.0000 9.06E-04 45 0.00 0.000 0.011 0.1393 0.0000 0.0000 0.00E+00 0.0000 0.0000 9.07E-04 46 0.00 0.000 0.011 0.1357 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.14E-03 47 0.00 0.000 0.011 0.1322 0.0000 0.0000 0.00E+00 0.0000 0.0000 7.89E-04 48 0.00 0.000 0.011 0.1287 0.0000 0.0000 0.00E+00 0.0000 0.0000 2.17E-03 49 0.00 0.000 0.010 0.1252 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.09E-03 50 * 0.60 0.000 0.027 0.1317 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.58E-03 51 * 0.00 0.000 0.030 0.1383 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.31E-03 52 * 0.00 0.000 0.023 0.1449 0.0000 0.0000 0.00E+00 0.0000 0.0000 9.31E-04 53 * 0.00 0.000 0.020 0.1514 0.0000 0.0000 0.00E+00 0.0000 0.0000 6.39E-04 54 * 0.00 0.000 0.022 0.1580 0.0000 0.0000 0.00E+00 0.0000 0.0000 7.40E-04 55 * 0.00 0.000 0.023 0.1646 0.0000 0.0000 0.00E+00 0.0000 0.0000 4.62E-04 56 * 0.00 0.000 0.026 0.1711 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 57 * 0.30 0.000 0.026 0.1777 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 58 * 0.00 0.000 0.022 0.1842 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 59 * 0.00 0.000 0.024 0.1908 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 60 * 0.00 0.000 0.023 0.1974 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 61 * * 0.00 0.000 0.023 0.1974 0.0000 0.0000 0.00E+00 0.0000 0.0000 9.80E-04 62 * * 0.00 0.000 0.026 0.1974 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.40E-03 Page 7 of 128 63 * 0.10 0.029 0.000 0.2559 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.15E-03 64 * * 0.00 0.000 0.029 0.2559 0.0000 0.0000 0.00E+00 0.0000 0.0000 9.03E-04 65 * * 0.10 0.000 0.026 0.2559 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.32E-04 66 * * 0.40 0.000 0.028 0.2559 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.07E-03 67 * 0.00 0.000 0.031 0.2559 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 68 * 0.00 0.235 0.000 0.3093 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 69 * 0.00 0.168 0.070 0.3158 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 70 * 0.00 0.000 0.000 0.3158 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 71 * 0.00 0.000 0.000 0.3158 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 72 * 0.00 0.000 0.000 0.3158 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 73 0.00 0.000 0.042 0.2697 0.7065 0.0000 9.66E-02 0.0000 0.0000 0.00E+00 74 0.00 0.000 0.098 0.1945 0.7229 0.0000 1.27E-01 0.0000 0.0000 0.00E+00 75 0.20 0.000 0.109 0.1988 0.1574 0.0000 7.83E-02 0.0000 0.0000 0.00E+00 76 0.20 0.000 0.089 0.2358 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 77 * 0.00 0.000 0.061 0.2156 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 78 * 0.00 0.000 0.051 0.1986 0.0000 0.0000 0.00E+00 0.0000 0.0000 9.61E-04 79 0.00 0.000 0.069 0.1756 0.0000 0.0000 0.00E+00 0.0000 0.0000 6.98E-04 80 0.00 0.000 0.121 0.1353 0.0000 0.0000 0.00E+00 0.0000 0.0000 8.41E-04 81 0.00 0.000 0.058 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.11E-03 82 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 7.63E-04 83 0.10 0.000 0.063 0.1283 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.37E-03 84 0.00 0.000 0.026 0.1196 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.20E-03 85 0.20 0.000 0.041 0.1728 0.0000 0.0000 0.00E+00 0.0000 0.0000 9.74E-04 86 0.00 0.000 0.042 0.1587 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.13E-03 87 0.10 0.000 0.045 0.1769 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 88 0.00 0.000 0.038 0.1641 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 89 0.00 0.000 0.034 0.1527 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 90 0.00 0.000 0.031 0.1422 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 91 0.00 0.000 0.031 0.1318 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 92 0.00 0.000 0.029 0.1220 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 93 0.30 0.000 0.033 0.2111 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.28E-03 94 0.00 0.000 0.120 0.1712 0.0000 0.0000 0.00E+00 0.0000 0.0000 3.50E-04 95 0.00 0.000 0.028 0.1620 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 96 0.00 0.000 0.026 0.1533 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 97 0.10 0.000 0.029 0.1768 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 Page 8 of 128 98 0.10 0.000 0.029 0.2006 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 99 0.30 0.000 0.028 0.2810 0.0284 0.0000 3.08E-02 0.0000 0.0000 0.00E+00 100 0.00 0.000 0.188 0.1951 0.1002 0.0000 6.95E-02 0.0000 0.0000 0.00E+00 101 0.00 0.000 0.196 0.1298 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 102 0.00 0.000 0.041 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.77E-03 103 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 4.44E-16 104 0.10 0.000 0.030 0.1395 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 105 0.00 0.000 0.021 0.1325 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 106 0.00 0.000 0.030 0.1225 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 107 0.00 0.000 0.018 0.1167 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.40E-03 108 0.20 0.000 0.022 0.1762 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.04E-04 109 0.00 0.000 0.028 0.1667 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.80E-03 110 0.20 0.000 0.034 0.2219 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.68E-04 111 0.00 0.000 0.029 0.2121 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.98E-03 112 0.00 0.000 0.029 0.2025 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 113 0.20 0.000 0.032 0.2584 0.0000 0.0000 0.00E+00 0.0000 0.0000 3.30E-03 114 0.40 0.000 0.031 0.3499 0.3766 0.0000 9.44E-02 0.0000 0.0000 3.33E-04 115 0.50 0.000 0.123 0.4311 1.6349 0.0000 1.34E-01 0.0000 0.0000 3.06E-04 116 0.10 0.000 0.188 0.3559 2.2439 0.0000 1.38E-01 0.0000 0.0000 0.00E+00 117 0.00 0.000 0.164 0.2571 1.4229 0.0000 1.32E-01 0.0000 0.0000 0.00E+00 118 0.00 0.000 0.156 0.1629 0.6400 0.0000 1.27E-01 0.0000 0.0000 7.29E-04 119 0.00 0.000 0.117 0.1160 0.0544 0.0000 2.32E-02 0.0000 0.0000 1.37E-03 120 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.00E-03 121 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.41E-03 122 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 5.51E-04 123 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 124 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 9.08E-04 125 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 8.82E-04 126 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 2.70E-03 127 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 3.47E-03 128 0.30 0.000 0.026 0.2073 0.0000 0.0000 0.00E+00 0.0000 0.0000 2.88E-03 129 0.90 0.032 0.035 0.4630 0.7239 0.0000 6.62E-02 0.0000 0.0000 1.27E-03 130 0.10 0.000 0.221 0.3760 2.6173 0.0000 1.40E-01 0.0000 0.0000 1.48E-03 131 0.20 0.000 0.136 0.3523 1.7835 0.0000 1.35E-01 0.0000 0.0000 2.24E-03 132 0.00 0.000 0.141 0.2617 1.2618 0.0000 1.31E-01 0.0000 0.0000 4.94E-04 Page 9 of 128 133 0.00 0.000 0.215 0.1481 0.5529 0.0000 1.26E-01 0.0000 0.0000 1.58E-03 134 0.00 0.000 0.083 0.1161 0.0402 0.0000 1.34E-02 0.0000 0.0000 7.78E-04 135 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 136 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 137 0.10 0.000 0.029 0.1396 0.0000 0.0000 0.00E+00 0.0000 0.0000 4.42E-05 138 0.80 0.000 0.050 0.3793 0.0561 0.0000 3.10E-02 0.0000 0.0000 6.39E-04 139 0.50 0.000 0.122 0.4597 2.1016 0.0000 1.37E-01 0.0000 0.0000 1.81E-04 140 0.10 0.000 0.139 0.3999 2.6517 0.0000 1.40E-01 0.0000 0.0000 6.30E-04 141 0.00 0.000 0.239 0.2756 1.7388 0.0000 1.34E-01 0.0000 0.0000 3.58E-03 142 0.00 0.000 0.223 0.1588 0.7075 0.0000 1.27E-01 0.0000 0.0000 3.67E-03 143 0.20 0.000 0.211 0.1475 0.0531 0.0000 2.23E-02 0.0000 0.0000 3.27E-03 144 0.00 0.000 0.078 0.1216 0.0000 0.0000 0.00E+00 0.0000 0.0000 3.79E-03 145 0.00 0.000 0.013 0.1174 0.0000 0.0000 0.00E+00 0.0000 0.0000 2.82E-03 146 0.00 0.000 0.003 0.1163 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.36E-03 147 0.00 0.000 0.001 0.1161 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.07E-03 148 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 4.44E-16 149 0.10 0.000 0.024 0.1415 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.54E-03 150 0.10 0.000 0.022 0.1674 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.77E-03 151 0.00 0.000 0.033 0.1566 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.83E-03 152 0.00 0.000 0.033 0.1456 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.82E-03 153 0.00 0.000 0.034 0.1343 0.0000 0.0000 0.00E+00 0.0000 0.0000 2.00E-03 154 0.00 0.000 0.031 0.1239 0.0000 0.0000 0.00E+00 0.0000 0.0000 2.07E-03 155 0.00 0.000 0.022 0.1167 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.24E-03 156 0.00 0.000 0.002 0.1162 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 157 0.00 0.000 0.001 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 158 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 6.15E-04 159 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 7.11E-04 160 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 161 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 162 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.53E-03 163 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.62E-03 164 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 2.25E-03 165 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.63E-03 166 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.64E-03 167 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.74E-03 Page 10 of 128 168 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 3.62E-03 169 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 3.50E-03 170 0.60 0.000 0.025 0.3076 0.0000 0.0000 0.00E+00 0.0000 0.0000 3.35E-03 171 0.00 0.000 0.024 0.2576 0.5408 0.0000 1.26E-01 0.0000 0.0000 3.23E-03 172 0.00 0.000 0.027 0.2095 0.2768 0.0000 1.17E-01 0.0000 0.0000 3.21E-03 173 0.00 0.000 0.024 0.2010 0.0000 0.0000 1.31E-03 0.0000 0.0000 2.83E-03 174 0.00 0.000 0.027 0.1920 0.0000 0.0000 0.00E+00 0.0000 0.0000 2.46E-03 175 0.00 0.000 0.025 0.1836 0.0000 0.0000 0.00E+00 0.0000 0.0000 2.21E-03 176 0.00 0.000 0.031 0.1734 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.93E-03 177 0.00 0.000 0.028 0.1639 0.0000 0.0000 0.00E+00 0.0000 0.0000 2.17E-03 178 0.00 0.000 0.031 0.1537 0.0000 0.0000 0.00E+00 0.0000 0.0000 3.21E-03 179 0.00 0.000 0.030 0.1437 0.0000 0.0000 0.00E+00 0.0000 0.0000 2.81E-03 180 0.00 0.000 0.031 0.1334 0.0000 0.0000 0.00E+00 0.0000 0.0000 2.54E-03 181 0.00 0.000 0.030 0.1234 0.0000 0.0000 0.00E+00 0.0000 0.0000 3.34E-04 182 0.00 0.000 0.022 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 183 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 2.31E-04 184 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.02E-03 185 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 9.60E-04 186 0.10 0.000 0.017 0.1437 0.0000 0.0000 0.00E+00 0.0000 0.0000 5.78E-04 187 0.10 0.000 0.033 0.1659 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.45E-04 188 0.00 0.000 0.030 0.1560 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.92E-04 189 0.70 0.000 0.042 0.3649 0.0666 0.0000 3.11E-02 0.0000 0.0000 2.47E-04 190 0.20 0.000 0.220 0.3143 1.3695 0.0000 1.32E-01 0.0000 0.0000 6.64E-04 191 0.00 0.000 0.192 0.2078 0.6986 0.0000 1.27E-01 0.0000 0.0000 9.71E-04 192 0.10 0.000 0.326 0.1222 0.0988 0.0000 3.12E-02 0.0000 0.0000 4.11E-04 193 0.20 0.000 0.109 0.1526 0.0000 0.0000 0.00E+00 0.0000 0.0000 2.67E-03 194 0.10 0.000 0.085 0.1576 0.0000 0.0000 0.00E+00 0.0000 0.0000 3.44E-03 195 0.00 0.000 0.084 0.1298 0.0000 0.0000 0.00E+00 0.0000 0.0000 5.98E-04 196 0.00 0.000 0.031 0.1194 0.0000 0.0000 0.00E+00 0.0000 0.0000 3.20E-03 197 0.00 0.000 0.008 0.1169 0.0000 0.0000 0.00E+00 0.0000 0.0000 2.48E-03 198 0.50 0.000 0.060 0.2637 0.0000 0.0000 0.00E+00 0.0000 0.0000 3.12E-04 199 0.00 0.000 0.158 0.1853 0.0763 0.0000 7.69E-02 0.0000 0.0000 3.12E-04 200 0.20 0.000 0.190 0.1887 0.0000 0.0000 0.00E+00 0.0000 0.0000 8.44E-04 201 0.00 0.000 0.146 0.1401 0.0000 0.0000 0.00E+00 0.0000 0.0000 3.90E-03 202 0.10 0.000 0.144 0.1254 0.0000 0.0000 0.00E+00 0.0000 0.0000 2.88E-03 Page 11 of 128 203 0.00 0.000 0.022 0.1180 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.18E-03 204 0.00 0.000 0.004 0.1165 0.0000 0.0000 0.00E+00 0.0000 0.0000 6.81E-04 205 0.00 0.000 0.001 0.1161 0.0000 0.0000 0.00E+00 0.0000 0.0000 5.77E-04 206 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 207 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 208 0.30 0.000 0.030 0.2058 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 209 0.00 0.000 0.031 0.1954 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 210 0.00 0.000 0.031 0.1850 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.00E-03 211 0.40 0.000 0.036 0.3062 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.52E-03 212 0.40 0.000 0.219 0.3242 0.6822 0.0000 1.27E-01 0.0000 0.0000 0.00E+00 213 0.10 0.000 0.209 0.2452 0.7956 0.0000 1.28E-01 0.0000 0.0000 8.92E-04 214 0.00 0.000 0.239 0.1350 0.2137 0.0000 9.21E-02 0.0000 0.0000 1.06E-03 215 0.30 0.000 0.190 0.1717 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 216 0.10 0.000 0.215 0.1334 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 217 0.10 0.000 0.077 0.1410 0.0000 0.0000 0.00E+00 0.0000 0.0000 9.47E-04 218 0.00 0.000 0.036 0.1289 0.0000 0.0000 0.00E+00 0.0000 0.0000 4.52E-05 219 0.00 0.000 0.030 0.1187 0.0000 0.0000 0.00E+00 0.0000 0.0000 9.56E-04 220 0.00 0.000 0.006 0.1167 0.0000 0.0000 0.00E+00 0.0000 0.0000 3.63E-03 221 0.00 0.000 0.002 0.1162 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.66E-03 222 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 4.93E-04 223 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.37E-03 224 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 7.29E-04 225 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 3.34E-04 226 0.10 0.000 0.032 0.1387 0.0000 0.0000 0.00E+00 0.0000 0.0000 3.67E-03 227 0.00 0.000 0.030 0.1287 0.0000 0.0000 0.00E+00 0.0000 0.0000 2.78E-03 228 0.00 0.000 0.029 0.1191 0.0000 0.0000 0.00E+00 0.0000 0.0000 2.12E-03 229 0.00 0.000 0.007 0.1168 0.0000 0.0000 0.00E+00 0.0000 0.0000 9.38E-04 230 0.00 0.000 0.002 0.1162 0.0000 0.0000 0.00E+00 0.0000 0.0000 6.24E-05 231 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.03E-03 232 0.90 0.000 0.117 0.3772 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 233 0.00 0.000 0.230 0.2568 1.3319 0.0000 1.32E-01 0.0000 0.0000 0.00E+00 234 0.00 0.000 0.235 0.1366 0.5058 0.0000 1.26E-01 0.0000 0.0000 0.00E+00 235 0.00 0.000 0.062 0.1160 0.0042 0.0000 0.00E+00 0.0000 0.0000 1.80E-03 236 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.59E-04 237 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 Page 12 of 128 238 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 239 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 240 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 241 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.67E-03 242 0.20 0.000 0.090 0.1527 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 243 0.00 0.000 0.048 0.1366 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 244 0.00 0.000 0.055 0.1183 0.0000 0.0000 0.00E+00 0.0000 0.0000 2.11E-03 245 0.00 0.000 0.003 0.1171 0.0000 0.0000 0.00E+00 0.0000 0.0000 2.58E-03 246 0.00 0.000 0.003 0.1163 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.59E-03 247 0.00 0.000 0.001 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 6.72E-04 248 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.42E-03 249 0.10 0.000 0.047 0.1337 0.0000 0.0000 0.00E+00 0.0000 0.0000 8.58E-04 250 0.00 0.000 0.024 0.1255 0.0000 0.0000 0.00E+00 0.0000 0.0000 2.38E-04 251 0.00 0.000 0.022 0.1182 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 252 0.10 0.000 0.052 0.1342 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 253 0.10 0.000 0.099 0.1344 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 254 0.10 0.000 0.101 0.1342 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 255 0.00 0.000 0.030 0.1244 0.0000 0.0000 0.00E+00 0.0000 0.0000 9.08E-04 256 0.00 0.000 0.019 0.1179 0.0000 0.0000 0.00E+00 0.0000 0.0000 9.97E-04 257 0.50 0.000 0.164 0.2299 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.31E-03 258 0.10 0.000 0.137 0.2174 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.84E-03 259 0.30 0.000 0.212 0.2466 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.83E-03 260 0.40 0.000 0.182 0.2883 0.1837 0.0000 9.31E-02 0.0000 0.0000 1.49E-03 261 0.00 0.000 0.164 0.1976 0.2465 0.0000 1.08E-01 0.0000 0.0000 9.64E-04 262 0.00 0.000 0.116 0.1588 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.01E-05 263 0.00 0.000 0.108 0.1229 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 264 0.00 0.000 0.021 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 265 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 266 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.14E-03 267 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.32E-03 268 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.08E-03 269 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 7.49E-04 270 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 271 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.18E-03 272 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 Page 13 of 128 273 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 274 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 275 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 276 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 277 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.67E-03 278 0.50 0.000 0.029 0.2729 0.0000 0.0000 0.00E+00 0.0000 0.0000 3.96E-04 279 0.40 0.000 0.032 0.3637 0.5710 0.0000 9.57E-02 0.0000 0.0000 1.17E-03 280 0.00 0.000 0.103 0.2854 1.4074 0.0000 1.32E-01 0.0000 0.0000 1.22E-03 281 0.00 0.000 0.109 0.2064 0.8505 0.0000 1.28E-01 0.0000 0.0000 3.95E-04 282 0.00 0.000 0.098 0.1413 0.2216 0.0000 9.73E-02 0.0000 0.0000 0.00E+00 283 0.00 0.000 0.046 0.1260 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.15E-03 284 0.00 0.000 0.030 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 285 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.29E-03 286 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 3.21E-04 287 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 288 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 9.84E-04 289 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 7.35E-04 290 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.42E-03 291 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 4.19E-05 292 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 293 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 294 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 8.73E-04 295 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.94E-04 296 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 297 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 298 0.10 0.000 0.017 0.1435 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 299 0.10 0.000 0.023 0.1693 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.02E-03 300 0.00 0.000 0.018 0.1633 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 301 0.00 0.000 0.019 0.1568 0.0000 0.0000 0.00E+00 0.0000 0.0000 9.18E-04 302 * 0.00 0.000 0.018 0.1509 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.06E-03 303 * 0.00 0.000 0.000 0.1509 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 304 * 0.00 0.000 0.018 0.1448 0.0000 0.0000 0.00E+00 0.0000 0.0000 6.17E-04 305 * 0.00 0.000 0.019 0.1384 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.84E-03 306 0.00 0.000 0.019 0.1322 0.0000 0.0000 0.00E+00 0.0000 0.0000 2.14E-03 307 0.00 0.000 0.018 0.1261 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.72E-03 Page 14 of 128 308 0.20 0.000 0.026 0.1842 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.50E-03 309 0.00 0.000 0.018 0.1783 0.0000 0.0000 0.00E+00 0.0000 0.0000 2.10E-03 310 0.10 0.000 0.026 0.2031 0.0000 0.0000 0.00E+00 0.0000 0.0000 2.21E-03 311 0.20 0.000 0.025 0.2538 0.0208 0.0000 2.28E-02 0.0000 0.0000 2.10E-03 312 0.00 0.000 0.017 0.2303 0.0728 0.0000 5.32E-02 0.0000 0.0000 1.97E-03 313 0.00 0.000 0.017 0.2221 0.0047 0.0000 7.85E-03 0.0000 0.0000 1.94E-03 314 0.00 0.000 0.017 0.2163 0.0008 0.0000 6.00E-04 0.0000 0.0000 1.04E-03 315 0.00 0.000 0.016 0.2108 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 316 0.00 0.000 0.016 0.2054 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 317 0.30 0.000 0.024 0.2976 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.74E-03 318 0.00 0.000 0.016 0.2502 0.5574 0.0000 1.26E-01 0.0000 0.0000 2.62E-04 319 0.00 0.000 0.016 0.2178 0.1356 0.0000 8.19E-02 0.0000 0.0000 2.13E-03 320 0.00 0.000 0.015 0.2107 0.0037 0.0000 5.78E-03 0.0000 0.0000 9.30E-04 321 0.00 0.000 0.015 0.2057 0.0000 0.0000 0.00E+00 0.0000 0.0000 2.77E-03 322 0.00 0.000 0.015 0.2007 0.0000 0.0000 0.00E+00 0.0000 0.0000 2.23E-03 323 * 0.00 0.000 0.015 0.1958 0.0000 0.0000 0.00E+00 0.0000 0.0000 2.83E-03 324 0.00 0.000 0.015 0.1909 0.0000 0.0000 0.00E+00 0.0000 0.0000 2.82E-03 325 * 0.10 0.000 0.032 0.1975 0.0000 0.0000 0.00E+00 0.0000 0.0000 2.70E-03 326 0.00 0.000 0.035 0.2020 0.0000 0.0000 0.00E+00 0.0000 0.0000 5.08E-04 327 * 0.00 0.000 0.014 0.1972 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.02E-03 328 0.00 0.000 0.014 0.1924 0.0000 0.0000 0.00E+00 0.0000 0.0000 7.90E-04 329 0.00 0.000 0.014 0.1877 0.0000 0.0000 0.00E+00 0.0000 0.0000 6.19E-04 330 0.00 0.000 0.014 0.1831 0.0000 0.0000 0.00E+00 0.0000 0.0000 7.14E-06 331 0.00 0.000 0.014 0.1785 0.0000 0.0000 0.00E+00 0.0000 0.0000 6.32E-04 332 0.00 0.000 0.014 0.1740 0.0000 0.0000 0.00E+00 0.0000 0.0000 3.41E-03 333 0.00 0.000 0.013 0.1695 0.0000 0.0000 0.00E+00 0.0000 0.0000 3.58E-03 334 * 0.00 0.000 0.013 0.1651 0.0000 0.0000 0.00E+00 0.0000 0.0000 3.68E-03 335 * 0.10 0.000 0.021 0.1716 0.0000 0.0000 0.00E+00 0.0000 0.0000 2.66E-03 336 * 0.10 0.000 0.025 0.1782 0.0000 0.0000 0.00E+00 0.0000 0.0000 3.39E-04 337 0.00 0.000 0.027 0.1847 0.0000 0.0000 0.00E+00 0.0000 0.0000 4.25E-05 338 * 0.00 0.000 0.026 0.1914 0.0000 0.0000 0.00E+00 0.0000 0.0000 3.63E-03 339 * 0.00 0.000 0.021 0.1915 0.0000 0.0000 0.00E+00 0.0000 0.0000 3.35E-03 340 * 0.00 0.000 0.013 0.1871 0.0000 0.0000 0.00E+00 0.0000 0.0000 5.88E-04 341 * 0.00 0.000 0.013 0.1828 0.0000 0.0000 0.00E+00 0.0000 0.0000 6.10E-05 342 * 0.00 0.000 0.013 0.1785 0.0000 0.0000 0.00E+00 0.0000 0.0000 4.91E-04 Page 15 of 128 343 * 0.00 0.000 0.000 0.1785 0.0000 0.0000 0.00E+00 0.0000 0.0000 3.46E-03 344 * 0.00 0.000 0.000 0.1785 0.0000 0.0000 0.00E+00 0.0000 0.0000 8.05E-04 345 * * 0.00 0.000 0.000 0.1785 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 346 * * 0.10 0.000 0.016 0.1785 0.0000 0.0000 0.00E+00 0.0000 0.0000 8.07E-04 347 * * 0.00 0.000 0.016 0.1785 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 348 * * 0.00 0.000 0.017 0.1785 0.0000 0.0000 0.00E+00 0.0000 0.0000 2.84E-03 349 * * 0.00 0.000 0.016 0.1785 0.0000 0.0000 0.00E+00 0.0000 0.0000 2.41E-03 350 * * 0.00 0.000 0.018 0.1785 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.01E-03 351 * * 0.00 0.000 0.016 0.1785 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 352 * * 0.00 0.000 0.000 0.1785 0.0000 0.0000 0.00E+00 0.0000 0.0000 2.54E-04 353 * * 0.00 0.000 0.000 0.1785 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.45E-04 354 * * 0.00 0.000 0.000 0.1785 0.0000 0.0000 0.00E+00 0.0000 0.0000 3.06E-04 355 * * 0.00 0.000 0.000 0.1785 0.0000 0.0000 0.00E+00 0.0000 0.0000 3.46E-04 356 * * 0.00 0.000 0.000 0.1785 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.93E-03 357 * 0.00 0.000 0.000 0.1785 0.0000 0.0000 0.00E+00 0.0000 0.0000 3.39E-03 358 * 0.00 0.000 0.000 0.1785 0.0000 0.0000 0.00E+00 0.0000 0.0000 2.78E-03 359 * 0.00 0.000 0.000 0.1785 0.0000 0.0000 0.00E+00 0.0000 0.0000 2.29E-03 360 * 0.00 0.000 0.000 0.1785 0.0000 0.0000 0.00E+00 0.0000 0.0000 2.19E-03 361 * 0.00 0.000 0.000 0.1785 0.0000 0.0000 0.00E+00 0.0000 0.0000 2.27E-03 362 * 0.00 0.000 0.000 0.1785 0.0000 0.0000 0.00E+00 0.0000 0.0000 3.00E-03 363 * * 0.00 0.000 0.000 0.1785 0.0000 0.0000 0.00E+00 0.0000 0.0000 3.09E-03 364 * * 0.00 0.000 0.000 0.1785 0.0000 0.0000 0.00E+00 0.0000 0.0000 3.09E-03 365 * * 0.00 0.000 0.000 0.1785 0.0000 0.0000 0.00E+00 0.0000 0.0000 3.01E-03 * = Frozen (air or soil) inches cubic feet percent Precipitation 18.70 4,751,670.0 100.00 Runoff 0.522 132,698.8 2.79 Evapotranspiration 13.569 3,447,766.7 72.56 Percolation/Leakage through Layer 2 4.607985 1,170,889.1 24.64 Average Head on Top of Layer 2 0.0923 ------ Percolation/Leakage through Layer 12 0.382757 97,258.6 2.05 Annual Totals for Year 1 Page 16 of 128 Change in Water Storage 4.2265 1,073,945.9 22.60 Soil Water at Start of Year 214.7496 #########1148.39 Soil Water at End of Year 218.9760 #########1170.99 Snow Water at Start of Year 0.0000 0.0000 0.00 Snow Water at End of Year 0.0000 0.0000 0.00 Annual Water Budget Balance 0.0000 0.0000 0.00 Page 17 of 128 Daily Output for Year 2 Column key:Head #1: drainage from Layer 2 Title:Long Valley Landfill Simulated On:Leak #1: leakage thru Layer 2 Leak #2: leakage thru Layer 12 Day Rain Runoff ET Evap. Zone Water Head #1 Drain #1 Leak #1 Head #2 Drain #2 Leak #2 Air Soil (inches)(inches)(inches)(in/in)(inches)(inches)(inches)(inches)(inches)(inches) 1 * * 0.00 0.000 0.000 0.1785 0.0000 0.0000 0.00E+00 0.0000 0.0000 2.86E-03 2 * * 0.00 0.000 0.000 0.1785 0.0000 0.0000 0.00E+00 0.0000 0.0000 2.29E-03 3 * * 0.00 0.000 0.000 0.1785 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.34E-03 4 * * 0.00 0.000 0.000 0.1785 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.60E-03 5 * * 0.00 0.000 0.000 0.1785 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.85E-03 6 * * 0.00 0.000 0.000 0.1785 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.68E-03 7 * * 0.10 0.000 0.026 0.1785 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.40E-03 8 * * 0.00 0.000 0.032 0.1785 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.13E-03 9 * * 0.00 0.000 0.030 0.1785 0.0000 0.0000 0.00E+00 0.0000 0.0000 8.90E-04 10 * * 0.00 0.000 0.012 0.1785 0.0000 0.0000 0.00E+00 0.0000 0.0000 6.84E-04 11 * 0.00 0.000 0.000 0.1785 0.0000 0.0000 0.00E+00 0.0000 0.0000 3.31E-03 12 * 0.00 0.000 0.000 0.1785 0.0000 0.0000 0.00E+00 0.0000 0.0000 3.34E-03 13 * 0.00 0.000 0.000 0.1785 0.0000 0.0000 0.00E+00 0.0000 0.0000 3.33E-03 14 * * 0.00 0.000 0.000 0.1785 0.0000 0.0000 0.00E+00 0.0000 0.0000 9.70E-04 15 * * 0.00 0.000 0.000 0.1785 0.0000 0.0000 0.00E+00 0.0000 0.0000 7.78E-04 16 * * 0.00 0.000 0.000 0.1785 0.0000 0.0000 0.00E+00 0.0000 0.0000 3.85E-04 17 * * 0.00 0.000 0.000 0.1785 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.11E-03 18 * * 0.00 0.000 0.000 0.1785 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 19 * 0.00 0.000 0.000 0.1785 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 20 * 0.00 0.000 0.000 0.1785 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 21 * 0.50 0.181 0.005 0.2830 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 22 * 0.00 0.000 0.000 0.2830 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 23 * 0.10 0.021 0.005 0.3076 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 24 * 0.00 0.000 0.000 0.3076 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 25 0.00 0.000 0.036 0.2634 0.6705 0.0000 9.64E-02 0.0000 0.0000 0.00E+00 26 0.00 0.000 0.049 0.2049 0.6619 0.0000 1.27E-01 0.0000 0.0000 0.00E+00 27 0.20 0.000 0.058 0.2276 0.1265 0.0000 7.33E-02 0.0000 0.0000 9.45E-04 7/19/2024 11:05 Freezing Status* Page 18 of 128 28 0.00 0.000 0.048 0.2116 0.0000 0.0000 0.00E+00 0.0000 0.0000 4.81E-05 29 * 0.00 0.000 0.043 0.1974 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 30 * 0.00 0.000 0.000 0.1974 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.56E-03 31 * * 0.00 0.000 0.000 0.1974 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.28E-03 32 * * 0.00 0.000 0.000 0.1974 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.78E-03 33 * * 0.20 0.000 0.021 0.1974 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.89E-03 34 * * 0.00 0.000 0.022 0.1974 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.87E-03 35 * * 0.00 0.000 0.025 0.1974 0.0000 0.0000 0.00E+00 0.0000 0.0000 2.11E-03 36 * * 0.00 0.000 0.046 0.1974 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.92E-03 37 * 0.00 0.000 0.031 0.2157 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.85E-03 38 * 0.00 0.000 0.000 0.2157 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.10E-03 39 * * 0.00 0.000 0.000 0.2157 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.26E-03 40 * 0.00 0.000 0.000 0.2157 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.47E-03 41 * * 0.00 0.000 0.000 0.2157 0.0000 0.0000 0.00E+00 0.0000 0.0000 2.13E-03 42 * * 0.00 0.000 0.000 0.2157 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.96E-03 43 * * 0.30 0.000 0.029 0.2157 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.75E-03 44 * * 0.10 0.000 0.029 0.2157 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.66E-03 45 * 0.10 0.052 0.000 0.2846 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.88E-03 46 * 0.00 0.060 0.042 0.3118 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.86E-03 47 * 0.00 0.000 0.000 0.3118 0.0000 0.0000 0.00E+00 0.0000 0.0000 2.00E-03 48 * 0.00 0.000 0.000 0.3118 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.52E-03 49 * 0.00 0.000 0.000 0.3118 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.73E-03 50 * 0.10 0.029 0.004 0.3340 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.58E-03 51 0.00 0.000 0.041 0.2871 1.1520 0.0000 9.97E-02 0.0000 0.0000 1.94E-03 52 0.00 0.000 0.053 0.2265 0.9788 0.0000 1.29E-01 0.0000 0.0000 8.94E-04 53 0.00 0.000 0.060 0.1650 0.3730 0.0000 1.25E-01 0.0000 0.0000 9.60E-04 54 0.10 0.000 0.093 0.1641 0.0112 0.0000 9.63E-03 0.0000 0.0000 0.00E+00 55 0.00 0.000 0.066 0.1420 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.25E-03 56 0.00 0.000 0.073 0.1176 0.0000 0.0000 0.00E+00 0.0000 0.0000 2.75E-04 57 0.00 0.000 0.004 0.1164 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 58 0.00 0.000 0.001 0.1161 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 59 0.40 0.000 0.043 0.2350 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 60 0.00 0.000 0.077 0.2092 0.0000 0.0000 0.00E+00 0.0000 0.0000 9.55E-04 61 0.80 0.000 0.060 0.4344 0.5008 0.0000 6.46E-02 0.0000 0.0000 5.19E-04 62 0.30 0.000 0.100 0.4542 2.7045 0.0000 1.41E-01 0.0000 0.0000 9.83E-04 Page 19 of 128 63 0.00 0.000 0.106 0.3723 2.5309 0.0000 1.40E-01 0.0000 0.0000 6.07E-04 64 0.00 0.000 0.062 0.3069 1.7022 0.0000 1.34E-01 0.0000 0.0000 3.77E-03 65 0.00 0.000 0.067 0.2415 1.0407 0.0000 1.30E-01 0.0000 0.0000 3.23E-04 66 0.00 0.000 0.066 0.1776 0.4284 0.0000 1.25E-01 0.0000 0.0000 8.29E-04 67 0.10 0.000 0.079 0.1773 0.0246 0.0000 2.21E-02 0.0000 0.0000 1.15E-04 68 0.00 0.000 0.104 0.1425 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.64E-03 69 0.00 0.000 0.074 0.1179 0.0000 0.0000 0.00E+00 0.0000 0.0000 3.22E-03 70 0.00 0.000 0.004 0.1165 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.36E-03 71 0.00 0.000 0.001 0.1161 0.0000 0.0000 0.00E+00 0.0000 0.0000 8.93E-04 72 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.52E-04 73 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.22E-03 74 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.74E-03 75 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 3.48E-04 76 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 77 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 78 0.50 0.000 0.053 0.2650 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.94E-03 79 0.20 0.000 0.079 0.2741 0.1951 0.0000 9.32E-02 0.0000 0.0000 1.16E-03 80 0.00 0.000 0.128 0.2004 0.1915 0.0000 9.31E-02 0.0000 0.0000 4.44E-16 81 0.00 0.000 0.065 0.1787 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 82 0.00 0.000 0.069 0.1558 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 83 0.00 0.000 0.063 0.1345 0.0023 0.0000 8.12E-04 0.0000 0.0000 0.00E+00 84 0.00 0.000 0.055 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 85 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.14E-03 86 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.89E-03 87 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.39E-03 88 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.55E-03 89 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.25E-03 90 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.05E-03 91 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.59E-03 92 0.10 0.000 0.018 0.1432 0.0000 0.0000 0.00E+00 0.0000 0.0000 2.06E-03 93 0.00 0.000 0.022 0.1360 0.0000 0.0000 0.00E+00 0.0000 0.0000 2.93E-03 94 0.00 0.000 0.020 0.1292 0.0000 0.0000 0.00E+00 0.0000 0.0000 2.38E-03 95 0.00 0.000 0.024 0.1213 0.0000 0.0000 0.00E+00 0.0000 0.0000 6.60E-04 96 0.00 0.000 0.014 0.1167 0.0000 0.0000 0.00E+00 0.0000 0.0000 8.27E-04 97 0.00 0.000 0.002 0.1162 0.0000 0.0000 0.00E+00 0.0000 0.0000 2.48E-04 Page 20 of 128 98 0.00 0.000 0.001 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.01E-03 99 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 9.60E-04 100 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 5.52E-04 101 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 2.75E-03 102 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.01E-03 103 0.50 0.000 0.022 0.2754 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.69E-03 104 0.00 0.000 0.021 0.2373 0.2812 0.0000 9.38E-02 0.0000 0.0000 4.74E-04 105 0.40 0.000 0.025 0.3211 0.2087 0.0000 1.24E-01 0.0000 0.0000 4.83E-04 106 0.00 0.000 0.116 0.2398 0.7369 0.0000 1.27E-01 0.0000 0.0000 1.61E-03 107 0.00 0.000 0.194 0.1400 0.2714 0.0000 1.06E-01 0.0000 0.0000 1.03E-03 108 0.00 0.000 0.068 0.1172 0.0000 0.0000 0.00E+00 0.0000 0.0000 2.59E-03 109 0.00 0.000 0.003 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 3.23E-03 110 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 2.14E-03 111 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 2.66E-04 112 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.36E-03 113 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.41E-03 114 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 7.97E-05 115 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 116 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.58E-03 117 0.10 0.000 0.017 0.1438 0.0000 0.0000 0.00E+00 0.0000 0.0000 8.57E-04 118 0.00 0.000 0.019 0.1373 0.0000 0.0000 0.00E+00 0.0000 0.0000 2.26E-04 119 0.00 0.000 0.021 0.1305 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 120 0.00 0.000 0.022 0.1232 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 121 0.00 0.000 0.019 0.1169 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 122 0.00 0.000 0.002 0.1162 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 123 0.00 0.000 0.001 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 124 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 125 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 126 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 127 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 128 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 129 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 130 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 131 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 9.87E-04 132 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 Page 21 of 128 133 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 134 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 135 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 136 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 9.83E-04 137 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.15E-03 138 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.74E-03 139 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 9.20E-04 140 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 141 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 142 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 143 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.91E-03 144 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.42E-06 145 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 5.77E-05 146 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.40E-04 147 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 2.23E-04 148 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 4.01E-03 149 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 4.03E-03 150 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 3.95E-03 151 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 2.45E-03 152 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 9.97E-07 153 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.16E-03 154 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 8.29E-04 155 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 2.82E-04 156 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.09E-03 157 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 158 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 159 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 160 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 161 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 162 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 163 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 164 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 165 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 166 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 167 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 Page 22 of 128 168 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 169 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 170 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 171 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 172 0.00 0.000 0.000 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0.0000 0.00E+00 186 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 187 0.50 0.000 0.012 0.2785 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 188 0.00 0.000 0.010 0.2437 0.3477 0.0000 9.42E-02 0.0000 0.0000 0.00E+00 189 0.00 0.000 0.011 0.2095 0.1739 0.0000 9.20E-02 0.0000 0.0000 0.00E+00 190 0.00 0.000 0.011 0.2026 0.0056 0.0000 9.88E-03 0.0000 0.0000 0.00E+00 191 0.00 0.000 0.012 0.1976 0.0023 0.0000 3.31E-03 0.0000 0.0000 0.00E+00 192 0.00 0.000 0.012 0.1931 0.0010 0.0000 1.62E-03 0.0000 0.0000 0.00E+00 193 0.00 0.000 0.012 0.1891 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 194 0.00 0.000 0.012 0.1852 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 195 0.00 0.000 0.011 0.1813 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 196 0.30 0.000 0.015 0.2764 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 197 0.10 0.000 0.014 0.2737 0.2746 0.0000 9.37E-02 0.0000 0.0000 0.00E+00 198 0.10 0.000 0.014 0.2606 0.3843 0.0000 1.25E-01 0.0000 0.0000 0.00E+00 199 0.00 0.000 0.010 0.2333 0.0744 0.0000 7.17E-02 0.0000 0.0000 0.00E+00 200 0.00 0.000 0.010 0.2256 0.0076 0.0000 1.31E-02 0.0000 0.0000 0.00E+00 201 0.00 0.000 0.010 0.2197 0.0046 0.0000 7.55E-03 0.0000 0.0000 0.00E+00 202 0.10 0.000 0.013 0.2483 0.0010 0.0000 8.86E-04 0.0000 0.0000 0.00E+00 Page 23 of 128 203 0.00 0.000 0.010 0.2235 0.0918 0.0000 6.46E-02 0.0000 0.0000 0.00E+00 204 0.50 0.000 0.013 0.3642 0.2977 0.0000 6.49E-02 0.0000 0.0000 0.00E+00 205 0.30 0.000 0.013 0.4152 1.7232 0.0000 1.34E-01 0.0000 0.0000 0.00E+00 206 0.00 0.000 0.009 0.3664 2.1211 0.0000 1.37E-01 0.0000 0.0000 0.00E+00 207 0.00 0.000 0.009 0.3189 1.5637 0.0000 1.33E-01 0.0000 0.0000 0.00E+00 208 0.00 0.000 0.009 0.2728 0.9692 0.0000 1.29E-01 0.0000 0.0000 0.00E+00 209 0.50 0.000 0.013 0.3926 0.7919 0.0000 1.28E-01 0.0000 0.0000 0.00E+00 210 0.50 0.000 0.178 0.4539 2.2059 0.0000 1.37E-01 0.0000 0.0000 0.00E+00 211 0.10 0.000 0.310 0.3377 2.3952 0.0000 1.39E-01 0.0000 0.0000 0.00E+00 212 0.70 0.005 0.184 0.4630 1.8668 0.0000 1.35E-01 0.0000 0.0000 0.00E+00 213 0.20 0.021 0.192 0.4115 2.7477 0.0000 1.41E-01 0.0000 0.0000 0.00E+00 214 0.00 0.000 0.186 0.3044 1.8961 0.0000 1.35E-01 0.0000 0.0000 0.00E+00 215 0.00 0.000 0.175 0.2030 0.9953 0.0000 1.29E-01 0.0000 0.0000 1.16E-03 216 0.00 0.000 0.182 0.1215 0.1936 0.0000 6.25E-02 0.0000 0.0000 3.38E-04 217 0.00 0.000 0.016 0.1161 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.00E-03 218 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.00E-03 219 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 220 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 221 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 222 0.30 0.000 0.037 0.2036 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 223 0.10 0.000 0.044 0.2223 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 224 0.00 0.000 0.040 0.2091 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 225 0.20 0.000 0.042 0.2618 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.53E-03 226 0.40 0.000 0.039 0.3405 0.3327 0.0000 1.25E-01 0.0000 0.0000 1.48E-03 227 0.00 0.000 0.188 0.2349 0.9711 0.0000 1.29E-01 0.0000 0.0000 1.89E-03 228 0.00 0.000 0.247 0.1290 0.2772 0.0000 7.08E-02 0.0000 0.0000 4.49E-05 229 0.00 0.000 0.039 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 230 0.10 0.000 0.037 0.1371 0.0000 0.0000 0.00E+00 0.0000 0.0000 9.82E-04 231 0.00 0.000 0.027 0.1282 0.0000 0.0000 0.00E+00 0.0000 0.0000 6.80E-04 232 0.00 0.000 0.031 0.1179 0.0000 0.0000 0.00E+00 0.0000 0.0000 5.83E-04 233 0.00 0.000 0.004 0.1165 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 234 0.00 0.000 0.001 0.1161 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.18E-03 235 0.20 0.000 0.020 0.1760 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 236 0.20 0.000 0.033 0.2316 0.0000 0.0000 0.00E+00 0.0000 0.0000 7.20E-04 237 0.00 0.000 0.034 0.2193 0.0029 0.0000 3.29E-03 0.0000 0.0000 1.98E-03 Page 24 of 128 238 0.00 0.000 0.035 0.2048 0.0046 0.0000 8.37E-03 0.0000 0.0000 8.44E-04 239 0.00 0.000 0.034 0.1929 0.0016 0.0000 2.02E-03 0.0000 0.0000 2.05E-03 240 0.00 0.000 0.031 0.1825 0.0000 0.0000 0.00E+00 0.0000 0.0000 8.61E-04 241 0.00 0.000 0.030 0.1726 0.0000 0.0000 0.00E+00 0.0000 0.0000 8.77E-04 242 0.00 0.000 0.031 0.1622 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 243 0.00 0.000 0.030 0.1521 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.91E-03 244 0.10 0.000 0.031 0.1751 0.0000 0.0000 0.00E+00 0.0000 0.0000 6.92E-04 245 0.00 0.000 0.027 0.1659 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.58E-03 246 0.00 0.000 0.029 0.1564 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.88E-03 247 0.00 0.000 0.026 0.1476 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.19E-03 248 0.00 0.000 0.026 0.1389 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.24E-03 249 0.00 0.000 0.027 0.1299 0.0000 0.0000 0.00E+00 0.0000 0.0000 8.14E-04 250 0.00 0.000 0.026 0.1212 0.0000 0.0000 0.00E+00 0.0000 0.0000 2.07E-03 251 0.10 0.000 0.030 0.1446 0.0000 0.0000 0.00E+00 0.0000 0.0000 5.29E-04 252 0.00 0.000 0.017 0.1388 0.0000 0.0000 0.00E+00 0.0000 0.0000 6.31E-04 253 0.00 0.000 0.023 0.1313 0.0000 0.0000 0.00E+00 0.0000 0.0000 9.60E-04 254 0.00 0.000 0.020 0.1245 0.0000 0.0000 0.00E+00 0.0000 0.0000 4.08E-04 255 0.60 0.000 0.025 0.3160 0.0000 0.0000 0.00E+00 0.0000 0.0000 2.97E-03 256 0.10 0.000 0.194 0.2420 0.7810 0.0000 1.28E-01 0.0000 0.0000 7.19E-04 257 0.00 0.000 0.027 0.1913 0.4704 0.0000 1.26E-01 0.0000 0.0000 1.06E-03 258 0.00 0.000 0.026 0.1721 0.0323 0.0000 3.11E-02 0.0000 0.0000 0.00E+00 259 0.00 0.000 0.024 0.1642 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 260 0.00 0.000 0.024 0.1560 0.0005 0.0000 9.70E-04 0.0000 0.0000 1.49E-03 261 0.00 0.000 0.024 0.1480 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.20E-03 262 0.00 0.000 0.027 0.1389 0.0000 0.0000 0.00E+00 0.0000 0.0000 8.72E-04 263 0.00 0.000 0.026 0.1304 0.0000 0.0000 0.00E+00 0.0000 0.0000 2.38E-03 264 0.00 0.000 0.024 0.1224 0.0000 0.0000 0.00E+00 0.0000 0.0000 2.10E-03 265 0.00 0.000 0.019 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 2.19E-03 266 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 2.52E-03 267 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.21E-03 268 0.30 0.000 0.020 0.2093 0.0000 0.0000 0.00E+00 0.0000 0.0000 9.54E-04 269 0.00 0.000 0.138 0.1634 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.73E-03 270 0.00 0.000 0.026 0.1549 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.04E-03 271 0.10 0.000 0.028 0.1790 0.0000 0.0000 0.00E+00 0.0000 0.0000 6.51E-04 272 0.00 0.000 0.026 0.1704 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.47E-03 Page 25 of 128 273 0.00 0.000 0.023 0.1629 0.0000 0.0000 0.00E+00 0.0000 0.0000 2.04E-04 274 0.00 0.000 0.024 0.1549 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 275 0.00 0.000 0.022 0.1476 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 276 0.00 0.000 0.018 0.1417 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 277 0.00 0.000 0.012 0.1375 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 278 0.00 0.000 0.014 0.1330 0.0000 0.0000 0.00E+00 0.0000 0.0000 9.06E-04 279 0.00 0.000 0.013 0.1285 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.26E-04 280 0.00 0.000 0.013 0.1240 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.13E-03 281 0.00 0.000 0.013 0.1196 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.06E-03 282 0.00 0.000 0.011 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.18E-03 283 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 5.54E-04 284 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.56E-03 285 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 8.92E-04 286 1.00 0.000 0.015 0.4331 0.3663 0.0000 3.31E-02 0.0000 0.0000 1.00E-03 287 0.00 0.000 0.121 0.3467 2.2651 0.0000 1.38E-01 0.0000 0.0000 2.44E-04 288 0.00 0.000 0.122 0.2619 1.4340 0.0000 1.32E-01 0.0000 0.0000 0.00E+00 289 0.00 0.000 0.057 0.2004 0.7539 0.0000 1.28E-01 0.0000 0.0000 0.00E+00 290 0.00 0.000 0.052 0.1534 0.1868 0.0000 8.90E-02 0.0000 0.0000 0.00E+00 291 0.00 0.000 0.051 0.1364 0.0000 0.0000 0.00E+00 0.0000 0.0000 8.29E-04 292 0.00 0.000 0.045 0.1213 0.0000 0.0000 0.00E+00 0.0000 0.0000 2.82E-04 293 0.00 0.000 0.016 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 294 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 295 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 7.33E-04 296 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.71E-03 297 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 298 0.10 0.000 0.019 0.1431 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 299 0.00 0.000 0.028 0.1339 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 300 0.00 0.000 0.027 0.1248 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 301 0.00 0.000 0.023 0.1171 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 302 0.00 0.000 0.002 0.1163 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 303 0.00 0.000 0.001 0.1161 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 304 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 2.01E-03 305 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 2.14E-03 306 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 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320 0.00 0.000 0.020 0.1671 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 321 0.10 0.000 0.023 0.1928 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 322 0.00 0.000 0.019 0.1864 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 323 0.00 0.000 0.019 0.1801 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 324 0.00 0.000 0.019 0.1739 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 325 0.00 0.000 0.018 0.1678 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 326 0.00 0.000 0.018 0.1619 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 327 * 0.00 0.000 0.018 0.1560 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 328 * 0.00 0.000 0.017 0.1502 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 329 * 0.00 0.000 0.017 0.1446 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 330 * 0.00 0.000 0.017 0.1390 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 331 0.00 0.000 0.016 0.1335 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 332 0.00 0.000 0.016 0.1281 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 333 * 0.00 0.000 0.016 0.1228 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 334 * 0.00 0.000 0.016 0.1176 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 335 * 0.00 0.000 0.005 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 336 * 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 337 * 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 338 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 339 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 340 * 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 341 * 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 342 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 Page 27 of 128 343 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 344 * 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 345 * 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 346 * 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 347 * 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 348 * * 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 349 * * 0.10 0.000 0.018 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 350 * * 0.00 0.000 0.018 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 351 * * 0.00 0.000 0.019 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 352 * * 0.00 0.000 0.015 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 353 * * 0.10 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 354 * * 0.00 0.000 0.016 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 355 * * 0.00 0.000 0.018 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 356 * * 0.00 0.000 0.022 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 357 * * 0.00 0.000 0.022 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 9.98E-04 358 * * 0.00 0.000 0.021 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.50E-03 359 * * 0.30 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 4.44E-16 360 * * 0.10 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.03E-03 361 * * 0.10 0.000 0.016 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 362 * * 0.60 0.000 0.016 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 363 * * 0.00 0.000 0.019 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 364 * 0.00 0.000 0.020 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 365 * * 0.00 0.000 0.013 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 * = Frozen (air or soil) inches cubic feet percent Precipitation 14.70 3,735,270.0 100.00 Runoff 0.370 93,994.2 2.52 Evapotranspiration 8.089 2,055,533.8 55.03 Percolation/Leakage through Layer 2 5.381014 1,367,315.6 36.61 Average Head on Top of Layer 2 0.1200 ------ Percolation/Leakage through Layer 12 0.241961 61,482.2 1.65 Annual Totals for Year 2 Page 28 of 128 Change in Water Storage 5.9987 1,524,259.9 40.81 Soil Water at Start of Year 218.9760 #########1489.63 Soil Water at End of Year 223.9277 #########1523.32 Snow Water at Start of Year 0.0000 0.0000 0.00 Snow Water at End of Year 1.0470 266,038.7 7.12 Annual Water Budget Balance 0.0000 0.0000 0.00 Page 29 of 128 Daily Output for Year 3 Column key:Head #1: drainage from Layer 2 Title:Long Valley Landfill Simulated On:Leak #1: leakage thru Layer 2 Leak #2: leakage thru Layer 12 Day Rain Runoff ET Evap. Zone Water Head #1 Drain #1 Leak #1 Head #2 Drain #2 Leak #2 Air Soil (inches)(inches)(inches)(in/in)(inches)(inches)(inches)(inches)(inches)(inches) 1 * * 0.00 0.000 0.015 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 2 * * 0.00 0.000 0.013 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 3 * * 0.00 0.000 0.014 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 4 * * 0.00 0.000 0.021 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 5 * * 0.00 0.000 0.013 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 6 * * 0.00 0.000 0.014 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 7 * * 0.00 0.000 0.011 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 8 * * 0.00 0.000 0.010 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 9 * * 0.00 0.000 0.018 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 10 * * 0.50 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.22E-03 11 * * 0.00 0.000 0.015 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.21E-03 12 * * 0.00 0.000 0.017 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.31E-03 13 * * 0.00 0.000 0.018 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 2.22E-04 14 * * 0.00 0.000 0.017 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 15 * * 0.10 0.000 0.014 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 16 * * 0.00 0.000 0.020 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 17 * * 0.00 0.000 0.020 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 18 * * 0.00 0.000 0.017 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 19 * * 0.00 0.000 0.023 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 20 * * 0.00 0.000 0.020 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 21 * * 0.00 0.000 0.014 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 22 * * 0.00 0.000 0.021 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 23 * * 0.00 0.000 0.014 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 24 * * 0.10 0.000 0.016 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 9.70E-04 25 * * 0.10 0.000 0.015 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 8.86E-04 26 * * 0.30 0.000 0.015 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 5.91E-04 27 * * 0.30 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.96E-03 7/19/2024 11:05 Freezing Status* Page 30 of 128 28 * * 0.00 0.000 0.015 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 9.78E-04 29 * * 0.50 0.000 0.015 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 2.21E-03 30 * * 0.00 0.000 0.013 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 8.60E-04 31 * * 0.00 0.000 0.019 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 32 * * 0.00 0.000 0.015 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 33 * * 0.00 0.000 0.017 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 34 * * 0.00 0.000 0.018 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 35 * * 0.00 0.000 0.024 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 36 * * 0.00 0.000 0.019 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 37 * * 0.00 0.000 0.021 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 38 * * 0.00 0.000 0.019 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 39 * * 0.00 0.000 0.019 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 40 * * 0.20 0.000 0.014 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 41 * * 0.00 0.000 0.015 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 42 * * 0.10 0.000 0.012 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 43 * * 0.00 0.000 0.013 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 44 * * 0.00 0.000 0.019 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 45 * * 0.00 0.000 0.020 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 46 * * 0.00 0.000 0.023 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 47 * * 0.00 0.000 0.024 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 48 * * 0.00 0.000 0.025 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 49 * * 0.00 0.000 0.018 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 50 * * 0.00 0.000 0.021 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 51 * * 0.10 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 52 * * 0.20 0.000 0.015 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 53 * * 0.00 0.000 0.013 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 54 * * 0.40 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.94E-03 55 * * 0.20 0.000 0.014 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 5.52E-04 56 * * 0.00 0.000 0.017 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 57 * * 0.20 0.000 0.013 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 58 * * 0.00 0.000 0.014 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.94E-03 59 * * 0.00 0.000 0.017 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 7.02E-04 60 * * 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.24E-03 61 * 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.07E-03 62 * 0.30 0.643 0.000 0.2591 0.0000 0.0000 0.00E+00 0.0000 0.0000 6.65E-04 Page 31 of 128 63 * * 0.00 0.000 0.016 0.2674 0.0000 0.0000 0.00E+00 0.0000 0.0000 5.25E-04 64 * * 0.00 0.000 0.024 0.2674 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.46E-03 65 * 0.00 0.012 0.029 0.2770 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.40E-03 66 * 0.00 0.005 0.028 0.2817 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.18E-03 67 * * 0.30 0.000 0.030 0.2817 0.0000 0.0000 0.00E+00 0.0000 0.0000 4.44E-16 68 * * 0.40 0.000 0.025 0.2817 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 69 * * 0.00 0.000 0.022 0.2817 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 70 * * 0.00 0.000 0.025 0.2817 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 71 * * 0.00 0.000 0.032 0.2817 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 72 * 0.00 0.064 0.020 0.3001 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 73 * 0.00 0.688 0.000 0.3325 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 74 * 0.00 0.772 0.000 0.3556 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 75 * 0.00 0.266 0.000 0.3711 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 76 * 0.00 0.011 0.034 0.3711 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.68E-03 77 * * 0.00 0.000 0.033 0.3711 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.00E-03 78 * 0.00 0.099 0.021 0.3758 0.0000 0.0000 0.00E+00 0.0000 0.0000 7.47E-04 79 * 0.00 0.163 0.012 0.3833 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.01E-03 80 * * 0.10 0.000 0.032 0.3833 0.0000 0.0000 0.00E+00 0.0000 0.0000 4.44E-16 81 * * 0.00 0.000 0.030 0.3833 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 82 * * 0.00 0.000 0.020 0.3833 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 83 * * 0.00 0.000 0.028 0.3833 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 84 * * 0.00 0.000 0.030 0.3833 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 85 * 0.00 0.195 0.006 0.3916 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 86 * 0.00 0.216 0.067 0.3916 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 87 * 0.00 0.000 0.000 0.3916 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 88 * 0.00 0.000 0.000 0.3916 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 89 * 0.00 0.000 0.000 0.3916 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 90 0.00 0.000 0.051 0.3407 1.5224 0.0000 1.02E-01 0.0000 0.0000 0.00E+00 91 0.10 0.000 0.058 0.3105 1.4345 0.0000 1.32E-01 0.0000 0.0000 0.00E+00 92 0.00 0.000 0.128 0.2253 0.8001 0.0000 1.28E-01 0.0000 0.0000 0.00E+00 93 0.00 0.000 0.122 0.1546 0.1925 0.0000 9.05E-02 0.0000 0.0000 8.72E-04 94 0.00 0.000 0.103 0.1203 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.96E-04 95 0.00 0.000 0.013 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 96 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 97 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 Page 32 of 128 98 0.40 0.000 0.033 0.2385 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 99 * 0.10 0.000 0.080 0.2335 0.0075 0.0000 3.47E-02 0.0000 0.0000 1.94E-03 100 * 0.00 0.000 0.041 0.2169 0.0053 0.0000 9.56E-03 0.0000 0.0000 1.98E-03 101 0.10 0.000 0.040 0.2362 0.0011 0.0000 2.70E-03 0.0000 0.0000 9.40E-04 102 0.00 0.000 0.034 0.2224 0.0034 0.0000 6.99E-03 0.0000 0.0000 1.64E-03 103 0.00 0.000 0.032 0.2076 0.0075 0.0000 1.23E-02 0.0000 0.0000 3.44E-04 104 0.00 0.000 0.030 0.1964 0.0019 0.0000 3.13E-03 0.0000 0.0000 9.21E-04 105 0.10 0.000 0.032 0.2192 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.04E-03 106 * 0.30 0.000 0.056 0.2257 0.0000 0.0000 0.00E+00 0.0000 0.0000 9.66E-04 107 * 0.20 0.000 0.044 0.2323 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.37E-03 108 * 0.00 0.000 0.050 0.2389 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.84E-05 109 * 0.00 0.000 0.054 0.2449 0.0016 0.0000 1.51E-03 0.0000 0.0000 0.00E+00 110 0.10 0.000 0.000 0.3179 0.2963 0.0000 9.39E-02 0.0000 0.0000 1.32E-03 111 0.00 0.000 0.092 0.2462 0.7741 0.0000 1.28E-01 0.0000 0.0000 2.58E-04 112 0.00 0.000 0.163 0.1529 0.3059 0.0000 1.17E-01 0.0000 0.0000 0.00E+00 113 * 0.00 0.000 0.049 0.1316 0.0000 0.0000 1.51E-02 0.0000 0.0000 0.00E+00 114 0.00 0.000 0.047 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 115 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 116 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 117 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 118 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.50E-03 119 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 8.84E-04 120 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 6.38E-04 121 * 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 122 * 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.84E-03 123 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 2.22E-03 124 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 125 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 126 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 7.30E-04 127 0.30 0.000 0.020 0.2092 0.0000 0.0000 0.00E+00 0.0000 0.0000 3.44E-03 128 0.00 0.000 0.023 0.2014 0.0000 0.0000 0.00E+00 0.0000 0.0000 2.76E-03 129 0.00 0.000 0.025 0.1932 0.0000 0.0000 0.00E+00 0.0000 0.0000 2.46E-03 130 0.00 0.000 0.024 0.1853 0.0000 0.0000 0.00E+00 0.0000 0.0000 2.79E-03 131 0.00 0.000 0.023 0.1776 0.0000 0.0000 0.00E+00 0.0000 0.0000 2.98E-03 132 0.00 0.000 0.022 0.1701 0.0000 0.0000 0.00E+00 0.0000 0.0000 3.00E-03 Page 33 of 128 133 0.00 0.000 0.022 0.1628 0.0000 0.0000 0.00E+00 0.0000 0.0000 2.88E-03 134 0.00 0.000 0.021 0.1558 0.0000 0.0000 0.00E+00 0.0000 0.0000 2.67E-03 135 0.00 0.000 0.021 0.1489 0.0000 0.0000 0.00E+00 0.0000 0.0000 2.62E-03 136 0.00 0.000 0.020 0.1421 0.0000 0.0000 0.00E+00 0.0000 0.0000 2.56E-03 137 0.10 0.000 0.022 0.1680 0.0000 0.0000 0.00E+00 0.0000 0.0000 2.20E-03 138 0.10 0.000 0.022 0.1941 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.93E-03 139 0.20 0.000 0.021 0.2536 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.92E-03 140 0.00 0.000 0.019 0.2358 0.0331 0.0000 3.50E-02 0.0000 0.0000 2.53E-03 141 0.00 0.000 0.018 0.2260 0.0058 0.0000 1.10E-02 0.0000 0.0000 2.29E-03 142 0.00 0.000 0.018 0.2178 0.0033 0.0000 6.96E-03 0.0000 0.0000 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0.0000 4.13E-04 0.0000 0.0000 3.24E-04 291 0.00 0.000 0.018 0.1966 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.94E-03 292 0.00 0.000 0.017 0.1909 0.0000 0.0000 0.00E+00 0.0000 0.0000 2.40E-03 293 0.00 0.000 0.017 0.1852 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.64E-03 294 0.00 0.000 0.017 0.1796 0.0000 0.0000 0.00E+00 0.0000 0.0000 2.97E-03 295 0.00 0.000 0.016 0.1742 0.0000 0.0000 0.00E+00 0.0000 0.0000 3.63E-03 296 0.00 0.000 0.016 0.1688 0.0000 0.0000 0.00E+00 0.0000 0.0000 2.75E-03 297 0.00 0.000 0.016 0.1634 0.0000 0.0000 0.00E+00 0.0000 0.0000 6.97E-04 298 0.00 0.000 0.016 0.1582 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 299 0.00 0.000 0.016 0.1530 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 300 0.00 0.000 0.015 0.1479 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.31E-03 301 1.00 0.000 0.025 0.4618 0.4080 0.0000 3.34E-02 0.0000 0.0000 2.01E-03 302 * 0.00 0.000 0.021 0.4079 2.7215 0.0000 1.41E-01 0.0000 0.0000 9.97E-07 303 * 0.00 0.000 0.039 0.3496 2.0407 0.0000 1.36E-01 0.0000 0.0000 1.16E-03 304 * 0.00 0.000 0.022 0.2982 1.4065 0.0000 1.32E-01 0.0000 0.0000 8.29E-04 305 0.00 0.000 0.045 0.2407 0.7949 0.0000 1.28E-01 0.0000 0.0000 2.82E-04 306 0.00 0.000 0.025 0.1985 0.2152 0.0000 1.02E-01 0.0000 0.0000 0.00E+00 307 0.00 0.000 0.042 0.1842 0.0000 0.0000 5.32E-04 0.0000 0.0000 1.10E-03 Page 38 of 128 308 * 0.10 0.000 0.019 0.1908 0.0000 0.0000 0.00E+00 0.0000 0.0000 8.48E-04 309 * 0.00 0.000 0.028 0.1974 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.25E-03 310 * 0.00 0.000 0.040 0.1885 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 311 0.00 0.000 0.039 0.1754 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.01E-03 312 0.00 0.000 0.025 0.1671 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.06E-03 313 0.00 0.000 0.043 0.1529 0.0000 0.0000 0.00E+00 0.0000 0.0000 9.01E-04 314 0.00 0.000 0.025 0.1444 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.03E-03 315 0.00 0.000 0.045 0.1294 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.63E-04 316 0.00 0.000 0.040 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.41E-03 317 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.13E-03 318 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.72E-03 319 * 0.20 0.000 0.026 0.1226 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.74E-03 320 * 0.00 0.000 0.030 0.1291 0.0000 0.0000 0.00E+00 0.0000 0.0000 9.91E-04 321 0.00 0.000 0.034 0.1357 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.27E-03 322 0.00 0.000 0.026 0.1441 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 323 0.00 0.000 0.023 0.1364 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 324 * 0.10 0.000 0.031 0.1429 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 325 0.30 0.000 0.000 0.2595 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 326 * 0.00 0.000 0.028 0.2270 0.0400 0.0000 6.93E-02 0.0000 0.0000 8.42E-04 327 * 0.30 0.000 0.019 0.2295 0.0043 0.0000 1.23E-02 0.0000 0.0000 1.15E-03 328 * 0.00 0.000 0.018 0.2328 0.0054 0.0000 9.86E-03 0.0000 0.0000 6.91E-04 329 * 0.00 0.000 0.016 0.2373 0.0035 0.0000 5.94E-03 0.0000 0.0000 6.59E-04 330 * * 0.00 0.000 0.021 0.2373 0.0000 0.0000 0.00E+00 0.0000 0.0000 6.24E-04 331 * * 0.00 0.000 0.024 0.2373 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.68E-03 332 * * 0.00 0.000 0.028 0.2373 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.59E-03 333 * * 0.10 0.000 0.018 0.2373 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.82E-03 334 * * 0.00 0.000 0.018 0.2373 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.12E-03 335 * * 0.00 0.000 0.024 0.2373 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.05E-03 336 * 0.00 0.013 0.012 0.2809 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.73E-03 337 * * 0.30 0.000 0.017 0.2809 0.0000 0.0000 0.00E+00 0.0000 0.0000 8.94E-04 338 * * 0.00 0.000 0.007 0.2809 0.0000 0.0000 0.00E+00 0.0000 0.0000 6.66E-04 339 * * 0.00 0.000 0.006 0.2809 0.0000 0.0000 0.00E+00 0.0000 0.0000 2.02E-03 340 * * 0.00 0.000 0.007 0.2809 0.0000 0.0000 0.00E+00 0.0000 0.0000 2.17E-03 341 * * 0.40 0.000 0.000 0.2809 0.0000 0.0000 0.00E+00 0.0000 0.0000 6.68E-04 342 * * 0.00 0.000 0.006 0.2809 0.0000 0.0000 0.00E+00 0.0000 0.0000 3.06E-03 Page 39 of 128 343 * * 0.00 0.000 0.007 0.2809 0.0000 0.0000 0.00E+00 0.0000 0.0000 8.58E-04 344 * * 0.00 0.000 0.011 0.2809 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.36E-03 345 * * 0.00 0.000 0.000 0.2809 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.73E-03 346 * * 0.00 0.000 0.000 0.2809 0.0000 0.0000 0.00E+00 0.0000 0.0000 8.78E-04 347 * * 0.00 0.000 0.013 0.2809 0.0000 0.0000 0.00E+00 0.0000 0.0000 9.60E-04 348 * * 0.00 0.000 0.013 0.2809 0.0000 0.0000 0.00E+00 0.0000 0.0000 3.73E-05 349 * * 0.00 0.000 0.019 0.2809 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.58E-03 350 * * 0.00 0.000 0.019 0.2809 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 351 * 0.10 0.022 0.000 0.3142 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 352 * 0.10 0.127 0.000 0.3503 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 353 * * 0.10 0.000 0.018 0.3503 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 354 * * 0.00 0.000 0.014 0.3503 0.0000 0.0000 0.00E+00 0.0000 0.0000 8.91E-04 355 * * 0.10 0.000 0.014 0.3503 0.0000 0.0000 0.00E+00 0.0000 0.0000 2.71E-03 356 * * 0.00 0.000 0.014 0.3503 0.0000 0.0000 0.00E+00 0.0000 0.0000 2.06E-03 357 * * 0.00 0.000 0.017 0.3503 0.0000 0.0000 0.00E+00 0.0000 0.0000 2.75E-03 358 * * 0.00 0.000 0.014 0.3503 0.0000 0.0000 0.00E+00 0.0000 0.0000 2.14E-03 359 * * 0.00 0.000 0.014 0.3503 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 360 * * 0.00 0.000 0.014 0.3503 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.18E-03 361 * * 0.00 0.000 0.019 0.3503 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.60E-03 362 * * 0.00 0.000 0.016 0.3503 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 363 * * 0.00 0.000 0.012 0.3503 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 364 * * 0.00 0.000 0.016 0.3503 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 365 * * 0.00 0.000 0.016 0.3503 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 * = Frozen (air or soil) inches cubic feet percent Precipitation 20.30 5,158,230.0 100.00 Runoff 5.200 1,321,291.6 25.62 Evapotranspiration 11.486 2,918,483.2 56.58 Percolation/Leakage through Layer 2 3.538194 899,055.1 17.43 Average Head on Top of Layer 2 0.0698 ------ Percolation/Leakage through Layer 12 0.316737 80,482.8 1.56 Annual Totals for Year 3 Page 40 of 128 Change in Water Storage 3.2978 837,972.4 16.25 Soil Water at Start of Year 223.9277 #########1103.09 Soil Water at End of Year 227.8522 #########1122.42 Snow Water at Start of Year 1.0470 266,038.7 5.16 Snow Water at End of Year 0.4203 106,804.8 2.07 Annual Water Budget Balance 0.0000 0.0000 0.00 Page 41 of 128 Daily Output for Year 4 Column key:Head #1: drainage from Layer 2 Title:Long Valley Landfill Simulated On:Leak #1: leakage thru Layer 2 Leak #2: leakage thru Layer 12 Day Rain Runoff ET Evap. Zone Water Head #1 Drain #1 Leak #1 Head #2 Drain #2 Leak #2 Air Soil (inches)(inches)(inches)(in/in)(inches)(inches)(inches)(inches)(inches)(inches) 1 * * 0.00 0.000 0.024 0.3503 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 2 * * 0.00 0.000 0.025 0.3503 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 3 * * 0.00 0.000 0.025 0.3503 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.64E-03 4 * * 0.00 0.000 0.020 0.3503 0.0000 0.0000 0.00E+00 0.0000 0.0000 4.93E-04 5 * * 0.00 0.000 0.016 0.3503 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 6 * * 0.00 0.000 0.022 0.3503 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 7 * * 0.00 0.000 0.026 0.3503 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 8 * * 0.00 0.000 0.025 0.3503 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 9 * * 0.00 0.000 0.023 0.3503 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 10 * * 0.00 0.000 0.026 0.3503 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 11 * * 0.00 0.000 0.031 0.3503 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 12 * * 0.20 0.000 0.024 0.3503 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 13 * * 0.00 0.000 0.025 0.3503 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 14 * * 0.00 0.000 0.025 0.3503 0.0000 0.0000 0.00E+00 0.0000 0.0000 2.12E-03 15 * * 0.00 0.000 0.025 0.3503 0.0000 0.0000 0.00E+00 0.0000 0.0000 2.08E-06 16 * * 0.00 0.000 0.025 0.3503 0.0000 0.0000 0.00E+00 0.0000 0.0000 6.05E-05 17 * * 0.00 0.000 0.026 0.3503 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.44E-04 18 * * 0.00 0.000 0.025 0.3503 0.0000 0.0000 0.00E+00 0.0000 0.0000 2.26E-04 19 * * 0.00 0.000 0.038 0.3503 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.42E-03 20 * * 0.00 0.000 0.031 0.3503 0.0000 0.0000 0.00E+00 0.0000 0.0000 4.14E-03 21 * * 0.00 0.000 0.037 0.3503 0.0000 0.0000 0.00E+00 0.0000 0.0000 4.06E-03 22 * * 0.00 0.000 0.035 0.3503 0.0000 0.0000 0.00E+00 0.0000 0.0000 3.98E-03 23 * * 0.00 0.000 0.024 0.3503 0.0000 0.0000 0.00E+00 0.0000 0.0000 3.03E-03 24 * * 0.00 0.000 0.018 0.3503 0.0000 0.0000 0.00E+00 0.0000 0.0000 9.70E-04 25 * * 0.00 0.000 0.000 0.3503 0.0000 0.0000 0.00E+00 0.0000 0.0000 7.77E-04 26 * * 0.00 0.000 0.000 0.3503 0.0000 0.0000 0.00E+00 0.0000 0.0000 3.86E-04 27 * * 0.00 0.000 0.000 0.3503 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 7/19/2024 11:05 Freezing Status* Page 42 of 128 28 * * 0.00 0.000 0.000 0.3503 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 29 * 0.00 0.000 0.000 0.3503 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 30 * * 0.30 0.000 0.023 0.3503 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 31 * * 0.00 0.000 0.017 0.3503 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 32 * * 0.00 0.000 0.013 0.3503 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 33 * * 0.00 0.000 0.014 0.3503 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 34 * * 0.10 0.000 0.000 0.3503 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 35 * * 0.10 0.000 0.017 0.3503 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 36 * * 0.00 0.000 0.015 0.3503 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 37 * * 0.00 0.000 0.017 0.3503 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 38 * * 0.10 0.000 0.000 0.3503 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 39 * 0.10 0.062 0.000 0.3686 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 40 * 0.30 0.597 0.000 0.3886 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 41 * * 0.30 0.000 0.023 0.3886 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 42 * * 0.00 0.000 0.021 0.3886 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 43 * * 0.00 0.000 0.024 0.3886 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 44 * 0.00 0.305 0.000 0.4009 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 45 * 0.00 0.000 0.000 0.4009 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 46 * 0.00 0.000 0.000 0.4009 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 47 * 0.00 0.000 0.000 0.4009 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 48 * * 0.00 0.000 0.000 0.4009 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 49 * 0.00 0.000 0.000 0.4009 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 50 * * 0.10 0.000 0.036 0.4009 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 51 * * 0.00 0.000 0.046 0.4009 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 52 * * 0.00 0.000 0.018 0.4009 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 53 * 0.00 0.000 0.000 0.4009 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 54 * 0.00 0.000 0.000 0.4009 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 55 * * 0.00 0.000 0.000 0.4009 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 56 * * 0.00 0.000 0.000 0.4009 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 57 * 0.00 0.000 0.000 0.4009 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 58 * * 0.30 0.000 0.025 0.4009 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 59 * * 0.10 0.000 0.029 0.4009 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 60 * * 0.10 0.000 0.026 0.4009 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 61 * * 0.00 0.000 0.025 0.4009 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 62 * * 0.00 0.000 0.028 0.4009 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 Page 43 of 128 63 * * 0.10 0.000 0.000 0.4009 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 64 * * 0.00 0.000 0.028 0.4009 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 65 * 0.10 0.147 0.000 0.4103 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 66 * * 0.10 0.000 0.029 0.4103 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 67 * * 0.00 0.000 0.027 0.4103 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 68 * 0.00 0.000 0.031 0.4103 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 69 * 0.00 0.134 0.015 0.4129 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 70 * * 0.00 0.000 0.025 0.4129 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 71 * * 0.00 0.000 0.046 0.4129 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 72 * * 0.00 0.000 0.076 0.4129 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 73 * * 0.10 0.000 0.071 0.4129 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 74 * * 0.00 0.000 0.075 0.4129 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 75 * 0.00 0.000 0.029 0.4129 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 76 * 0.00 0.000 0.000 0.4129 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 77 * * 0.00 0.000 0.000 0.4129 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 78 * * 0.00 0.000 0.000 0.4129 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 79 * * 0.00 0.000 0.000 0.4129 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 80 * 0.00 0.000 0.000 0.4129 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 81 * * 0.00 0.000 0.000 0.4129 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 82 * * 0.00 0.000 0.000 0.4129 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 83 * 0.00 0.000 0.000 0.4129 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 84 * 0.00 0.000 0.000 0.4129 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 85 * 0.10 0.080 0.009 0.4168 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 86 * * 0.10 0.000 0.043 0.4168 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 87 * * 0.00 0.000 0.043 0.4168 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 88 * 0.00 0.000 0.013 0.4168 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 89 * * 0.30 0.000 0.033 0.4168 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 90 * * 0.00 0.000 0.027 0.4168 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 91 * * 0.00 0.000 0.039 0.4168 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 92 * * 0.10 0.000 0.049 0.4168 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 93 * * 0.00 0.000 0.052 0.4168 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 94 * * 0.10 0.000 0.000 0.4168 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 95 * 0.00 0.000 0.060 0.4168 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 96 * 0.00 0.000 0.060 0.4168 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 97 * 0.00 0.059 0.122 0.4168 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 Page 44 of 128 98 * 0.00 0.000 0.000 0.4168 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 99 * 0.00 0.000 0.000 0.4168 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 100 * 0.00 0.000 0.000 0.4168 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 101 0.00 0.000 0.073 0.3579 1.7209 0.0000 1.04E-01 0.0000 0.0000 0.00E+00 102 0.00 0.000 0.152 0.2629 1.5341 0.0000 1.33E-01 0.0000 0.0000 0.00E+00 103 * 0.10 0.000 0.101 0.2198 0.8199 0.0000 1.28E-01 0.0000 0.0000 0.00E+00 104 * 0.00 0.000 0.111 0.1494 0.2297 0.0000 9.99E-02 0.0000 0.0000 0.00E+00 105 0.00 0.000 0.090 0.1195 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 106 0.00 0.000 0.011 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 107 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 108 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 109 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 110 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 111 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 112 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 113 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 114 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 115 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 116 0.20 0.000 0.025 0.1743 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 117 * 0.10 0.000 0.073 0.1809 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 118 * 0.00 0.000 0.041 0.1697 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 119 * 0.00 0.000 0.031 0.1593 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 120 * 0.00 0.000 0.029 0.1496 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 121 0.00 0.000 0.029 0.1401 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 122 0.00 0.000 0.028 0.1307 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 123 0.00 0.000 0.027 0.1218 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 124 0.00 0.000 0.015 0.1169 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 125 0.00 0.000 0.003 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 126 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 127 * 0.50 0.000 0.061 0.1226 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 128 0.00 0.000 0.030 0.2526 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 129 0.00 0.000 0.023 0.2241 0.1810 0.0000 6.25E-02 0.0000 0.0000 0.00E+00 130 0.30 0.000 0.031 0.2890 0.1121 0.0000 7.40E-02 0.0000 0.0000 0.00E+00 131 * 0.40 0.000 0.061 0.2538 0.4254 0.0000 1.25E-01 0.0000 0.0000 0.00E+00 132 * 0.00 0.000 0.065 0.2399 0.0726 0.0000 6.13E-02 0.0000 0.0000 0.00E+00 Page 45 of 128 133 * 0.00 0.000 0.059 0.2422 0.0064 0.0000 1.29E-02 0.0000 0.0000 0.00E+00 134 0.00 0.000 0.158 0.2400 0.0036 0.0000 4.23E-03 0.0000 0.0000 0.00E+00 135 0.00 0.000 0.140 0.1903 0.0042 0.0000 8.97E-03 0.0000 0.0000 0.00E+00 136 0.00 0.000 0.128 0.1471 0.0030 0.0000 1.75E-03 0.0000 0.0000 0.00E+00 137 0.00 0.000 0.084 0.1192 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 138 0.00 0.000 0.010 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 139 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 140 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.65E-03 141 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 7.58E-04 142 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.00E-03 143 0.20 0.000 0.023 0.1749 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.99E-03 144 0.10 0.000 0.036 0.1963 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.71E-03 145 0.00 0.000 0.031 0.1859 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.66E-03 146 0.00 0.000 0.030 0.1760 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.49E-03 147 0.00 0.000 0.028 0.1666 0.0000 0.0000 0.00E+00 0.0000 0.0000 9.87E-04 148 0.00 0.000 0.027 0.1576 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 149 0.00 0.000 0.026 0.1488 0.0000 0.0000 0.00E+00 0.0000 0.0000 9.06E-04 150 0.00 0.000 0.026 0.1403 0.0000 0.0000 0.00E+00 0.0000 0.0000 7.31E-04 151 0.00 0.000 0.025 0.1320 0.0000 0.0000 0.00E+00 0.0000 0.0000 2.19E-03 152 0.00 0.000 0.025 0.1238 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.10E-03 153 0.00 0.000 0.018 0.1178 0.0000 0.0000 0.00E+00 0.0000 0.0000 8.02E-04 154 0.00 0.000 0.005 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 3.36E-04 155 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 156 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 157 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 158 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 159 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 160 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 161 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 2.13E-03 162 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.90E-03 163 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 8.52E-04 164 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.06E-03 165 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 9.58E-04 166 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.09E-03 167 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.30E-03 Page 46 of 128 168 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 2.80E-04 169 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.51E-03 170 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 2.19E-03 171 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.21E-03 172 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.42E-03 173 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 5.82E-05 174 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.10E-03 175 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 176 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 177 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 178 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 8.87E-04 179 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.26E-03 180 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 3.52E-03 181 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 9.97E-07 182 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.16E-03 183 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 4.44E-16 184 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 185 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 186 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 187 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 188 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 189 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 190 0.10 0.000 0.014 0.1447 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 191 0.10 0.000 0.018 0.1719 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 192 0.00 0.000 0.012 0.1679 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.58E-03 193 0.00 0.000 0.015 0.1630 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.85E-03 194 0.00 0.000 0.015 0.1579 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.60E-03 195 0.00 0.000 0.016 0.1524 0.0000 0.0000 0.00E+00 0.0000 0.0000 9.29E-04 196 0.30 0.000 0.023 0.2446 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.85E-03 197 0.00 0.000 0.018 0.2278 0.0199 0.0000 3.23E-02 0.0000 0.0000 1.56E-03 198 0.00 0.000 0.019 0.2152 0.0094 0.0000 1.85E-02 0.0000 0.0000 1.49E-03 199 0.00 0.000 0.020 0.2069 0.0036 0.0000 5.19E-03 0.0000 0.0000 1.56E-03 200 0.00 0.000 0.022 0.1996 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.27E-03 201 0.00 0.000 0.024 0.1917 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.22E-03 202 0.00 0.000 0.022 0.1842 0.0000 0.0000 0.00E+00 0.0000 0.0000 4.44E-16 Page 47 of 128 203 0.00 0.000 0.023 0.1765 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 204 0.00 0.000 0.029 0.1667 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 205 0.00 0.000 0.024 0.1587 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.61E-03 206 0.00 0.000 0.032 0.1479 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.04E-03 207 0.10 0.000 0.042 0.1672 0.0000 0.0000 0.00E+00 0.0000 0.0000 4.41E-04 208 0.00 0.000 0.032 0.1564 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 209 0.20 0.000 0.048 0.2071 0.0000 0.0000 0.00E+00 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0.024 0.1299 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.11E-03 224 0.00 0.000 0.029 0.1204 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.60E-03 225 0.20 0.000 0.049 0.1707 0.0000 0.0000 0.00E+00 0.0000 0.0000 3.60E-04 226 0.00 0.000 0.069 0.1478 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.59E-03 227 0.00 0.000 0.058 0.1286 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.49E-03 228 0.00 0.000 0.034 0.1172 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.46E-03 229 0.00 0.000 0.003 0.1163 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 230 0.00 0.000 0.001 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.03E-03 231 0.30 0.000 0.072 0.1921 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.49E-03 232 0.20 0.000 0.118 0.2196 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.38E-03 233 0.00 0.000 0.190 0.1562 0.0000 0.0000 0.00E+00 0.0000 0.0000 2.14E-04 234 0.50 0.000 0.207 0.2538 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 235 0.00 0.000 0.156 0.1949 0.0161 0.0000 2.03E-02 0.0000 0.0000 0.00E+00 236 0.00 0.000 0.192 0.1309 0.0012 0.0000 0.00E+00 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250 0.00 0.000 0.084 0.1323 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 251 0.50 0.000 0.174 0.2410 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 252 0.20 0.000 0.156 0.2532 0.0091 0.0000 7.33E-03 0.0000 0.0000 0.00E+00 253 0.00 0.000 0.167 0.1863 0.0290 0.0000 3.33E-02 0.0000 0.0000 0.00E+00 254 0.00 0.000 0.161 0.1326 0.0046 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 255 0.00 0.000 0.050 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 256 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 257 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 258 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 259 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 260 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 261 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 262 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 263 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 264 1.00 0.000 0.127 0.3966 0.0565 0.0000 3.10E-02 0.0000 0.0000 0.00E+00 265 0.10 0.000 0.128 0.3422 1.7933 0.0000 1.35E-01 0.0000 0.0000 0.00E+00 266 0.00 0.000 0.125 0.2569 1.2388 0.0000 1.31E-01 0.0000 0.0000 0.00E+00 267 0.00 0.000 0.169 0.1584 0.5537 0.0000 1.26E-01 0.0000 0.0000 0.00E+00 268 0.00 0.000 0.097 0.1191 0.0406 0.0000 2.13E-02 0.0000 0.0000 0.00E+00 269 0.00 0.000 0.009 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 270 0.60 0.000 0.119 0.2762 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 271 0.10 0.000 0.110 0.2415 0.2904 0.0000 9.38E-02 0.0000 0.0000 0.00E+00 272 0.00 0.000 0.097 0.1856 0.1055 0.0000 7.08E-02 0.0000 0.0000 0.00E+00 Page 49 of 128 273 0.00 0.000 0.093 0.1546 0.0018 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 274 0.20 0.000 0.113 0.1836 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 275 0.00 0.000 0.085 0.1551 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 276 0.00 0.000 0.093 0.1240 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 277 0.00 0.000 0.017 0.1181 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 278 0.00 0.000 0.005 0.1165 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 279 0.00 0.000 0.002 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 280 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 281 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 282 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 283 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 284 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 285 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 286 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 287 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 288 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 289 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 290 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 291 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 292 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 293 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 294 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 295 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 296 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 297 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 298 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 299 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 300 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 301 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 302 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 303 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 304 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 305 0.20 0.000 0.022 0.1755 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 306 * 0.10 0.000 0.041 0.1820 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 307 * 0.20 0.000 0.017 0.1886 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 Page 50 of 128 308 * 0.00 0.000 0.039 0.1952 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 309 0.00 0.000 0.034 0.2316 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 310 0.00 0.000 0.019 0.2251 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 311 0.00 0.000 0.019 0.2177 0.0011 0.0000 3.42E-03 0.0000 0.0000 0.00E+00 312 0.00 0.000 0.019 0.2100 0.0032 0.0000 4.31E-03 0.0000 0.0000 0.00E+00 313 0.00 0.000 0.018 0.2039 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 314 0.00 0.000 0.018 0.1980 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 315 0.00 0.000 0.018 0.1921 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 316 * 0.00 0.000 0.017 0.1864 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 317 * 0.30 0.000 0.019 0.1929 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 318 0.00 0.000 0.000 0.2644 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 319 * 0.20 0.000 0.016 0.2479 0.0851 0.0000 6.94E-02 0.0000 0.0000 0.00E+00 320 * 0.00 0.000 0.012 0.2456 0.0147 0.0000 2.64E-02 0.0000 0.0000 0.00E+00 321 * 0.00 0.000 0.019 0.2503 0.0062 0.0000 5.73E-03 0.0000 0.0000 0.00E+00 322 * 0.00 0.000 0.024 0.2521 0.0154 0.0000 1.43E-02 0.0000 0.0000 0.00E+00 323 * 0.00 0.000 0.032 0.2492 0.0197 0.0000 2.83E-02 0.0000 0.0000 0.00E+00 324 * 0.00 0.000 0.033 0.2468 0.0005 0.0000 1.97E-02 0.0000 0.0000 0.00E+00 325 * 0.00 0.000 0.017 0.2348 0.0071 0.0000 1.89E-02 0.0000 0.0000 0.00E+00 326 * 0.10 0.000 0.029 0.2371 0.0086 0.0000 1.27E-02 0.0000 0.0000 0.00E+00 327 * 0.00 0.000 0.017 0.2417 0.0020 0.0000 5.94E-03 0.0000 0.0000 0.00E+00 328 * 0.20 0.000 0.023 0.2466 0.0055 0.0000 5.12E-03 0.0000 0.0000 0.00E+00 329 * * 0.00 0.000 0.018 0.2466 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 330 * 0.00 0.000 0.022 0.2466 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 331 * 0.00 0.007 0.017 0.2822 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 332 * 0.00 0.000 0.000 0.2822 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 333 * 0.00 0.000 0.000 0.2822 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 334 * 0.00 0.000 0.000 0.2822 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 335 * * 0.00 0.000 0.000 0.2822 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 336 * 0.10 0.011 0.011 0.3082 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 337 * 0.10 0.020 0.011 0.3312 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 338 0.10 0.000 0.026 0.3223 1.2558 0.0000 1.00E-01 0.0000 0.0000 0.00E+00 339 * 0.00 0.000 0.018 0.2729 1.1431 0.0000 1.30E-01 0.0000 0.0000 0.00E+00 340 0.00 0.000 0.026 0.2223 0.5321 0.0000 1.26E-01 0.0000 0.0000 0.00E+00 341 0.00 0.000 0.025 0.1966 0.0673 0.0000 5.18E-02 0.0000 0.0000 0.00E+00 342 0.00 0.000 0.025 0.1882 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 Page 51 of 128 343 0.00 0.000 0.022 0.1810 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 344 0.00 0.000 0.022 0.1737 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 345 0.00 0.000 0.025 0.1653 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 346 0.00 0.000 0.026 0.1567 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 347 * 0.20 0.000 0.024 0.1632 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 348 * 0.10 0.000 0.011 0.1698 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 349 * * 0.00 0.000 0.012 0.1698 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 350 * * 0.00 0.000 0.018 0.1698 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 351 * * 0.10 0.000 0.016 0.1698 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 352 * * 0.00 0.000 0.014 0.1698 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 353 * * 0.00 0.000 0.014 0.1698 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 354 * * 0.10 0.000 0.000 0.1698 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 355 * * 0.20 0.000 0.000 0.1698 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 356 * * 0.80 0.000 0.000 0.1698 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 357 * * 0.00 0.000 0.012 0.1698 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 358 * * 0.00 0.000 0.015 0.1698 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 359 * * 0.40 0.000 0.014 0.1698 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 360 * * 0.20 0.000 0.011 0.1698 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 361 * * 0.00 0.000 0.008 0.1698 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 362 * * 0.00 0.000 0.014 0.1698 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 363 * * 0.10 0.000 0.012 0.1698 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 364 * * 0.10 0.000 0.010 0.1698 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 365 * * 0.00 0.000 0.012 0.1698 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 * = Frozen (air or soil) inches cubic feet percent Precipitation 15.00 3,811,500.0 100.00 Runoff 1.422 361,244.6 9.48 Evapotranspiration 10.249 2,604,364.2 68.33 Percolation/Leakage through Layer 2 2.255996 573,248.6 15.04 Average Head on Top of Layer 2 0.0344 ------ Percolation/Leakage through Layer 12 0.115696 29,398.3 0.77 Annual Totals for Year 4 Page 52 of 128 Change in Water Storage 3.2133 816,492.9 21.42 Soil Water at Start of Year 227.8522 #########1519.01 Soil Water at End of Year 229.4508 #########1529.67 Snow Water at Start of Year 0.4203 106,804.8 2.80 Snow Water at End of Year 2.0349 517,073.9 13.57 Annual Water Budget Balance 0.0000 0.0000 0.00 Page 53 of 128 Daily Output for Year 5 Column key:Head #1: drainage from Layer 2 Title:Long Valley Landfill Simulated On:Leak #1: leakage thru Layer 2 Leak #2: leakage thru Layer 12 Day Rain Runoff ET Evap. Zone Water Head #1 Drain #1 Leak #1 Head #2 Drain #2 Leak #2 Air Soil (inches)(inches)(inches)(in/in)(inches)(inches)(inches)(inches)(inches)(inches) 1 * * 0.00 0.000 0.016 0.1698 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 2 * * 0.00 0.000 0.016 0.1698 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 3 * * 0.00 0.000 0.019 0.1698 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 4 * * 0.00 0.000 0.021 0.1698 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 5 * * 0.00 0.000 0.026 0.1698 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 6 * 0.00 0.000 0.021 0.1969 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 7 * 0.00 0.025 0.007 0.2474 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 8 * 0.00 0.051 0.006 0.2906 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 9 * 0.00 0.003 0.025 0.2990 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 10 * * 0.00 0.000 0.027 0.2990 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 11 * 0.00 0.000 0.029 0.2991 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 12 * * 0.10 0.000 0.025 0.2991 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 13 * * 0.00 0.000 0.022 0.2991 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 14 * * 0.00 0.000 0.020 0.2991 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 15 * * 0.00 0.000 0.024 0.2991 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 16 * * 0.00 0.000 0.024 0.2991 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 17 * * 0.00 0.000 0.025 0.2991 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 18 * * 0.00 0.000 0.027 0.2991 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 19 * 0.00 0.000 0.028 0.2991 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 20 * * 0.00 0.000 0.025 0.2991 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 21 * * 0.00 0.000 0.019 0.2991 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 22 * * 0.00 0.000 0.015 0.2991 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 23 * * 0.00 0.000 0.021 0.2991 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 24 * * 0.00 0.000 0.023 0.2991 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 25 * 0.00 0.018 0.024 0.3134 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 26 * 0.00 0.034 0.019 0.3299 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 27 * 0.00 0.086 0.010 0.3498 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 7/19/2024 11:05 Freezing Status* Page 54 of 128 28 * * 0.00 0.000 0.028 0.3498 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 29 * * 0.00 0.000 0.026 0.3498 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 30 * * 0.20 0.000 0.027 0.3498 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 31 * * 0.00 0.000 0.022 0.3498 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 32 * * 0.00 0.000 0.022 0.3498 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 33 * 0.00 0.000 0.029 0.3498 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 34 * 0.00 0.166 0.000 0.3714 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 35 * 0.00 0.225 0.000 0.3886 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 36 * 0.00 0.215 0.023 0.3931 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 37 * 0.00 0.073 0.028 0.3935 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 38 * 0.00 0.000 0.000 0.3935 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 39 0.00 0.000 0.037 0.3472 1.5637 0.0000 1.02E-01 0.0000 0.0000 0.00E+00 40 0.00 0.000 0.061 0.2827 1.5003 0.0000 1.33E-01 0.0000 0.0000 0.00E+00 41 0.00 0.000 0.056 0.2211 0.8539 0.0000 1.28E-01 0.0000 0.0000 0.00E+00 42 * 0.00 0.000 0.028 0.1743 0.2540 0.0000 1.12E-01 0.0000 0.0000 0.00E+00 43 0.00 0.000 0.056 0.1552 0.0003 0.0000 1.77E-03 0.0000 0.0000 0.00E+00 44 0.00 0.000 0.069 0.1321 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 45 0.00 0.000 0.048 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 46 * 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 47 * 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 48 * * 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 49 * 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 50 * 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 51 * 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 52 * * 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 53 * * 0.30 0.000 0.023 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 54 * * 0.30 0.000 0.023 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 55 * * 0.00 0.000 0.023 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 56 * * 0.00 0.000 0.025 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 57 * * 0.00 0.000 0.021 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 58 * * 0.00 0.000 0.025 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 59 * * 0.20 0.000 0.022 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 60 * * 0.10 0.000 0.020 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 61 * * 0.30 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 62 * * 0.30 0.000 0.021 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 Page 55 of 128 63 * * 0.00 0.000 0.015 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 64 * * 0.00 0.000 0.019 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 65 * * 0.00 0.000 0.024 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 66 * * 0.00 0.000 0.027 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 67 * * 0.00 0.000 0.029 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 68 * * 0.00 0.000 0.028 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 69 * * 0.00 0.000 0.030 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 70 * 0.00 0.008 0.013 0.1648 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 71 * 0.00 0.004 0.021 0.1937 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 72 * 0.00 0.025 0.016 0.2302 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 73 * 0.00 0.257 0.000 0.2828 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 74 * 0.00 0.181 0.016 0.3106 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 75 * 0.00 0.000 0.000 0.3106 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 76 0.00 0.000 0.041 0.2647 0.6556 0.0000 9.63E-02 0.0000 0.0000 0.00E+00 77 0.00 0.000 0.052 0.2049 0.6819 0.0000 1.27E-01 0.0000 0.0000 0.00E+00 78 0.00 0.000 0.050 0.1619 0.1437 0.0000 7.92E-02 0.0000 0.0000 0.00E+00 79 0.00 0.000 0.102 0.1279 0.0000 0.0000 0.00E+00 0.0000 0.0000 2.16E-03 80 0.00 0.000 0.036 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 2.93E-04 81 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 9.28E-04 82 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.55E-03 83 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.41E-03 84 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.77E-03 85 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.55E-03 86 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.35E-04 87 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 88 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 89 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.30E-03 90 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 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1.88E-03 158 0.20 0.000 0.031 0.2238 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.28E-03 159 0.00 0.000 0.030 0.2138 0.0000 0.0000 0.00E+00 0.0000 0.0000 4.44E-16 160 0.00 0.000 0.030 0.2038 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 161 0.80 0.000 0.033 0.4381 0.4682 0.0000 6.44E-02 0.0000 0.0000 0.00E+00 162 0.10 0.000 0.224 0.3507 2.3436 0.0000 1.38E-01 0.0000 0.0000 0.00E+00 163 0.00 0.000 0.114 0.2684 1.4886 0.0000 1.33E-01 0.0000 0.0000 0.00E+00 164 0.00 0.000 0.128 0.1833 0.7634 0.0000 1.28E-01 0.0000 0.0000 0.00E+00 165 0.00 0.000 0.171 0.1160 0.1092 0.0000 3.12E-02 0.0000 0.0000 0.00E+00 166 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 167 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 Page 58 of 128 168 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 169 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 170 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 171 0.00 0.000 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0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 199 0.20 0.000 0.026 0.1741 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 200 0.00 0.000 0.040 0.1610 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 201 0.10 0.000 0.045 0.1794 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 202 0.20 0.000 0.043 0.2319 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 Page 59 of 128 203 0.00 0.000 0.045 0.2168 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 204 0.00 0.000 0.046 0.1988 0.0031 0.0000 7.97E-03 0.0000 0.0000 0.00E+00 205 0.00 0.000 0.047 0.1831 0.0007 0.0000 2.60E-04 0.0000 0.0000 0.00E+00 206 0.00 0.000 0.045 0.1683 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 207 0.00 0.000 0.050 0.1516 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 208 0.00 0.000 0.052 0.1341 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 209 0.00 0.000 0.038 0.1214 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 210 0.00 0.000 0.016 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 211 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 212 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 213 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 214 1.00 0.000 0.061 0.4185 0.0977 0.0000 3.13E-02 0.0000 0.0000 0.00E+00 215 0.00 0.000 0.183 0.3120 2.0662 0.0000 1.37E-01 0.0000 0.0000 0.00E+00 216 0.00 0.000 0.230 0.1923 1.0222 0.0000 1.29E-01 0.0000 0.0000 0.00E+00 217 0.00 0.000 0.132 0.1274 0.2023 0.0000 6.25E-02 0.0000 0.0000 0.00E+00 218 0.00 0.000 0.034 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 219 0.20 0.000 0.098 0.1501 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 220 0.00 0.000 0.074 0.1255 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 221 0.00 0.000 0.024 0.1176 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 222 0.00 0.000 0.004 0.1164 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 223 0.30 0.000 0.066 0.1945 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 224 0.80 0.001 0.102 0.4161 0.2985 0.0000 3.26E-02 0.0000 0.0000 0.00E+00 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0.1932 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 239 0.00 0.000 0.082 0.1659 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 240 0.00 0.000 0.071 0.1422 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 241 0.00 0.000 0.067 0.1200 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 242 0.10 0.000 0.052 0.1360 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 243 0.00 0.000 0.026 0.1274 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 244 0.00 0.000 0.025 0.1190 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 245 0.00 0.000 0.007 0.1167 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 246 0.00 0.000 0.002 0.1162 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 247 0.10 0.000 0.037 0.1370 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 248 0.00 0.000 0.024 0.1292 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 249 0.00 0.000 0.035 0.1176 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 250 0.00 0.000 0.004 0.1164 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 251 0.00 0.000 0.001 0.1161 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 252 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 253 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 254 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 255 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 256 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 257 0.20 0.000 0.059 0.1629 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 258 0.20 0.000 0.073 0.2051 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 259 0.10 0.000 0.087 0.2093 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 260 0.00 0.000 0.111 0.1724 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 261 0.00 0.000 0.085 0.1443 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 262 0.00 0.000 0.077 0.1188 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 263 0.00 0.000 0.008 0.1162 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 264 0.00 0.000 0.001 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 265 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 266 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 267 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 268 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 269 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 270 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 271 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 272 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 Page 61 of 128 273 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 274 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 275 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 276 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 277 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 278 0.60 0.000 0.019 0.3095 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 279 0.00 0.000 0.034 0.2562 0.5688 0.0000 1.26E-01 0.0000 0.0000 0.00E+00 280 0.00 0.000 0.036 0.2036 0.3040 0.0000 1.22E-01 0.0000 0.0000 0.00E+00 281 0.00 0.000 0.038 0.1908 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 282 0.00 0.000 0.040 0.1774 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 283 0.00 0.000 0.089 0.1477 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 284 0.00 0.000 0.062 0.1270 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 285 0.00 0.000 0.033 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 286 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 287 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 288 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 289 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 290 0.20 0.000 0.021 0.1756 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 291 0.60 0.000 0.037 0.3528 0.0885 0.0000 3.12E-02 0.0000 0.0000 0.00E+00 292 0.10 0.000 0.072 0.3183 1.3101 0.0000 1.31E-01 0.0000 0.0000 0.00E+00 293 0.10 0.000 0.071 0.2851 0.8989 0.0000 1.29E-01 0.0000 0.0000 0.00E+00 294 0.10 0.000 0.071 0.2531 0.4438 0.0000 1.25E-01 0.0000 0.0000 0.00E+00 295 0.00 0.000 0.060 0.2212 0.0308 0.0000 3.61E-02 0.0000 0.0000 0.00E+00 296 0.00 0.000 0.029 0.2082 0.0061 0.0000 9.45E-03 0.0000 0.0000 0.00E+00 297 0.00 0.000 0.061 0.1881 0.0001 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 298 0.00 0.000 0.060 0.1682 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 299 0.00 0.000 0.060 0.1481 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 300 0.00 0.000 0.042 0.1339 0.0036 0.0000 1.16E-03 0.0000 0.0000 0.00E+00 301 0.00 0.000 0.051 0.1168 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 302 0.10 0.000 0.030 0.1401 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 303 0.00 0.000 0.021 0.1332 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 304 0.00 0.000 0.036 0.1213 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 305 0.00 0.000 0.014 0.1168 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 306 0.00 0.000 0.002 0.1162 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 307 0.10 0.000 0.026 0.1407 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 Page 62 of 128 308 * 0.00 0.000 0.014 0.1362 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 309 * 0.00 0.000 0.015 0.1313 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 310 * 0.00 0.000 0.000 0.1313 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 311 * 0.00 0.000 0.027 0.1222 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 312 * 0.00 0.000 0.016 0.1169 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 313 0.00 0.000 0.002 0.1162 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 314 * 0.30 0.000 0.017 0.1228 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 315 * 0.00 0.000 0.014 0.1294 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 316 * 0.00 0.000 0.017 0.1359 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.75E-03 317 * 0.00 0.000 0.022 0.1425 0.0000 0.0000 0.00E+00 0.0000 0.0000 2.69E-03 318 * 0.00 0.000 0.022 0.1490 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.67E-03 319 * 0.00 0.000 0.032 0.1556 0.0000 0.0000 0.00E+00 0.0000 0.0000 7.58E-04 320 * 0.70 0.000 0.015 0.1622 0.0000 0.0000 0.00E+00 0.0000 0.0000 8.26E-05 321 * 0.00 0.000 0.016 0.1687 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 322 * 0.00 0.000 0.019 0.1753 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 323 0.00 0.000 0.012 0.2036 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 324 * 0.00 0.000 0.019 0.2102 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 325 * * 0.00 0.000 0.017 0.2102 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 326 * 0.00 0.000 0.020 0.2102 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 327 * 0.00 0.000 0.014 0.2277 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 328 * 0.00 0.000 0.013 0.2477 0.0000 0.0000 0.00E+00 0.0000 0.0000 5.67E-04 329 * * 0.00 0.000 0.016 0.2477 0.0000 0.0000 0.00E+00 0.0000 0.0000 6.84E-04 330 * * 0.10 0.000 0.014 0.2477 0.0000 0.0000 0.00E+00 0.0000 0.0000 9.45E-04 331 * * 0.00 0.000 0.011 0.2477 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.39E-03 332 * * 0.00 0.000 0.011 0.2477 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.80E-03 333 * * 0.10 0.000 0.011 0.2477 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.94E-03 334 * * 0.00 0.000 0.012 0.2477 0.0000 0.0000 0.00E+00 0.0000 0.0000 2.06E-03 335 * * 0.00 0.000 0.013 0.2477 0.0000 0.0000 0.00E+00 0.0000 0.0000 2.25E-03 336 * * 0.00 0.000 0.017 0.2477 0.0000 0.0000 0.00E+00 0.0000 0.0000 2.56E-03 337 * * 0.00 0.000 0.000 0.2477 0.0000 0.0000 0.00E+00 0.0000 0.0000 2.94E-03 338 * * 0.00 0.000 0.020 0.2477 0.0000 0.0000 0.00E+00 0.0000 0.0000 3.36E-03 339 * * 0.00 0.000 0.017 0.2477 0.0000 0.0000 0.00E+00 0.0000 0.0000 3.78E-03 340 * * 0.00 0.000 0.020 0.2477 0.0000 0.0000 0.00E+00 0.0000 0.0000 4.14E-03 341 * 0.00 0.000 0.020 0.2477 0.0000 0.0000 0.00E+00 0.0000 0.0000 4.43E-03 342 * 0.00 0.045 0.006 0.2898 0.0000 0.0000 0.00E+00 0.0000 0.0000 4.62E-03 Page 63 of 128 343 * 0.00 0.077 0.001 0.3238 0.0000 0.0000 0.00E+00 0.0000 0.0000 4.58E-03 344 * 0.00 0.000 0.000 0.3238 0.0000 0.0000 0.00E+00 0.0000 0.0000 4.48E-03 345 * * 0.30 0.000 0.018 0.3238 0.0000 0.0000 0.00E+00 0.0000 0.0000 4.39E-03 346 * * 0.00 0.000 0.010 0.3238 0.0000 0.0000 0.00E+00 0.0000 0.0000 4.30E-03 347 * * 0.00 0.000 0.014 0.3238 0.0000 0.0000 0.00E+00 0.0000 0.0000 4.16E-03 348 * * 0.50 0.000 0.014 0.3238 0.0000 0.0000 0.00E+00 0.0000 0.0000 3.84E-03 349 * * 0.20 0.000 0.012 0.3238 0.0000 0.0000 0.00E+00 0.0000 0.0000 3.46E-03 350 * * 0.00 0.000 0.011 0.3238 0.0000 0.0000 0.00E+00 0.0000 0.0000 3.06E-03 351 * * 0.10 0.000 0.013 0.3238 0.0000 0.0000 0.00E+00 0.0000 0.0000 2.64E-03 352 * * 0.00 0.000 0.016 0.3238 0.0000 0.0000 0.00E+00 0.0000 0.0000 2.23E-03 353 * * 0.00 0.000 0.018 0.3238 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.83E-03 354 * * 0.10 0.000 0.000 0.3238 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.46E-03 355 * * 0.40 0.000 0.000 0.3238 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.12E-03 356 * * 1.00 0.000 0.000 0.3238 0.0000 0.0000 0.00E+00 0.0000 0.0000 9.45E-04 357 * * 0.20 0.000 0.011 0.3238 0.0000 0.0000 0.00E+00 0.0000 0.0000 9.83E-04 358 * * 0.00 0.000 0.009 0.3238 0.0000 0.0000 0.00E+00 0.0000 0.0000 5.83E-04 359 * * 0.50 0.000 0.011 0.3238 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.01E-04 360 * * 0.00 0.000 0.009 0.3238 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 361 * * 0.00 0.000 0.009 0.3238 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 362 * * 0.00 0.000 0.011 0.3238 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 363 * * 0.00 0.000 0.010 0.3238 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.56E-05 364 * * 0.00 0.000 0.011 0.3238 0.0000 0.0000 0.00E+00 0.0000 0.0000 5.10E-04 365 * * 0.00 0.000 0.007 0.3238 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.17E-03 * = Frozen (air or soil) inches cubic feet percent Precipitation 18.40 4,675,440.0 100.00 Runoff 1.637 415,897.8 8.90 Evapotranspiration 10.678 2,713,153.8 58.03 Percolation/Leakage through Layer 2 4.574515 1,162,384.4 24.86 Average Head on Top of Layer 2 0.0970 ------ Percolation/Leakage through Layer 12 0.190615 48,435.2 1.04 Annual Totals for Year 5 Page 64 of 128 Change in Water Storage 5.8951 1,497,953.3 32.04 Soil Water at Start of Year 229.4508 #########1247.02 Soil Water at End of Year 234.2969 #########1273.35 Snow Water at Start of Year 2.0349 517,073.9 11.06 Snow Water at End of Year 3.0840 783,648.5 16.76 Annual Water Budget Balance 0.0000 0.0000 0.00 Page 65 of 128 Daily Output for Year 6 Column key:Head #1: drainage from Layer 2 Title:Long Valley Landfill Simulated On:Leak #1: leakage thru Layer 2 Leak #2: leakage thru Layer 12 Day Rain Runoff ET Evap. Zone Water Head #1 Drain #1 Leak #1 Head #2 Drain #2 Leak #2 Air Soil (inches)(inches)(inches)(in/in)(inches)(inches)(inches)(inches)(inches)(inches) 1 * * 0.00 0.000 0.014 0.3238 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.67E-03 2 * * 0.00 0.000 0.019 0.3238 0.0000 0.0000 0.00E+00 0.0000 0.0000 2.04E-03 3 * * 0.00 0.000 0.023 0.3238 0.0000 0.0000 0.00E+00 0.0000 0.0000 2.12E-03 4 * * 0.00 0.000 0.025 0.3238 0.0000 0.0000 0.00E+00 0.0000 0.0000 2.09E-03 5 * * 0.00 0.000 0.026 0.3238 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.97E-03 6 * * 0.10 0.000 0.000 0.3238 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.82E-03 7 * * 0.20 0.000 0.017 0.3238 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.68E-03 8 * * 0.10 0.000 0.014 0.3238 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.56E-03 9 * * 0.00 0.000 0.015 0.3238 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.51E-03 10 * * 0.00 0.000 0.012 0.3238 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.52E-03 11 * * 0.00 0.000 0.013 0.3238 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.50E-03 12 * * 0.00 0.000 0.018 0.3238 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.54E-03 13 * * 0.00 0.000 0.019 0.3238 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.93E-03 14 * * 0.00 0.000 0.020 0.3238 0.0000 0.0000 0.00E+00 0.0000 0.0000 2.38E-03 15 * * 0.30 0.000 0.000 0.3238 0.0000 0.0000 0.00E+00 0.0000 0.0000 2.75E-03 16 * * 0.00 0.000 0.022 0.3238 0.0000 0.0000 0.00E+00 0.0000 0.0000 2.99E-03 17 * * 0.00 0.000 0.021 0.3238 0.0000 0.0000 0.00E+00 0.0000 0.0000 3.13E-03 18 * * 0.00 0.000 0.022 0.3238 0.0000 0.0000 0.00E+00 0.0000 0.0000 3.19E-03 19 * * 0.10 0.000 0.000 0.3238 0.0000 0.0000 0.00E+00 0.0000 0.0000 3.22E-03 20 * * 0.20 0.000 0.017 0.3238 0.0000 0.0000 0.00E+00 0.0000 0.0000 3.23E-03 21 * * 0.00 0.000 0.018 0.3238 0.0000 0.0000 0.00E+00 0.0000 0.0000 3.25E-03 22 * * 0.00 0.000 0.024 0.3238 0.0000 0.0000 0.00E+00 0.0000 0.0000 3.29E-03 23 * * 0.00 0.000 0.026 0.3238 0.0000 0.0000 0.00E+00 0.0000 0.0000 3.34E-03 24 * * 0.30 0.000 0.022 0.3238 0.0000 0.0000 0.00E+00 0.0000 0.0000 3.40E-03 25 * * 0.50 0.000 0.015 0.3238 0.0000 0.0000 0.00E+00 0.0000 0.0000 3.45E-03 26 * * 0.00 0.000 0.015 0.3238 0.0000 0.0000 0.00E+00 0.0000 0.0000 3.49E-03 27 * * 0.00 0.000 0.021 0.3238 0.0000 0.0000 0.00E+00 0.0000 0.0000 3.49E-03 7/19/2024 11:05 Freezing Status* Page 66 of 128 28 * 0.00 0.000 0.028 0.3238 0.0000 0.0000 0.00E+00 0.0000 0.0000 3.46E-03 29 * 0.00 0.000 0.032 0.3238 0.0000 0.0000 0.00E+00 0.0000 0.0000 3.39E-03 30 * 0.10 0.029 0.000 0.3412 0.0000 0.0000 0.00E+00 0.0000 0.0000 3.27E-03 31 * * 0.10 0.004 0.018 0.3438 0.0000 0.0000 0.00E+00 0.0000 0.0000 3.12E-03 32 * * 0.00 0.000 0.017 0.3438 0.0000 0.0000 0.00E+00 0.0000 0.0000 2.92E-03 33 * * 0.00 0.000 0.013 0.3438 0.0000 0.0000 0.00E+00 0.0000 0.0000 2.69E-03 34 * * 0.00 0.000 0.011 0.3438 0.0000 0.0000 0.00E+00 0.0000 0.0000 2.45E-03 35 * * 0.00 0.000 0.014 0.3438 0.0000 0.0000 0.00E+00 0.0000 0.0000 2.18E-03 36 * * 0.00 0.000 0.017 0.3438 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.92E-03 37 * * 0.00 0.000 0.021 0.3438 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.65E-03 38 * * 0.00 0.000 0.025 0.3438 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.40E-03 39 * * 0.00 0.000 0.026 0.3438 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.17E-03 40 * * 0.00 0.000 0.028 0.3438 0.0000 0.0000 0.00E+00 0.0000 0.0000 9.65E-04 41 * * 0.00 0.000 0.028 0.3438 0.0000 0.0000 0.00E+00 0.0000 0.0000 7.85E-04 42 * 0.00 0.000 0.028 0.3438 0.0000 0.0000 0.00E+00 0.0000 0.0000 6.34E-04 43 * 0.00 0.142 0.005 0.3609 0.0000 0.0000 0.00E+00 0.0000 0.0000 5.13E-04 44 * * 0.00 0.021 0.022 0.3637 0.0000 0.0000 0.00E+00 0.0000 0.0000 4.21E-04 45 * * 0.00 0.000 0.027 0.3637 0.0000 0.0000 0.00E+00 0.0000 0.0000 3.58E-04 46 * * 0.00 0.000 0.027 0.3637 0.0000 0.0000 0.00E+00 0.0000 0.0000 3.21E-04 47 * 0.00 0.000 0.031 0.3637 0.0000 0.0000 0.00E+00 0.0000 0.0000 3.09E-04 48 * * 0.00 0.000 0.029 0.3637 0.0000 0.0000 0.00E+00 0.0000 0.0000 3.20E-04 49 * * 0.10 0.000 0.026 0.3637 0.0000 0.0000 0.00E+00 0.0000 0.0000 3.53E-04 50 * * 0.00 0.000 0.025 0.3637 0.0000 0.0000 0.00E+00 0.0000 0.0000 4.05E-04 51 * * 0.00 0.000 0.028 0.3637 0.0000 0.0000 0.00E+00 0.0000 0.0000 4.76E-04 52 * * 0.00 0.000 0.027 0.3637 0.0000 0.0000 0.00E+00 0.0000 0.0000 5.65E-04 53 * * 0.40 0.000 0.024 0.3637 0.0000 0.0000 0.00E+00 0.0000 0.0000 6.70E-04 54 * * 0.00 0.000 0.020 0.3637 0.0000 0.0000 0.00E+00 0.0000 0.0000 7.90E-04 55 * * 0.00 0.000 0.021 0.3637 0.0000 0.0000 0.00E+00 0.0000 0.0000 9.25E-04 56 * * 0.00 0.000 0.030 0.3637 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.07E-03 57 * 0.00 0.000 0.029 0.3637 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.23E-03 58 * 0.00 0.015 0.031 0.3637 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.40E-03 59 * 0.00 0.132 0.008 0.3746 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.57E-03 60 * 0.00 0.060 0.019 0.3787 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.75E-03 61 * 0.00 0.306 0.000 0.3904 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.93E-03 62 * 0.00 0.252 0.000 0.3999 0.0000 0.0000 0.00E+00 0.0000 0.0000 2.10E-03 Page 67 of 128 63 * 0.00 0.359 0.000 0.4076 0.0000 0.0000 0.00E+00 0.0000 0.0000 2.27E-03 64 * 0.00 0.334 0.000 0.4139 0.0000 0.0000 0.00E+00 0.0000 0.0000 2.44E-03 65 * 0.00 0.478 0.000 0.4203 0.0000 0.0000 0.00E+00 0.0000 0.0000 2.59E-03 66 * 0.30 0.284 0.000 0.4245 0.0004 0.0000 4.63E-03 0.0000 0.0000 2.74E-03 67 * * 0.20 0.000 0.027 0.4245 0.0000 0.0000 0.00E+00 0.0000 0.0000 2.87E-03 68 * * 0.00 0.000 0.026 0.4245 0.0000 0.0000 0.00E+00 0.0000 0.0000 3.85E-03 69 * * 0.00 0.000 0.030 0.4245 0.0000 0.0000 0.00E+00 0.0000 0.0000 8.12E-04 70 * 0.00 0.080 0.023 0.4245 0.0000 0.0000 0.00E+00 0.0000 0.0000 3.49E-03 71 * 0.00 0.316 0.000 0.4245 0.0083 0.0000 1.53E-02 0.0000 0.0000 4.62E-03 72 * 0.00 0.212 0.005 0.4245 0.0055 0.0000 1.02E-02 0.0000 0.0000 4.26E-03 73 * 0.00 0.213 0.005 0.4245 0.0054 0.0000 9.93E-03 0.0000 0.0000 3.56E-03 74 * 0.20 0.339 0.000 0.4245 0.0082 0.0000 1.52E-02 0.0000 0.0000 3.00E-03 75 * * 0.00 0.000 0.032 0.4245 0.0000 0.0000 0.00E+00 0.0000 0.0000 2.73E-03 76 * 0.00 0.000 0.035 0.4245 0.0000 0.0000 0.00E+00 0.0000 0.0000 2.73E-03 77 * 0.00 0.250 0.000 0.4245 0.0082 0.0000 1.52E-02 0.0000 0.0000 3.68E-03 78 * * 0.00 0.000 0.033 0.4245 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.16E-03 79 * * 0.00 0.000 0.035 0.4245 0.0000 0.0000 0.00E+00 0.0000 0.0000 4.13E-03 80 * 0.00 0.527 0.000 0.4245 0.0084 0.0000 1.55E-02 0.0000 0.0000 5.63E-03 81 * 0.00 0.055 0.045 0.4245 0.0000 0.0000 0.00E+00 0.0000 0.0000 2.04E-03 82 * * 0.10 0.000 0.042 0.4245 0.0000 0.0000 0.00E+00 0.0000 0.0000 4.61E-03 83 * * 0.10 0.000 0.036 0.4245 0.0000 0.0000 0.00E+00 0.0000 0.0000 4.60E-03 84 * * 0.10 0.000 0.029 0.4245 0.0000 0.0000 0.00E+00 0.0000 0.0000 3.79E-03 85 * * 0.00 0.000 0.042 0.4245 0.0000 0.0000 0.00E+00 0.0000 0.0000 3.01E-03 86 * * 0.20 0.000 0.030 0.4245 0.0000 0.0000 0.00E+00 0.0000 0.0000 2.57E-03 87 * * 0.00 0.000 0.036 0.4245 0.0000 0.0000 0.00E+00 0.0000 0.0000 2.54E-03 88 * 0.10 0.268 0.000 0.4245 0.0082 0.0000 1.52E-02 0.0000 0.0000 3.40E-03 89 * * 0.10 0.000 0.032 0.4245 0.0000 0.0000 0.00E+00 0.0000 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5.26E-03 103 0.00 0.000 0.072 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 7.27E-03 104 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 5.61E-03 105 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 4.11E-03 106 * 0.20 0.000 0.068 0.1226 0.0000 0.0000 0.00E+00 0.0000 0.0000 3.90E-03 107 * 0.00 0.000 0.068 0.1291 0.0000 0.0000 0.00E+00 0.0000 0.0000 4.86E-03 108 0.00 0.000 0.050 0.1210 0.0000 0.0000 0.00E+00 0.0000 0.0000 6.37E-03 109 * 0.00 0.000 0.011 0.1173 0.0000 0.0000 0.00E+00 0.0000 0.0000 8.36E-03 110 0.00 0.000 0.003 0.1163 0.0000 0.0000 0.00E+00 0.0000 0.0000 8.67E-03 111 0.00 0.000 0.001 0.1161 0.0000 0.0000 0.00E+00 0.0000 0.0000 8.20E-03 112 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 8.46E-03 113 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 8.92E-03 114 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 8.82E-03 115 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 8.34E-03 116 0.40 0.000 0.030 0.2392 0.0000 0.0000 0.00E+00 0.0000 0.0000 7.35E-03 117 * 0.10 0.000 0.118 0.2301 0.0105 0.0000 9.68E-03 0.0000 0.0000 5.97E-03 118 0.10 0.000 0.038 0.2428 0.0167 0.0000 2.41E-02 0.0000 0.0000 4.36E-03 119 * 0.70 0.000 0.059 0.2358 0.0352 0.0000 4.08E-02 0.0000 0.0000 3.61E-03 120 0.10 0.000 0.000 0.2780 0.0965 0.0000 7.70E-02 0.0000 0.0000 4.38E-03 121 0.00 0.000 0.043 0.3839 0.7809 0.0000 1.28E-01 0.0000 0.0000 5.72E-03 122 0.00 0.000 0.133 0.3048 1.6015 0.0000 1.33E-01 0.0000 0.0000 6.29E-03 123 0.00 0.000 0.082 0.2342 1.0402 0.0000 1.30E-01 0.0000 0.0000 9.35E-03 124 0.00 0.000 0.089 0.1627 0.4230 0.0000 1.25E-01 0.0000 0.0000 9.13E-03 125 0.00 0.000 0.098 0.1260 0.0227 0.0000 1.17E-02 0.0000 0.0000 8.99E-03 126 0.00 0.000 0.030 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 8.81E-03 127 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 8.53E-03 128 0.40 0.000 0.110 0.2126 0.0000 0.0000 0.00E+00 0.0000 0.0000 6.88E-03 129 0.30 0.000 0.093 0.2713 0.0485 0.0000 3.09E-02 0.0000 0.0000 6.91E-03 130 0.50 0.000 0.190 0.3329 0.3622 0.0000 1.25E-01 0.0000 0.0000 8.38E-03 131 0.00 0.000 0.157 0.2377 0.8742 0.0000 1.28E-01 0.0000 0.0000 7.58E-03 132 0.00 0.000 0.164 0.1415 0.3672 0.0000 1.25E-01 0.0000 0.0000 7.82E-03 Page 69 of 128 133 0.00 0.000 0.072 0.1175 0.0005 0.0000 0.00E+00 0.0000 0.0000 7.48E-03 134 0.00 0.000 0.004 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 3.98E-03 135 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.72E-03 136 0.10 0.000 0.050 0.1326 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.11E-03 137 0.10 0.000 0.040 0.1525 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.38E-03 138 0.10 0.000 0.047 0.1702 0.0000 0.0000 0.00E+00 0.0000 0.0000 2.05E-03 139 0.00 0.000 0.041 0.1564 0.0000 0.0000 0.00E+00 0.0000 0.0000 2.82E-03 140 0.00 0.000 0.040 0.1429 0.0000 0.0000 0.00E+00 0.0000 0.0000 3.51E-03 141 0.00 0.000 0.037 0.1308 0.0000 0.0000 0.00E+00 0.0000 0.0000 4.04E-03 142 0.00 0.000 0.034 0.1195 0.0000 0.0000 0.00E+00 0.0000 0.0000 4.39E-03 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0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.03E-02 184 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.04E-02 185 0.20 0.000 0.013 0.1782 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.02E-02 186 0.00 0.000 0.013 0.1740 0.0000 0.0000 0.00E+00 0.0000 0.0000 9.90E-03 187 0.00 0.000 0.014 0.1694 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.01E-02 188 0.00 0.000 0.015 0.1643 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.04E-02 189 0.00 0.000 0.016 0.1589 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.08E-02 190 0.00 0.000 0.018 0.1530 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.10E-02 191 0.00 0.000 0.018 0.1471 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.12E-02 192 0.00 0.000 0.020 0.1406 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.13E-02 193 0.00 0.000 0.020 0.1338 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.14E-02 194 0.00 0.000 0.021 0.1269 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.12E-02 195 0.00 0.000 0.018 0.1209 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.09E-02 196 0.00 0.000 0.011 0.1172 0.0000 0.0000 0.00E+00 0.0000 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0.00 0.000 0.045 0.1483 0.0000 0.0000 0.00E+00 0.0000 0.0000 9.26E-03 211 0.00 0.000 0.049 0.1320 0.0000 0.0000 0.00E+00 0.0000 0.0000 8.74E-03 212 0.00 0.000 0.034 0.1207 0.0000 0.0000 0.00E+00 0.0000 0.0000 8.91E-03 213 0.10 0.000 0.043 0.1398 0.0000 0.0000 0.00E+00 0.0000 0.0000 9.40E-03 214 0.00 0.000 0.024 0.1319 0.0000 0.0000 0.00E+00 0.0000 0.0000 9.96E-03 215 0.00 0.000 0.036 0.1199 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.05E-02 216 0.00 0.000 0.009 0.1170 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.08E-02 217 0.10 0.000 0.033 0.1394 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.10E-02 218 0.20 0.000 0.048 0.1903 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.10E-02 219 0.00 0.000 0.062 0.1695 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.06E-02 220 0.00 0.000 0.069 0.1465 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.02E-02 221 0.00 0.000 0.054 0.1286 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.03E-02 222 0.00 0.000 0.035 0.1169 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.03E-02 223 0.00 0.000 0.003 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.00E-02 224 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 9.44E-03 225 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 8.77E-03 226 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 8.15E-03 227 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 7.61E-03 228 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 7.18E-03 229 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 6.87E-03 230 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 6.67E-03 231 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 6.57E-03 232 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 6.54E-03 233 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 6.46E-03 234 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 6.71E-03 235 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 7.17E-03 236 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 7.68E-03 237 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 8.17E-03 Page 72 of 128 238 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 8.57E-03 239 0.20 0.000 0.031 0.1724 0.0000 0.0000 0.00E+00 0.0000 0.0000 8.86E-03 240 0.00 0.000 0.045 0.1574 0.0000 0.0000 0.00E+00 0.0000 0.0000 9.04E-03 241 0.00 0.000 0.052 0.1401 0.0000 0.0000 0.00E+00 0.0000 0.0000 9.11E-03 242 0.00 0.000 0.052 0.1228 0.0000 0.0000 0.00E+00 0.0000 0.0000 9.09E-03 243 0.00 0.000 0.017 0.1171 0.0000 0.0000 0.00E+00 0.0000 0.0000 8.99E-03 244 0.50 0.000 0.084 0.2557 0.0000 0.0000 0.00E+00 0.0000 0.0000 8.82E-03 245 0.10 0.000 0.096 0.2361 0.1612 0.0000 6.23E-02 0.0000 0.0000 8.62E-03 246 0.10 0.000 0.176 0.1866 0.1360 0.0000 7.21E-02 0.0000 0.0000 8.38E-03 247 0.10 0.000 0.082 0.1928 0.0000 0.0000 0.00E+00 0.0000 0.0000 8.13E-03 248 0.10 0.000 0.130 0.1828 0.0000 0.0000 0.00E+00 0.0000 0.0000 7.88E-03 249 0.00 0.000 0.120 0.1430 0.0000 0.0000 0.00E+00 0.0000 0.0000 7.62E-03 250 0.00 0.000 0.079 0.1167 0.0000 0.0000 0.00E+00 0.0000 0.0000 7.38E-03 251 0.00 0.000 0.001 0.1162 0.0000 0.0000 0.00E+00 0.0000 0.0000 7.16E-03 252 0.00 0.000 0.001 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 6.95E-03 253 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 6.76E-03 254 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 6.58E-03 255 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 6.30E-03 256 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 6.18E-03 257 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 6.26E-03 258 0.10 0.000 0.042 0.1352 0.0000 0.0000 0.00E+00 0.0000 0.0000 6.28E-03 259 0.00 0.000 0.027 0.1261 0.0000 0.0000 0.00E+00 0.0000 0.0000 6.21E-03 260 0.00 0.000 0.024 0.1182 0.0000 0.0000 0.00E+00 0.0000 0.0000 6.29E-03 261 0.00 0.000 0.005 0.1166 0.0000 0.0000 0.00E+00 0.0000 0.0000 6.43E-03 262 0.00 0.000 0.001 0.1161 0.0000 0.0000 0.00E+00 0.0000 0.0000 6.52E-03 263 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 6.52E-03 264 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 6.40E-03 265 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 6.21E-03 266 1.60 0.440 0.083 0.4630 0.7500 0.0000 3.57E-02 0.0000 0.0000 6.47E-03 267 0.20 0.188 0.091 0.3900 2.6478 0.0000 1.40E-01 0.0000 0.0000 4.36E-03 268 0.00 0.000 0.093 0.3142 1.8131 0.0000 1.35E-01 0.0000 0.0000 5.36E-03 269 0.00 0.000 0.134 0.2264 1.0857 0.0000 1.30E-01 0.0000 0.0000 5.45E-03 270 0.00 0.000 0.141 0.1393 0.3912 0.0000 1.20E-01 0.0000 0.0000 7.42E-03 271 0.00 0.000 0.070 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 8.47E-03 272 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 6.16E-03 Page 73 of 128 273 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 4.25E-03 274 0.10 0.000 0.072 0.1254 0.0000 0.0000 0.00E+00 0.0000 0.0000 3.72E-03 275 0.00 0.000 0.023 0.1177 0.0000 0.0000 0.00E+00 0.0000 0.0000 5.07E-03 276 0.00 0.000 0.004 0.1163 0.0000 0.0000 0.00E+00 0.0000 0.0000 4.99E-03 277 0.10 0.000 0.042 0.1358 0.0000 0.0000 0.00E+00 0.0000 0.0000 6.16E-03 278 0.00 0.000 0.012 0.1317 0.0000 0.0000 0.00E+00 0.0000 0.0000 7.11E-03 279 0.00 0.000 0.033 0.1207 0.0000 0.0000 0.00E+00 0.0000 0.0000 9.33E-03 280 0.00 0.000 0.012 0.1169 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.07E-02 281 0.00 0.000 0.002 0.1161 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.06E-02 282 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 9.39E-03 283 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 7.67E-03 284 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 6.02E-03 285 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 4.83E-03 286 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 4.26E-03 287 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 4.30E-03 288 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 4.83E-03 289 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 5.67E-03 290 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 6.63E-03 291 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 7.54E-03 292 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 8.29E-03 293 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 8.80E-03 294 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 9.03E-03 295 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 8.95E-03 296 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 8.61E-03 297 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 8.29E-03 298 0.20 0.000 0.019 0.1763 0.0000 0.0000 0.00E+00 0.0000 0.0000 7.77E-03 299 0.00 0.000 0.017 0.1705 0.0000 0.0000 0.00E+00 0.0000 0.0000 7.45E-03 300 0.00 0.000 0.019 0.1642 0.0000 0.0000 0.00E+00 0.0000 0.0000 5.59E-03 301 0.00 0.000 0.018 0.1581 0.0000 0.0000 0.00E+00 0.0000 0.0000 4.77E-03 302 0.00 0.000 0.018 0.1520 0.0000 0.0000 0.00E+00 0.0000 0.0000 4.49E-03 303 0.00 0.000 0.018 0.1460 0.0000 0.0000 0.00E+00 0.0000 0.0000 4.72E-03 304 0.10 0.000 0.028 0.1699 0.0000 0.0000 0.00E+00 0.0000 0.0000 4.79E-03 305 0.00 0.000 0.018 0.1639 0.0000 0.0000 0.00E+00 0.0000 0.0000 4.62E-03 306 0.00 0.000 0.018 0.1580 0.0000 0.0000 0.00E+00 0.0000 0.0000 4.36E-03 307 0.00 0.000 0.017 0.1523 0.0000 0.0000 0.00E+00 0.0000 0.0000 4.20E-03 Page 74 of 128 308 0.00 0.000 0.018 0.1464 0.0000 0.0000 0.00E+00 0.0000 0.0000 4.26E-03 309 0.00 0.000 0.017 0.1407 0.0000 0.0000 0.00E+00 0.0000 0.0000 4.57E-03 310 0.00 0.000 0.016 0.1353 0.0000 0.0000 0.00E+00 0.0000 0.0000 5.12E-03 311 0.00 0.000 0.016 0.1299 0.0000 0.0000 0.00E+00 0.0000 0.0000 5.81E-03 312 0.00 0.000 0.014 0.1254 0.0000 0.0000 0.00E+00 0.0000 0.0000 6.79E-03 313 0.00 0.000 0.016 0.1201 0.0000 0.0000 0.00E+00 0.0000 0.0000 7.59E-03 314 0.00 0.000 0.010 0.1167 0.0000 0.0000 0.00E+00 0.0000 0.0000 7.94E-03 315 0.00 0.000 0.002 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 8.05E-03 316 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 8.06E-03 317 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 8.04E-03 318 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 8.05E-03 319 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 8.09E-03 320 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 8.16E-03 321 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 8.25E-03 322 * 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 8.36E-03 323 * 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 8.46E-03 324 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 8.54E-03 325 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 8.60E-03 326 0.70 0.000 0.021 0.3422 0.0000 0.0000 0.00E+00 0.0000 0.0000 8.61E-03 327 * 0.10 0.000 0.019 0.3051 1.2321 0.0000 1.31E-01 0.0000 0.0000 8.59E-03 328 * 0.10 0.000 0.020 0.2690 0.8347 0.0000 1.28E-01 0.0000 0.0000 8.53E-03 329 * 0.00 0.000 0.023 0.2387 0.2433 0.0000 1.11E-01 0.0000 0.0000 8.43E-03 330 * 0.00 0.000 0.020 0.2441 0.0012 0.0000 3.47E-03 0.0000 0.0000 8.29E-03 331 * 0.00 0.000 0.028 0.2462 0.0060 0.0000 5.57E-03 0.0000 0.0000 8.13E-03 332 * 0.40 0.000 0.016 0.2480 0.0083 0.0000 1.43E-02 0.0000 0.0000 7.94E-03 333 * 0.50 0.000 0.015 0.2494 0.0101 0.0000 1.55E-02 0.0000 0.0000 7.73E-03 334 * 0.10 0.000 0.011 0.2507 0.0170 0.0000 1.58E-02 0.0000 0.0000 7.51E-03 335 * 0.00 0.000 0.009 0.2509 0.0101 0.0000 1.91E-02 0.0000 0.0000 7.28E-03 336 * * 0.00 0.000 0.012 0.2507 0.0005 0.0000 4.25E-04 0.0000 0.0000 7.05E-03 337 * * 0.00 0.000 0.011 0.2507 0.0000 0.0000 0.00E+00 0.0000 0.0000 6.82E-03 338 * * 0.00 0.000 0.012 0.2507 0.0000 0.0000 0.00E+00 0.0000 0.0000 6.61E-03 339 * * 0.00 0.000 0.016 0.2507 0.0000 0.0000 0.00E+00 0.0000 0.0000 6.40E-03 340 * * 0.00 0.000 0.013 0.2507 0.0000 0.0000 0.00E+00 0.0000 0.0000 6.21E-03 341 * * 0.00 0.000 0.015 0.2507 0.0000 0.0000 0.00E+00 0.0000 0.0000 6.04E-03 342 * * 0.00 0.000 0.009 0.2507 0.0000 0.0000 0.00E+00 0.0000 0.0000 6.06E-03 Page 75 of 128 343 * * 0.00 0.000 0.014 0.2507 0.0000 0.0000 0.00E+00 0.0000 0.0000 7.91E-03 344 * 0.00 0.000 0.000 0.2507 0.0000 0.0000 0.00E+00 0.0000 0.0000 5.61E-03 345 * 0.00 0.000 0.020 0.2507 0.0000 0.0000 0.00E+00 0.0000 0.0000 4.45E-03 346 * * 0.10 0.000 0.019 0.2507 0.0000 0.0000 0.00E+00 0.0000 0.0000 4.04E-03 347 * * 0.00 0.000 0.017 0.2507 0.0000 0.0000 0.00E+00 0.0000 0.0000 4.11E-03 348 * * 0.00 0.000 0.017 0.2507 0.0000 0.0000 0.00E+00 0.0000 0.0000 4.46E-03 349 * 0.00 0.062 0.000 0.3178 0.0000 0.0000 0.00E+00 0.0000 0.0000 4.96E-03 350 * 0.10 0.193 0.000 0.3629 0.0000 0.0000 0.00E+00 0.0000 0.0000 5.50E-03 351 * * 0.60 0.000 0.019 0.3629 0.0000 0.0000 0.00E+00 0.0000 0.0000 6.03E-03 352 * * 0.00 0.000 0.009 0.3629 0.0000 0.0000 0.00E+00 0.0000 0.0000 6.50E-03 353 * * 0.00 0.000 0.008 0.3629 0.0000 0.0000 0.00E+00 0.0000 0.0000 6.91E-03 354 * * 0.10 0.000 0.000 0.3629 0.0000 0.0000 0.00E+00 0.0000 0.0000 7.23E-03 355 * * 0.00 0.000 0.018 0.3629 0.0000 0.0000 0.00E+00 0.0000 0.0000 7.49E-03 356 * * 0.00 0.000 0.018 0.3629 0.0000 0.0000 0.00E+00 0.0000 0.0000 7.68E-03 357 * * 0.20 0.000 0.000 0.3629 0.0000 0.0000 0.00E+00 0.0000 0.0000 7.82E-03 358 * * 0.00 0.000 0.015 0.3629 0.0000 0.0000 0.00E+00 0.0000 0.0000 7.92E-03 359 * * 0.30 0.000 0.000 0.3629 0.0000 0.0000 0.00E+00 0.0000 0.0000 7.98E-03 360 * * 0.10 0.000 0.009 0.3629 0.0000 0.0000 0.00E+00 0.0000 0.0000 8.03E-03 361 * * 0.00 0.000 0.008 0.3629 0.0000 0.0000 0.00E+00 0.0000 0.0000 7.76E-03 362 * * 0.00 0.000 0.014 0.3629 0.0000 0.0000 0.00E+00 0.0000 0.0000 8.41E-03 363 * * 0.10 0.000 0.000 0.3629 0.0000 0.0000 0.00E+00 0.0000 0.0000 8.31E-03 364 * * 0.00 0.000 0.016 0.3629 0.0000 0.0000 0.00E+00 0.0000 0.0000 8.27E-03 365 * * 0.00 0.000 0.018 0.3629 0.0000 0.0000 0.00E+00 0.0000 0.0000 8.28E-03 * = Frozen (air or soil) inches cubic feet percent Precipitation 15.10 3,836,910.0 100.00 Runoff 5.560 1,412,836.5 36.82 Evapotranspiration 8.178 2,077,928.3 54.16 Percolation/Leakage through Layer 2 2.778709 706,070.0 18.40 Average Head on Top of Layer 2 0.0527 ------ Percolation/Leakage through Layer 12 2.104905 534,856.4 13.94 Annual Totals for Year 6 Page 76 of 128 Change in Water Storage -0.7427 -188,711.2 -4.92 Soil Water at Start of Year 234.2969 #########1551.63 Soil Water at End of Year 235.0878 #########1556.87 Snow Water at Start of Year 3.0840 783,648.5 20.42 Snow Water at End of Year 1.5504 393,965.6 10.27 Annual Water Budget Balance 0.0000 0.0000 0.00 Page 77 of 128 Daily Output for Year 7 Column key:Head #1: drainage from Layer 2 Title:Long Valley Landfill Simulated On:Leak #1: leakage thru Layer 2 Leak #2: leakage thru Layer 12 Day Rain Runoff ET Evap. Zone Water Head #1 Drain #1 Leak #1 Head #2 Drain #2 Leak #2 Air Soil (inches)(inches)(inches)(in/in)(inches)(inches)(inches)(inches)(inches)(inches) 1 * * 0.00 0.000 0.020 0.3629 0.0000 0.0000 0.00E+00 0.0000 0.0000 8.34E-03 2 * * 0.00 0.000 0.024 0.3629 0.0000 0.0000 0.00E+00 0.0000 0.0000 8.42E-03 3 * * 0.00 0.000 0.023 0.3629 0.0000 0.0000 0.00E+00 0.0000 0.0000 8.22E-03 4 * * 0.10 0.000 0.000 0.3629 0.0000 0.0000 0.00E+00 0.0000 0.0000 8.39E-03 5 * * 0.30 0.000 0.020 0.3629 0.0000 0.0000 0.00E+00 0.0000 0.0000 8.85E-03 6 * * 0.00 0.000 0.012 0.3629 0.0000 0.0000 0.00E+00 0.0000 0.0000 9.62E-03 7 * * 0.00 0.000 0.016 0.3629 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.03E-02 8 * 0.20 0.024 0.000 0.3760 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.06E-02 9 * 0.20 0.165 0.000 0.3924 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.07E-02 10 * * 0.00 0.000 0.027 0.3924 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.06E-02 11 * * 0.50 0.000 0.027 0.3924 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.05E-02 12 * * 0.30 0.000 0.025 0.3924 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.04E-02 13 * * 0.00 0.000 0.025 0.3924 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.04E-02 14 * * 0.00 0.000 0.022 0.3924 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.06E-02 15 * * 0.10 0.000 0.023 0.3924 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.09E-02 16 * * 0.00 0.000 0.017 0.3924 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.13E-02 17 * * 0.00 0.000 0.019 0.3924 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.17E-02 18 * * 0.00 0.000 0.019 0.3924 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.01E-02 19 * * 0.10 0.000 0.000 0.3924 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.23E-02 20 * * 0.10 0.000 0.000 0.3924 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.40E-02 21 * * 0.40 0.000 0.017 0.3924 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.49E-02 22 * * 0.10 0.000 0.019 0.3924 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.51E-02 23 * * 0.20 0.000 0.000 0.3924 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.49E-02 24 * * 0.00 0.000 0.016 0.3924 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.43E-02 25 * * 0.10 0.000 0.010 0.3924 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.37E-02 26 * * 0.00 0.000 0.011 0.3924 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.29E-02 27 * * 0.00 0.000 0.010 0.3924 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.23E-02 7/19/2024 11:05 Freezing Status* Page 78 of 128 28 * * 0.00 0.000 0.018 0.3924 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.21E-02 29 * * 0.00 0.000 0.000 0.3924 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.21E-02 30 * * 0.00 0.000 0.025 0.3924 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.22E-02 31 * * 0.00 0.000 0.025 0.3924 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.23E-02 32 * 0.00 0.000 0.029 0.3924 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.24E-02 33 * 0.00 0.000 0.030 0.3924 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.25E-02 34 * * 0.00 0.000 0.027 0.3924 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.25E-02 35 * 0.00 0.002 0.029 0.3924 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.25E-02 36 * * 0.00 0.000 0.025 0.3924 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.17E-02 37 * * 0.00 0.000 0.027 0.3924 0.0000 0.0000 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0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 5.46E-03 185 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 5.37E-03 186 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 5.30E-03 187 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 5.24E-03 188 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 5.19E-03 189 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 5.13E-03 190 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 5.08E-03 191 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 5.01E-03 192 0.10 0.000 0.013 0.1451 0.0000 0.0000 0.00E+00 0.0000 0.0000 4.50E-03 193 0.30 0.000 0.016 0.2398 0.0000 0.0000 0.00E+00 0.0000 0.0000 4.86E-03 194 0.00 0.000 0.012 0.2318 0.0017 0.0000 1.25E-02 0.0000 0.0000 6.00E-03 195 0.10 0.000 0.020 0.2438 0.0104 0.0000 4.41E-02 0.0000 0.0000 4.97E-03 196 0.00 0.000 0.012 0.2252 0.0376 0.0000 4.37E-02 0.0000 0.0000 3.73E-03 197 0.00 0.000 0.012 0.2181 0.0035 0.0000 8.93E-03 0.0000 0.0000 3.35E-03 198 0.10 0.000 0.020 0.2424 0.0041 0.0000 6.75E-03 0.0000 0.0000 2.23E-03 199 0.00 0.000 0.013 0.2376 0.0015 0.0000 1.17E-03 0.0000 0.0000 3.66E-03 200 0.20 0.000 0.021 0.2663 0.0958 0.0000 9.25E-02 0.0000 0.0000 4.73E-03 201 0.00 0.000 0.015 0.2420 0.0339 0.0000 5.86E-02 0.0000 0.0000 2.90E-03 202 0.00 0.000 0.014 0.2304 0.0062 0.0000 2.03E-02 0.0000 0.0000 3.22E-03 Page 83 of 128 203 0.00 0.000 0.014 0.2217 0.0071 0.0000 1.15E-02 0.0000 0.0000 5.17E-03 204 0.00 0.000 0.016 0.2149 0.0032 0.0000 4.26E-03 0.0000 0.0000 4.21E-03 205 0.00 0.000 0.015 0.2100 0.0000 0.0000 0.00E+00 0.0000 0.0000 3.57E-03 206 1.40 0.549 0.022 0.4630 1.4044 0.0000 7.08E-02 0.0000 0.0000 3.21E-03 207 0.00 0.000 0.136 0.3709 2.5706 0.0000 1.40E-01 0.0000 0.0000 1.91E-03 208 0.00 0.000 0.150 0.2764 1.6239 0.0000 1.34E-01 0.0000 0.0000 2.10E-03 209 0.10 0.000 0.229 0.1905 0.8267 0.0000 1.28E-01 0.0000 0.0000 4.71E-03 210 0.00 0.000 0.159 0.1223 0.1348 0.0000 4.55E-02 0.0000 0.0000 4.79E-03 211 0.00 0.000 0.018 0.1163 0.0000 0.0000 0.00E+00 0.0000 0.0000 4.62E-03 212 0.10 0.000 0.065 0.1280 0.0000 0.0000 0.00E+00 0.0000 0.0000 4.37E-03 213 0.00 0.000 0.028 0.1188 0.0000 0.0000 0.00E+00 0.0000 0.0000 4.70E-03 214 0.00 0.000 0.007 0.1166 0.0000 0.0000 0.00E+00 0.0000 0.0000 2.68E-03 215 0.00 0.000 0.002 0.1161 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.47E-03 216 0.50 0.000 0.065 0.2610 0.0000 0.0000 0.00E+00 0.0000 0.0000 5.77E-03 217 0.30 0.000 0.194 0.2655 0.1488 0.0000 9.29E-02 0.0000 0.0000 9.63E-03 218 1.10 0.146 0.231 0.4630 1.2341 0.0000 1.31E-01 0.0000 0.0000 1.03E-02 219 0.00 0.000 0.216 0.3445 2.4478 0.0000 1.39E-01 0.0000 0.0000 9.64E-03 220 0.00 0.000 0.141 0.2534 1.4169 0.0000 1.32E-01 0.0000 0.0000 8.28E-03 221 0.10 0.000 0.216 0.1723 0.6321 0.0000 1.27E-01 0.0000 0.0000 7.27E-03 222 0.00 0.000 0.143 0.1173 0.0535 0.0000 2.26E-02 0.0000 0.0000 6.63E-03 223 0.10 0.000 0.080 0.1238 0.0000 0.0000 0.00E+00 0.0000 0.0000 3.85E-03 224 0.00 0.000 0.020 0.1173 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.54E-03 225 0.00 0.000 0.003 0.1163 0.0000 0.0000 0.00E+00 0.0000 0.0000 4.81E-03 226 0.10 0.000 0.080 0.1231 0.0000 0.0000 0.00E+00 0.0000 0.0000 7.94E-03 227 0.00 0.000 0.017 0.1176 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.11E-02 228 0.00 0.000 0.004 0.1164 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.20E-02 229 0.00 0.000 0.001 0.1161 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.13E-02 230 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 9.73E-03 231 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 8.01E-03 232 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 6.59E-03 233 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 5.71E-03 234 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 5.41E-03 235 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 5.64E-03 236 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 6.23E-03 237 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 7.03E-03 Page 84 of 128 238 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 7.58E-03 239 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 8.71E-03 240 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 9.84E-03 241 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.03E-02 242 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.02E-02 243 0.10 0.000 0.026 0.1407 0.0000 0.0000 0.00E+00 0.0000 0.0000 9.88E-03 244 0.00 0.000 0.018 0.1347 0.0000 0.0000 0.00E+00 0.0000 0.0000 9.50E-03 245 0.00 0.000 0.030 0.1246 0.0000 0.0000 0.00E+00 0.0000 0.0000 9.46E-03 246 0.00 0.000 0.023 0.1167 0.0000 0.0000 0.00E+00 0.0000 0.0000 9.74E-03 247 0.00 0.000 0.002 0.1162 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.01E-02 248 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.03E-02 249 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.04E-02 250 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.05E-02 251 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.05E-02 252 0.30 0.000 0.032 0.2053 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.05E-02 253 0.00 0.000 0.033 0.1944 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.05E-02 254 0.10 0.000 0.043 0.2134 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.05E-02 255 1.00 0.144 0.040 0.4630 1.0274 0.0000 6.82E-02 0.0000 0.0000 1.07E-02 256 0.00 0.000 0.139 0.3702 2.5673 0.0000 1.40E-01 0.0000 0.0000 1.11E-02 257 0.90 0.324 0.158 0.4630 2.4791 0.0000 1.39E-01 0.0000 0.0000 1.14E-02 258 0.20 0.191 0.149 0.3698 2.5656 0.0000 1.40E-01 0.0000 0.0000 1.11E-02 259 0.00 0.000 0.140 0.2786 1.6235 0.0000 1.33E-01 0.0000 0.0000 1.20E-02 260 0.00 0.000 0.141 0.1890 0.8524 0.0000 1.28E-01 0.0000 0.0000 1.26E-02 261 0.00 0.000 0.084 0.1326 0.2083 0.0000 8.51E-02 0.0000 0.0000 1.26E-02 262 0.00 0.000 0.050 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.28E-02 263 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.34E-02 264 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.12E-02 265 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.13E-02 266 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.30E-02 267 * 0.20 0.000 0.096 0.1226 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.50E-02 268 0.00 0.000 0.095 0.1190 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.62E-02 269 0.00 0.000 0.007 0.1166 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.66E-02 270 0.00 0.000 0.001 0.1162 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.63E-02 271 0.10 0.000 0.033 0.1384 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.56E-02 272 0.00 0.000 0.022 0.1312 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.46E-02 Page 85 of 128 273 0.00 0.000 0.032 0.1204 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.36E-02 274 0.10 0.000 0.036 0.1417 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.30E-02 275 * 0.20 0.000 0.029 0.1483 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.27E-02 276 0.00 0.000 0.015 0.1938 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.28E-02 277 0.00 0.000 0.031 0.1834 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.30E-02 278 0.00 0.000 0.031 0.1730 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.34E-02 279 0.00 0.000 0.029 0.1632 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.38E-02 280 0.00 0.000 0.028 0.1538 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.41E-02 281 0.00 0.000 0.027 0.1449 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.44E-02 282 * 0.00 0.000 0.026 0.1363 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.46E-02 283 0.00 0.000 0.025 0.1281 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.52E-02 284 0.00 0.000 0.019 0.1218 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.49E-02 285 0.00 0.000 0.014 0.1172 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.41E-02 286 0.00 0.000 0.004 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.35E-02 287 * 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.34E-02 288 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.35E-02 289 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.42E-02 290 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.48E-02 291 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.51E-02 292 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.49E-02 293 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.44E-02 294 * 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.44E-02 295 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.42E-02 296 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.38E-02 297 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.33E-02 298 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.28E-02 299 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.25E-02 300 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.23E-02 301 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.24E-02 302 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.27E-02 303 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.32E-02 304 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.37E-02 305 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.43E-02 306 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.48E-02 307 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.53E-02 Page 86 of 128 308 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.57E-02 309 0.10 0.000 0.014 0.1446 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.60E-02 310 0.00 0.000 0.010 0.1413 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.61E-02 311 * 0.00 0.000 0.012 0.1374 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.62E-02 312 * 0.00 0.000 0.012 0.1334 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.62E-02 313 0.00 0.000 0.012 0.1295 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.62E-02 314 0.00 0.000 0.012 0.1257 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.61E-02 315 0.00 0.000 0.011 0.1219 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.61E-02 316 0.00 0.000 0.013 0.1177 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.57E-02 317 0.00 0.000 0.004 0.1162 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.53E-02 318 0.00 0.000 0.000 0.1161 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.50E-02 319 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.49E-02 320 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.49E-02 321 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.48E-02 322 * 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.46E-02 323 * 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.41E-02 324 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.38E-02 325 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.35E-02 326 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.34E-02 327 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.29E-02 328 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.23E-02 329 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.17E-02 330 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.16E-02 331 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.19E-02 332 * 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.18E-02 333 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.39E-02 334 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.48E-02 335 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.41E-02 336 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.43E-02 337 * 0.10 0.000 0.028 0.1226 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.49E-02 338 * 0.00 0.000 0.017 0.1291 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.54E-02 339 * 0.00 0.000 0.016 0.1291 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.58E-02 340 * 0.00 0.000 0.000 0.1291 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.64E-02 341 * 0.00 0.000 0.000 0.1291 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.70E-02 342 * 0.00 0.000 0.008 0.1266 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.77E-02 Page 87 of 128 343 0.00 0.000 0.008 0.1241 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.85E-02 344 0.00 0.000 0.008 0.1215 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.93E-02 345 0.00 0.000 0.008 0.1190 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.96E-02 346 0.00 0.000 0.007 0.1167 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.97E-02 347 0.00 0.000 0.002 0.1161 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.96E-02 348 * 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.94E-02 349 * 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.91E-02 350 * 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.93E-02 351 * 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.89E-02 352 * 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.82E-02 353 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.75E-02 354 * 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.69E-02 355 * * 0.10 0.000 0.014 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.65E-02 356 * * 0.00 0.000 0.015 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.61E-02 357 * * 0.00 0.000 0.025 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.59E-02 358 * * 0.00 0.000 0.025 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.56E-02 359 * 0.00 0.000 0.021 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.52E-02 360 * * 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.48E-02 361 * 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.43E-02 362 * 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.37E-02 363 * 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.30E-02 364 * 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.25E-02 365 * 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.23E-02 * = Frozen (air or soil) inches cubic feet percent Precipitation 16.10 4,091,010.0 100.00 Runoff 5.374 1,365,475.9 33.38 Evapotranspiration 8.968 2,278,775.3 55.70 Percolation/Leakage through Layer 2 4.049269 1,028,919.4 25.15 Average Head on Top of Layer 2 0.0938 ------ Percolation/Leakage through Layer 12 3.916065 995,072.1 24.32 Annual Totals for Year 7 Page 88 of 128 Change in Water Storage -2.1579 -548,313.3 -13.40 Soil Water at Start of Year 235.0878 #########1460.17 Soil Water at End of Year 234.4804 #########1456.40 Snow Water at Start of Year 1.5504 393,965.6 9.63 Snow Water at End of Year 0.0000 0.0000 0.00 Annual Water Budget Balance 0.0000 0.0000 0.00 Page 89 of 128 Daily Output for Year 8 Column key:Head #1: drainage from Layer 2 Title:Long Valley Landfill Simulated On:Leak #1: leakage thru Layer 2 Leak #2: leakage thru Layer 12 Day Rain Runoff ET Evap. Zone Water Head #1 Drain #1 Leak #1 Head #2 Drain #2 Leak #2 Air Soil (inches)(inches)(inches)(in/in)(inches)(inches)(inches)(inches)(inches)(inches) 1 * * 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.23E-02 2 * * 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.24E-02 3 * * 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.25E-02 4 * 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.27E-02 5 * * 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.34E-02 6 * 0.30 0.057 0.008 0.1943 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.40E-02 7 * * 0.00 0.000 0.000 0.1943 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.45E-02 8 * * 0.00 0.000 0.000 0.1943 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.49E-02 9 * 0.20 0.053 0.008 0.2406 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.53E-02 10 * * 0.50 0.000 0.027 0.2406 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.57E-02 11 * * 0.00 0.000 0.021 0.2406 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.63E-02 12 * * 0.00 0.000 0.023 0.2406 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.69E-02 13 * * 0.00 0.000 0.024 0.2406 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.74E-02 14 * 0.00 0.000 0.028 0.2406 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.78E-02 15 * * 0.00 0.000 0.026 0.2406 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.80E-02 16 * * 0.00 0.000 0.024 0.2406 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.81E-02 17 * * 0.00 0.000 0.026 0.2406 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.82E-02 18 * 0.00 0.000 0.029 0.2406 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.81E-02 19 * 0.00 0.081 0.012 0.2747 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.79E-02 20 * * 0.20 0.000 0.023 0.2747 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.77E-02 21 * * 0.00 0.000 0.012 0.2747 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.74E-02 22 * * 0.00 0.000 0.015 0.2747 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.69E-02 23 * * 0.00 0.000 0.020 0.2747 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.64E-02 24 * * 0.00 0.000 0.023 0.2747 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.59E-02 25 * * 0.10 0.000 0.000 0.2747 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.54E-02 26 * * 0.00 0.000 0.017 0.2747 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.48E-02 27 * * 0.00 0.000 0.018 0.2747 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.43E-02 7/19/2024 11:05 Freezing Status* Page 90 of 128 28 * * 0.00 0.000 0.024 0.2747 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.38E-02 29 * 0.00 0.000 0.028 0.2747 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.32E-02 30 * 0.00 0.017 0.043 0.2798 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.26E-02 31 * 0.00 0.049 0.041 0.2903 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.21E-02 32 * 0.00 0.000 0.000 0.2903 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.15E-02 33 * 0.00 0.000 0.000 0.2903 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.09E-02 34 * 0.00 0.000 0.000 0.2903 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.03E-02 35 0.00 0.000 0.010 0.2554 0.4824 0.0000 9.51E-02 0.0000 0.0000 9.81E-03 36 0.00 0.000 0.011 0.2099 0.5071 0.0000 1.26E-01 0.0000 0.0000 9.32E-03 37 * 0.10 0.000 0.032 0.2008 0.0537 0.0000 4.69E-02 0.0000 0.0000 8.89E-03 38 * 0.00 0.000 0.031 0.2043 0.0036 0.0000 6.17E-03 0.0000 0.0000 8.52E-03 39 0.00 0.000 0.010 0.2006 0.0009 0.0000 7.05E-04 0.0000 0.0000 8.21E-03 40 0.00 0.000 0.010 0.1971 0.0000 0.0000 0.00E+00 0.0000 0.0000 7.97E-03 41 * 0.00 0.000 0.000 0.1971 0.0000 0.0000 0.00E+00 0.0000 0.0000 7.88E-03 42 * 0.00 0.000 0.000 0.1971 0.0000 0.0000 0.00E+00 0.0000 0.0000 7.78E-03 43 * * 0.10 0.000 0.049 0.1971 0.0000 0.0000 0.00E+00 0.0000 0.0000 7.63E-03 44 * * 0.00 0.000 0.032 0.1971 0.0000 0.0000 0.00E+00 0.0000 0.0000 7.55E-03 45 * 0.00 0.000 0.018 0.1971 0.0000 0.0000 0.00E+00 0.0000 0.0000 7.56E-03 46 * * 0.10 0.000 0.033 0.1971 0.0000 0.0000 0.00E+00 0.0000 0.0000 7.65E-03 47 * * 0.00 0.000 0.040 0.1971 0.0000 0.0000 0.00E+00 0.0000 0.0000 7.82E-03 48 * * 0.00 0.000 0.027 0.1971 0.0000 0.0000 0.00E+00 0.0000 0.0000 8.16E-03 49 * 0.00 0.000 0.000 0.1971 0.0000 0.0000 0.00E+00 0.0000 0.0000 8.52E-03 50 * * 0.60 0.000 0.017 0.1971 0.0000 0.0000 0.00E+00 0.0000 0.0000 8.77E-03 51 * * 0.00 0.000 0.011 0.1971 0.0000 0.0000 0.00E+00 0.0000 0.0000 8.89E-03 52 * * 0.00 0.000 0.012 0.1971 0.0000 0.0000 0.00E+00 0.0000 0.0000 8.90E-03 53 * * 0.00 0.000 0.016 0.1971 0.0000 0.0000 0.00E+00 0.0000 0.0000 8.82E-03 54 * * 0.20 0.000 0.000 0.1971 0.0000 0.0000 0.00E+00 0.0000 0.0000 8.69E-03 55 * * 0.10 0.000 0.016 0.1971 0.0000 0.0000 0.00E+00 0.0000 0.0000 8.52E-03 56 * * 0.20 0.000 0.018 0.1971 0.0000 0.0000 0.00E+00 0.0000 0.0000 8.31E-03 57 * * 0.00 0.000 0.021 0.1971 0.0000 0.0000 0.00E+00 0.0000 0.0000 8.09E-03 58 * * 0.00 0.000 0.017 0.1971 0.0000 0.0000 0.00E+00 0.0000 0.0000 7.86E-03 59 * * 0.00 0.000 0.018 0.1971 0.0000 0.0000 0.00E+00 0.0000 0.0000 7.63E-03 60 * * 0.00 0.000 0.020 0.1971 0.0000 0.0000 0.00E+00 0.0000 0.0000 7.41E-03 61 * 0.00 0.000 0.029 0.1971 0.0000 0.0000 0.00E+00 0.0000 0.0000 7.19E-03 62 * 0.00 0.018 0.007 0.2541 0.0000 0.0000 0.00E+00 0.0000 0.0000 6.99E-03 Page 91 of 128 63 * * 0.20 0.000 0.017 0.2541 0.0000 0.0000 0.00E+00 0.0000 0.0000 6.79E-03 64 * * 0.00 0.000 0.017 0.2541 0.0000 0.0000 0.00E+00 0.0000 0.0000 6.62E-03 65 * * 0.00 0.000 0.020 0.2541 0.0000 0.0000 0.00E+00 0.0000 0.0000 6.46E-03 66 * * 0.00 0.000 0.025 0.2541 0.0000 0.0000 0.00E+00 0.0000 0.0000 6.32E-03 67 * * 0.00 0.000 0.030 0.2541 0.0000 0.0000 0.00E+00 0.0000 0.0000 6.20E-03 68 * 0.00 0.010 0.021 0.2801 0.0000 0.0000 0.00E+00 0.0000 0.0000 6.09E-03 69 * 0.00 0.017 0.021 0.3040 0.0000 0.0000 0.00E+00 0.0000 0.0000 6.01E-03 70 * 0.10 0.072 0.000 0.3378 0.0000 0.0000 0.00E+00 0.0000 0.0000 5.94E-03 71 * 0.00 0.109 0.010 0.3603 0.0000 0.0000 0.00E+00 0.0000 0.0000 5.90E-03 72 * 0.00 0.258 0.053 0.3638 0.0000 0.0000 0.00E+00 0.0000 0.0000 6.08E-03 73 * 0.40 0.340 0.006 0.3818 0.0000 0.0000 0.00E+00 0.0000 0.0000 6.32E-03 74 * * 0.10 0.000 0.077 0.3818 0.0000 0.0000 0.00E+00 0.0000 0.0000 6.50E-03 75 * * 0.00 0.000 0.023 0.3818 0.0000 0.0000 0.00E+00 0.0000 0.0000 6.63E-03 76 * * 0.20 0.000 0.031 0.3818 0.0000 0.0000 0.00E+00 0.0000 0.0000 6.72E-03 77 * * 0.20 0.000 0.020 0.3818 0.0000 0.0000 0.00E+00 0.0000 0.0000 6.73E-03 78 * * 0.00 0.000 0.025 0.3818 0.0000 0.0000 0.00E+00 0.0000 0.0000 6.49E-03 79 * * 0.00 0.000 0.031 0.3818 0.0000 0.0000 0.00E+00 0.0000 0.0000 6.62E-03 80 * 0.00 0.252 0.026 0.3871 0.0000 0.0000 0.00E+00 0.0000 0.0000 6.91E-03 81 * 0.00 0.000 0.000 0.3871 0.0000 0.0000 0.00E+00 0.0000 0.0000 7.14E-03 82 * 0.10 0.068 0.005 0.3958 0.0000 0.0000 0.00E+00 0.0000 0.0000 7.17E-03 83 * 0.00 0.000 0.000 0.3958 0.0000 0.0000 0.00E+00 0.0000 0.0000 6.81E-03 84 * * 0.00 0.000 0.000 0.3958 0.0000 0.0000 0.00E+00 0.0000 0.0000 6.47E-03 85 * * 0.00 0.000 0.000 0.3958 0.0000 0.0000 0.00E+00 0.0000 0.0000 6.21E-03 86 * * 0.00 0.000 0.000 0.3958 0.0000 0.0000 0.00E+00 0.0000 0.0000 6.03E-03 87 * 0.00 0.000 0.000 0.3958 0.0000 0.0000 0.00E+00 0.0000 0.0000 5.91E-03 88 * 0.00 0.000 0.000 0.3958 0.0000 0.0000 0.00E+00 0.0000 0.0000 5.68E-03 89 * 0.00 0.000 0.000 0.3958 0.0000 0.0000 0.00E+00 0.0000 0.0000 5.52E-03 90 * 0.00 0.000 0.000 0.3958 0.0000 0.0000 0.00E+00 0.0000 0.0000 5.56E-03 91 * 0.00 0.000 0.000 0.3958 0.0000 0.0000 0.00E+00 0.0000 0.0000 5.74E-03 92 0.00 0.000 0.068 0.3390 1.5317 0.0000 1.02E-01 0.0000 0.0000 6.02E-03 93 0.00 0.000 0.010 0.2915 1.4429 0.0000 1.32E-01 0.0000 0.0000 6.36E-03 94 0.00 0.000 0.010 0.2453 0.8392 0.0000 1.28E-01 0.0000 0.0000 6.58E-03 95 0.00 0.000 0.010 0.2046 0.2487 0.0000 1.12E-01 0.0000 0.0000 6.72E-03 96 0.00 0.000 0.010 0.1995 0.0033 0.0000 5.08E-03 0.0000 0.0000 6.88E-03 97 0.30 0.000 0.015 0.2842 0.0005 0.0000 3.06E-02 0.0000 0.0000 7.06E-03 Page 92 of 128 98 0.10 0.000 0.086 0.2473 0.2706 0.0000 1.24E-01 0.0000 0.0000 6.54E-03 99 0.00 0.000 0.135 0.1895 0.0376 0.0000 3.82E-02 0.0000 0.0000 7.03E-03 100 0.00 0.000 0.090 0.1595 0.0000 0.0000 0.00E+00 0.0000 0.0000 7.92E-03 101 0.00 0.000 0.107 0.1236 0.0000 0.0000 0.00E+00 0.0000 0.0000 8.10E-03 102 0.20 0.000 0.060 0.1702 0.0000 0.0000 0.00E+00 0.0000 0.0000 8.28E-03 103 * 0.00 0.000 0.000 0.1702 0.0000 0.0000 0.00E+00 0.0000 0.0000 8.47E-03 104 * 0.00 0.000 0.053 0.1525 0.0000 0.0000 0.00E+00 0.0000 0.0000 8.37E-03 105 0.00 0.000 0.046 0.1372 0.0000 0.0000 0.00E+00 0.0000 0.0000 7.68E-03 106 0.00 0.000 0.040 0.1238 0.0000 0.0000 0.00E+00 0.0000 0.0000 8.81E-03 107 * 0.20 0.000 0.060 0.1303 0.0000 0.0000 0.00E+00 0.0000 0.0000 9.24E-03 108 * 0.00 0.000 0.121 0.1301 0.0000 0.0000 0.00E+00 0.0000 0.0000 9.23E-03 109 0.00 0.000 0.033 0.1193 0.0000 0.0000 0.00E+00 0.0000 0.0000 9.03E-03 110 0.00 0.000 0.008 0.1166 0.0000 0.0000 0.00E+00 0.0000 0.0000 8.83E-03 111 0.00 0.000 0.001 0.1161 0.0000 0.0000 0.00E+00 0.0000 0.0000 9.12E-03 112 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 9.38E-03 113 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 8.87E-03 114 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 8.60E-03 115 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 9.35E-03 116 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.01E-02 117 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.08E-02 118 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.14E-02 119 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.19E-02 120 0.10 0.000 0.014 0.1446 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.24E-02 121 0.30 0.000 0.020 0.2381 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.33E-02 122 0.60 0.000 0.025 0.4080 0.5320 0.0000 6.48E-02 0.0000 0.0000 1.41E-02 123 0.10 0.000 0.142 0.3486 1.9880 0.0000 1.36E-01 0.0000 0.0000 1.44E-02 124 0.00 0.000 0.097 0.2724 1.3026 0.0000 1.31E-01 0.0000 0.0000 1.45E-02 125 0.00 0.000 0.130 0.1867 0.6377 0.0000 1.27E-01 0.0000 0.0000 1.36E-02 126 0.00 0.000 0.114 0.1308 0.0977 0.0000 5.38E-02 0.0000 0.0000 1.50E-02 127 0.00 0.000 0.044 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.52E-02 128 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.31E-02 129 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.27E-02 130 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.29E-02 131 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.31E-02 132 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.33E-02 Page 93 of 128 133 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.35E-02 134 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.44E-02 135 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.47E-02 136 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.42E-02 137 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.33E-02 138 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.33E-02 139 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.34E-02 140 0.10 0.000 0.016 0.1441 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.35E-02 141 0.00 0.000 0.017 0.1383 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.36E-02 142 0.00 0.000 0.019 0.1319 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.45E-02 143 0.00 0.000 0.020 0.1253 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.53E-02 144 0.10 0.000 0.024 0.1506 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.57E-02 145 0.00 0.000 0.020 0.1438 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.58E-02 146 0.00 0.000 0.019 0.1374 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.57E-02 147 0.00 0.000 0.019 0.1312 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.54E-02 148 0.00 0.000 0.018 0.1252 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.49E-02 149 0.00 0.000 0.020 0.1187 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.43E-02 150 0.00 0.000 0.007 0.1163 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.38E-02 151 0.00 0.000 0.001 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.32E-02 152 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.27E-02 153 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.22E-02 154 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.19E-02 155 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.16E-02 156 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.14E-02 157 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.13E-02 158 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.13E-02 159 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.13E-02 160 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.13E-02 161 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.14E-02 162 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.15E-02 163 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.14E-02 164 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.14E-02 165 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.15E-02 166 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.16E-02 167 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.16E-02 Page 94 of 128 168 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.15E-02 169 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.12E-02 170 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.09E-02 171 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.06E-02 172 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.02E-02 173 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 9.86E-03 174 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 9.51E-03 175 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 9.17E-03 176 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 8.86E-03 177 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 8.57E-03 178 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 8.38E-03 179 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 8.08E-03 180 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 7.65E-03 181 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 7.32E-03 182 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 7.09E-03 183 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 6.93E-03 184 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 6.77E-03 185 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 6.58E-03 186 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 6.33E-03 187 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 6.03E-03 188 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 5.69E-03 189 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 5.25E-03 190 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 4.80E-03 191 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 4.38E-03 192 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 4.03E-03 193 0.10 0.000 0.010 0.1459 0.0000 0.0000 0.00E+00 0.0000 0.0000 3.78E-03 194 0.00 0.000 0.009 0.1428 0.0000 0.0000 0.00E+00 0.0000 0.0000 3.60E-03 195 0.10 0.000 0.017 0.1706 0.0000 0.0000 0.00E+00 0.0000 0.0000 3.39E-03 196 0.00 0.000 0.013 0.1662 0.0000 0.0000 0.00E+00 0.0000 0.0000 3.19E-03 197 0.00 0.000 0.012 0.1621 0.0000 0.0000 0.00E+00 0.0000 0.0000 2.86E-03 198 0.00 0.000 0.013 0.1577 0.0000 0.0000 0.00E+00 0.0000 0.0000 3.48E-03 199 0.00 0.000 0.015 0.1529 0.0000 0.0000 0.00E+00 0.0000 0.0000 2.98E-03 200 0.00 0.000 0.015 0.1477 0.0000 0.0000 0.00E+00 0.0000 0.0000 2.56E-03 201 0.00 0.000 0.017 0.1422 0.0000 0.0000 0.00E+00 0.0000 0.0000 2.59E-03 202 0.00 0.000 0.018 0.1363 0.0000 0.0000 0.00E+00 0.0000 0.0000 2.78E-03 Page 95 of 128 203 0.20 0.000 0.025 0.1948 0.0000 0.0000 0.00E+00 0.0000 0.0000 2.98E-03 204 0.00 0.000 0.018 0.1888 0.0000 0.0000 0.00E+00 0.0000 0.0000 3.11E-03 205 0.00 0.000 0.022 0.1814 0.0000 0.0000 0.00E+00 0.0000 0.0000 3.15E-03 206 0.00 0.000 0.024 0.1736 0.0000 0.0000 0.00E+00 0.0000 0.0000 3.10E-03 207 0.10 0.000 0.031 0.1965 0.0000 0.0000 0.00E+00 0.0000 0.0000 2.98E-03 208 0.00 0.000 0.029 0.1870 0.0000 0.0000 0.00E+00 0.0000 0.0000 2.81E-03 209 0.00 0.000 0.028 0.1778 0.0000 0.0000 0.00E+00 0.0000 0.0000 2.62E-03 210 0.00 0.000 0.033 0.1668 0.0000 0.0000 0.00E+00 0.0000 0.0000 2.43E-03 211 0.00 0.000 0.025 0.1586 0.0000 0.0000 0.00E+00 0.0000 0.0000 2.25E-03 212 0.00 0.000 0.025 0.1501 0.0000 0.0000 0.00E+00 0.0000 0.0000 2.11E-03 213 0.00 0.000 0.037 0.1376 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.83E-03 214 0.90 0.000 0.045 0.4118 0.3377 0.0000 3.29E-02 0.0000 0.0000 1.91E-03 215 0.10 0.000 0.052 0.3820 2.2400 0.0000 1.38E-01 0.0000 0.0000 2.17E-03 216 0.00 0.000 0.049 0.3208 1.7566 0.0000 1.34E-01 0.0000 0.0000 2.36E-03 217 0.00 0.000 0.044 0.2628 1.1162 0.0000 1.30E-01 0.0000 0.0000 2.42E-03 218 0.00 0.000 0.037 0.2084 0.5091 0.0000 1.26E-01 0.0000 0.0000 2.40E-03 219 0.00 0.000 0.059 0.1753 0.0512 0.0000 4.01E-02 0.0000 0.0000 2.51E-03 220 0.00 0.000 0.066 0.1534 0.0000 0.0000 0.00E+00 0.0000 0.0000 2.26E-03 221 0.00 0.000 0.053 0.1357 0.0000 0.0000 0.00E+00 0.0000 0.0000 2.24E-03 222 0.00 0.000 0.039 0.1228 0.0000 0.0000 0.00E+00 0.0000 0.0000 2.65E-03 223 0.00 0.000 0.019 0.1165 0.0000 0.0000 0.00E+00 0.0000 0.0000 3.26E-03 224 0.00 0.000 0.001 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 3.92E-03 225 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 4.52E-03 226 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 5.00E-03 227 0.10 0.000 0.032 0.1387 0.0000 0.0000 0.00E+00 0.0000 0.0000 4.86E-03 228 0.00 0.000 0.027 0.1296 0.0000 0.0000 0.00E+00 0.0000 0.0000 6.04E-03 229 0.10 0.000 0.059 0.1432 0.0000 0.0000 0.00E+00 0.0000 0.0000 6.58E-03 230 0.00 0.000 0.038 0.1305 0.0000 0.0000 0.00E+00 0.0000 0.0000 6.23E-03 231 0.00 0.000 0.029 0.1207 0.0000 0.0000 0.00E+00 0.0000 0.0000 5.91E-03 232 0.00 0.000 0.012 0.1168 0.0000 0.0000 0.00E+00 0.0000 0.0000 5.77E-03 233 0.00 0.000 0.002 0.1162 0.0000 0.0000 0.00E+00 0.0000 0.0000 5.75E-03 234 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 5.82E-03 235 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 5.97E-03 236 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 6.19E-03 237 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 6.45E-03 Page 96 of 128 238 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 6.75E-03 239 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 7.09E-03 240 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 7.45E-03 241 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 7.82E-03 242 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 8.20E-03 243 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 8.58E-03 244 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 8.94E-03 245 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 9.28E-03 246 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 9.60E-03 247 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 9.89E-03 248 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 9.56E-03 249 0.10 0.000 0.027 0.1404 0.0000 0.0000 0.00E+00 0.0000 0.0000 9.42E-03 250 0.00 0.000 0.017 0.1348 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.11E-02 251 0.00 0.000 0.026 0.1260 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.22E-02 252 0.00 0.000 0.028 0.1168 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.23E-02 253 0.00 0.000 0.002 0.1162 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.16E-02 254 0.00 0.000 0.000 0.1161 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.07E-02 255 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 9.92E-03 256 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 9.40E-03 257 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 9.22E-03 258 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 9.33E-03 259 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 9.61E-03 260 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 9.97E-03 261 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.03E-02 262 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.05E-02 263 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.06E-02 264 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.05E-02 265 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.03E-02 266 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 9.99E-03 267 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 9.60E-03 268 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 9.17E-03 269 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 8.73E-03 270 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 8.31E-03 271 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 7.93E-03 272 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 7.61E-03 Page 97 of 128 273 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 7.34E-03 274 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 7.13E-03 275 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 6.98E-03 276 0.20 0.000 0.014 0.1781 0.0000 0.0000 0.00E+00 0.0000 0.0000 6.88E-03 277 0.20 0.000 0.016 0.2396 0.0000 0.0000 0.00E+00 0.0000 0.0000 6.82E-03 278 0.10 0.000 0.015 0.2433 0.0521 0.0000 7.34E-02 0.0000 0.0000 6.79E-03 279 0.40 0.000 0.015 0.3415 0.2659 0.0000 9.01E-02 0.0000 0.0000 6.78E-03 280 0.30 0.000 0.034 0.3861 1.3880 0.0000 1.32E-01 0.0000 0.0000 6.77E-03 281 0.10 0.000 0.075 0.3498 1.7907 0.0000 1.35E-01 0.0000 0.0000 6.76E-03 282 0.10 0.000 0.076 0.3138 1.4131 0.0000 1.32E-01 0.0000 0.0000 5.74E-03 283 0.50 0.000 0.074 0.4121 1.2698 0.0000 1.31E-01 0.0000 0.0000 8.34E-03 284 0.20 0.000 0.075 0.4076 2.3122 0.0000 1.38E-01 0.0000 0.0000 7.77E-03 285 0.00 0.000 0.053 0.3444 1.9991 0.0000 1.36E-01 0.0000 0.0000 6.46E-03 286 0.00 0.000 0.068 0.2780 1.3343 0.0000 1.32E-01 0.0000 0.0000 5.47E-03 287 * 0.00 0.000 0.046 0.2202 0.6802 0.0000 1.27E-01 0.0000 0.0000 5.07E-03 288 * 0.00 0.000 0.022 0.1864 0.1446 0.0000 7.98E-02 0.0000 0.0000 5.66E-03 289 * 0.00 0.000 0.031 0.1756 0.0015 0.0000 1.54E-03 0.0000 0.0000 5.26E-03 290 0.10 0.000 0.064 0.1875 0.0000 0.0000 0.00E+00 0.0000 0.0000 5.59E-03 291 0.00 0.000 0.056 0.1687 0.0000 0.0000 0.00E+00 0.0000 0.0000 6.04E-03 292 0.00 0.000 0.029 0.1590 0.0000 0.0000 0.00E+00 0.0000 0.0000 6.57E-03 293 0.00 0.000 0.065 0.1374 0.0000 0.0000 0.00E+00 0.0000 0.0000 6.78E-03 294 0.10 0.000 0.073 0.1466 0.0000 0.0000 0.00E+00 0.0000 0.0000 6.38E-03 295 0.10 0.000 0.058 0.1604 0.0000 0.0000 0.00E+00 0.0000 0.0000 5.68E-03 296 0.00 0.000 0.046 0.1450 0.0000 0.0000 0.00E+00 0.0000 0.0000 5.63E-03 297 0.00 0.000 0.049 0.1286 0.0000 0.0000 0.00E+00 0.0000 0.0000 5.37E-03 298 0.00 0.000 0.031 0.1182 0.0000 0.0000 0.00E+00 0.0000 0.0000 4.68E-03 299 0.00 0.000 0.006 0.1164 0.0000 0.0000 0.00E+00 0.0000 0.0000 3.71E-03 300 0.00 0.000 0.001 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 2.71E-03 301 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.93E-03 302 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.53E-03 303 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.55E-03 304 * 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.96E-03 305 0.10 0.000 0.017 0.1437 0.0000 0.0000 0.00E+00 0.0000 0.0000 2.48E-03 306 0.00 0.000 0.035 0.1321 0.0000 0.0000 0.00E+00 0.0000 0.0000 3.35E-03 307 0.00 0.000 0.035 0.1203 0.0000 0.0000 0.00E+00 0.0000 0.0000 4.71E-03 Page 98 of 128 308 0.00 0.000 0.012 0.1164 0.0000 0.0000 0.00E+00 0.0000 0.0000 5.41E-03 309 0.00 0.000 0.001 0.1161 0.0000 0.0000 0.00E+00 0.0000 0.0000 5.72E-03 310 * 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 5.83E-03 311 * 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 5.22E-03 312 * 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 4.83E-03 313 * 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 4.53E-03 314 * 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 4.11E-03 315 * 0.10 0.000 0.014 0.1226 0.0000 0.0000 0.00E+00 0.0000 0.0000 3.57E-03 316 * 0.00 0.000 0.025 0.1291 0.0000 0.0000 0.00E+00 0.0000 0.0000 2.95E-03 317 * 0.00 0.000 0.026 0.1273 0.0000 0.0000 0.00E+00 0.0000 0.0000 2.37E-03 318 0.00 0.000 0.018 0.1213 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.43E-03 319 0.00 0.000 0.012 0.1171 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.19E-03 320 0.00 0.000 0.003 0.1163 0.0000 0.0000 0.00E+00 0.0000 0.0000 2.18E-03 321 0.00 0.000 0.001 0.1161 0.0000 0.0000 0.00E+00 0.0000 0.0000 2.92E-03 322 * 0.00 0.000 0.000 0.1161 0.0000 0.0000 0.00E+00 0.0000 0.0000 3.12E-03 323 * 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 2.93E-03 324 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 2.64E-03 325 * 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 2.48E-03 326 * * 0.40 0.000 0.018 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 2.55E-03 327 * * 0.00 0.000 0.018 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 2.86E-03 328 * * 0.20 0.000 0.014 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 3.36E-03 329 * * 0.00 0.000 0.014 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 3.96E-03 330 * * 0.00 0.000 0.017 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 4.56E-03 331 * * 0.00 0.000 0.019 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 5.08E-03 332 * 0.20 0.014 0.000 0.1745 0.0000 0.0000 0.00E+00 0.0000 0.0000 5.46E-03 333 * 0.60 0.361 0.000 0.2637 0.0000 0.0000 0.00E+00 0.0000 0.0000 5.68E-03 334 * * 0.60 0.000 0.018 0.2637 0.0000 0.0000 0.00E+00 0.0000 0.0000 5.70E-03 335 * * 0.00 0.000 0.016 0.2637 0.0000 0.0000 0.00E+00 0.0000 0.0000 5.74E-03 336 * * 0.30 0.000 0.011 0.2637 0.0000 0.0000 0.00E+00 0.0000 0.0000 5.71E-03 337 * * 0.00 0.000 0.008 0.2637 0.0000 0.0000 0.00E+00 0.0000 0.0000 5.03E-03 338 * * 0.00 0.000 0.010 0.2637 0.0000 0.0000 0.00E+00 0.0000 0.0000 4.01E-03 339 * * 0.00 0.000 0.016 0.2637 0.0000 0.0000 0.00E+00 0.0000 0.0000 2.88E-03 340 * * 0.00 0.000 0.017 0.2637 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.78E-03 341 * * 0.00 0.000 0.017 0.2637 0.0000 0.0000 0.00E+00 0.0000 0.0000 7.92E-04 342 * * 0.00 0.000 0.016 0.2637 0.0000 0.0000 0.00E+00 0.0000 0.0000 7.39E-05 Page 99 of 128 343 * * 0.00 0.000 0.015 0.2637 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 344 * * 0.00 0.000 0.018 0.2637 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 345 * * 0.00 0.000 0.017 0.2637 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 346 * * 0.10 0.000 0.016 0.2637 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 347 * * 0.00 0.000 0.012 0.2637 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 348 * * 0.00 0.000 0.018 0.2637 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 349 * * 0.00 0.000 0.020 0.2637 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 350 * * 0.00 0.000 0.020 0.2637 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 351 * * 0.00 0.000 0.019 0.2637 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 352 * * 0.00 0.000 0.016 0.2637 0.0000 0.0000 0.00E+00 0.0000 0.0000 0.00E+00 353 * * 0.00 0.000 0.017 0.2637 0.0000 0.0000 0.00E+00 0.0000 0.0000 2.05E-04 354 * * 0.00 0.000 0.020 0.2637 0.0000 0.0000 0.00E+00 0.0000 0.0000 7.40E-04 355 * 0.00 0.000 0.020 0.2637 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.29E-03 356 * * 0.00 0.000 0.013 0.2637 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.83E-03 357 * * 0.00 0.000 0.018 0.2637 0.0000 0.0000 0.00E+00 0.0000 0.0000 2.38E-03 358 * * 0.10 0.000 0.000 0.2637 0.0000 0.0000 0.00E+00 0.0000 0.0000 2.91E-03 359 * * 0.10 0.000 0.000 0.2637 0.0000 0.0000 0.00E+00 0.0000 0.0000 3.50E-03 360 * * 0.10 0.000 0.011 0.2637 0.0000 0.0000 0.00E+00 0.0000 0.0000 4.18E-03 361 * * 0.00 0.000 0.009 0.2637 0.0000 0.0000 0.00E+00 0.0000 0.0000 4.61E-03 362 * * 0.00 0.000 0.008 0.2637 0.0000 0.0000 0.00E+00 0.0000 0.0000 4.95E-03 363 * * 0.00 0.000 0.009 0.2637 0.0000 0.0000 0.00E+00 0.0000 0.0000 5.39E-03 364 * * 0.00 0.000 0.000 0.2637 0.0000 0.0000 0.00E+00 0.0000 0.0000 5.74E-03 365 * * 0.20 0.000 0.008 0.2637 0.0000 0.0000 0.00E+00 0.0000 0.0000 5.88E-03 * = Frozen (air or soil) inches cubic feet percent Precipitation 13.40 3,404,940.0 100.00 Runoff 1.776 451,326.4 13.26 Evapotranspiration 6.270 1,593,080.9 46.79 Percolation/Leakage through Layer 2 3.368938 856,047.2 25.14 Average Head on Top of Layer 2 0.0783 ------ Percolation/Leakage through Layer 12 2.852907 724,923.7 21.29 Annual Totals for Year 8 Page 100 of 128 Change in Water Storage 2.5014 635,609.1 18.67 Soil Water at Start of Year 234.4804 #########1749.85 Soil Water at End of Year 235.4395 #########1757.01 Snow Water at Start of Year 0.0000 0.0000 0.00 Snow Water at End of Year 1.5423 391,900.7 11.51 Annual Water Budget Balance 0.0000 0.0000 0.00 Page 101 of 128 Daily Output for Year 9 Column key:Head #1: drainage from Layer 2 Title:Long Valley Landfill Simulated On:Leak #1: leakage thru Layer 2 Leak #2: leakage thru Layer 12 Day Rain Runoff ET Evap. Zone Water Head #1 Drain #1 Leak #1 Head #2 Drain #2 Leak #2 Air Soil (inches)(inches)(inches)(in/in)(inches)(inches)(inches)(inches)(inches)(inches) 1 * * 0.00 0.000 0.009 0.2637 0.0000 0.0000 0.00E+00 0.0000 0.0000 6.61E-03 2 * * 0.00 0.000 0.014 0.2637 0.0000 0.0000 0.00E+00 0.0000 0.0000 7.18E-03 3 * * 0.00 0.000 0.000 0.2637 0.0000 0.0000 0.00E+00 0.0000 0.0000 7.77E-03 4 * * 0.00 0.000 0.000 0.2637 0.0000 0.0000 0.00E+00 0.0000 0.0000 8.07E-03 5 * * 0.10 0.000 0.000 0.2637 0.0000 0.0000 0.00E+00 0.0000 0.0000 8.33E-03 6 * * 0.10 0.000 0.000 0.2637 0.0000 0.0000 0.00E+00 0.0000 0.0000 8.79E-03 7 * * 0.00 0.000 0.023 0.2637 0.0000 0.0000 0.00E+00 0.0000 0.0000 9.34E-03 8 * * 0.00 0.000 0.023 0.2637 0.0000 0.0000 0.00E+00 0.0000 0.0000 9.90E-03 9 * * 0.00 0.000 0.026 0.2637 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.04E-02 10 * * 0.00 0.000 0.023 0.2637 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.09E-02 11 * * 0.00 0.000 0.019 0.2637 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.13E-02 12 * * 0.00 0.000 0.019 0.2637 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.17E-02 13 * * 0.00 0.000 0.022 0.2637 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.19E-02 14 * * 0.00 0.000 0.022 0.2637 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.21E-02 15 * * 0.20 0.000 0.000 0.2637 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.23E-02 16 * * 0.10 0.000 0.000 0.2637 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.24E-02 17 * * 0.50 0.000 0.000 0.2637 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.25E-02 18 * * 0.20 0.000 0.017 0.2637 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.26E-02 19 * * 0.00 0.000 0.019 0.2637 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.26E-02 20 * * 0.00 0.000 0.025 0.2637 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.27E-02 21 * * 0.20 0.000 0.000 0.2637 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.28E-02 22 * * 0.00 0.000 0.014 0.2637 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.28E-02 23 * * 0.00 0.000 0.015 0.2637 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.29E-02 24 * * 0.00 0.000 0.023 0.2637 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.30E-02 25 * * 0.00 0.000 0.016 0.2637 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.26E-02 26 * * 0.00 0.000 0.021 0.2637 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.26E-02 27 * * 0.00 0.000 0.024 0.2637 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.31E-02 7/19/2024 11:05 Freezing Status* Page 102 of 128 28 * * 0.00 0.000 0.022 0.2637 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.37E-02 29 * * 0.00 0.000 0.021 0.2637 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.42E-02 30 * * 0.00 0.000 0.020 0.2637 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.48E-02 31 * * 0.00 0.000 0.023 0.2637 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.53E-02 32 * * 0.00 0.000 0.025 0.2637 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.53E-02 33 * * 0.10 0.000 0.000 0.2637 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.50E-02 34 * * 0.20 0.000 0.000 0.2637 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.46E-02 35 * * 0.00 0.000 0.025 0.2637 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.42E-02 36 * * 0.70 0.000 0.023 0.2637 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.38E-02 37 * * 0.20 0.000 0.015 0.2637 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.35E-02 38 * * 0.10 0.000 0.012 0.2637 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.33E-02 39 * * 0.00 0.000 0.014 0.2637 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.32E-02 40 * * 0.00 0.000 0.017 0.2637 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.32E-02 41 * * 0.30 0.000 0.015 0.2637 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.33E-02 42 * * 0.00 0.000 0.014 0.2637 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.34E-02 43 * * 0.00 0.000 0.017 0.2637 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.36E-02 44 * * 0.10 0.000 0.000 0.2637 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.39E-02 45 * 0.50 0.098 0.000 0.2969 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.44E-02 46 * * 0.20 0.010 0.022 0.3041 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.44E-02 47 * * 0.20 0.000 0.014 0.3041 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.43E-02 48 * * 0.00 0.000 0.012 0.3041 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.41E-02 49 * * 0.00 0.000 0.013 0.3041 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.40E-02 50 * * 0.00 0.000 0.012 0.3041 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.39E-02 51 * * 0.20 0.000 0.013 0.3041 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.38E-02 52 * * 0.20 0.000 0.000 0.3041 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.36E-02 53 * * 0.00 0.000 0.013 0.3041 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.35E-02 54 * * 0.00 0.000 0.014 0.3041 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.34E-02 55 * * 0.00 0.000 0.016 0.3041 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.33E-02 56 * * 0.00 0.000 0.021 0.3041 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.31E-02 57 * * 0.00 0.000 0.024 0.3041 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.30E-02 58 * * 0.00 0.000 0.025 0.3041 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.28E-02 59 * * 0.10 0.000 0.000 0.3041 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.26E-02 60 * 0.10 0.146 0.000 0.3296 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.23E-02 61 * 0.50 0.689 0.000 0.3532 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.20E-02 62 * 0.40 0.549 0.000 0.3696 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.16E-02 Page 103 of 128 63 * * 0.00 0.036 0.016 0.3743 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.12E-02 64 * * 0.00 0.000 0.023 0.3743 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.08E-02 65 * 0.50 0.571 0.000 0.3872 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.03E-02 66 * 0.00 0.267 0.000 0.3974 0.0000 0.0000 0.00E+00 0.0000 0.0000 9.87E-03 67 * * 0.20 0.027 0.025 0.3974 0.0000 0.0000 0.00E+00 0.0000 0.0000 9.40E-03 68 * * 0.00 0.000 0.027 0.3974 0.0000 0.0000 0.00E+00 0.0000 0.0000 8.93E-03 69 * * 0.00 0.000 0.028 0.3974 0.0000 0.0000 0.00E+00 0.0000 0.0000 8.46E-03 70 * 0.00 0.000 0.033 0.3974 0.0000 0.0000 0.00E+00 0.0000 0.0000 8.00E-03 71 * 0.10 0.383 0.000 0.4054 0.0000 0.0000 0.00E+00 0.0000 0.0000 7.56E-03 72 * * 0.10 0.034 0.021 0.4054 0.0000 0.0000 0.00E+00 0.0000 0.0000 7.15E-03 73 * * 0.00 0.000 0.022 0.4054 0.0000 0.0000 0.00E+00 0.0000 0.0000 6.76E-03 74 * * 0.00 0.000 0.022 0.4054 0.0000 0.0000 0.00E+00 0.0000 0.0000 6.40E-03 75 * * 0.00 0.000 0.028 0.4054 0.0000 0.0000 0.00E+00 0.0000 0.0000 6.08E-03 76 * * 0.00 0.000 0.032 0.4054 0.0000 0.0000 0.00E+00 0.0000 0.0000 5.79E-03 77 * * 0.00 0.000 0.032 0.4054 0.0000 0.0000 0.00E+00 0.0000 0.0000 5.56E-03 78 * 0.00 0.000 0.035 0.4054 0.0000 0.0000 0.00E+00 0.0000 0.0000 5.37E-03 79 * 0.00 0.000 0.033 0.4054 0.0000 0.0000 0.00E+00 0.0000 0.0000 5.23E-03 80 * * 0.30 0.000 0.000 0.4054 0.0000 0.0000 0.00E+00 0.0000 0.0000 5.16E-03 81 * * 0.00 0.000 0.028 0.4054 0.0000 0.0000 0.00E+00 0.0000 0.0000 5.14E-03 82 * 0.00 0.193 0.009 0.4086 0.0000 0.0000 0.00E+00 0.0000 0.0000 5.18E-03 83 * 0.00 0.120 0.018 0.4086 0.0000 0.0000 0.00E+00 0.0000 0.0000 5.28E-03 84 * * 0.00 0.000 0.033 0.4086 0.0000 0.0000 0.00E+00 0.0000 0.0000 5.45E-03 85 * 0.00 0.132 0.018 0.4088 0.0000 0.0000 0.00E+00 0.0000 0.0000 5.67E-03 86 * 0.00 0.772 0.000 0.4153 0.0000 0.0000 0.00E+00 0.0000 0.0000 5.95E-03 87 * 0.00 0.495 0.000 0.4217 0.0000 0.0000 0.00E+00 0.0000 0.0000 6.28E-03 88 * * 0.00 0.000 0.032 0.4217 0.0000 0.0000 0.00E+00 0.0000 0.0000 6.66E-03 89 * * 0.00 0.000 0.030 0.4217 0.0000 0.0000 0.00E+00 0.0000 0.0000 7.07E-03 90 * * 0.00 0.000 0.033 0.4217 0.0000 0.0000 0.00E+00 0.0000 0.0000 7.50E-03 91 * * 0.00 0.000 0.040 0.4217 0.0000 0.0000 0.00E+00 0.0000 0.0000 7.95E-03 92 * 0.10 0.235 0.000 0.4245 0.0040 0.0000 7.74E-03 0.0000 0.0000 8.41E-03 93 * 0.30 0.722 0.000 0.4245 0.0083 0.0000 1.53E-02 0.0000 0.0000 8.86E-03 94 * 0.00 0.390 0.011 0.4245 0.0025 0.0000 4.60E-03 0.0000 0.0000 9.37E-03 95 * 0.00 0.615 0.007 0.4245 0.0046 0.0000 8.59E-03 0.0000 0.0000 9.48E-03 96 * 0.00 0.094 0.074 0.4245 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.01E-02 97 * 0.00 0.000 0.000 0.4245 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.05E-02 Page 104 of 128 98 0.00 0.000 0.123 0.3492 1.6939 0.0000 1.03E-01 0.0000 0.0000 1.13E-02 99 0.30 0.000 0.147 0.3559 1.5757 0.0000 1.33E-01 0.0000 0.0000 9.77E-03 100 * 0.20 0.000 0.074 0.3184 1.4194 0.0000 1.32E-01 0.0000 0.0000 9.64E-03 101 * 0.00 0.000 0.095 0.2794 0.9132 0.0000 1.29E-01 0.0000 0.0000 1.23E-02 102 * * 0.00 0.000 0.000 0.2409 0.3143 0.0000 1.16E-01 0.0000 0.0000 1.35E-02 103 * * 0.00 0.000 0.000 0.2409 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.22E-02 104 * 0.00 0.000 0.000 0.2409 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.11E-02 105 * 0.00 0.000 0.000 0.2409 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.04E-02 106 * 0.30 0.079 0.007 0.3122 0.0000 0.0000 0.00E+00 0.0000 0.0000 9.90E-03 107 * 0.00 0.000 0.000 0.3122 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.01E-02 108 * 0.00 0.000 0.000 0.3122 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.06E-02 109 * 0.00 0.000 0.000 0.3122 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.10E-02 110 0.00 0.000 0.110 0.2437 0.5994 0.0000 9.59E-02 0.0000 0.0000 1.10E-02 111 0.00 0.000 0.157 0.1495 0.4520 0.0000 1.26E-01 0.0000 0.0000 1.08E-02 112 0.10 0.000 0.127 0.1382 0.0195 0.0000 6.56E-03 0.0000 0.0000 1.02E-02 113 0.00 0.000 0.051 0.1213 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.26E-02 114 0.00 0.000 0.012 0.1172 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.13E-02 115 0.00 0.000 0.003 0.1162 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.01E-02 116 0.10 0.000 0.049 0.1331 0.0000 0.0000 0.00E+00 0.0000 0.0000 9.31E-03 117 0.00 0.000 0.040 0.1199 0.0000 0.0000 0.00E+00 0.0000 0.0000 8.24E-03 118 0.00 0.000 0.009 0.1169 0.0000 0.0000 0.00E+00 0.0000 0.0000 7.65E-03 119 0.20 0.000 0.076 0.1584 0.0000 0.0000 0.00E+00 0.0000 0.0000 7.82E-03 120 0.20 0.000 0.108 0.1891 0.0000 0.0000 0.00E+00 0.0000 0.0000 8.33E-03 121 * 0.10 0.000 0.109 0.1862 0.0000 0.0000 0.00E+00 0.0000 0.0000 8.64E-03 122 0.00 0.000 0.078 0.1601 0.0000 0.0000 0.00E+00 0.0000 0.0000 8.65E-03 123 0.00 0.000 0.103 0.1257 0.0000 0.0000 0.00E+00 0.0000 0.0000 8.45E-03 124 0.00 0.000 0.025 0.1173 0.0000 0.0000 0.00E+00 0.0000 0.0000 8.15E-03 125 0.00 0.000 0.004 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 7.85E-03 126 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 7.61E-03 127 0.30 0.000 0.036 0.2040 0.0000 0.0000 0.00E+00 0.0000 0.0000 7.45E-03 128 0.20 0.000 0.043 0.2564 0.0000 0.0000 0.00E+00 0.0000 0.0000 7.38E-03 129 0.10 0.000 0.116 0.2361 0.0378 0.0000 4.42E-02 0.0000 0.0000 7.38E-03 130 0.20 0.000 0.167 0.2429 0.0036 0.0000 1.23E-02 0.0000 0.0000 7.41E-03 131 0.00 0.000 0.164 0.1852 0.0077 0.0000 9.83E-03 0.0000 0.0000 7.46E-03 132 0.00 0.000 0.181 0.1248 0.0000 0.0000 0.00E+00 0.0000 0.0000 6.97E-03 Page 105 of 128 133 0.00 0.000 0.027 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 8.98E-03 134 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 7.98E-03 135 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 6.89E-03 136 0.30 0.000 0.036 0.2040 0.0000 0.0000 0.00E+00 0.0000 0.0000 6.56E-03 137 0.20 0.000 0.043 0.2565 0.0000 0.0000 0.00E+00 0.0000 0.0000 6.89E-03 138 0.00 0.000 0.037 0.2293 0.0347 0.0000 4.48E-02 0.0000 0.0000 7.62E-03 139 0.20 0.000 0.040 0.2694 0.0661 0.0000 3.94E-02 0.0000 0.0000 8.25E-03 140 0.10 0.000 0.104 0.2320 0.1462 0.0000 1.08E-01 0.0000 0.0000 8.72E-03 141 0.40 0.000 0.153 0.2835 0.0799 0.0000 9.24E-02 0.0000 0.0000 8.70E-03 142 * 0.30 0.000 0.068 0.2485 0.3065 0.0000 1.25E-01 0.0000 0.0000 8.53E-03 143 0.00 0.000 0.060 0.2583 0.1497 0.0000 1.23E-01 0.0000 0.0000 8.40E-03 144 0.00 0.000 0.092 0.2157 0.0337 0.0000 3.58E-02 0.0000 0.0000 8.36E-03 145 0.00 0.000 0.183 0.1526 0.0029 0.0000 5.63E-03 0.0000 0.0000 8.43E-03 146 0.00 0.000 0.097 0.1204 0.0000 0.0000 0.00E+00 0.0000 0.0000 9.68E-03 147 1.10 0.003 0.086 0.4462 0.3750 0.0000 3.32E-02 0.0000 0.0000 8.71E-03 148 0.10 0.000 0.182 0.3725 2.3987 0.0000 1.39E-01 0.0000 0.0000 7.68E-03 149 0.20 0.000 0.184 0.3333 1.6134 0.0000 1.33E-01 0.0000 0.0000 8.46E-03 150 0.20 0.000 0.161 0.3031 1.1287 0.0000 1.30E-01 0.0000 0.0000 8.92E-03 151 0.00 0.000 0.181 0.2005 0.6689 0.0000 1.27E-01 0.0000 0.0000 9.26E-03 152 0.00 0.000 0.212 0.1195 0.0842 0.0000 3.11E-02 0.0000 0.0000 1.11E-02 153 0.00 0.000 0.010 0.1161 0.0000 0.0000 0.00E+00 0.0000 0.0000 7.80E-03 154 0.20 0.000 0.093 0.1516 0.0000 0.0000 0.00E+00 0.0000 0.0000 7.98E-03 155 0.00 0.000 0.088 0.1224 0.0000 0.0000 0.00E+00 0.0000 0.0000 8.71E-03 156 0.00 0.000 0.014 0.1176 0.0000 0.0000 0.00E+00 0.0000 0.0000 9.05E-03 157 0.00 0.000 0.004 0.1164 0.0000 0.0000 0.00E+00 0.0000 0.0000 8.82E-03 158 0.00 0.000 0.001 0.1161 0.0000 0.0000 0.00E+00 0.0000 0.0000 8.36E-03 159 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 7.87E-03 160 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 7.45E-03 161 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 7.35E-03 162 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 7.27E-03 163 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 6.91E-03 164 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 6.64E-03 165 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 6.62E-03 166 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 6.85E-03 167 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 7.28E-03 Page 106 of 128 168 0.10 0.000 0.018 0.1433 0.0000 0.0000 0.00E+00 0.0000 0.0000 7.78E-03 169 0.00 0.000 0.019 0.1370 0.0000 0.0000 0.00E+00 0.0000 0.0000 8.28E-03 170 0.00 0.000 0.019 0.1308 0.0000 0.0000 0.00E+00 0.0000 0.0000 8.56E-03 171 0.00 0.000 0.022 0.1233 0.0000 0.0000 0.00E+00 0.0000 0.0000 8.77E-03 172 0.00 0.000 0.019 0.1170 0.0000 0.0000 0.00E+00 0.0000 0.0000 9.36E-03 173 0.00 0.000 0.002 0.1162 0.0000 0.0000 0.00E+00 0.0000 0.0000 9.53E-03 174 0.00 0.000 0.001 0.1161 0.0000 0.0000 0.00E+00 0.0000 0.0000 9.23E-03 175 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 8.70E-03 176 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 7.75E-03 177 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 7.05E-03 178 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 6.81E-03 179 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 6.92E-03 180 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 7.31E-03 181 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 7.38E-03 182 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 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1.25E-02 330 * * 0.20 0.000 0.010 0.2931 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.28E-02 331 * * 0.00 0.000 0.016 0.2931 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.33E-02 332 * * 0.50 0.000 0.000 0.2931 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.37E-02 333 * * 0.10 0.000 0.016 0.2931 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.43E-02 334 * * 0.00 0.000 0.010 0.2931 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.48E-02 335 * * 0.00 0.000 0.014 0.2931 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.50E-02 336 * * 0.00 0.000 0.018 0.2931 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.54E-02 337 * 0.00 0.000 0.020 0.2931 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.53E-02 338 * 0.40 0.121 0.000 0.3708 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.60E-02 339 * * 0.00 0.000 0.018 0.3723 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.75E-02 340 * * 0.00 0.000 0.019 0.3723 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.78E-02 341 * * 0.00 0.000 0.020 0.3723 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.69E-02 342 * * 0.20 0.000 0.019 0.3723 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.57E-02 Page 111 of 128 343 * * 0.00 0.000 0.013 0.3723 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.48E-02 344 * * 0.00 0.000 0.016 0.3723 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.45E-02 345 * * 0.00 0.000 0.015 0.3723 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.47E-02 346 * * 0.00 0.000 0.017 0.3723 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.51E-02 347 * 0.00 0.000 0.021 0.3723 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.56E-02 348 * * 0.00 0.000 0.014 0.3723 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.59E-02 349 * * 0.20 0.000 0.013 0.3723 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.62E-02 350 * * 0.00 0.000 0.008 0.3723 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.61E-02 351 * * 0.00 0.000 0.010 0.3723 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.55E-02 352 * * 0.00 0.000 0.015 0.3723 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.46E-02 353 * * 0.00 0.000 0.015 0.3723 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.35E-02 354 * * 0.00 0.000 0.017 0.3723 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.25E-02 355 * * 0.00 0.000 0.019 0.3723 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.15E-02 356 * * 0.00 0.000 0.020 0.3723 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.05E-02 357 * * 0.00 0.000 0.020 0.3723 0.0000 0.0000 0.00E+00 0.0000 0.0000 9.64E-03 358 * * 0.10 0.000 0.000 0.3723 0.0000 0.0000 0.00E+00 0.0000 0.0000 8.88E-03 359 * * 0.10 0.000 0.017 0.3723 0.0000 0.0000 0.00E+00 0.0000 0.0000 7.86E-03 360 * * 0.00 0.000 0.013 0.3723 0.0000 0.0000 0.00E+00 0.0000 0.0000 7.77E-03 361 * * 0.10 0.000 0.014 0.3723 0.0000 0.0000 0.00E+00 0.0000 0.0000 8.00E-03 362 * * 0.10 0.000 0.010 0.3723 0.0000 0.0000 0.00E+00 0.0000 0.0000 8.01E-03 363 * * 0.00 0.000 0.011 0.3723 0.0000 0.0000 0.00E+00 0.0000 0.0000 7.76E-03 364 * * 0.00 0.000 0.014 0.3723 0.0000 0.0000 0.00E+00 0.0000 0.0000 7.37E-03 365 * * 0.00 0.000 0.012 0.3723 0.0000 0.0000 0.00E+00 0.0000 0.0000 6.98E-03 * = Frozen (air or soil) inches cubic feet percent Precipitation 19.20 4,878,720.0 100.00 Runoff 7.248 1,841,606.0 37.75 Evapotranspiration 7.760 1,971,825.2 40.42 Percolation/Leakage through Layer 2 3.387657 860,803.7 17.64 Average Head on Top of Layer 2 0.0669 ------ Percolation/Leakage through Layer 12 4.057631 1,031,044.0 21.13 Annual Totals for Year 9 Page 112 of 128 Change in Water Storage 0.1348 34,244.7 0.70 Soil Water at Start of Year 235.4395 #########1226.25 Soil Water at End of Year 235.0954 #########1224.46 Snow Water at Start of Year 1.5423 391,900.7 8.03 Snow Water at End of Year 2.0211 513,572.5 10.53 Annual Water Budget Balance 0.0000 0.0000 0.00 Page 113 of 128 Daily Output for Year 10 Column key:Head #1: drainage from Layer 2 Title:Long Valley Landfill Simulated On:Leak #1: leakage thru Layer 2 Leak #2: leakage thru Layer 12 Day Rain Runoff ET Evap. Zone Water Head #1 Drain #1 Leak #1 Head #2 Drain #2 Leak #2 Air Soil (inches)(inches)(inches)(in/in)(inches)(inches)(inches)(inches)(inches)(inches) 1 * * 0.40 0.000 0.000 0.3723 0.0000 0.0000 0.00E+00 0.0000 0.0000 6.68E-03 2 * * 0.00 0.000 0.022 0.3723 0.0000 0.0000 0.00E+00 0.0000 0.0000 6.53E-03 3 * * 0.00 0.000 0.025 0.3723 0.0000 0.0000 0.00E+00 0.0000 0.0000 6.53E-03 4 * * 0.00 0.000 0.025 0.3723 0.0000 0.0000 0.00E+00 0.0000 0.0000 6.64E-03 5 * * 0.00 0.000 0.023 0.3723 0.0000 0.0000 0.00E+00 0.0000 0.0000 6.85E-03 6 * * 0.00 0.000 0.019 0.3723 0.0000 0.0000 0.00E+00 0.0000 0.0000 7.08E-03 7 * * 0.00 0.000 0.022 0.3723 0.0000 0.0000 0.00E+00 0.0000 0.0000 7.31E-03 8 * * 0.00 0.000 0.021 0.3723 0.0000 0.0000 0.00E+00 0.0000 0.0000 7.50E-03 9 * * 0.00 0.000 0.018 0.3723 0.0000 0.0000 0.00E+00 0.0000 0.0000 7.61E-03 10 * * 0.10 0.000 0.014 0.3723 0.0000 0.0000 0.00E+00 0.0000 0.0000 7.66E-03 11 * * 0.00 0.000 0.022 0.3723 0.0000 0.0000 0.00E+00 0.0000 0.0000 7.60E-03 12 * * 0.00 0.000 0.016 0.3723 0.0000 0.0000 0.00E+00 0.0000 0.0000 7.41E-03 13 * * 0.00 0.000 0.021 0.3723 0.0000 0.0000 0.00E+00 0.0000 0.0000 7.15E-03 14 * * 0.00 0.000 0.023 0.3723 0.0000 0.0000 0.00E+00 0.0000 0.0000 6.86E-03 15 * * 0.00 0.000 0.021 0.3723 0.0000 0.0000 0.00E+00 0.0000 0.0000 6.56E-03 16 * * 0.00 0.000 0.023 0.3723 0.0000 0.0000 0.00E+00 0.0000 0.0000 6.28E-03 17 * * 0.30 0.000 0.016 0.3723 0.0000 0.0000 0.00E+00 0.0000 0.0000 6.02E-03 18 * * 0.00 0.000 0.019 0.3723 0.0000 0.0000 0.00E+00 0.0000 0.0000 5.83E-03 19 * * 0.00 0.000 0.022 0.3723 0.0000 0.0000 0.00E+00 0.0000 0.0000 5.71E-03 20 * * 0.00 0.000 0.027 0.3723 0.0000 0.0000 0.00E+00 0.0000 0.0000 5.74E-03 21 * * 0.10 0.000 0.000 0.3723 0.0000 0.0000 0.00E+00 0.0000 0.0000 5.82E-03 22 * * 0.00 0.000 0.024 0.3723 0.0000 0.0000 0.00E+00 0.0000 0.0000 5.98E-03 23 * * 0.00 0.000 0.023 0.3723 0.0000 0.0000 0.00E+00 0.0000 0.0000 6.27E-03 24 * * 0.00 0.000 0.023 0.3723 0.0000 0.0000 0.00E+00 0.0000 0.0000 6.71E-03 25 * * 0.00 0.000 0.022 0.3723 0.0000 0.0000 0.00E+00 0.0000 0.0000 7.29E-03 26 * * 0.00 0.000 0.027 0.3723 0.0000 0.0000 0.00E+00 0.0000 0.0000 7.98E-03 27 * * 0.10 0.000 0.000 0.3723 0.0000 0.0000 0.00E+00 0.0000 0.0000 8.76E-03 7/19/2024 11:05 Freezing Status* Page 114 of 128 28 * * 0.00 0.000 0.022 0.3723 0.0000 0.0000 0.00E+00 0.0000 0.0000 9.59E-03 29 * * 0.00 0.000 0.017 0.3723 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.04E-02 30 * * 0.00 0.000 0.019 0.3723 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.12E-02 31 * * 0.00 0.000 0.021 0.3723 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.20E-02 32 * * 0.00 0.000 0.029 0.3723 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.27E-02 33 * * 0.00 0.000 0.026 0.3723 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.24E-02 34 * * 0.20 0.000 0.019 0.3723 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.49E-02 35 * * 0.00 0.000 0.010 0.3723 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.51E-02 36 * * 0.00 0.000 0.012 0.3723 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.40E-02 37 * * 0.00 0.000 0.025 0.3723 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.38E-02 38 * * 0.00 0.000 0.027 0.3723 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.41E-02 39 * 0.00 0.000 0.030 0.3723 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.44E-02 40 * * 0.10 0.000 0.018 0.3723 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.46E-02 41 * * 0.00 0.000 0.017 0.3723 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.47E-02 42 * * 0.00 0.000 0.013 0.3723 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.46E-02 43 * * 0.00 0.000 0.022 0.3723 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.45E-02 44 * * 0.00 0.000 0.023 0.3723 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.42E-02 45 * * 0.00 0.000 0.024 0.3723 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.39E-02 46 * * 0.00 0.000 0.027 0.3723 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.36E-02 47 * 0.00 0.000 0.029 0.3723 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.32E-02 48 * * 0.00 0.000 0.026 0.3723 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.29E-02 49 * * 0.00 0.000 0.021 0.3723 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.26E-02 50 * * 0.00 0.000 0.022 0.3723 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.23E-02 51 * * 0.00 0.000 0.018 0.3723 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.21E-02 52 * * 0.00 0.000 0.023 0.3723 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.19E-02 53 * * 0.40 0.000 0.000 0.3723 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.17E-02 54 * * 0.20 0.000 0.000 0.3723 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.15E-02 55 * * 0.00 0.000 0.023 0.3723 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.12E-02 56 * * 0.00 0.000 0.016 0.3723 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.10E-02 57 * * 0.00 0.000 0.018 0.3723 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.09E-02 58 * * 0.00 0.000 0.023 0.3723 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.08E-02 59 * * 0.00 0.000 0.028 0.3723 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.07E-02 60 * * 0.00 0.000 0.024 0.3723 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.06E-02 61 * * 0.10 0.000 0.000 0.3723 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.04E-02 62 * * 0.00 0.000 0.021 0.3723 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.02E-02 Page 115 of 128 63 * * 0.00 0.000 0.023 0.3723 0.0000 0.0000 0.00E+00 0.0000 0.0000 9.93E-03 64 * * 0.00 0.000 0.027 0.3723 0.0000 0.0000 0.00E+00 0.0000 0.0000 9.75E-03 65 * 0.00 0.000 0.032 0.3723 0.0000 0.0000 0.00E+00 0.0000 0.0000 9.67E-03 66 * 0.00 0.019 0.025 0.3809 0.0000 0.0000 0.00E+00 0.0000 0.0000 9.25E-03 67 * 0.00 0.409 0.000 0.4078 0.0000 0.0000 0.00E+00 0.0000 0.0000 8.78E-03 68 * * 0.10 0.000 0.030 0.4078 0.0000 0.0000 0.00E+00 0.0000 0.0000 8.43E-03 69 * * 0.00 0.000 0.032 0.4078 0.0000 0.0000 0.00E+00 0.0000 0.0000 8.27E-03 70 * 0.00 0.070 0.023 0.4101 0.0000 0.0000 0.00E+00 0.0000 0.0000 8.30E-03 71 * 0.10 0.400 0.000 0.4212 0.0000 0.0000 0.00E+00 0.0000 0.0000 8.48E-03 72 * 0.00 0.505 0.000 0.4245 0.0003 0.0000 1.05E-02 0.0000 0.0000 8.75E-03 73 * * 0.80 0.000 0.033 0.4245 0.0000 0.0000 0.00E+00 0.0000 0.0000 9.08E-03 74 * 0.00 0.174 0.011 0.4245 0.0023 0.0000 4.24E-03 0.0000 0.0000 9.40E-03 75 * 0.00 0.217 0.005 0.4245 0.0052 0.0000 9.64E-03 0.0000 0.0000 9.69E-03 76 * 0.00 0.017 0.032 0.4245 0.0000 0.0000 0.00E+00 0.0000 0.0000 9.92E-03 77 * 0.00 0.209 0.008 0.4245 0.0040 0.0000 7.39E-03 0.0000 0.0000 1.01E-02 78 * 0.00 0.000 0.035 0.4245 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.02E-02 79 * * 0.10 0.000 0.032 0.4245 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.02E-02 80 * * 0.10 0.000 0.029 0.4245 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.01E-02 81 * 0.10 0.033 0.000 0.4245 0.0069 0.0000 1.27E-02 0.0000 0.0000 1.01E-02 82 * * 0.00 0.000 0.036 0.4245 0.0000 0.0000 0.00E+00 0.0000 0.0000 9.94E-03 83 * * 0.10 0.000 0.035 0.4245 0.0000 0.0000 0.00E+00 0.0000 0.0000 9.85E-03 84 * 0.00 0.095 0.027 0.4245 0.0000 0.0000 0.00E+00 0.0000 0.0000 9.76E-03 85 * 0.00 0.318 0.000 0.4245 0.0083 0.0000 1.53E-02 0.0000 0.0000 1.04E-02 86 * * 0.10 0.000 0.030 0.4245 0.0000 0.0000 0.00E+00 0.0000 0.0000 8.07E-03 87 * * 0.00 0.000 0.022 0.4245 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.03E-02 88 * * 0.00 0.000 0.029 0.4245 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.06E-02 89 * * 0.30 0.000 0.000 0.4245 0.0000 0.0000 0.00E+00 0.0000 0.0000 9.85E-03 90 * 0.00 0.000 0.035 0.4245 0.0000 0.0000 0.00E+00 0.0000 0.0000 9.37E-03 91 * 0.00 0.405 0.000 0.4245 0.0083 0.0000 1.54E-02 0.0000 0.0000 9.95E-03 92 * 0.00 0.557 0.000 0.4245 0.0082 0.0000 1.52E-02 0.0000 0.0000 8.72E-03 93 * * 0.00 0.000 0.046 0.4245 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.04E-02 94 * * 0.00 0.000 0.050 0.4245 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.38E-02 95 * * 0.00 0.000 0.058 0.4245 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.37E-02 96 * 0.00 0.069 0.121 0.4245 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.26E-02 97 * 0.00 0.000 0.000 0.4245 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.17E-02 Page 116 of 128 98 * 0.00 0.000 0.000 0.4245 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.15E-02 99 * 0.00 0.000 0.000 0.4245 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.19E-02 100 0.10 0.027 0.084 0.3862 1.7528 0.0000 1.04E-01 0.0000 0.0000 1.29E-02 101 0.00 0.000 0.091 0.3110 1.7318 0.0000 1.34E-01 0.0000 0.0000 1.19E-02 102 0.00 0.000 0.102 0.2339 1.0414 0.0000 1.30E-01 0.0000 0.0000 1.29E-02 103 * 0.10 0.000 0.113 0.1879 0.4239 0.0000 1.25E-01 0.0000 0.0000 1.30E-02 104 * 0.00 0.000 0.065 0.1583 0.0243 0.0000 2.43E-02 0.0000 0.0000 1.53E-02 105 * * 0.00 0.000 0.000 0.1583 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.49E-02 106 * * 0.10 0.000 0.100 0.1583 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.24E-02 107 * * 0.00 0.000 0.000 0.1583 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.08E-02 108 * 0.10 0.000 0.001 0.1913 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.04E-02 109 * 0.00 0.000 0.000 0.1913 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.06E-02 110 * 0.10 0.001 0.001 0.2240 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.10E-02 111 * 0.10 0.006 0.001 0.2551 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.16E-02 112 * 0.00 0.000 0.000 0.2551 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.11E-02 113 * 0.00 0.000 0.000 0.2551 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.15E-02 114 0.00 0.000 0.099 0.2118 0.0721 0.0000 3.11E-02 0.0000 0.0000 1.36E-02 115 0.00 0.000 0.173 0.1406 0.0598 0.0000 4.10E-02 0.0000 0.0000 1.51E-02 116 0.00 0.000 0.074 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.42E-02 117 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.62E-02 118 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.37E-02 119 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.23E-02 120 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.15E-02 121 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.06E-02 122 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.08E-02 123 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.13E-02 124 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.19E-02 125 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.23E-02 126 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.25E-02 127 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.27E-02 128 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.27E-02 129 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.27E-02 130 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.27E-02 131 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.26E-02 132 0.20 0.000 0.012 0.1786 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.25E-02 Page 117 of 128 133 0.00 0.000 0.022 0.1713 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.24E-02 134 0.00 0.000 0.023 0.1635 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.23E-02 135 0.00 0.000 0.023 0.1560 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.21E-02 136 0.00 0.000 0.022 0.1485 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.18E-02 137 0.00 0.000 0.022 0.1411 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.15E-02 138 0.00 0.000 0.022 0.1338 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.13E-02 139 0.00 0.000 0.021 0.1267 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.13E-02 140 0.00 0.000 0.021 0.1197 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.06E-02 141 0.00 0.000 0.009 0.1169 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.03E-02 142 0.00 0.000 0.003 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.02E-02 143 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.01E-02 144 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.04E-02 145 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.07E-02 146 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.08E-02 147 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.08E-02 148 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.08E-02 149 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.08E-02 150 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.10E-02 151 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.13E-02 152 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.16E-02 153 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.19E-02 154 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.22E-02 155 0.00 0.000 0.000 0.1160 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.23E-02 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0.00E+00 0.0000 0.0000 8.20E-03 304 0.00 0.000 0.007 0.1332 0.0000 0.0000 0.00E+00 0.0000 0.0000 8.39E-03 305 0.00 0.000 0.007 0.1310 0.0000 0.0000 0.00E+00 0.0000 0.0000 8.67E-03 306 0.00 0.000 0.007 0.1287 0.0000 0.0000 0.00E+00 0.0000 0.0000 8.87E-03 307 0.00 0.000 0.007 0.1265 0.0000 0.0000 0.00E+00 0.0000 0.0000 8.98E-03 Page 122 of 128 308 0.00 0.000 0.007 0.1243 0.0000 0.0000 0.00E+00 0.0000 0.0000 9.01E-03 309 0.00 0.000 0.005 0.1224 0.0000 0.0000 0.00E+00 0.0000 0.0000 9.00E-03 310 0.00 0.000 0.008 0.1198 0.0000 0.0000 0.00E+00 0.0000 0.0000 8.98E-03 311 0.00 0.000 0.008 0.1172 0.0000 0.0000 0.00E+00 0.0000 0.0000 8.99E-03 312 0.20 0.000 0.010 0.1805 0.0000 0.0000 0.00E+00 0.0000 0.0000 9.04E-03 313 * 0.10 0.000 0.032 0.1871 0.0000 0.0000 0.00E+00 0.0000 0.0000 9.24E-03 314 * 0.30 0.000 0.012 0.1936 0.0000 0.0000 0.00E+00 0.0000 0.0000 9.28E-03 315 * 0.30 0.000 0.012 0.2002 0.0000 0.0000 0.00E+00 0.0000 0.0000 9.32E-03 316 * 0.00 0.000 0.014 0.2067 0.0000 0.0000 0.00E+00 0.0000 0.0000 9.48E-03 317 * 0.00 0.000 0.017 0.2133 0.0000 0.0000 0.00E+00 0.0000 0.0000 9.75E-03 318 * 0.00 0.000 0.017 0.2199 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.01E-02 319 * 0.30 0.000 0.000 0.2264 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.04E-02 320 0.00 0.000 0.020 0.2330 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.07E-02 321 0.00 0.000 0.000 0.3018 0.1552 0.0000 9.29E-02 0.0000 0.0000 1.10E-02 322 0.00 0.000 0.000 0.3749 0.8420 0.0000 1.28E-01 0.0000 0.0000 1.11E-02 323 0.00 0.000 0.046 0.3389 1.6391 0.0000 1.34E-01 0.0000 0.0000 1.12E-02 324 0.00 0.000 0.010 0.2922 1.1754 0.0000 1.30E-01 0.0000 0.0000 1.12E-02 325 0.00 0.000 0.010 0.2469 0.5683 0.0000 1.26E-01 0.0000 0.0000 1.12E-02 326 0.00 0.000 0.010 0.2239 0.0823 0.0000 5.96E-02 0.0000 0.0000 1.12E-02 327 0.00 0.000 0.009 0.2194 0.0030 0.0000 4.05E-03 0.0000 0.0000 1.13E-02 328 * 0.10 0.000 0.025 0.2259 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.14E-02 329 * 0.00 0.000 0.015 0.2320 0.0008 0.0000 1.50E-03 0.0000 0.0000 1.15E-02 330 * 0.00 0.000 0.029 0.2287 0.0002 0.0000 2.84E-04 0.0000 0.0000 1.20E-02 331 * 0.00 0.000 0.000 0.2284 0.0001 0.0000 9.73E-04 0.0000 0.0000 1.36E-02 332 * 0.00 0.000 0.000 0.2276 0.0014 0.0000 2.39E-03 0.0000 0.0000 9.83E-03 333 * 0.00 0.000 0.009 0.2245 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.05E-02 334 * * 0.00 0.000 0.000 0.2245 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.40E-02 335 * * 0.00 0.000 0.000 0.2245 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.67E-02 336 * * 0.00 0.000 0.000 0.2245 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.76E-02 337 * * 0.00 0.000 0.000 0.2245 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.69E-02 338 * * 0.00 0.000 0.000 0.2245 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.58E-02 339 * 0.00 0.000 0.000 0.2245 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.51E-02 340 * 0.00 0.000 0.000 0.2245 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.52E-02 341 * * 0.00 0.000 0.000 0.2245 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.54E-02 342 * 0.00 0.000 0.000 0.2245 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.59E-02 Page 123 of 128 343 * 0.00 0.000 0.000 0.2245 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.67E-02 344 * * 0.00 0.000 0.000 0.2245 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.76E-02 345 * * 0.00 0.000 0.000 0.2245 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.86E-02 346 * * 0.00 0.000 0.000 0.2245 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.95E-02 347 * * 0.40 0.000 0.011 0.2245 0.0000 0.0000 0.00E+00 0.0000 0.0000 2.00E-02 348 * * 0.00 0.000 0.011 0.2245 0.0000 0.0000 0.00E+00 0.0000 0.0000 2.02E-02 349 * * 0.10 0.000 0.015 0.2245 0.0000 0.0000 0.00E+00 0.0000 0.0000 2.00E-02 350 * * 0.00 0.000 0.012 0.2245 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.96E-02 351 * * 0.00 0.000 0.016 0.2245 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.89E-02 352 * * 0.20 0.000 0.000 0.2245 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.81E-02 353 * * 0.10 0.000 0.013 0.2245 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.72E-02 354 * * 0.00 0.000 0.014 0.2245 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.67E-02 355 * * 0.00 0.000 0.015 0.2245 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.62E-02 356 * 0.00 0.000 0.000 0.2245 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.56E-02 357 * * 0.00 0.000 0.018 0.2245 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.54E-02 358 * * 0.00 0.000 0.010 0.2245 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.54E-02 359 * * 0.10 0.000 0.014 0.2245 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.56E-02 360 * * 0.00 0.000 0.017 0.2245 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.59E-02 361 * * 0.00 0.000 0.017 0.2245 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.64E-02 362 * * 0.00 0.000 0.014 0.2245 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.69E-02 363 * * 0.20 0.000 0.000 0.2245 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.75E-02 364 * * 0.10 0.000 0.012 0.2245 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.79E-02 365 * * 0.00 0.000 0.010 0.2245 0.0000 0.0000 0.00E+00 0.0000 0.0000 1.82E-02 * = Frozen (air or soil) inches cubic feet percent Precipitation 10.10 2,566,410.0 100.00 Runoff 3.531 897,278.5 34.96 Evapotranspiration 5.783 1,469,505.7 57.26 Percolation/Leakage through Layer 2 2.267607 576,199.0 22.45 Average Head on Top of Layer 2 0.0401 ------ Percolation/Leakage through Layer 12 3.227106 820,007.8 31.95 Annual Totals for Year 10 Page 124 of 128 Change in Water Storage -2.4415 -620,382.0 -24.17 Soil Water at Start of Year 235.0954 #########2327.68 Soil Water at End of Year 233.6924 #########2313.79 Snow Water at Start of Year 2.0211 513,572.5 20.01 Snow Water at End of Year 0.9827 249,699.9 9.73 Annual Water Budget Balance 0.0000 0.0000 0.00 Page 125 of 128 Average Annual Totals Summary Title:Long Valley Landfill Simulated on:7/19/2024 11:05 (inches)[std dev](cubic feet)(percent) 16.10 [3.1]4,091,010.0 100.00 3.264 [2.439]829,365.0 20.27 9.103 [2.408]2,313,041.7 56.54 3.620989 [1.037818]920,093.2 22.49 0.0745 [0.0271]------ 1.740638 [1.661349]442,296.1 10.81 Water storage 1.9926 [3.1188]506,307.2 12.38 * Note: Average inches are converted to volume based on the user-specified area. Average Head on Top of Layer 2 Subprofile2 Percolation/leakage through Layer 12 Change in water storage Average Annual Totals for Years 1 - 10* Precipitation Runoff Evapotranspiration Subprofile1 Percolation/leakage through Layer 2 Page 126 of 128 Peak Values Summary Title:Long Valley Landfill Simulated on:7/19/2024 11:05 (inches)(cubic feet) 2.70 686,070.0 1.808 459,468.0 0.141614 35,984.1 2.8162 0.020376 5,177.5 Other Parameters Snow water 4.9911 1,268,230.0 Maximum vegetation soil water 0.4630 (vol/vol) Minimum vegetation soil water 0.1160 (vol/vol) Subprofile2 Percolation/leakage through Layer 12 Peak Values for Years 1 - 10* Precipitation Runoff Subprofile1 Percolation/leakage through Layer 2 Average head on Layer 2 Page 127 of 128 Final Water Storage in Landfill Profile at End of Simulation Period Title:Long Valley Landfill Simulated on:7/19/2024 11:05 Simulation period:10 years Layer (inches)(vol/vol) 1 0.6735 0.2245 2 7.8659 0.4370 3 1.3920 0.2320 4 30.2881 0.2524 5 3.0487 0.2541 6 30.4695 0.2539 7 3.1620 0.2635 8 31.4794 0.2623 9 31.1104 0.2593 10 31.4708 0.2623 11 31.1911 0.2599 12 31.5411 0.2628 Snow water 0.9827 --- Final Water Storage Page 128 of 128 X X X X X X X X XX X X X X X X X X X X X X X X X X X X X X X X X XXXXXXX X X X X X X X X X X X X X X X FUTURE CLASS II CELL FUTURE CONSTRUCTION BOUNDARY LINE MAINTENANCE BUILDING LO A L A N D F I L L R D . 240.0' TYP. 48 0 . 0 ' T Y P . FUTURE CLASS II CELL FUTURE CLASS II CELL FUTURE CLASS II CELL FUTURE CLASS II CELL FUTURE CLASS II CELL FUTURE CLASS II CELL 16 0 . 0 ' 480.0' FUTURE CLASS II CELL FUTURE CLASS II CELL FUTURE CLASS II CELL FUTURE CLASS II CELL 24 0 . 0 ' T Y P . 480 . 0 ' T Y P . FUTURE CONSTRUCTION/ DEMOLITION WASTES FUTURE CONSTRUCTION/ DEMOLITION WASTES FUTURE CONSTRUCTION/ DEMOLITION WASTES DESIGNED BY PROJECT NUMBER FOR: PROJECT MANAGER PRINT DATE PHONE: CONTACT: WWW.ENSIGNENG.COM RICHFIELD 225 N 100 E Richfield, UT 84701 Phone: 435.896.2983 SANDY Phone: 801.255.0529 LAYTON Phone: 801.547.1100 TOOELE Phone: 435.843.3590 CEDAR CITY Phone: 435.865.1453 13336 LO N G H O L L O W L A N D F I L L LO A L A N D F I L L R D . LO A , U T A H WAYNE COUNTY CLIENT'S ADDRESS CLIENT CITY STATE ZIP CLIENT CONTACT 801.000.0000 K. CHAPPELL B.REES 2024-08-01 HORIZONTAL GRAPHIC SCALE 0 ( IN FEET ) HORZ: 1 inch = ft.200 200 100 200 400 EXHIBIT #9 CELL PROGRESSION MAP 30 ' 6% 2:1 SCALE:3 NONE SECTION D 6% 2:1 30' 2' 4:1 4:1 NATURAL GRADE PERIMETER DITCH FUTURE CAP PERIMETER ROAD SCALE:4 NONE CELL BERM DETAIL NOTE: 1. GRADE CELL PERIMETER DITCHES TO DRAIN AWAY FROM CELL 6% NATIVE VEGETATION TOP SOIL IMPERMEABLE SOIL SOLID WASTE 6" 18 " SCALE:5 NONE CAP DETAIL 40 ' 20 '6%6% 40' 2:1 BOTTOM OF CELL TO BE SCARIFIED 8" DEEP AND RECOMPACTED TO 95% AASHTO T-99 STOCK PILE EXCAVATED MATERIAL SCALE:2 NONE SECTION C-C 40 ' 200' 22 0 ' 28 0 ' 380' 440' C C D SCALE:1 NONE CLASS II LANDFILL PITS EXHIBIT #10 DETAILS CHECKED BYDRAWN BY PROJECT NUMBER FOR: PROJECT MANAGER PRINT DATE PHONE: CONTACT: RICHFIELD 225 N. 100 E. Richfield, UT 84701 Phone: 435.896.2983 LAYTON Phone: 801.547.1100 TOOELE Phone: 435.843.3590 CEDAR CITY Phone: 435.865.1453 SALT LAKE CITY Phone: 801.255.0529 WWW.ENSIGNENG.COM E N S I G N THE STANDARD IN ENGINEERING 13336 LO N G H O L L O W L A N D F I L L LO A L A N D F I L L R D . LO A , U T A H WAYNE COUNTY 18 SOUTH MAIN ST. LOA, UT 84747 DENNIS BLACKBURN 435-836-1300 K. CHAPPELL B. REESD. SCHAUGAARD 7/25/24 SANDY 45 W 10000 S, STE 500 Sandy, UT 84070 P: 801.255.0529 LAYTON 919 North 400 West Layton, UT 84041 P: 801.547.1100 CEDAR CITY 88 E Fiddler’s Canyon Rd, STE 210 Cedar City, UT 84721 P: 435.865.1453 TOOELE 169 N. Main St, Unit 1 Tooele, UT 84074 P: 435.843.3590 RICHFIELD 225 N 100 E Richfield, UT 84701 P: 435.896.2983 www.ensigneng.com Structural Engineering Municipal Services Civil Engineering Land Surveying July 25, 2024 Ensign Engineering 225 North 100 East Richfield, UT 84701 Dr. Christopher W. Merritt, Ph.D. Utah State Historic Preservation Office 300 South Rio Grande Street, Room 218 Salt Lake City, UT 84101 RE: Long Hollow Class II Permit Renewal and Expansion Dear Dr. Merritt Wayne County is in the process of renewing and expanding the Long Hollow Landfill in Loa, Utah. The landfill is currently operating as a Class II landfill. The existing landfill main gate is located at Latitude 38.358662° North and Longitude -111.687593° West located approximately 4 miles southwest of Loa, Utah. A map has been attached for your reference. The site has been and will continue to be used as a Class II landfill. Class II landfills can accept all household waste, yard waste, construction/ demolition, white goods and crap metal, tires, dead animals, commercial, and non-hazardous industrial waste. It is anticipated that there would be approximately 60-90 tons of waste per week. The landfill is requesting approval to be expanded beyond the previously approved area. No historical items are assumed to be discovered. The landfill will expand within its existing property boundary therefore risk to discovering other Historical items is not of concern. All work will be done within existing right-of-way and easements. Due to the site being approved for Class II landfill in the past and no new property will be disturbed outside the property boundaries it is recommended a finding of No Historic Properties Affected. Please provide your concurrence, or objection within thirty-days of your receipt of this recommended finding. In accordance with 36 CFR §800.3(c)(4), we will proceed to the next step in the review if a response is not received within thirty-days. If you have questions concerning this letter please contact me at 435-896-2983 Sincerely, Brennan Rees, PE Assistant Project Manager brees@ensignutah.com Tla To To Qac Tpml Tpml Qac Qac Tpml Qac Qac Tpml Qac Qac Qal Qal Tpml Qal To To Qap To Qal Qal Qal Tpml To Tb Tb Ts Tb Qac Tpml Tpml Ts Tl Tpml Tb Tb Tl Tb Tl Tpml Tpml Tpml Tla Tl Tl Tl Tl Tpml Tla Tpml Tla Tla Tla Tl Tla To Tla Tl Tl Tl Tla Tpml Tl Tpml Qac Tpml Qac Tpml Tla Tl Qac Qac Qac To Qal Qal Tl Tpml Tpml Tpml Tpml Tpml Tpml Tpml Tpml Tpml Tpml Tpml Tl Qal Qal Qac Qac To To To To To Tb To Tpml Tb To Tpml Tpml Qal Qal Qal Qal Qal Qac Qac Qac Qac Tl Qal Qal Qal Tpml Qal Tpml Tpml Tpml Tpml Tpml AP60, AP62, AP63 Tb AP65, AP67 5 1 2 Tb AP107 AP101, AP103 AP104 AP105 4 Base map from U. S. Geological Survey Moroni Peak, Utah 7.5’ Quadrangle, 1969. The Miscellaneous Publication Maps provide an outlet for authors who are not Utah Geological Survey staff. Not all aspects of this publication have been reviewed by the UGS. Qal B Qac AP64 To 2001 MAGNETIC DECLINATION AT CENTER OF SHEET 12 53 229 MIL 2 A A B UTAH GEOLOGICAL SURVEY a division of UTAH DEPARTMENT OF NATURAL RESOURCES Plate 1 Utah Geological Survey Miscellaneous Publication 01-5 Geologic Map of the Moroni Peak Quadrangle GEOLOGIC MAP OF THE MORONI PEAK QUADRANGLE, WAYNE COUNTY, UTAH by Stephen R. Mattox 2001 1 0.5 0 1 0.5 0 1 KILOMETER 1 MILE SCALE 1:24,000 01000 1000 2000 3000 4000 5000 6000 7000 FEET CONTOUR INTERVAL 20 FEET UTAH QUADRANGLE LOCATION APPROX. PROPERTY BOUNDARY EXPLANATION Contact Fault - long dashed where uncertain; short dashed where covered; bar and ball on downthrown side. Strike and dip Horizontal beds Strike of vertical joints Sample locations Vent Gravel pit AP65 84 0 0 80 0 0 76 0 0 Tb Tl a El s i e s N i p p l e Tb Tl a Sa g e F l a t D r a w Tp m l Tl Bi g H o l l o w Tl Tl a Tl 76 0 0 80 0 0 84 0 0 So u t h B B No r t h Su r f i c i a l d e p o s i t s n o t s h o w n . 80 0 0 70 0 0 A A 80 0 0 70 0 0 Ea s t We s t To Tl a Tp m l Tl a Tp m l Tl a Lo n g H o l l o w Tp m l To To Bu l l h e a d B e n c h Ra b b i t V a l l e y Su r f i c i a l d e p o s i t s n o t s h o w n . QUATERNARY Alluvium (Late Pleistocene and Holocene) -- Gray and light brown, unconsolidated, silt, sand, and gravel along active streams and washes. Maximum exposed thickness is 20 feet (6 m). Mixed alluvium and colluvium (Pleistocene and Holocene) -- Gray and light-brown, unconsolidated to weakly consolidated mud, sand, cobbles and boulders in valley-fill deposits, older stream deposits, and gentle slopes below steep escarpments. Dissected by modern streams. The deposit in Long Hollow is estimated to be at least 100 feet (30 m) thick; other deposits are generally less than 20 feet (6 m) thick. Pediment-mantle alluvium (Pleistocene) -- Gray and light-brown, unconsolidated, fine gravel on sloping erosional surfaces. Gravel consists of eroded Osiris Tuff. Maximum exposed thickness is 40 feet (12 m). TERTIARY Unconformity Basalt lava flows (Miocene) -- Black, dark-gray, and reddish-brown, dense lava flows of olivine basalt. Contains abundant olivine phenocrysts, with less abundant phenocrysts of clinopyroxene and plagioclase in groundmass of plagioclase microlites, iron oxides, and glass. Maximum thickness, near vent, is about 270 feet (80 m). Sevier River Formation (Miocene) -- Gray, light-brown, and greenish- gray, moderately consolidated, medium- to thick-bedded sandstone and conglomerate. Conglomerate contains clasts from the volcanic rocks of Langdon Mountain. Maximum thickness is about 100 feet (30 m). Unconformity Osiris Tuff (Miocene) -- Orange, reddish-brown, and light-gray, resistant, densely welded, vitric-crystal ash-flow tuff with black basal vitrophyre. Light-gray, thin-bedded ash beneath vitrophyre at one locality. Maximum exposed thickness is 130 feet (40 m). Unconformity Potassium-rich mafic lava flows (Oligocene-Miocene) -- Medium-gray to black, porphyritic lava flows containing nearly equal amounts of clinopyroxene and plagioclase and less abundant olivine, orthopyroxene, and iron oxide phenocrysts in a groundmass of plagioclase microlites, iron oxides, and glass. Maximum exposed thickness is 400 feet (120 m). Latite lava flows (Oligocene-Miocene) -- Black, glassy lava flows containing a few percent resorbed plagioclase, clinopyroxene, hornblende, and iron oxide phenocrysts; also medium-gray, structureless or flow-banded lava flows with conspicuous plagioclase and absence of hornblende. Maximum exposed thickness is 400 feet (120 m). Volcanic rocks of Langdon Mountain (Oligocene-Miocene) -- Red, gray, and white mudflow breccia, with minor beds of sandstone and conglomerate. Individual beds of mudflow breccia range from well sorted, clast-supported cobbles to poorly sorted, matrix-supported cobbles and boulders; clasts are andesitic in composition. Sandstones are well sorted and tuffaceous. Beds are structureless, inversely graded, and normally graded. Maximum exposed thickness is 350 feet (105 m). UTAH GEOLOGICAL SURVEY a division of UTAH DEPARTMENT OF NATURAL RESOURCES Plate 2 Utah Geological Survey Miscellaneous Publication 01-5 Geologic Map of the Moroni Peak Quadrangle DESCRIPTION OF MAP UNITS Tla Tl Tpml To Ts Tb Qap Qac Qal TE R T I A R Y Quaternary Surficial deposits Basalt lava flows Sevier River Formation Osiris Tuff Potassium-rich mafic lava flows Latite lava flows Volcanic rocks of Langdon Mountain Alluvial facies Q Ts Tb To Tpml Tl Tla 0-100 (0-30) 0-270 (0-80) 0-100 (0-30) 0-130 (0-40) 0-400 (0-120) 0-400 (0-120) 0-350 (0-105) MAP UNIT LITHOLOGY SY S T E M SE R I E S SY M B O L MI O C E N E OL I G O C E N E TH I C K N E S S Fe e t ( m e t e r s ) CORRELATION OF MAP UNITS 4 unconformity unconformity unconformity Qal Qac Qap Tb Ts To Tla Tpml Tl Holocene Pleistocene QUATERNARY TERTIARY Oligocene Miocene GEOLOGIC MAP OF THE MORONI PEAK QUADRANGLE, WAYNE COUNTY, UTAH by Stephen R. Mattox Department of Geology Grand Valley State University Allendale, MI 49401-9403 ISBN 1 -55791 -661 -6 The Miscellaneous Publication series from the Utah Geological Survey provides non-UGS authors with a high- quality fonnat for papers concerning Utah geology. Although reviews have been incorporated , thi s publication does not necessarily conform to UGS technical, policy, or editorial standards . 1.F' MISCELLANEOUS PUBLICATION 01 -5 'tl-=W UTAH 6EOL061CAL SURVEY .,, a division of 2001 Utah Department of Natural Resources STATE OF UTAH Michael 0. Leavitt, Governor DEPARTMENT OF NATURAL RESOURCES Kathleen Clarke, Executive Director UTAH GEOLOGICAL SURVEY Richard G. Allis, Director UGS Board Member Representing Robert Robison (Chairman) ...................................................................................................... Minerals (Industrial) Geoffrey Bedell .............................................................................................................................. Minerals (Metals) Stephen Church .................................................................................................................... Minerals (Oil and Gas) E.H. Deedee O'Brien ........................................................................................................................ Public-at-Large Craig Nelson ............................................................................................................................ Engineering Geology Charles Semborski ............................................................................................................................ Minerals (Coal) Ronald Bruhn .............................................................................................................................................. Scientific Stephen Boyden, Trust Lands Administration ............................................................................. Ex officio member UTAH GEOLOGICAL SURVEY The UTAH GEOLOGICAL SURVEY is organized into five geologic programs with Administration and Editorial providing neces- sary support to the program . The ENERGY & MINERAL RESOURCES PROGRAM undertakes studies to identify coal, geothermal, uranium, hydrocarbon, and industrial and metallic resources; initiates detailed studies of these resources including mining district and field studies; develops computerized resource data bases , to answer state, federal, and industry requests for information; and encourages the pru- dent development of Utah 's geologic resources. The GEOLOGIC HAZARDS PROGRAM responds to requests from local and state gov- ernmental entities for engineering-geologic investigations; and identifies , documents , and interprets Utah's geologic hazards. The GEO- LOGIC MAPPING PROGRAM maps the bedrock and surficial geology of the state at a regional scale by county and at a more detailed scale by quadrangle. The GEOLOGIC INFORMATION & OUTREACH PROGRAM answers inquiries from the public and provides information about Utah's geology in a non-technical format. The ENVIRONMENTAL SCIENCES PROGRAM maintains and publish- es records of Utah's fossil resources, provides paleontological and archeological recovery services to state and local governments, conducts studies of environmental change to aid resource management, and evaluates the quantity and quality of Utah's ground-water resources. The UGS Library is open to the public and contains many reference works on Utah geology and many unpublished documents on aspects of Utah geology by UGS staff and others. The UGS has several computer databases with information on mineral and energy resources, geologic hazards , stratigraphic sect ions , and bibliographic references. Most files may be viewed by using the UGS Library. The UGS also manages the Utah Core Research Center which contains core, cuttings, and soil samples from mineral and petroleum drill holes and engineering geology investigations. Samples may be viewed at the Utah Core Research Center or requested as a loan for outside study. The UGS publishes the results of its investigations in the fonn of maps, reports, and compilations of data that are accessible to the pub- lic. For information on UGS publications , contact the Natural Resources Map/Bookstore, 1594 W. North Temple, Salt Lake City, Utah 84116, (801) 537-3320 or 1-888-UTAH MAP. E-mail: nrugs.geostore@state.ut.us and visit our web site at http://www.ugs.state.ut.us. UGS Editorial Staff J. Stringfellow .................................................................................................................................................... Editor Vicky Clarke, Sharon Hamre ............................................................................................................... Graphic Artists Patricia H. Speranza, James W. Parker, Lori Douglas .......................................................................... Cartographers The Utah Departmellf of Natural Resources receives federal aid and prohibits discrimination 011 the basis of race, color. sex, age, national origin, or disability. For information or complaints regarding discrimi11atio11, contact Execurive Director, Utah Department a/Natural Resources, 1594 West North Temple #3710, Box 145610 , Salt Lake City, UT 84/16-5610 or Equal Employmem Opport1111iry Commission, /801 L Street, NW, Washington DC 20507. ft . ~, Pnnted on recycled paper 10/01 GEOLOGIC MAP OF THE MORONI PEAK QUADRANGLE7 WAYNE COUNTY7 UTAH by Stephen R. Mattox Department of Geology Grand Valley State University Allendale, MI 49401-9403 email: mattoxs@gvsu.edu ABSTRACT The Moronj Peak quadrangle is 2 miles (3 km) south- west of the town of Loa in Wayne County and is near the cen- ter of the Awapa Plateau, one of the easternmost High Plateaus of central Utah. The High Plateaus represent a tran- sition zone between the fault-dominated Basin and Range Province and the relatively undeformed, subhorizontal strata of the Colorado Plateau. The quadrangle's landscape is only slightly modified by extensional faults and its strata dip gen- tly east, features more characteristic of the Colorado Plateau. Most of the surface of the quadrangle is a low-relief table- land that slopes gently to the northeast. Several hollows and draws dissect the surface to expose volcaniclastic , volcanic, and sedimentary rocks . Exposed bedrock units range in age from Oligocene-Miocene to Miocene. In ascending order, the units include the Ol igocene-Miocene volcanic rocks of Lang- don Mountain, latite lava flows, and potassium-rich mafic lava flows; and Miocene Osiris Tuff, Sevier River Forma- tion, and basalt lava flows . The volcanic rocks of Langdon Mountain record the eastward extension of a thick wedge of volcaniclastic sediment from a source on the northern Sevier Plateau . The lat ite lava flows erupted from vents on the Awapa P latea u . The potassium-rich mafic lava flows erupt- ed from ve nts on the Awapa Plateau , possibly just northwest of the Moroni Peak q uadrangle, as tectonism shifted from compression to extension. The Osiris Tuff, a widespread ash-flow tuff in the High Plateaus, assists in the correlation of units to areas outside of the q uadrangle. The Sevier River Formation preserves locally derived elastic sediments that collected in topographic lows. Basalt lava flows erupted from a vent at Elsies Nipple. Quaternary sediments are lim- ited to a few small areas and include all uvium , mixed alluvi- um and collu vi um, and pediment-mantle alluvium. Earth- quakes, flooding, rock falls, and radon pose minimal geolog- ic hazards because of the q uadrangle's remote, undeveloped location. Sand and gravel are extracted from the quadrangle for local uses. INTRODUCTION The Moron i Peak quadrangle is near the center of the Awapa Plateau, which is part of the High Plateaus of central and southwestern Utah (figure la). The Plateaus represent a transition zone between the gently dipping and flat-lying strata of the Colorado Plateau to the east and the fault-domi- nated mountains and alluvial valleys in the Basin and Range Province to the west. The Awapa Plateau is one of the east- ernmost High Plateaus and is bordered by the Fishlake Plateau to the north and Aquarius Plateau to the south (figure la). According to Van Cott (1990), Awapa is a Paiute term that means "a water hole among the cedars." The volcanic rocks of the Awapa Plateau are part of the Marysvale volcanic field (figure la). The Marysvale field covers much of the High Plateaus and extends westward into the Basin and Range Province . The volcanic rocks of the Marysvale field overlie lower Cenozoic, Mesozoic, and Pale- ozoic rocks with angular unconformity. Extensive volcanic activity began at Marysvale about 34 million years ago and continued to 19 million years ago (Rowley and others, 1994). Subsequent volcanism has been episodic, consisting of basaltic lava flows and rhyo litic ash-fall tuffs (Cunningham and Steven , 1979; Rowley and others, 1994). The volcanic rocks of the Moroni Peak quadrangle represent the east mar- gin of the Marysvale volcanic field. The surface of the Awapa Plateau , and that of the Moroni Peak quadrangle, is semi-barren, low in relief, and slopes gently to the northeast. The maximum elevation in the quad- rangle is 8,595 feet (2,620 m) at the summit of Little Flat Top and the minimum elevation is about 6,980 feet (2,128 m) along Spring Creek in Rabbit Valley (figure 1 b). Although total relief in the quadrangle is about 1,600 feet ( 488 m), suit- able locations to examine the physical characteristics of the strata are limited to local drainages. Exposures are poor on the gently sloping areas between drainages and consist of loose, weathered boulders, cobbles, slabs, or small chjps of rock. All streams in the quadrangle are ephemeral and drain east to the Fremont River. The streams dissect the plateau, creating canyons as much as 400 feet (120 m) deep and areas with good exposures . Moroni Peak, the namesake of the quadrangle, is an erosional remnant of resistant Osiris Tuff. Improved dirt roads provide access to both the plateau and the quadrangle . Geologic maps of the Awapa Plateau have been pub- lished at small scales or covering limited areas. The Awapa Plateau is part of a map at a scale of 1 :250,000 by Williams and Hackman ( 1971). A small area on the west front of the 2 114° 40° 113° 112" 111 ° 60 KILOM ETERS 40 M ILES ( Abes"Knoll / ,,-", FISHLAKE PLATEAU Loa ' ' AWAPA _,., __ , '-~·-~1•.J.l.'•~ .. ~ {' " .. _ .. _!31~o!l~w /" ,' Utah Geological Suney 111°30"00" THOUSAND LAKE MOUNTAIN L man Jakes Knoll ,, /._,/'" __ ,-,,t!l'(j Moroni Peak ~0.i-, /Q." Bicknell PLATEAU . J -WAYNE CO • - -GARFIELD co· - ' ', BOULDER 'MOUNTAIN \ 3 8"07'30.. Flossie Knoll B . Smooth Knoll Government Point Figure 1. A. Index map sho wing locations of the plateaus and ranges of the High Plateaus, Marysvale volcanic field, and adjacent areas , simplified from Rowley and others (1994). Patterned areas are underlain largely by vo lcanic rocks. B. Index map showing lo cations of plateaus , Moroni Peak and adjacent 7.5 minute quadrangles, counties , highway s. major drainages, and towns. plateau was mapped by Rowley and others (1986). T he Moroni Peak quadrangle was chosen as the first com plete quadrangle on the Awapa Plateau to be mapped at a scale of 1 :24,000 because it contains the best available exposures of most of the stratigraphic units found on the plateau. Mattox (1991b) provided an overview of the geology of the Awapa Plateau and described the petrology, age, geo- chemistry, and correlation of the volcanic rocks. For th is study, one new sample was analyzed for its major-element chemistry by X-ray fluorescence at Northern Illinois Univer- sity. Geochron Laboratories analyzed plagioclase separated from a basalt sample to provide a new K-Ar age determina- tion. All isotopic ages in this report use or have been con- verted to the decay constants of the JUGS Subcommission on Geochronology (Dalrymple, 1979; Steiger and Jager, 1977). Mapping was done during the summers of 1988, 1989, 1991, and 1992. MAP UNITS Consolidated volcanic, volcaniclastic, and sedimentary rocks exposed at the surface in the quadrangle include strata of upper Oligocene to Miocene age (plates 1 and 2). In ascending order, the bedrock units include the Oligocene- Miocene volcanic rocks of Langdon Mountain, latite lava flows, and potassium-rich mafic lava flows; and Miocene Osiris Tuff, Sevier River Formation, and basalt lava flows. Quaternary sediments include alluvium , mixed alluvium and colluvium, and pediment-mantle alluvium. Oligocene/Miocene Rocks Volcanic Rocks of Langdon Mountain (Tia) The upper Oligocene-lower Miocene volcanic rocks of Langdon Mountain are the o ldest exposed stratigraphic unit in the quadrangle. This informal stratigraphic unit was orig- inally defined by Rowley (1979) and Rowley and others (1979) for exposures of andesitic rocks at Langdon Mountain on the Sevier Plateau, 15 miles (24 km) northwest of the Awapa Plateau (figure la). Mapping by Rowley and others (1986) showed that the alluvial facies of the volcanic rocks of Langdon Mountain extended to the west front of the Awapa Plateau. Williams and Hackman (1971) mapped this unit as andesite breccia. Most of the west half of the quad- rangle consists of the volcanic rocks of Langdon Mountain. Exposures of this unit are poor on gently sloping surfaces; however, excellent exposures are found in the deeper canyons (figure 2). The unit is predominantly mudflow breccia, with minor beds of sandstone and conglomerate. The mudtlow breccia is red, gray, and white and ranges from well sorted, clast-sup- ported cobbles to poorly sorted, matrix-supported cobbles and boulders. The sandstone is well sorted and tuffaceous , Geologic map of th e Moroni Peak quadrangle Figure 2. We ll-exposed rhin beds of mudflow breccia of th e ,•olcan ic roc ks of Langdon Mountain in upper Big Hollow opposit e Cyclone Dra w (section 12 , T. 29 S., R. 2 £.). Nore geo lo g is r near top righr for scale. West Section no. 12 7 8 Figure 3. A. Diagrammatic represe nra - tion of inte1fin ge rin g of vo lcanic rocks of Lan gdon Mounrain (Tia ) and /arir e lal'G flows (Ti) in Big H ollow based on rhis mapping. 8 . lnr erprerati on of strarigra- phic relari ons based on previo us mapping by William s and Ha ckman ( 197 1 ). volcanic rocks 8. West East 3 with structureless, inversely graded, and normally graded beds. Clasts within these rocks are light-or dark-gray and plagioclase-or hornblende-phyric. Maximum long dimen- sion observed for a clast was 1.8 feet (0.55 m). In Big Hol- low (figure I b), well-stratified beds of volcaniclastic rocks range in thickness from I to 6 feet (0.3 to 2 m ) (figure 2). Maximum exposed thickness of the volcanic rocks of Lang- don Mountain in the Moroni Peak quadrangle is 350 feet (105 m); these rocks are 2,600 feet (800 m) thick at Parker Mountain, on the west, fault-bounded side of the Awapa Plateau (Mattox , 199 lb). In the western part of the quadran- gle, the base of the unit is not exposed and it is overlain by the potassium-rich mafic lava flow s (Tpml) and the Osiris Tuff (To). In Big Hollow, near the center of the quadrangle, the volcanic rocks of Langdon Mountain (Tia) interfinger with the latite lava flows (Tl) (figure 3, plate 1 ). The volcanic rocks of Langdon Mountain have not been dated directly because of the difficulties of interpreting K-Ar dates of elastic rocks. Stratigraphic relations and ages of samples from overlying strata suggest a late Oligocene to early Miocene age. Two potassium-rich mafic lava flow s on the Awapa Plateau that overlie the volcanic rock s of Langdon Mountain yielded ages of about 25 million years (Mattox, 1991 b). On the western margin of the Awapa Plateau , the Osiris Tuff (To), a 23-miJlion-year-old ash-flow tuff (Fleck and others, 1975), is interlayered with the upper part of the mudflow breccia (Rowley and others , 1986). The stratigraphic position, lithology, mineralogy, and geochemistry of the volcanic rocks of Langdon Mountain on the Awapa Plateau (Mattox, 199 lb) are similar to rocks in th e western High Plateaus, specifically the Bullion Canyon Vol- canics and the Mount Dutton Formation of Rowley and oth- ers (1994), but may not be correlative. The source area of the volcanic rocks of Langdon Moun- tain on the Awapa Plateau is probably the northern Sevi e r Plateau (figure la). Although Rowley and others (1986) pro- posed a local source on the Awapa Plateau for the unit where East Elevation (feet) 9 15 14 13 8 ,3 00 8 ,200 8,100 8,000 Langdon Mountain 7,900 7,800 7,700 7,600 latite lava flows '?, 1-- 7,500 '?- ...., '?...._ ?-. ..,.. mile '<;> '?...._ Vertical Exaggeration 1 Ox ?...... , 7,400 4 exposed along the western front of the plateau, Mattox (1991 b) argued that the gentle eastward dip of these strata and an eastward decrease in maximum clast size, abundance of breccia, and bed thickness indicated a source to the west of the Awapa Plateau (figure la). Latite Lava Flows (TI) Upper Oligocene-lower Miocene latite lava flows of the Iatite unit of Williams and Hackman (1971) underlie most of the southeast part of the quadrangle. Although this unit is trachyte based on geochemistry (figure 7), the nomenclature established by Williams and Hackman (1971) is used. On gentle slopes, the latite flows have weathered to poor expo- sures of small chips or thin slabs . However, as much as 400 feet (120 m) of flows are well exposed along steep canyon walls, such as at Big Hollow (figure 4). In Wildcat Hollow, three flows, with a combined thickness of 300 feet (90 m), are exposed as discontinuous outcrops of platy lava. Based on petrography, two types of latite lava flows are exposed in the quadrangle: black, glassy flows that contain a few per- cent phenocrysts of resorbed plagioclase, clinopyroxene, hornblende, and iron oxides; and medium-gray, structureless or flow-banded latite lava flows that have more conspicuous phenocrysts of plagioclase and lack hornblende. Latite lava flows form the base of the exposed strati- graphic section in the southeast part of the quadrangle. In Big Hollow, the lava flows interfinger with the volcanic rocks of Langdon Mountain (plate 1, figure 3). The lava flows crop out beneath the volcanic rocks of Langdon Mountain (Tla) in NEI/4 section 15, T. 29 S., R. 2 E. and climb rapidly to the east, relative to the volcanic rocks of Langdon Mountain (Tla), reaching near the rim of the hollow in NWl/4 section 14, T. 29 S., R. 2 E. A thin flow of latite caps the wedge of volcanic rocks of Langdon Mountain (Tla) and extends 2.5 miles (4 km) to the west to NEl/4 section 8, T. 29 S., R. 2 E. This flow, in turn, is overlain by a higher eastward-thinning Utah Geological Survey wedge of volcanic rocks of Langdon Mountain that extends eastward to NWl/4 section 16, T. 29 S., R. 2 E. and NWl/4 section 9, T. 29 S., R.2 E. The maximum exposed thickness of the latite lava flows is 400 feet (120 m) in Big Hollow (fig- ure 4). The latite lava flows (Tl) are conformably overlain by thin wedges of volcanic rocks of Langdon Mountain (Tla) and by the potassium-rich mafic lava flows (Tpml). The unit is unconformably overlain by the Osiris Tuff (To) and basalt lava flows (Tb). The late Oligocene to early Miocene age for the latite lava flows is constrained by a single K-Ar date and by strati- graphic position. A date of 23.1 ± 1.0 million years ago was reported by Mattox (1991b) for a sample (AP 119) collected in Wildcat Hollow just outside of the southeast corner of the quadrangle. The 23-million-year-old Osiris Tuff (Fleck and others, 1975) overlies the latite lava flows. Correlation of the latite lava flows beyond the Awapa Plateau is difficult. Three stratigraphic units mapped else- where in the High Plateaus -the Antimony Tuff Member of the Mount Dutton Formation (Anderson and Rowley, 1975), the tuff of Albinus Canyon (Steven and others, 1979; Cun- ningham and others, 1983; Willis, 1986), and the lava flows of Deer Spring Draw (Nelson, 1989) -share a similar strati- graphic position and mineralogy with the latite lava flows but differ considerably in geochemistry and age. Both the Anti- mony Tuff Member and the tuff of Albinus Canyon, which are below the Osiris Tuff, are crystal poor and feldspar bear- ing, characteristics shared with the latite lava flows. Because of the reconnaissance nature of the mapping of Williams and Hackman (1971), all three tuff units may have been lumped within the latite unit. However, unpublished geochemical data of Stephen Mattox and Grant Willis (Utah Geological Survey) are distinctive for each of the units, and K-Ar ages reported by Rowley and others (1994) show the Antimony Tuff and the tuff of Albinus Canyon to be 25 million years old, significantly older than the 23-million-year-old date on the latite. The lava flows of Deer Spring Draw, exposed Figure 4. Latite lava flows that are well exposed in the walls of Big Hollow in SI /2 section 12 and N 1 h section 13, T. 29 S., R. 2 E. Thousand Lake Mountain in background. View is to the east. G eologic map of th e M o roni Peak quadrang le north of Thousand Lake Mountain, have been described by Nelson (1989). Characteristics shared with the latite lava flows on the Awapa Plateau include stratigraphic position and low abundance of phenocrysts . However, the lava flows of Deer Spring Draw are older (26.3 million years old) a nd significantly different in chemical composition (figure 7; Nelson, 1989). Field relations between the latite and other stratigraphic units of the Awapa Plateau clearly demonstrate that the latite lava flows are relatively thin and laterally dis- continuous (Mattox, 1991 b ), suggesting that they erupted in s mall volumes from local vents and never extended beyond the margins of the plateau. Potassium-Rich Mafic Lava Flows (T pml) The basaltic andesite unit of Williams and Hackman (1971) is herein referred to as potassi um-rich mafic lava flows . Williams and Hackman (1971) based the name of the unit on mineralogy. Chemically, the rocks are latite or banakite using the classification schemes of Le Bas and oth- e r s (1986) and Peccerillo and Tay lor (1976), respective ly. The new des ignation is based on s tratigraphic nomenclature of s imilar rocks to the west, on mineralogy, and on the chem- ical compo ition of the lava flows. On the Markagunt Plateau and adjacent valleys (fi g ure la), mafic lava flow s with greate r than 3 weight-percent potass ium are informally desig na ted potassium -rich m afic lava flows by Anderson and others (1980, 1981) and Cunningham and others (1983). This chemical criterion distingui s hes these flows from upper Cenozoic (less than 16 million years old) mafic flows that are lithologically s imilar but contain less than 3 weight percent potass ium (Best and others, 1980; Mattox, 1994 and 1997 ; Rowl ey and others, 1994). The potassium-rich mafi c lav a flow s are exposed over large areas in th e northe rn and northeastern part of the quad- rangle. The flows are also exposed in s maller outcrops of limited extent in the south-central part of the quadrangle and in Wildcat Hollow. The best exposures are in Long Hollow (figure 5 ). Most of the flows weather to di scontinuous led ges or boulder-strewn hills ides. They are medium-gray to bl ack and porphyritic, with n early equal amounts of clinopyroxene and s ieve-textured, embayed pl agioc lase ph e nocrysts. The flow s conta in less abundant phe nocrysts of olivine, some altered to iddings ite, orthopyroxene, and iron oxides. The phe nocrys ts are in a groundmass of plagioclase rnicrolites and less abundant iron oxides and g lass. Ve s icles are com- mon and e lon gate in the direction of flow. In the Moroni Peak quadrangle, the potassium-rich mafic lava flows con - formably overli e th e volcanic rocks of Langdon Mountain (Tla) and latite lava fl ows (Tl) and un conformably und e rli e th e O s iri s Tuff (To), the S ev ier Rive r Formation (Ts), and the basalt lava flows (Tb). The stratigraphic position of the po tass ium -ri c h mafic lava flow s, be neath th e O siris Tuff, dif- fers from the re lations to the west, where the potassium-rich m afic volcanic rocks li e tratigraphically above th e Osiris T uff (R ow ley and others, 1994). Maximum thi c kness of the flows is approx imate ly 400 feet (1 2 0 m) in a hill southeast of E ls ies Nipple (secti on 34, T. 28 S., R. 2 E .) where flows filled a broad topographic d e press ion in th e volcanic rocks of Langdon Mountain. Ve nts for th e flows were not found in the quadrangle. However, th e flow s can be fo llowed gradu - a ll y uphill to the northwest for four mil es (2.5 km) to Black 5 Figure 5 . Potassium -rich mafic lava flows that are well exposed along much of Long Hollow. Point, a po ss ible vent in the adjacent Abes Knoll quadrangle. Based on K -Ar dates and s tratigraphic relations , th e potassium-rich mafic lava flows in the Moroni Peak qu ad - ran g le are Oligocene to Miocene. B est and others (1980) determined a K -Ar whole-rock d a te of 24.5 ± 0.4 million year s for a sampl e from a lava flow so uth of F is h Lake th at was originally mapped b y Williams and Hackman (197 1) as la tite and basaltic andesite undifferentiated. Geochemical data presented in Mattox ( I 991 b) s howed that thi s lava flow is potassium-rich and is not a latite . Three K -Ar plagioclase dates were reported for the potassium-rich mafic lava flow in Mattox ( 1991 b). Two of these, from th e eastern ( AP 126) a nd so uth ern (AP 4 7) marg ins of th e plateau , yield e d dates of 25.8 ± 1.4 and 25.2 ± 1.6 million years, respectively. The third sampl e (A P 99) from the top of a section of th e unit and jus t beneath th e Osiris Tuff, provided a date of 23.3 ± 1.5 million years . On the Awapa Pla teau , all potassium-rich m afic lava flows und erlie the Osiris Tuff, a reg ional s trati- graphi c marker that has b een dated at about 23 million years o ld (Fleck and othe rs, 1975 ). Lithology, mineralo g y, texture, and ch emical compo i- tion indicate th at th e potass ium-rich mafic lava flows of the Awa p a Plateau (Mattox, 1991 b) are s imilar in c haracter to th e potassium -rich m afic volcanic rocks to the west (Rowl ey a nd others , 1994) a nd the lava flows of Riley Springs to the north (Nelson , 1989). 6 The potassium-rich mafic volcanic rocks to the west were interpreted by Rowley and others (1994) to be the first eruptive products associated with an increase in extensional deformation in west-central Utah. Mattox (1991a) and Mat- tox and Walker ( 1989), however, used geochemistry to sug- gest that the volcanics are related to the demise of subduction beneath western North America. Miocene Rocks Osiris Tuff (To) A welded, vitric-crystal ash-flow tuff on the Sevier, Fishlake, and Awapa plateaus was mapped and informally designated the tuff of Osiris by Williams and Hackman (1971). Anderson and Rowley (1975) recognized the tuff throughout the Marysvale volcanic field and formally defined it as the Osiris Tuff. Excellent exposures of the Osiris Tuff can be found in upper Long Hollow in the extreme northwest comer of the quadrangle. In the south, two mesas, Big Flat Top and Little Flat Top, provide expo- sures of moderate quality suITounded by large, weathered boulders of tuff. At Big Rocks, in the northeast corner of the quadrangle, the tuff is poorly exposed in small knobs and shallow drainages. The Osiris Tuff consists of orange, reddish-brown, or light-gray, resistant, densely welded, crystal-poor ash-flow tuff. Black vitrophyre is exposed at the base of the tuff in upper Long Hollow. South of Big Rocks, the basal vitro- phyre is underlain by 2 feet (0.5 m) of light-gray, thin-bed- ded ash, possibly a base surge deposit (figure 6). In the main body of the tuff, plagioclase is the most common phenocryst. Sanidine and biotite are present in minor amounts. Phe- nocrysts of clinopyroxene and iron oxides are rare. The tuff weathers to pebble-s ized chips, ledges, boulders, and cliffs. Poor exposures of the tuff resemble weathered Jatite Java flows but are distinguished by the presence of biotite. Max- imum exposed thickness of the tuff in the quadrangle is about 130 feet (40 m) at Big Flat Top. The basal vitrophyre is a few feet thick. The Osiris Tuff unconformably overlies the vol- canic rocks of Langdon Mountain (Tia), the latite lava flows (Tl), and the potassium-rich mafic lava flows (Tpml). The Osiris Tuff is 23 million years old (Rowley and oth- ers, 1994), based on three concordant K-Ar dates reported in Fleck and others (1975). The Osiris Tuff erupted during sub- sidence associated with development of the Monroe Peak caldera in the northern part of the Sevier Plateau (Steven and others, 1984 ). Sevier River Formation (Ts) Williams and Hackman (1971) informally assigned well- bedded conglomerate, sandstone, and siltstone to their vol- canic sediments unit. They recognized that this unit was at least partly equivalent to the Sevier River Formation of Callaghan ( 1938). The Sevier River Formation consists of alluvium that was derived from uplifted areas and deposited in adjacent valleys. Based on stratigraphic position , litholo- gy, and age, similar sedimentary strata of the Moroni Peak quadrangle will be referred to as the Sevier River Formation. The Sevier River Formation is well exposed in the first drainage north of Blackburn Hollow (section 36, T. 28 S., R. Utah Geological Survey Figure 6. Thin beds of ash, possibly of base surge origin, exposed beneath the basal vitrophyre of the Osiris Tuff in SEl/4 section 25, T. 28 S., R. 2 E. 2 E.). The best exposures are in and immediately adjacent to the stream bed. Upslope, away from the stream bed, the stra- ta have weathered to pebble-and cobble-covered slopes. A continuous section of Sevier River Formation is exposed in road cuts in Big Hollow about 0.5 mile (0.8 km) east of the east margin of the quadrangle. In the Moroni Peak quadrangle, the Sevier River Forma- tion consists of gray, light-brown, or greenish-gray, moder- ately consolidated, medium-to thick-bedded sandstone and conglomerate. Subrounded clasts within the conglomerate were derived from the volcanic rocks of Langdon Mountain, latite lava flows, and potassium-rich mafic lava flows . The formation was probably of fluvial origin and represents an early episode of sedimentation that filled some paleo-valleys. Subsequent erosion removed most of the sediment, leaving remnants on valley floors (section 36, T. 28 S., R. 2 E.), and, just east of the quadrangle, plastered against valley walls (section 7, T. 29 S., R. 3 E.) and protected beneath resistant caprock (section 6, T. 29 S., R. 3 E.). In the Moroni Peak quadrangle, the Sevier River Formation unconformably overlies the potassium-rich mafic lava flows (Tpml) and Osiris Tuff (To). The contact with the overlying basalt lava flows (Tb) is sharp. Maximum thickness in the quadrangle is about 100 feet (30 m). In road cuts about 0.5 mile (0.8 km) east of the quadrangle, the formation is 200 feet (60 m) thick. Geologic map of th e Moron i Peak quadrang le The age of the Sevier River Formation in the Moroni Peak quadrangle is probably Miocene but is difficult to bet- ter constrain. It overlies Osiris Tuff (To) and, in section 25 , T. 29 S ., R. 2 E., underlies basalt lava flows (Tb) that have not been dated. The basalt lava flows in section 25, howev- er, may be an erosional remnant of flows that originated from Elsies Nipple. The flows from Elsies Nipple have been dated at 6.9 ± 0.3 million years (late Miocene) (see below) where they overlie the Sevier River Formation immediately east of the Moroni Peak quadrangle. Basalt Lava Flows (Tb) Late Cenozoic basaltic volcanic centers are concentrated along the periphery of the Marysvale field (Dutton, 1880; William s and Hackman, 1971; Cunningham and others, 1983 ; Steven and others, 1990). Basaltic vents are rare in the interior of the volcanic field (Rowley and others , 1994). On the Awapa Plateau , basaltic volcanic centers are common because th e plateau is on the extreme east margin of the Marysvale volcanic field (figure la; Williams and Hackman, 1971). A single basalt volcanic center, Elsies Nipple , located near the center of the quadrangle, contains pahoehoe lava that spread radially as much as 4 ,000 feet (1,220 m) in all directions from the vent. Two flow s extend still farther east. The northern of these flows (Nl/2 section 34, T. 28 S., R. 2 E .) followed a valley for about 4,000 feet (1 ,220 m) beyond the margin of the main flow. The south flow (section 3, T. 29 S., R. 2 E.) moved to the s outheast, passed through a topo- graphic constriction, ponded in Terza Flat, and continued east, terminating about 500 feet (150 m) outside the quad- rangle. After this flow was emplaced, the topography has reversed and the lava flow, which originally filled a topo- graphic low, now s tands above adjacent rocks. This reversal is mos t pronounced in Sage Flat Draw where the stream has preferentially cut into the older latite lava flows. In most places, the margin of the flow is a steep cliff 10 to 20 feet (3- 6 m) high that provides good exposures. The surface of the flow weathers to slabby float. A second area of basalt lava flow i s between Big Rocks and Blackbum Hollow. There is no recognizable vent associated with this lava and it may be the erosional remnant of the northern flow from Elsies Nip- ple. The margin of thi s flow is not a steep cliff and exposures are poor, consisting of small boulders and slabby float. The basalt lava flows are dense and black, dark gray, and reddish brown in color. They contain olivine phenocrysts, commonly altered to iddingsite, and less abundant phe- nocrysts of plagioclase and clinopyroxene in a gro undmas s of plagioclase microlites, iron oxides, and glass. Basalt lava 7 flows unconformably overlie all of the older stratigraphic units . Near the vent, lava has accumulated to a thickness of about 270 feet (80 m). The maximum thickness of the distal margin of the flow is 25 feet (8 m). The basalt flows in the quadrangle are probably Miocene. A new K-Ar date of 6.9 ± 0.3 million years was determined on a feldspar concentrate from a sample collect- ed north of Sage Flat Draw at the terminus of the lava flow (table 1) just east of the quadrangle boundary. A similar date, 5.9 ± 0.6 million years was reported in Mattox (1991b , AP 127) for a basalt flow on the extreme eastern margin of the Awapa Plateau. Best and others (1980) reported three dates, ranging from 5.0 to 6.6 million years old, for basalt flows near the southwestern margin of the plateau. Just north of the Awapa Plateau , a basalt flow was dated at 16.4 ± 1.0 million years, the oldest so far reported in the High Plateaus (Mattox, 1991b, AP 26). Northeast of the Awapa Plateau, basalt lava flows dated by Delaney and others (1986) and Nelson (1989) range in age from 3.8 to 5.4 million years old. Quaternary Deposits Three Quaternary units were mapped in the Moroni Peak quadrangle. All are derived by fluvial and sheetwash erosion of local bedrock units and unconformably overlie older units. Talus and colluvial deposits, common near the base of steep hillsides , were not mapped due to limitations of map scale and the generally poorly defined morphology of such deposits. Pediment-Mantle Alluvium (Qap) Bullhead Bench in the northeastern comer of the quad- rangle consists of gray or light-brown, unconsolidated, fine gravel that mantles pediment surfaces. The gravel was derived from erosion of the underlying Osiris Tuff. Streams have dissected the gravels down to the pediment surface, exposing a maximum thickness of 40 feet (12 m). The deposit is interpreted to be Pleistocene. Mixed Alluvial and Colluvial Deposits (Qac) Mixed alluvial and colluvial deposits form gentle slopes below steep escarpments, fill valleys, and include older stream deposits. The deposits consist of gray or light-brown, unconsolidated to weakly consolidated mud, sand, cobbles, and boulders. Modem streams have dissected the deposits in Long Hollow. An extensive deposit in Long Hollow exceeds 100 feet (30 m) in thickness. Relatively thin, less than 20 feet (6 m) thick, mixed alluvial and colluvial deposits were Table 1. Data for new potass ium-argon date , Moroni Peak quadrangle ,Utah.1 Rock Unit Basa lt lava Location Awapa Plateau3 Sample AP 173 4 1 Age detennination by Geochron Labora tori es, Cambridge, MA. Material2 feldspar 1.27 0.000399 2 Constant s: A~= 4.962 x 10·10/year, (Ae + Ae') = 0.58JxJ0·10/year, and 4°K/K=l.93x l0-4g/g . 3 NE 1/4 secti on 7, T.29S., R.3E.; 38°18' 3 I "N, I 11 °37' 25" W. In Bi cknell quadrangle (fi g ure lb) near boundary with Moroni Peak quadrangle . 4 Same lava flow as AP I 07 , see tab le 2. Apparent Age 6.9 ± 0 .3 Ma 8 mapped along several upland draws south of Long Hollow and in tributaries just west of Wildcat Hollow. The deposits are interpreted to be Pleistocene and Holocene. Alluvium (Qal) Alluvium covers low areas in Long Hollow, at Big Rocks, in the first drainage north of Blackbum Hollow, and along Spring Creek in Rabbit Valley. Alluvium is also found in Sage Flat Draw, Big Hollow, Balsam Hollow, and Wildcat Hollow where, due to limitations of map scale, it has been mapped as narrow discontinuous deposits. The alluvium consists of gray or light-brown silt, sand, and gravel that were deposited by intermittent streams. Maximum exposed thickness is 20 feet (6 m). The deposits are late Pleistocene and Holocene. GEOCHEMISTRY Volcanic rocks from the Moroni Peak quadrangle range in composition from basalt to trachyte (appendix 1, table 2, figure 7). Most map units are chemically distinct with the notable exception of the latite lava flows and the Osiris Tuff, which are remarkably similar. Classification of volcanic rocks is based on the scheme of Le Bas and others (1986). Mattox (1991b) presented additional geochemical data on volcanic rocks collected on the Awapa Plateau outside of the quadrangle. Clasts within the volcanic rocks of Langdon Mountain (Tla) are andesite and dacite (figure 7). They are very simi- lar in composition to lava flows in the Mount Dutton Forma- tion, a unit on the south flank of the Marysvale volcanic field (figure 7) (Mattox, 1991b). Mattox and Walker (1992) stud- ied the chemistry of Mount Dutton andesite and noted its similarity to modern orogenic andesite and suggested a mag- matic source in Proterozoic lithosphere. The latite lava flows (Tl) plot within the field defined for trachyte rather than latite (figure 7). Their major-element chemistry is very similar to the Osiris Tuff except iron oxide and calcium oxide concentrations are slightly higher and lower, respectively. The chemical similarity of the two units may indicate a common source, perhaps in the crust, or a par- allel magmatic history. Although the latite lava flows are tra- chyte based on their chemical composition, they are latite based on their mineral composition, which is a more useful classification for field mapping. Based on their chemistry, the potassium-rich mafic lava flows (Tprnl) are latite. These same rocks are banakites using the classification scheme for potassium-rich rocks pro- posed by Peccerillo and Taylor (1976). The lava flows are chemically similar to potassium-rich mafic volcanic rocks of Rowley and others (1994) to the west (Mattox, 1991b) and the lava flows of Riley Spring, north of Thousand Lake Mountain (Nelson, 1989) (figure 7). Mattox (1992a) ana- lyzed representative samples from all potassium-rich mafic volcanic rocks on the High Plateaus and found a range in sil- ica compositions from 48 to 59 weight percent, with rocks from the Awapa Plateau being relatively rich in silica. Row- ley and others (1994) interpreted the potassium-rich mafic volcanic rocks in the High Plateaus as marking an increase in extensional deformation in the area about 23 million years B OOM-NV"'l-OON\OV')O O\r-NON-OMMMV')'"d'" -r....:--=v.;ooo°'C"')NOO 'SI" ---~ N V 00 0 \0 -V1 - -V V oo r-_, -N -r-0 0 000 N -\O_;v-iciciOciMNciO\ V ----0\ \0 v=; ~ = ~ ~ &;; ~ ~ ~ ~ ~ -\Oor....:oooN\OMC"')ciO.: "' -°' ,....;NOO\ONVill"'IV0\\00 V) ~ q ~ "1 -; ~ -: ~ q ~ ~ -oo-\Or-ONV)C"")VOr- v, -°' r-MVO\OOOOl/iO\V)V) ('f')O\('f')V)--0\0\-MVO -00 _; \0 ci ci ~ 0\ M _; ci _; 'SI" 0 V-N-NOOO\t"-O\t"-00 NONr--OOV"'lO\r-Vr- r-a.: .....: \0 \0 ci N V) M M ci 0\ "' °' r-O\-VOO\Or-r-\O- V)\OOOOO-V1VVM-O\ V) . . . . . . . . . . . r--Ov.NOO-'S!"-0000 '° °' 0\ 00 \0 V"'l V) 0 0\ 00 V"'l V"'l 0\ V\OOt"-0\0 ('f")'V C"')-O\ (""') .......... . r-0 \0 NO O -V \00 r-'° °' ....J <'> <'> <( N N O o o o O o O o"'E-' Q Q N CS ~ bJl N 0 ·-·-::;; " ""' '" z'" S ' N Cl'.) E-...... ~ ""u ..... c.. E-' 6;' 00 °' C: 0 "' 0 z .s cl ~ 0 0. ~ "' J !i: ....; r-- ~ 2!; 8 t~~ E " " ~ 0.. c.. ;J' ~ ~ oci ...... Geolog ic map of the Moroni Peak quadrangle ~ 0 -g 0 N ::.::: + 0 N ro z 16 14 12 10 8 6 4 2 foidites picro- basalt basalt phonolite trachyte,.p basaltic andesite andesite dacite rhyolite 37 41 45 49 53 57 Si02wt.% 61 65 69 73 Q) 0) C cu I.... "'O cu ::, O" (/) .c ..... (/) cu ~ cu >, .0 I.... cu Q) C + X D • ~ liiiii 0 • .6. .... V T 0 * e Q I] • i volcanic rocks of Langdon Mountain (Mattox, 1991 b) sample AP65 . volcanic rocks of Langdon Mountain (Mattox, 1991 b) sample AP67. latite lava flows (Mattox, 1991b) sample AP60 . latite lava flows (Mattox, 1991 b) sample AP62. latite lava flows (Mattox, 1991 b) sample AP63. latite lava flows (NE1/4 , sec. 15, T29S, R2E) sample AP171 . potassium-rich mafic lava flows (Mattox, 1991 b) sample AP104. potassium-rich mafic lava flows (Mattox, 1991 b) sample AP105 . Osiris Tuff (Mattox, 1991 b) sample AP101. Osiris Tuff (Mattox, 1991 b) sample AP103 . Osiris Tuff (Mattox, 1991 b) sample AP110 . Osiris Tuff (Mattox, 1991b) sample AP64. basalt lava flows (Mattox, 1991 b) sample AP107 . Mount Dutton Formation (Mattox, 1991 b) sample BC5. potassium-rich mafic lava flows (M.G. Best, unpublished data, 1986) sample HPL-3 (reported in Nelson, 1989). lava flow of Riley Spring (Nelson, 1989) sample 2. lava flow of Deer Spring Draw (Nelson, 1989) sample 12 . trachybasalt lava flow of Geyser Peak (Nelson, 1989) sample 17. trachybasalt lava flow of Forsyth Reservoir (Nelson, 1989) sa mple 18. trachybasalt dike (Gartner, 1986) sample AVG 18. 77 Figure 7. IUGS classification of vo lcanic rocks (Le Bas and others, 1986) in the Moroni Peak quadrang le with comparisons from nearby areas. 9 ago . The potassium-rich mafic lava flows of the Awapa Plateau are sli g htly older, 25 to 23 million years old, and probably erupted during a compressional, transitional, or less extensional tectonic regime (Mattox, 1992a). Mattox (1992a, 1993) proposed mixing of two sources in the litho- spheric mantle, veins of mica-ri c h minette and mica-ric h me lan ephe le nite (see Tingey and others, 1991), to explain the geochemical characteristics of the potassium-ri c h mafic vol - cani c rocks. One of these sources, veins of mica-ri c h melanephe lenite in the mantle, was dominant during earlier andesitic Mount Dutton volcanism in the southeast part of Marysvale. A sample coll ected from the basalt lava flows (Tb) erupt- ed from E lsies Nipple plot in the basalt fi eld (fig ure 7). JO Mattox (1991b) analyzed 28 late Cenozoic Java flows on the Awapa Plateau and found most samples to be basalt or tra- chybasalt with only a few basaltic trachyandesites. Mafic rocks at Geyser Peak and Forsyth Reservoir (Nelson, 1989), just north of Thousand Lake Mountain, and in the San Rafael and Capitol Reef areas (Gartner, 1986), are slightly more alkalic relative to the basalt in the Moroni Peak quadrangle (figure 7). The composition of basalts changes systematical- ly across the High Plateaus (Mattox, 1992b). Tholeiitic basalts are abundant in the west, on the Markagunt Plateau and adjacent areas (figure 1 a). Alkali basalts are abundant in the east, on the Sevier and Awapa plateaus. Mattox (1994, 1997) suggested that this pattern reflects progressively lower degrees of partial melting at greater depths from west to east beneath the High Plateaus. STRUCTURE AND TECTONICS The Awapa Plateau is one of the easternmost plateaus in the High Plateaus of Utah. In general, these plateaus consist of gently dipping strata bounded by steep normal faults and separated by alluvium-filled valleys. Rowley and others (1979) noted that the interior of each plateau is cut by rela- tively few faults and that the abundance of faults and their stratigraphic displacement decreases eastward across the High Plateaus to the edge of the nearly unfaulted Colorado Plateau. The west front of the Awapa Plateau is bounded by a normal fault with about 1,600 feet (500 m) of vertical dis- placement. Movement along this fault, to produce the Awapa and Aquarius Plateaus, probably occurred in the last 5 mil- lion years (Rowley and others, 1981). The east margin of the Awapa Plateau is defined by the contact of gently east-dip- ping bedrock units and overlying valley-fill deposits. Strata are displaced by two main faults in the Moroni Peak quadrangle. The western fault, in the north-central part of the quadrangle, strikes north and extends from Sage Flat Draw to north of Long Hollow; it creates the east margin of a shallow, alluvial-filled basin northeast of Moroni Peak. Vertical displacement on the fault adjacent to the basin is roughly 50 feet (15 m). The displacement decreases to the south to less than 10 feet (3 m) at Sage Flat Draw. The east- ern fault, in the northeast part of the quadrangle, strikes northwest and terminates to the south near Sage Flat Draw. This fault is well expressed 3 miles (5 km) north of the Moroni Peak quadrangle near Loa, where it forms a 150-foot (45 m) high, northwest-facing, arcuate escarpment defined by potassium-rich mafic lava flows. Displacement along this fault also decreases to the south and is approximately 10 feet (3 m) at Sage Flat Draw. Between these two faults, a minor north-northwest-striking fault bounds the east margin of Terza Flat and is truncated by the northwest-striking fault. Displacement on this fault at Terza Flat is roughly a few tens of feet. The timing of faulting in the Moroni Peak quadrangle is constrained by relations with the basalt lava flows (Tb). The north and north-northwest striking faults are well-expressed in the potassium-rich mafic lava flows (Tpml) but are buried by the basalt lava flows (Tb), suggesting that these faults formed between about 23 and 7 million years ago. It is pos- sible that these faults are related to the onset of extension, which appears to have began about 21 million years ago Utah Ge o lo gical Swwy (Rowley and others, 1981). In contrast, the northwest-strik- ing fault offsets the basalt lava flows north of Sage Flat Draw, indicating that this fault was active after about 7 mil- lion years ago. Rowley and others (1979) suggested that the greatest displacements on faults in the High Plateaus took place about 7 million years ago. On the Sevier Plateau, im- mediately west of the Awapa Plateau, Rowley and others (1981) bracketed the age of major faulting between 8 and 5 million years ago. Nelson (1989) reported faults younger than 5 million years old about 12 miles (19 km) northeast of the Moroni Peak quadrangle. It is likely that all of the fault- ing in the Moroni Peak quadrangle is in the range of 8 to 5 million years old as proposed by Rowley and others (1981 ). No faults that cut Quaternary deposits have been mapped in the quadrangle, and no fresh scarps were recognized in the older bedrock units. Joint sets are well exposed in the Osiris Tuff at Big Rocks. The near-vertical joints strike N. I 0 °E. at higher elevations and N. 1 °E. at lower elevations. The joints are uniformly spaced at about 50 feet (15 m). GEOLOGIC HISTORY The geologic history of exposed rocks in the Moroni Peak quadrangle begins with coeval volcaniclastic sedimen- tation and volcanism in the late Oligocene in the Marysvale volcanic belt. Volcanic debris eroded from volcanic centers in the northern part of the Sevier Plateau was shed to the southeast, constructing an eastward-thinning wedge of vol- caniclastic sediment (volcanic rocks of Langdon Mountain). Volcanic vents along the east margin of the Awapa Plateau erupted latite lavas that flowed to the west, filling topo- graphic lows and burying the edges of the volcaniclastic wedge. Pulses in sedimentation and volcanism resulted in interfingering volcaniclastic sediments and lava flows. Shortly after sedimentation and volcanism ceased, new vol- canic centers, possibly just northwest of the Moroni Peak quadrangle, erupted potassium-rich mafic lava flows. These eruptions began in the late Oligocene and continued into the early Miocene. Erosion followed, producing topography very similar to that of the present. In the early Miocene, the Osiris Tuff was erupted as the Monroe Peak caldera formed on what is now the Sevier Plateau and blanketed the High Plateaus in a layer of ash . Subsequent erosion removed much of the Osiris Tuff from the quadrangle and established a drainage system that flowed to the east and northeast. Some alluvium was trapped in local basins to produce the Sevier River Formation. In the late Miocene a single vol- canic vent near the center of the quadrangle erupted basalt that moved radially away from the vent and ultimately filled two shallow drainages to the east. Extensional faulting, per- haps associated with uplift of the plateau, occurred shortly before and after basaltic volcanism. Erosion continued, in some areas preferentially removing relatively soft latite lava flows in preference to more resistant basalt lava flows and thus generating reverse topography. ECONOMIC GEOLOGY Small operations remove sand and gravel from excava- tions in the pediment mantle alluvium (Qap) at Bullhead Geologic map of ri,e Mo roni Peak quadrang le Bench. The sand and gravel is used locally for construction of roadways and for fill. WATER RESOURCES Annual precipitation on the Awapa Plateau is between 20 and 40 inches (50 and lOO cm). The quadrangle serves as a recharge area for aquifers utilized by farmers and ranchers in the upper Fremont River valley. Ground water in the north- west part of the quadrangle migrates north-northeast to Roads Creek valley west of Loa. Ground water in the south part of the quadrangle migrates northeast where it supplies springs on the east margin of the plateau and at Bicknell Bot- toms . Artesian conditions at Roads Creek valley and Bick- neJI Bottoms result from water under pressure entering the valley fill from the underlying volcanic rocks (Bjorklund, 1969). No wells or s prings are located in the quadrangle. Ranchers have constructed tan.ks to trap surface water. GEOLOGIC HAZARDS The principal geologic hazards in the quadrangle are related to earthquakes, flooding , and radon. Black (1993) noted that the Moroni Peak quadrangle lies in an area with a moderate to hi g h radon-hazard potential. Although present- ly und eveloped , s teep slopes and cliffs throughout th e quad- rangle are susceptible to rock faJI hazards. Some slopes may be susceptible to mass movements, although none were iden- tified and mapped during thi s project. Earthquakes There is no evid ence to indicate that any historical earth- quakes produced s urface movement along faults within the II quadrangle. Two historical earthquakes with epicenters in the quadrangle (near section 23, T. 29 S., R. 2 E. and section 18 , T. 28 S., R. 2 E.) had magnitudes between 2 to 3.9 (Goter, 1990). An earthquake with a magnitude of roughly 3 occurred 15 miles (25 km) southwest of the quadrangle on November 18, 1945 (Sue Nava, University of Utah Seismo- graph Stations, verbal communication, 1995). The potential for damage in the quadrangle is small because of the lack of homes or major buildings. Flooding Inten se storms or long periods of rainfall may cause flooding along stream channels. Most roads parallel or cross major streams and may be damaged by, or be impassable during, a flood. The streams are confined to narrow bedrock canyons and have not developed floodplains. With the exception of the roads, no development has taken place along the streams. Significant rainfall events may also produce debris flows that could damage roads. ACKNOWLEDGMENTS Michael Ross, formerly with the Utah Geological Sur- vey, provided numerous useful s uggestion s in both the office and in the field. Bob Biek, also of the Survey, saw the man- uscript and map through final review and publication. Mal- colm Weiss , Rose O'Neill , and Lisa Sachnoff assisted with field work. Mr. and Mrs. Marion Wan.kier and Mr. and Mrs. Bill Rice provided logistical s upport. I thank Robert Ward and Neil Dickey of Northern Illinois University for new major-element analyses of volcanic rocks. Peter Rowley, Frank Ashland, Bryce Tripp, and Jon King provided us efu l reviews. 12 Ural, Geological Survey REFERENCES Anderson, J.J., and Rowley, P.D., 1975, Cenozoic stratigraphy of southwestern High Plateaus of Utah, in Anderson, J.J ., and Rowley, P.D., Fleck, R.J., and Nairn, A .E.M., editors, Cenozoic geology of the southwestern High Plateaus of Utah: Boulder, CO, Geological Society of America Special Paper 160, p . 1-51. Anderson, J.J., Lanigan, J.C., Cunningham, C.G., and Naeser, C.W., 1981, Geologic map of the Beaver SE quadrangle, Beaver County, Utah: U.S. Geological Survey Miscella- neous Field Studies Map MF-1274, scale 1:24,000. Anderson, J.J., Sigmund, J.M., Cunningham, C.G., Steven, T.A ., Lanigan, J.C., and Rowley, P.D., 1980, Geologic map of the Delano Peak SW quadrangle, Beaver County, Utah: U.S. Geological Survey Miscellaneous Field Studies Map MF-1255, scale 1 :24,000. Best, M.G., McKee, E.H., and Damon, P.E., 1980, Space-time- composition patterns of late Cenozoic mafic volcanism, southwestern Utah and adjoining areas: American Journal of Science, v. 280, p. 1,035-1,050. Bjorklund, L.J., 1969, Reconnaissance of the ground-water resources of the upper Fremont River Valley, Wayne Coun- ty, Utah: State of Utah, Department of Natural Resources Technical Publication No. 22, 54 p. Black, B.D., 1993, The radon-hazard-potential map of Utah: Utah Geological Survey Map 149, scale 1:1 ,000,000. Callaghan, Eugene, 1938, Preliminary report on the alunite deposits of the Marysvale region: U.S. Geological Survey Bulletin 886-D, p. 91-134. Cunningham, C.G., and Steven, T.A., 1979, Mount Belknap and Red Hills calderas and associated rocks , Marysvale vol - canic field, west-central Utah: U.S. Geological Survey Bul - letin 1468 , 34 p. Cunningham , C.G., Steven, T.A., Rowley, P.D., Glassgold , L.B., and Anderson, J.J., 1983, Geologic map of the Tushar Mountains and adjoining areas, Marysvale volcanic field, Utah: U.S. Geological Survey Miscellaneous Investigations Series Map 1-1430-A, scale 1:50,000. Dalrymple, G .B., 1979, Critical tables for conversion of K-Ar ages from old to new constants: Geology, v. 7, p. 558-560. Delaney, P.T., Pollard, D.D., Ziony, J.I., and McKee, E.H., 1986, Field relations betwe en dikes and joints : emplacement processes and paleostres s analysis: Journal of Geophysical Research, v. 91 , p. 4 ,920-4,938. Dutton, C.E., 1880, Report on the geology of the High Plateaus of Utah with atlas: U.S. Geographical and Geological Sur- vey, Rocky Mountain Region (Powe ll), 307 p. Fl eck, R.J., Anderson , J.J ., and Rowley, P.D., 1975 , Chronolo- gy of mid -Tertiary volcanism in High Plateaus region of Utah , in Anders on, J.J., Rowley, P.D., Fleck, R.J. and Nairn , A.E.M ., editors, Cenozoic geolog y of southwes te rn Hi gh Plateaus of Utah: Geological Society of America Special Paper 160, p. 53-62. Gartner, A .E , 1986, Geometry, emplace ment history, petrogra- phy, and ch emistry of a basalti c intrusive comple x , San Rafael and Capitol Reef areas, Utah: U .S . Geolog ical Sur- ve y Ope n-File R eport 86-61 , 112 p. Goter , S.K., 1990, E arthquakes in Utah, 1884-1989: U.S . Ge o- logical Surve y Open-File Re port 91 -128 , scale 1:500,000. Le Bas, M.J ., Le Maitre, R.W., Streckeisen , A., and Zanettin , B., 1986, A chemical classification of volcanic rocks based on the total alkali-silica diagram : Journal of P etrolog y, v. 27 , p. 745 -750. Mattox, S .R., 199 la, Origin of potassium-rich mafic lava flows , Marysvale volcanic field, Utah [abs.]: EOS , Transactions, American Geophysical Union Abstracts , p . 561. Mattox, S.R., 199 lb, Petrology, age, geochemistry, and correla- tion of the Tertiary volcanic rocks of the Awapa Plateau , Piute, Wayne, and Garfield Counties, Utah: U tah Geologi- cal and Mineral Survey Miscellaneous Publication 91-5, 46 p. Mattox, S .R., 1992a, Geochemistry, origin, and tectonic impli- cations of the mid-Tertiary and late Tertiary and Quaternary volcanic rocks southern Marysvale volcanic field, Utah: DeKalb, Northern Illinois University, Ph.D. dissertation, 498 p. Mattox, S.R., 1992b, Source and process control of the geo- chemical variation in late Cenozoic basalts across the Utah transition zone [abs .]: EOS , Transactions, American Geo- physical Union Program and Abstracts, v. 73 , p. 657. Mattox, S.R ., 1993, The influence of tectonics , regional stress, source, and magmatic processes on the geochemical evolu- tion of the southern Marysvale volcanic field, Utah [abs .]: EOS , Transactions, American Geophy sical Union Program and Abstracts, v. 74, p. 624. Mattox , S.R., 1994, Geochemistry and tectonic significance of Late Cenozoic basalts from the Basin and Range -Colorado Plateau transition zone, Utah, in Blackett, R.E., and Moore, J.N., editors, Cenozoic geology and geothermal systems of southwestern Utah: Utah Geological Association Publica- tion 23, p. 125-138. Mattox, S.R., 1997 , Geoche mistry, source characteristics , and tectonic implications of upper Cenozoic basalts of the Basin and Range-Colorado Plateau transition zone, Utah, in Maldonado, Florian, and Nealey, L.D., editors, Geologic studies in the Basin and Range-Colorado Plateau Transition in southeastern Nevada, southwestern Utah , and northwest- ern Arizona, 1995 : U.S. Geological Survey Bulletin 2 153 , p. 197-226. Mattox, S.R., and Walke r, J.A., 1989, G e ochemistry and tecton- ism of lavas erupted during the transition from compression to extension, southern Marysvale complex , southwestern Utah [abs.]: IAVCEI Abstracts, New Mexico Bureau of Mines & Mineral Resources Bulletin 131 , p. 178. Mattox, S.R., and Walke r, J.A., 1992, Mid-Tertiary volcani sm in the Utah transition zone and its relation ship to Farallon- Yancouver subduction [abs .]: Ge olog ical Society of Amer - ica Abstracts with Programs, v. 24, p. A26I. Nelson, S.T., 1989, Geologic map of the Geyser Peak quadran- gle, Wayne and Sevier Counties, Utah: Utah Geological and Mineral Survey Map 114, scale 1 :24,000. Pecce rillo, A., and Taylor, S .R ., 1976, Geochemis try of Eocene c al c-alkaline volcanic rocks from the Kas tamonu area, northern Turkey : Contributions to Mineralogy and Petrolo- g y, V. 58, p . 63-81. Rowley, P.D., 1979, Geologic map of the Marysvale SE quad- rangle, Piute County, Utah: U.S. Geological Survey Mis- cellaneous Fie ld Studies Map MF-1115 , scale 1:24,000. Rowley, P.D ., Steven, T.A., and M ehnert, H.H., 1981 , Orig in and struc tural implications of uppe r Mioce ne rhyolite in Kingston Canyon, Piute County, Utah: Geolog ical Society of America Bulle tin , v. 92, pt. 1, p. 5 90-602 . Rowle y, P.D., William s, P.L., and Kaplan , A.M., 1986, Geolog- ic map of the Greenwich quadrangle, Piute County, Utah : U .S. Geological Surve y Geolog ic Quadrangle Map GQ- 158 9 , scale 1 :24,000. Rowley, P.D ., Steve n, T.A., Ande rson , J.J., and Cunningham , Geologic map of th e Moroni Peak quadrangle C.G., 1979 , Cenozoic stratigraphic and structural frame- work of southwestern Utah: U.S. Geological Survey Pro- fessional Paper I 149, 22 p. Rowley, P.D., Mehnert, H.H., Naeser, C.W., Snee, L.W., Cun- ningham , C.G., Steven, TA., Anderson, J.J., Sable, E.G., and Anderson, R.E., 1994, Isotopic ages and strati graphy of Cenozoic rocks of the Marysvale volcanic field and adja- cent areas, west-central Utah: U.S. Geological Survey Bul- letin 2071, 35 p. Steiger, R.H., and Jager, E., 1977 , Subcommission on geo- chronology -Convention on use of decay constants in geo- and cosmochemistry: Earth and Planetary Science Letters, V. 36, p. 359-362. Steven TA., Cunningham, C.G., Naeser, C.W., and Mehnert, H.H., 1979, Revised stratigraphy and radiometric ages of volcanic rocks and mineral deposits in the Marysvale area , west-central Utah: U.S. Geological Survey Bulletin 1469 , 40 p. Steven, TA., Morris, H.T., and Rowley, P.D., 1990, Geologic 13 map of the Richfield 1 °x2 ° quadrangle, wes t-central Utah: U.S. Geological Survey Miscellaneous Investigations Series Map I-1901, scale 1:250,000. Steven, TA., Rowley, P.D., and Cunningham, C.G., 1984, Cal- deras of the Marysvale volcanic field, west-central Utah: Journal of Geophysical Research , v. 89, p. 8,751-8,764. Tingey, D.G., Christiansen, E.H., Best, M.G., Ruiz , J., and Lux, D .R., 1991, Tertiary minette and melanephelinite dikes , Wa atch Plateau, Utah: Records of mantle heterogeneities and changing tectonics: Journal of Geophysical Research , V. 91 , p. J 3,529-13,544. Van Cott, J.W., 1990, Utah Place Names: Salt Lake City, Uni- versity of Utah Press, 453 p. William s, P.L., and Hackman, R.J., 1971 , Geology of the Salina quadrangle, Utah: U.S. Geological Survey Miscellaneous Geologic Investigations Map I-591-A, scale 1:250,000. Willis, G.C., 1986, Geologic map of the Salina quadrangle, Sevier County, Utah: Utah Geological and Mineral Survey Map 83, scale 1 :24 ,000. 14 Utah Geological S urvey Appendix 1 Sample Locations Sample Unit Longitude Latitude 7.5' quadrangle Locality AP65 Tia 111 °44'45" 38°18'07" Moroni Peak Cyclone Draw AP67 Tla 111 °44'45" 38°18'07" Moroni Peak Cyclone Draw AP104 Tpml 111 °43'41" 38°22'04" Moroni Peak Long Hollow AP105 Tpml 111 °42'47" 38°21 '59" Moroni Peak Long Hollow AP60 Tl 111 °38'13" 38°17'48" Moroni Peak Big Hollow AP62 Tl 111 °38'14" 38°17'45" Moroni Peak Bi g HolJow AP63 Tl 111°38'15" 38°17'44" Moroni Peak Big Hollow AP171 Tl 111 °40'43" 38°17'30" Moroni Peak Big Hollow AP64 To 111°43'05" 38°17'10" Moroni Peak Big Flat Top AP101 To 111 °44'28" 38°22'04" Moroni Peak Long Hollow AP103 To 111 °44'28" 38°22'04" Moroni Peak Long Hollow AP107 Tb 111 °41'41" 38°20'10" Moroni Peak Elsies Nipple APllO To 111 °37'22" 38°21 '49" Bicknell Big Rocks BC5 Tmd 112°27'08" 38°12'30" Circleville Mtn Circleville Mtn