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mpus Technical Services. lnc.
ings, MTo Boise, ID o Havre, MTo Helena, MT
SITE REMEDIATION PLAN
LAUNDRY SUPPLY GOMPANY, ING.
SALT LAKE CITY, UTAH
Submitted to:
Utah Department of Environmental Quality
Division of Solid and Hazardous Waste
288 North1460 West
Salt Lake City, Utah 84114
Prepared for:
Laundry Supply Company
3785 West 1987 South
Salt Lake City, Utah 84145
August 4, 2000
Olympus Work Order No. A7008
RECEIVED
AUfi 'l n 2000
0C.CbtLq .a.
Divisionlt Soti-O & Hazardous Waste
Utah Department of Environmental 0uality
5409 Kendall Street o
(208) 376-5006 o Fax (208) 37&5091
Boise, lD 83706o E-mail: olympusid@rmci.net
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TABLE OF CONTENTS
1.0 TNTRODUCTTON ........................ 1
1.1 Purpose.............. .........,...1
1.2 Scope of Work.... ..............1
1.3 Summary of Previous Work ............. 1
1.3.1 Site Assessment Documents............ ....................2
2.0 slTE DESCR!PT!ON.......... .......2
2.1 Facility and Local Features ..............2
2.1.1 Area of lnvestigation............ ................2
2.1.2 Site History and Operations.......... ........................3
2.1.3 WaterWell lnventory... ........................3
2.2 Environmental Features... ................3
2.2.1 Site Topography and Surface Water Features... ...................3
2.2.2 Geo1o9y........... ..................3
2.2.3 Hydrogeology ....................4
3.0 srTE ASSESSMENT SUMMARY............ ......................4
3.1 Site Geology/Hydrogeology............... ................4
3.2 HVO Source..... ...............5
3.3 Presence of Dense Non-Aqueous Phase Liquid.... .............5
3.4 Extent of HVOs in Soil .....................5
3.5 Extent of HVOs in Ground Water....... ................5
3.6 Water Supplies At Risk ....................6
4.0 CONTAMINANT CHARACTERISTICS ........7
4.1 Characteristics of ldentified HVOs .....................7
4.2 Contaminant Toxicology ...................7
s.0 coRREcTME ACTTONS ...........8
5.1 HRC lnjection... ...............9
6.0 SITE MONITORING PLAN ........10
6.1 Aquifer Monitoring ...........10
6.2 Ground Water Monitoring. ................'t0
6.3 Additional Assessment......... ............. 10
7.0 REPORTTNG .............. 11
8.0 PROJECT C1OSURE............ ......................11
9.0 cAP TMPLEMENTATTON SCHEDULE .............. ............11
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TABLE OF CONTENTS
(continued)
10.0 LIM|TATIONS ...........12
11.0 REFERENCES .......13
FIGURES
Facility Location Map
Facility Map
Ground Water Elevation Contour Map, Apr-00
Proposed HRC lnjection Grid
Proposed Soil Probe Location Map
TABLES
Ground Water Sampling Field Parameters
Sampling Analyses
APPENDICES
A HRC Design Spreadsheet
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1.0 INTRODUCTION
1.1 PURPOSE
Olympus Technical Services, lnc. (Olympus), on behalf of Laundry Suppty Company lnc.
(LSC), prepared this Site Remediation Plan (SRP) for LSC's facility (Facility) located in Salt
Lake County, Utah at 3785 West 1987 South in Salt Lake City. Figures 1 and 2 show a
Facility Location Map and a Facility Map, respectively. The purpose of the SRP is to present a
plan of remediation for subsurface halogenated volatile organic {HVO) compound impad
resulting from a release of tetrachloroethene (perchloroethylene or PCE, an HVO compound)
from a decommissioned underground storage tank (UST) system at the Facility. The UST
system was decommissioned in April 1996. Analyses of soil and water samples collected
following the decommissioning indicated that a release of an unknown quantity of PCE had
likely occuned into the subsurface. Additionalassessment indicates that HVO impact extends
at least to the Facility property boundary, and may extend down gradient of the Facility. This
SRP presents remedial and monitoring plans as required under the Stipulation and Consent
Agreement No. 9609031, issued by the Utah Solid and Hazardous Waste Control Board.
Since LSC is proposing site remediation, at this time LSC is not submitting a Site Management
Plan (SMP). Should additional assessment (described in this report) indicate that subsurface
HVO impact will remain after the proposed remedial ac'tions are implemented, LSC will prepare
a SMP and its associated risk assessment.
1.2 SCOPE OF WORK
The SRP outlines corrective actions LSC proposes to remediate ground water at the Facility.
The proposed actions are designed to remove HVOs from ground water by enhanced
biodegradation by reductive dechlorination.
1.3 SUMMARY OF PREVIOUS WORK
On April4, 1996, Westech Environmental(Westech) of Salt Lake City, Utah, removed two
10,000gallon steel UST's, associated piping, product dispensers, and containment equipment
from the Facility. Following removal of the UST system, Westech collected soil and water
samples from the UST Basin for PCE analysis, as per the Underyrcund Storage Tank Closure
Plan (Westech, March 1996) for the Facility. The dosure plan had been submitted by
Westech to the Utah Department of EnvironmentalQuality, Division of Environmental
Response and Remediation (DEER) on March 6, 1996. Laboratory analyses of the samples
collected by Westech from the UST Basin detected PCE in soiland ground water. Westech
faxed laboratory reports of the soiland water sample analyses to DEER on April 18, 1996. An
Undergrcund Sfomge TanR Closure Nofice for the Facility, documenting the UST removal and
including laboratory analytical reports of the soil and water sample analyses, was delivered to
DEER by Westech on June 4, 1996.
ln a letterto LSC dated May 10, 1996, DSHW assumed regulatory jurisdiction of the release of
I PCE at the Facility. On July 10, 1996, representatives of LSC and DSHW met to discussI
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options in responding to the release. On June 4, 1997, LSC and the Utah Solid and
Hazardous Waste Control Board executed a Stipulation and Consent Agreement. ln the
Stipulation and Consent Agreement, LSC agreed to complete site investigation tasks outlined
in the agreement to determine the nature and eldent of the PCE release, and agreed to
prepare a ROI docurnenting the results of site investigation activities. The ROlwas also to
include a SRP, a SMP, or a recommendation of no further action.
Olympus performed site investigation activities between May 12,1998 and January 20, 2000.
Assessment activities included soitboring advancements and monitoring wellcompletions, soil
sampling, soil probe advancement with ground water sampling and monitoring well
completions, ground water elevation gauging, ground water monitoring, and waste disposal.
The site investigation is summarized in the Report of lnvestigation, Laundry Supply Company,
lnc., Salt Lake City, Ufah (ROl) submitted by Olympus to DSHW on May 2,2000.
1.3.1 Site Assessment Documents
Site investigation activities were performed in accordance with the Utah Department of
EnvironmentalQualig, Division of Solid and Hazardous Waste's (DSHW) work plans. A listing
of site assessment documents includes:
Srfe /nvestrgation Plan, Laundry Supply Company, prepared by JBR Consultants, lnc.
(JBR), submitted on November 10, 1997, approved by DSHW on December 23, 1997;
Revisions to the JBR Srte lnvestigation Plan, Laundry Supply Company submitted by
Olympus on March 4, April3 and April21, 1998, approved by DSHW on May 6, 1998;
Continuing Site lnvestigation, Laundry Supply Company, letter report submitted by
Olympus on October 30, 1998, amended January 13, 1999, approved by DSHW by E-mail
on January 21, 1999;
Continuing Site lnvestigation, Laundry Supply Company, letter report submitted by
Olympus on September 20, 1999, approved by DSHW by E-mail on October 8, 1999; and
Repoft of lnvestigation, Laundry Supply Company, lnc., Saft Lake City, Ufah submitted by
Olympus on May 2,2OOO
2.0 SITE DESCRIPTION
2.1 FACILITY AND LOCAL FEATURES
2.1.1 Area of lnvestigation
LSC's Facility is located in Salt Lake County, Utah at 3785 West 1987 South in Salt Lake City.
Fpure 1 shows the location of the Facility within the Salt Lake City area. U.S. Public Land
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Survey designation of the Facility location is: within the southwest 1/4, Section 17, Township 1
South, Range 1 East of the Salt Lake Meridian. Figure 2 shows the Facility and its immediate
sunoundings.
2.1.2 Site History and Operations
LSC built its Facility building at 3785 West 1987 South in 1979, and the Facility has been in
operation as a storage and distribution facili$ for laundry and dry cleaning supplies since that
date. Two 10,000gallon USTs and associated piping and distribution equipment used for
PCE storage and distribution were installed in 1979. The UST system was decommissioned in
April 1996.
2.1.3 Water Well lnventory
Olympus performed a search of the Water Right Records lnternet database maintained by the
Utah Department of Natural Resources, Division of Water Rights (DWR) to identify waterwells
reported to exist within a one-mile radius of the Facility. The wells were identified by a query of
the Water Right Records for underground diversions of unapproved, approved, and perfected
rights for water uses that included, but was not limited to: inigation, domestic, stock-water,
municipal, mining, and power uses. The DWR records review identified 29 points of diversion
from a totalof 17 wells located.within one mile of the Facility. Reported welldepths ranged
trom 1741o 1,473 feet BGS. The Water Right Search Record is included in the ROl.
2.2 ENVIRONMENTAL FEATURES
2.2.1 Site Topography and Surface Water Features
The Facility lies in the Salt Lake Valley at an approximate etevation of 4,240 feet above mean
sea level (National Geodetic Vertical Datum of 1929). The Facility is bounded by west-facing
slopes to the east (Salt Lake City area), and north- and northeast-facing slopes to the south.
ln the Facility area, topography is relatively flat, with a generalnorthwest slope with an
elevation drop of approximately five feet per mile.
The Jordan River, located approximately three miles east of the Facility, is the major surface-
water drainage feature in the area. Several canals, generally draining to the west and
northwest, are present in the Facility area. Canals nearest the Facility include the Brighton
Branch Extension Canal, located approximately onehatf mile north and northeast of the
Facility, and the Ridgeland Canal, located south and southwest of the Facility. Figure 1
illustrates the localtopography and shows the surrounding surface water features.
2.2.2 Geology
The Salt Lake Valley lies within the Lake Bonnevilkc Basin, which consists of approximately 40
largely interconnected smaller basins within the Basin and Range physiographic province
(Hunt, 1987). The Great Salt Lake occupies the lowest part of the Lake Bonneville Basin.
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2.2.3 Hydrogeology
According to Selier and Waddell (1984), ground water in the Salt Lake Valley occurs in:
a confined aquifer; a deep unconfined aquifer between the confined aquifer and the
mountains; a shallow unconfined aquifer overlying the confined aquifer; and locally in perched
aquifers. The shallow unconfined aquifer is described by Selier and Waddell as consisting of
mostly sand, silt, and clay, with a maximum thickness of approximately 50 feet, which b
recharged by upward leakage from the confined aquifer and infiltration from precipitation,
canals, inigated lands, and streams. The authors indicated that the ground water in this
surfical aquifer is seldom used as a source of water for domestic or industrial purposes
because of poorwater quality and slow yields.
Selier and Waddell (1984) prepared a contour map of December 1982 ground water
elevations. The map shows the general direction of ground water flow in the shallow
unconfined surfical aquifer in the Salt Lake Valley is towards the Jordan River, with the
exception of the area northwest of the Facility, where the flow direction is towards the Great
Salt Lake. The elevation contours show ground water flow direction in the Facility area to be
generally to the north and northeast. Ground water flow west of the Facility area is towards
the northwest.
3.0 SITE ASSESSMENT SUMMARY
3. 1 SITE GEOLOGY/HYDROGEOLOGY
Olympus'observations of samples collected during soil borings and soil probe advancement
indicate the Facility is underlain by approximately 20 to 25 feet of interbedded layers of poorly
graded, fine to mediumgrained sands and medium to high-plasticity clays; underlain by poorly
graded fine to medium-grained sand from approximately 25 feet BGS to 30 feet BGS. Based
upon the presence of heaving sands encountered during soilboring advancement, this sand
unit likely extends to a depth of at least 55 feet BGS.
Data and observations from the assessment suggest ground water at the Facility is contained
in the shallow unconfined aquifer described above.
Olympus gauges ground water elevations in the Facility monitoring wells on a quarterly basis.
Table 1 presents a summary of the ground water elevation gauging at the Facility. Figure 3
shows a ground water contour map generated using data collected during ground water
elevation gauging conducted in April2000. Based on the April 2000 ground water elevation
gauging, Olympus calculated a genera! Facility ground waterflow direction to the north-
norttwest. Generalground waterflow directions during the monitoring period have ranged
from north-northwest to the northwest.
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3.2 HVO SOURCE
PCE and other HVOs detected in laboratory analyses of soil and ground water samples
collected during the assessment, the locations of the samples, and the observed ground water
flow direction, indicate the source of HVO impact at the Facility is likely from the
decommissibned Facility UST system. Analyses of ground water samples collected from MW-
4 (Figure 2 - located upgradient of the UST basin) indicate a potential off-site sour@ of FIVOs
contributing to HVO impact at the Facility
3.3 PRESENCE OF DENSE NON-AQUEOUS PHASE LIQUID
Olympus did not detect DNAPL in Site monitoring wells completed in the vicinity of the
decommissioned UST basin. We measured dense non-aqueous phase liquid (DNAPL)
thicknesses in MW-1, MW-2, and MW-3 (Figure 2) during selected ground water monitoring
events.
3.4 EXTENT OF HVOS IN SOIL
The assessment of the Facility indicates HVO impacted soil is present within the boundaries of
the UST basin. Laboratory analyses of soil samples collected above the soil/ground water
interface during the advancement of soilborings in the UST basin detected PCE. TCE and
cis-1,2-DCE were also detected in the soil sample collected at SB-3. PCE gas detector tube
screening for PCE in soil samples collected in the vadose zone from soil borings outside the
UST basin did not detect PCE.
Based on an apparent single source of HVOs at the former location of the USTs, laboratory
analyses of collected soil samples, and an observed shallow ground water table at
approximately three to four feet BGS, the lateral extent of HVO impact to soil at the Facility is
most likely limited to soil at or directly adjacent to the UST Basin.
3.5 EXTENT OF HVOS IN GROUND WATER
The assessment identified HVO impacted groundwater both on- and off-site of the Facility-
PCE was detected in the analyses of ground water samples collected within an arc bounded
by bearings of approximately 45 degrees east of north (MW-6 and SP-12 - Figure 2) to
approximately 60 degrees west of north (MW-S) from the UST Basin. The area of greatest
I-IVO impact to ground water, with PCE concentrations exceeding 10,000 pg/|, was found at
and extending north and northwest from the UST Basin to 1987 South Street. This area of
impact follows the observed general down gradient ground water flow direction from the UST
basin.
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Based on the analyses of ground water samples collected from soil probes and off-site
monitoring wells, the lateral extent of HVO impact to ground water to the northeast, north, and
northwest would appear to be on or direcfly adjacent to Facility property, with the following
exceptions:
. PCE was detected in analyses of ground water samples collected at 35 feet BGS at SP-16
(Figure 2\ ata concentratiori of 4,950 pg/|, and 25 and 35 feet BGS at SP-17 at
concentrations of 5 pg/l and 43 pg/|, respectively.
o PCE was detected in analyses of ground water samples collected at 15, 25, and 35 feet
BGS at SP-8 at concentrations of 29 ygll,25 pg/l, and 16 yg/|, respectively.
Depth of HVO impact to ground water would appear to extend from the upper surface of the
unconfined aquifer to a depth of at least 35 feet BGS. Due to concems of breaching an
assumed confining unit at the base of the unconfined aquifer, Olympus did not advance soil
probes or soil borings at depths greater than 35 feet in areas of known HVO impact during the
course of this site investigation. However, analyses of ground water samples collected at 45
and 55 feet BGS from SP-14, located approximately 180 feet north of the UST Basin, did not
detect HVOs at laboratory reporting limits.
Greatest PCE impact to ground water found during the soil probe assessments down gradient
of the UST Basin was in water samples collected at approximately 15 feet BGS. PCE
concentrations detecled in soil probe ground water samples collected at 25 and 35 feet BGS
were generally an order of magnitude less than concentrations detected in the 15 foot BGS
soil probe samples and UST Basin monitoring well ground water samples.
3.6 WATER SUPPLIES AT RISK
The results of the site assessment suggest ground water in the shallow unconfined aquifer at
the Facility has Iikely been impacted as a result of a PCE release at the Facilig's UST Basin.
HVO impact to ground water appears to be limited to the UST Basin, and Facility proper$ and
areas directly adjacent to Facility property in a down gradient ground water flow direction from
the UST Basin. Ground water monitoring indicates that down gradient PCE impact does not
extend beyond MW-8 located in 3850 West Street (Figure 2).
Olympus' review of the Water Right Records lntemet database maintained by the DWR
identified 29 points of diversion from a totalof 17 wells located within one mile of the Facility.
The rccorded locations of the wells indicate four of the wells are located within a radius of one
mile in a possible downgradient flow direction from the Facility. Locations forthe wells, based
on information given in the database, range from 2,000 to 4,000 feet from the Facility at
bearings between 10 degrees east of north and 65 west of north from the Facility. Allfour
wells are listed as being owned by Union Pacific Land Resource Corporation, and allrecord
the water use as stock watering. Three of the well had depths ranging between 200 and 500
feet deep. One of the wells did not have a recorded depth. These wells appear to be
completed in the lower, confined aquifer. The welldepths and well locations, as recorded in
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the DWR database, indicate HVO impact to ground water at the wells from the identified
source at the Facility is unlikely.
4.0 CONTATINANT CHARACTERISTICS
4.1 CHARACTERISTICS OF IDENTIFIED HVOS
The HVOs in ground water at the Facility are likely dense non-aqueous phase liquids (D}.|APL).
DNAPL have a specific gravity of greater than 1.0; and as a result, DNAPL tend to sink in
water when in the free-product phase.
DNAPL are highly volatile compounds with high densities, low viscosities, low interfacial
tension, low absolute solubilities, and high solubilities (relative to drinking water contaminant
concentration limits). These compounds have a low partitioning to soil materials and low
degradabilities. As a result, DNAPL can travel through soil quickly in either the liquid and/or
the gaseous phases and readily contaminate ground water. (Pankow and Cherry, 1996)
Once in ground water, DNAPL tend to migrate downward (resulting from their high density/low
viscosity) as thin Tingers" that may form pools of product on top of less permeable layers.
These DNAPL pools present a very low cross section to the aquiferflow, and as a result,
absolute removal rates of dissolved product from such pools will usually be very low. The low
degradation rates of DNAPL suggest that their subsurface lifetime can be very long. (Pankow
and Cherry, 1996;Johnson and Pankow, 1992)
The low interfacialtension and the low partitioning to soil material mean that DNAPL products
will only bind weakly to soil and rock particles. This property allows rapid growth of dissofued
DNAPL product plumes in ground water. (Pankow and Cherry, 1996)
4.2 CONTAMINANT TOXICOLOGY
PCE is the major HVO ground water contaminant in soil and ground water at the Facility. The
following toxicologicalsummary is intended to present general information regarding PCE
affects on human health and the environment. The summary was prepared by the Office of
Pollution Prevention and Toxics, United States Envircnmental Protection Agency (EPA)
(August 1994).
Effects of PCE on human health and the environment depend on the amount of PCE present
and the length and frequency of exposure. Effects also depend on the health of a person or
the condition of the environment when exposure occurs. Breathing PCE for short periods can
adversely affect the human nervous system. Effects range from dizziness, fatigue, headaches
and sweating to incoordination and unconsciousness. Contact with PGE liquid or vapor
initates the skin, the eyes, the nose, and the throat. These effects are not likely to occur at
levels of PCE that are normally found in the environment.
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Breathing PCE over longer periods can cause liver and kidney damage in hurnans. Workers
erposed repeatedly to Iarge amounts of PCE in air can also experience memory loss and
confusion. Laboratory studies show that PCE causes kidney and liver damage, and cancer in
animals exposed repeatedly by inhalation and by mouth. Repeated exposure to large
amounts of PCE in air likewise may cause cancer in humans.
PCE can contribute to the formation of photochemical smog when it reacts with other volatile
organic carbon substances irt air. These reactions tend to eliminate PCE before it reaches the
upper atmosphere in amounts sufficient to damage the ozone layer.
5.0 GORRECTIVE ACTIONS
LSC is committed to remediating ground water adversely impacted by HVOs for which it is
responsible. Olympus evaluated several remediation technologies that may be applied at the
Facility. These technologies included:
o naturalattenuation;o grcurd water air sparging and soil vapor extraction;o groufld pumping and treatment; ando bioremediation.
Given the elevated HVO concentrations identified at the Facility, natural attenuation was not
considered a viable option.
Ground water air sparging and soil vapor extraction was not considered due to the shallow
(three feet) depth to water at the Facility. The shallow depth prevents the effective use of a
vapor extraction system to collect gases generated during air sparging.
Ground water pumping and treatment was also considered. Site hydrogeologic conditions are
not ideal for ground water pumping. The Facility aquifer consists of interbedded sand, silt, and
day. lf ground water pumping were implemented, it is expected that a large number of
recovery wells would be required. Ground water pumping would initially remove HVO but
would likely be stalled by its inability to remove HVOimpacted water held by capillary forces
within individualsoil grains. Ground water pumping would require between five and ten years
of treatment, if not more, to effectively remediate the Facility aquifer.
Enhanced biodegradation by reductive dechlorination at the Facility may be accomplished by
use of a benign polylactic ester manufactured by Regenesis Bioremediation Products
(Regenesis) called HRC (Hydrogen Release Compound). HRC is formulated forthe slow
rebase of lactic acid upon hydration. HRC, upon hydration after injection into the aquifer,
separates from the glycerol background as a polylactic acid complex. The polylactic acid
rebase results in a multi-step slow-release hydrogen release mechanism. lndigenous
anaerobic microbes ferment the lactic acid. The fermentation converts the lactic acid into other
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organic acids and produces hydrogen. The hydrogen can then be used by reductive
dehalogenating microorganisms to dechlorinateing HVOs (Koenigsberg, 2000).
Olympus selected HRC as the recommended remedial option based upon the following
assumptions:
o HRC injection is expected to remedial HVOs inSitu without conoems for wastewater
discharge;
o biodegradation by reductive dechlorination is expec'ted to remove HVO held by capillary
tension within the aquifer material, while pump and treat will require removal of several
pore volumes (of water in the aquifer) for complete HVO removal;
o HRC remediation time frames are estimated to be significantly less than pump and treat
methods; and
o HRC remediation can be accomplished with minimal site disturbance and no capital
equipment costs.
5.1 HRC INJECTION
HRC will be introduced to the aquifer by direct injection through GeoProbe advanced soil
probes. The HRC injections will be on a grid spacing of approximately 12 feet to a depth of
approximately 40 feet below the surface. An appropriate amount of HRC will be injected at
five-foot intervals in accordance with the manufacture/s instructions.
Olympus has estimated the HRC treatment area using existing data. Figure 4 shows the
estimated treatment area and HRC injection points.
Olympus calculated the HRC dosage and grid spacing based upon Regenesis' HRC Grid
Design spreadsheet (version 1). Appendix A includes a copy of the Regenesis spreadsheet
and supporting HRC design documentation.
The exact HRC dosage will be calculated after the Third Quarter 2000 ground water monitoring
event at the Facility and additional GeoProbe sampling to be conducted down gradient of the
Facility (ROland Section 6.3). Additionaldata from these monitoring events willprovide
design data to better ensure effective HVO remediation. Olympus will collect samples from
selected monitoring wells for analyses of nitrate, manganese, fenous iron, and sulfate. These
data will be used to replaced estimated values used in the HRC Grid Design spreadsheet.
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6.0 SITE MONffORING PI.AN
LSC will continue to perform environmental monitoring at the Facility to gauge ground water
elevations and monitor ground water HVO chemistry. This information will be reported to
DSHW through quarterly project status reports.
6.1 AQUIFER MONITORING
LSC will continue to gauge ground water elevations in the Facillty monitoring wells on a
quarterly basis. DNAPL thickness in wells MW-1, MW-2, MW-3 willalso be measured on a
quarterly basis. The ground water elevationgauging program will provide data to monitor
ground water flow direction and gradient.
Olympus wilt perform aquifer tests to collect data to calculate the hydraulic conductivity of the
surficial aquifer at the Facility. We wil! perform rising-head slug tests and collect data using a
pressure transducer and data logger in at least three Facility monitoring wells. The slug test
data will be analyzed using methods developed by Bauer and Rice (1976) and Bauer (1989).
The hydraulic conductivity, along with the ground water elevation gauging data and the known
aquifer lithology, will be used to calculate ground water flow velocity in the aquifer at the
Facility.
6.2 GROUND WATER MONITORING
LSC proposes to continue the Facili$ ground water monitoring program on a quarterly basis.
The ground water monitoring program willinclude:
o grourd water sampling of monitoring wells MW-1, MW-2, or MW-3, and MW-4 through
MW.8;
o preparation of equipment and trip blanks, and collection of a duplicate sample for
QA/QC purposes; and
o laboratory analyses of ground water and QA/QC samples for HVO cornpounds using
protocolestablished in SW-846 Method 8020.
Water generated during the sampling and monitoring events will be stored at the Facility in 55-
gallon drums pending disposal anangements.
6.3 ADDITIONAL ASSESSMENT
Olympus will continue down gradient ground *.i", soil probing to assess the extent and
magnitude of HVO impact to ground water at or adjacent to the locations of soil probes SP€,
and SP-16 and SP-l7 (Figure 2). Pending DSHW approval of the investigation, LSC will
advance two soil probes to depths of 35 feet BGS in the area of SP-8, and two soil probes to
depths of 55 feet BGS in the SP-16 and SP-17 area. Figure 5 shows the proposed soil probe
C:\ttABPrqccfs\AIGLSCATOOS\SRl, 8i4-00.dc Page 10
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locations. Ground water samples will be collected at 1O-foot intervals beginning at 15 feet
BGS. Collected ground water samples will be delivered, using chain of custbdy procedures, to
Enviropro for analyses. Enviropro will analyze the water samples for PCE and TCE using
methodology established in SW-846 Method 8260.
Following receipt and review of laboratory analyses of soil probe ground water samples,
additiona! monitoring wells and/or soil probing may be proposed to complete the assessment.
Results of the additional ground water assessment will be rcported in an addendum to this
report. Wastes generated during the soil probing will be stored at the Facility in S5gallon
drums pending disposal anangements.
7.0 REPORTING
Olympus, on LSC's behalf, will prepare guarterly project status reports for submittalto DSHW.
The reports will include:
o groU[d water elevation gauging data;o DNAPL thickness measurements;o ground water monitoring sample analyses; ando a written description of project activity during the reporting period.
LSC will submit the report to DSHW within 30 days following the quarterly reporting period.
8.0 PROJECT CLOSURE
Project closure will be recommended after ground water monitoring indicates that HVO
concentrations in ground water have been reduced to drinking water standards or background
levels, whichever is greater. lf HVO concentrations have not been reduced to desired levels
one year after the HRC injection, LSC will evaluate the additional remedial measures.
Potential measures may include additional HRC injections or a risk based assessment to
determine if closure is appropriate. A SMP will be prepared if a risk based closure is
recommended.
9.0 CAP TMPLEiIENTATION SCHEDULE
LSC proposes the following schedule to implement conective actions at the Facility:
. July 2000 - Slug testing, ground water monitoring;. August 2000 - additionalGeoProbe assessment;. August 2000 - Specification, ordering, and injection of HRC; ando October 2000 and January, April, and June 2001 - ground water monitoring;
, MTo Boise, lDo Hawe, MTo Hebna MT
C:\ilA8\Pniects\AlCa-LSCATOOenSRP ErHn.doc Page 11
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10.0 LtiilTATtoNs
Otympus performed the services documented in this report in a manner consistent with
generally accepted principles and practices for the nature of the work completed in the same
or similar localities, at the time the work was performed. No other wananty, express or implied,
is made.
Opinions contained in this report apply to conditions existing when the services were
performed. Allconclusions and recommendations are based on readily available and
reasonably ascertainable information on site conditions at the time of the work and for the laws
in effect at that time. We are not responsible for any changes in environmental standards,
practices, or regulations subsequent to performance of services. This report is not meant to
represent a legalopinion. We do not wanant the accuracy of information supplied by others,
nor the use of segregated portions of this report.
This report was prepared by:
OLYHPUS TECHNIGAL SERVICES, INC.
t*@
Michael Backe, P.G.
Senior Hydrogeologist
Date
MTo Boise, lDe Hawe, MTo Helena MT
C:\tlAB\Prciects\AIG,LSCATmAISRP &4-00.fl6s Page 12 u4tc0,
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Srfe Remediation Plan
Laundry Supply Company
Technical Servi
, MTo Boise, lDo Havre, MTo nebna MT
IT.O REFERENCES
Hunt, C.8., 1987, Physbgnphy of Westem Utah, in Cenozoic Geology of Westem Ufah, Srtes
for Precious Metal and Hydrocarbon Arcumulations: Utah GeologicalAssociation
Publication 16, p. 1-29.
JBR Consultants, lnc., Sffe lnvestigation Plan, Laundry Supply Company, November 10,
1997, Sandy, Utah, submitted to DSHW.
Johnson, R. L. and Pankow, J. F., 1992. Dissolution of Dense Chlorinated Solvents into
Grcundwater,2. Source functionsfor pools of solvents, Environmental Science
Technology.
Olympus Environmental, lnc., March 4, 1998, Site lnvestigation, Laundry Supply Company,
Salt Lake City, Utah: Olympus Work Order# 7585, Boise, ldaho, submifted to DSHW.
Olympus Environmental, lnc., April3, 1998, Site lnvestigation, Laundry Supply Company, Salt
Lake City, Utah: Olympus Work Order# 7585, Boise, ldaho, submitted to DSHW.
Olympus Environmental, lnc., April21, 1998, Site lnvestigation, Laundry Supply Company,
Salt Lake City, Utah: Olympus Work Order # 7585, Boise, ldaho, submitted to DSHW.
Olympus Environmental, lnc., June 19, 1998, Site lnvestigation, Laundry Supply Company,
Salt Lake City, Utah: Olympus Work Order # 7585, Boise, ldaho, submitted to DSHW.
Olympus Environmental, lnc., July 31, 1998, Site lnvestigation-SoilProbing, Laundry Supply
Company, Salt Lake City, Utah: Olympus Work Order# 7585, Boise, ldaho, submitted to
DSHW,
Olympus Environmental, lnc., October 30, 1998, Continuing Site lnvestigation, Laundry
Supply Company, Salt Lake City, Utah: Olympus Work Order# 7585, Boise, ldaho,
submitted to DSHW.
Otympus TechnicalServices, lnc., January 13, 1999, Continuing Site lnvestigation, Laundry
Supply Company, Salt Lake City, Utah: Olympus Work Order No. A7008, Boise, ldaho,
submltted to DSHW.
Olympus TechnicalServices, lnc., May 14, 1999, Assessment Results, Laundry Supply
Company, Salt Lake City, Utah: Olympus Work Order No. A7008, Boise, ldaho,
submitted to DSHW.
Olympus TechnicalServices, lnc., September 20, 1999, Continuing Site lnvestigation,
Laundry Supply Company, Salt Lake City, Utah: Olympus Work Order No. A7008, Boise,
ldaho, submited to DSHW.
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C:\MABU,roiecIs\AIGLSC.ATOOAISRP 8-4.o0.da Page 13
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I Srte Remediation Plan ln
MTr Boise, lDr Hawe, MTo Helena, MT
I
I
Laundrv Supplv Com
Olympus Technical Services, lnc., May 2,2000, Repoft of lnvestigatlnn, Laundry Supply
Company, Salt Lake City, Utah: Olympus Work Order No. A7008, Boise, ldaho,
submitted to DSHW.
Pankow, James F. and Cherry, John A., 1996. Dense Chloinated Soluenfs and other
DNAPLs in Grcundwafer, Waterloo Press, Portland, Oregon.
Seiler, R.L., and Waddell, K.M., 1984, Reconnaissance of the Shallow-unconfined aquiferin
Salt Lake Valley, Ufah: U.S. GeologicalSurvey Water Resources lnvestigations Report
834272,13 p., 3 maps.
United States Department of the lnterior, Geological Survey. Salt Lake City South
Quadrangle, Utah-Salt Lake County, 7.5 Minute Series (Topographic), 1963
(photorevised 1968 and 1975), Reston Virginia.
Utah Solid and Hazardous Waste Control Board, Stipulation and Consent Agreement No.
9609031, executed on June 4, 1997.
Westech Environmental, Underground Storage Tank Closure Plan, March 3, 1999, submitted
to DEQ/DEER.
Westech Environmental, Underground Storage Tank Closure Notice, June 4, 1996, submitted
to DEQ/DEER.
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C:\MABFrojects\NelLSCATmE\SRP 8!4-00.doc Page 14 u4t0p,
Srfe Remediation Plan
Laundry Supply Company
Technical Servioes. I
MTo Boise, lDr Hawe, MTo Helena MT
FIGURES
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TABLES
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TABLE 1 . GROUND WATER FIELD PARAMETERS
Laundry Supply Company
Salt Lake City, Utah
.U-gliPj!!9,!Ug[-9gp!?g- - - - L - - - - - -
Un r-1 4,?F€02 1+lrqbgs i 2.88
26-lur98
+Mar-99 i 3.30
$Mar-99 ! 3.30
^4 Jun-99
2C&-99 i 3.49
2&Dec-99 ! 3.45
1sMry.98 i 3.41
1S[,Iaf98
2SJun-98 i 2.43
+trrtr-gg i 3.70
$Ma-99 i 3.70
2fiJur99 ! 3.78
2OOct-99 i 3.82
?$Dec-99 i 3.71
17.ran{0 I 3.86
18rADr{O i 3.69
26-Jur98 i 2.60
+[rar-99 i 3.65
$lt tr-S i 3.71
Dudic#$tU{-99 i 3.71
24^Jur99 ! 3.81
2GOct-99 i 3.85
2$Dec-99 i 3.76
17.rfrO0 i 3.91
18rADr{0 I 3.6E
{-f,fg'-$ i 2.70
$Mar-99 | 2.U
^ 1 Jun-99
2O0ct-g9
2$Dec-99 ! 2.&
18^Jan{0 i 2.82
1&Apr{0 i 2.57
in r-5 4A7.% +ttrter-S i 3.St
$Ms-99 . 3.21
24-Jurr99 ! 3.34
Drrpli*
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2GOd-99
&Dec-99
rn$FrriectsLsC.AT00S\
SPM t*les.ns-T$le 1
Conrmentsfoboervdons
0.6 !Sanplelight@
Sanple brorn/opque
Sarple brown
1.0 ! Smrple broryn/brrglucent
2.3 i Sample ligm brwn/haslucent
Ssnple ffight gray/brrsfent
l#ttW€
Sanple ftaylbarrlucent
5.9 ! Ssnple ydlon/hrtshJcant
Santple gra),rqqre
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TABLE 1. GROUND WATER F]ELD PARAi'ETERS
Laundry Supply Company
Salt Lake City, Utah
ttltv€ 4,739.62
tr/tw-7 4,238.38
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Ndes: Elerdkms rederencod to Salt L.*e City Public Works Bench lUark
Cz-n, with a published elardion of 4235.586
oQ = Degre Centigrde
pStcrn = Micro.Siemens (micrumhc) per Centirnder
mdl = Milligrmrs per Liter
Terrperdure, Elecfical Cmdudivity, and Dissohrcd Oxygen rneasured insitu
- = ltld luleaured or Reorded .
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Dupllc& 17.,il{0
18rApr{0
9.2 7.98 7.80 4,900 4,7Xi 5.1 4.8 i L^*ded MW-g
3.24 4,7U.74 11.5 8.00 8.01 5,880 5,880 1.9 2.O !Sarrpb
Duplic& 1&Apr{0 11.5 7.96 8.01 5,870 5,880 2.1 2.0 i L$ded IIW-9
20€ct-99 I 4.81 4,2y.91 $.2 7.35 7.42 7,1&6,320 2.1 2.1 Smple lbht brwn/barsltrcent
23&-99 4.81 4,2U.81
18-Jan{0 4.99 4,ru.63 10.8 7.31 7.31 12,1fi 12,090 3.7 3.7 Sample wh ite/has I ucent
1&Apr{O 4.80 4,ZU.g2 10.5 7.79 7.79 2626 2,629 2.1 2.O Sanpleffiparent
20€ct-99 i 4.12 4,2U.26 17.7 8.60 8.66 3,068 3,m8 1.6 1.8 i Sanple fight bruruntrilElucent
2&Dec-99 i 3.89 4,ru.49 II
17-ran{0 i 4.02 4,ru36 12.7 7.63 7.U 9,420 9,'140 2.3 2.1 i Saqleffiparent
1&Apr{0 i 3.86 4,7U.52 12.0 8.s6 8.56 4,520 4,519 2.1 20.0 Sarnple colorless/bansparent
nl\ J€ 4,236.66 _20€ct-99
2$Dec-99
17.JamO
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4,233.95 18.9 8.30 8.3s 6,290 6,210 1.7 1.7 I Sarnple fight bromrtranslucent
4,2U.11 I
2.60 4,2U.6 13.2 7.73 7.73 9,000 9,010 2.4 2.6 i Ssnplewhitelhaslucerrt
2.57 4,ru.@ 13.0 8.66 8.66 3,817 3,815 2.3 2.4
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SPM t$lesrG-T$le 1 Page 2 of 2 oTsi/A7008 u4tm
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TABLE?. GROUND WATER SAMPLING ANALYSES
Laundry Supply Company
Salt Lake City, Utah
Fbld lnfqmdion sw{46 trleffiod 8260 a
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ND<6. 3 I Compcite sanple
24 BGS
ND<6.4!Cmrpcite
ite sanpb
IPCE/TCE scren @25 BGS
PCE/TCE scrsr @ 35 BGS
PCE/TCE scrsr@ 25 BGS
PCETCE screen @ 35'BGS
rcgTCEscren @-8 BGS
scngr @ 35'
PCE/TCE scrsr @ 25' BGS
rcgrcEscrsr@35
rcgTCEscrsr GD2g BGS
rcE/TCE ecrsr @ 35'BGS
D8
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SP2-25 ^6.Jun€8
SP2-35 26-Jun-98
SP}l5
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26-lun-98
26-Jurr98 i
SP+15 &.lun-98
SP+25 6^lun'98
SP+35 6-lum98
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. --a----------------ro)--a---aSP+15 2B..Jtm9E !
SPS25 26^Jun-9E
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3,(XlO ND<20 June98 GeoProbe decsr rrder
SIUar-99 ND<1 ND<1 ND<1 ND<1 ND<1 ND<1 320 ND<1 ND<1 FeF99 GeoProbe decon uYder
$ttla-9e ND<1 ND<1 ND<1 ND<1 NEl<l ND<1 1"000 1J ND<1 Febgg G€oPrSe ffisnrpb wder
2GG-99 NBl ND<1 1J NB1 ND<1 ND<1 ND<l.2 I ND<1 illw€,-7,€ det/sanding uder
21Oct-90 ND<1 ND<1 ND<1 ND<1 ND<1 ND<1 3 ND<1 ND<1 S&S/SH a€er&n wder
21€ct-99 ND<5 ND<5 ND<5 ND<5 ND<5 ND<5 &I 1(U ND<5 SB.5 sdl
21&-99 ND<5 ND<5 ND<5 NE}<5 ND<5 ND<5 7J T(U ND<5 S&5 scil
21e-99i ND<1 ND<1 ND<1 ND<1 ND<1 ND<1 u ND<1 ND<1 SgYgI{ auqer decon Y}der
Pagelcf4 oTSi/A7008 94t00
TABLE?. GROUND WATER SAMPLING ANALYSES
Laundry Supply Company
Salt Lake City, t tah
g
o
aa-fo(t-$-:3c,o!,
sP6-15
SP&25
SPS35
SP&15I ::ri
Fidd lnfqmdion
sP7-15
sP7-25
sP7-3s
tt €thod 8260 q
F E i.o,,ents
Jia-:
ralE=i
sE I
eFebg9l
iPCefiCE screen @19 BGS
ircE/TCE scren @?5 BGS
PCHTCE screen @ 35 BGS
PCHTCE screen @ 15 BGS
IPCETCE scren @29 BGS
ircE/TCE scrsr @ 38 BGS
iPCE/TCE screen @29 BGS
|PCE/TCE scrur @ 35'BG.S
IPCUTCE scrsr @28 BGS
IrcETCE scresr @ 35'BGS
IrcETCE scrcen @,%'BGS
PCE/TCE screerr @ 35'BGS
IPCHTCE screen @?,5'BGS
|PCE/TCE scrsen @ 35'BGS
PCFJTCE scren @ 15 BGS
rcgTCE screen @28 BGS
IPCBTCE scren @ 35 BGS
- IPCE/TGE scran @ 15 BGS
IPCE/TCE screen @-29 BGS
IPCE/TCE screen @ 35'BGS
!rcgTCE screen @29 BGS
IPCHTCE scrsr @ 35'BGS
PC9TCE scren @ 45 BGS
IPCE/TGE screen @ 55 BGS
rcEffCEscrsr@ 25'reS
rcE/TCE scren @ 35'BGS
IPCE/TCEscrsr @E BGS
!rcE/TCE screen @ 35'BGS
rcgTCE sseen @15'BGS
rcE/TCE screen @29 BGS
ircgTCE scren CD 35 BGS
"3FU.15-
SP925
SP935
"s'FiilG'
SPlo25
SP1G35
SPii:i,5-
SP1 1-E
sP11€5
"sFii:G-
sP1a15
sP12-25
sP12€5
SP13-15
SPl}|?5
sP1&36
NBs I ND<s
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sP1+25 Z7-F*99
SP1+36 Z7feb99
sPl+45 27+*99
sP14-55
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sP1625 Z7#.gg t -
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sP17-?5_
sP17€5
m$Fniects\LsCA7008\
SPM tablesrds-Table 2
=o={98oaEb
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Pqe2d1 oTvA7008 8t4t@
TABLE?. GROUND N,ATER SATI,IPLING AN/AIYSES
Laundry Supply Company
Salt Lake Clty, Utah
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i/Ml-1
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i,Tru-3
Duplic#
tvl\ ,-4
irt\ ,-5
Duplic&
Duplb#
Duplicde
Duplbe
tvMl-7
m&\Prciects\LsCA7008\
SPM tables.ns-TSle 2
Fidd lnfunndion Voldile Orqarics (SW€46 irethod E26O or eoui\ralenl I
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-5,r .iL5-a
=E,E€
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=Eaurg
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hciE;F :r.
6T-CD:a^r=l---,=ED!Y-o-YLlu .g8g
6T
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=- A
l--\.E9U0'-vLutEgE
gal
Fg i*,,ents
15F-nfaf98 ND<1 ND<1 ND<1 4tt a a,69,0(X'190 25
$trlar-$ND<1 ND<1 ND<1 130 52 1J 80,0(x,8Ur 76!
1 '{0 ND<l0 NDl<s ND<5 xn r00 ND<5 861000 730 ND<10
1 ND<1 ND<1 ND<1 6 340 15 gl,(xn 290 ,J -----
1$Mry.98 ND<10 ND<10 NE)<10 ND<10 390 I(U 79,(Xlo 2$)ND<10 labeled llrt 14
$'Mar-99 ND<1 ND<1 ND<1 ND<1 gn 45 17,(X)0 8(xl ND<1
20Oct-99 ND<1 ND<1 ND<1 IJ 1100 47 10,0fl1 610 ND<1
iiifrri6FUb-l'iiD.1U ilD:1-d 210 ND<10 'i{666"1"'35b- - -
$tvk-99 | ND<1 ND<1 ND<1 17 4m 31 17,(m 710 &Ji
$Mar-99 ! ND<1 ND<1 ND<1 u 4{n 27 tg,(x)0 790 19 il-#ed nn r€
24^Jur99 i ND<1 ND<1 ND<1 4:l 200 17 21,(Xl0 320 z2
17-Jan{0 | ND<1 ND<1 ND<1 69 r30 9.2 21,fi10 330 3s!
ND<1 ND<1 t3 ND<1
24-Jun-99 ND<1 ND<1 ND<1 ND<1 ND<1 ND<1 ND<1.2 ND<1 ND<1
2[},Oct-99 ND<1 ND<1 ND<1 ND<1 ND<1 NE}<1 NEFl.2 ND<1 ND<1
17-Jan{0 ND<1 ND<1 ND<T ND<1 Nt)<1 ND<1 u ND<1 ND<1
1 {0 ND<l0 ND<5 ND<5 ND<5 Nt)<5 ND<5 ND<s ND<5 ND<10
$tt ar-99
-------
ND<1
-Nii:i'-ft-ti:1''ir6:i'"306-'3s
---------960 l"'1i6''ifii.i'
24^Jutt-99 ND<1 ND<1 ND<1 ND<1 850 52 750 r90 ND<1
24^Jun-99 ND<1 ND<1 ND<1 u 830 52 750 r90 NB1 Labded lvlt l€
2GOct-g()ND<1 ND<1 ND<1 XJ 700 49 2r441p,340 NB1
200ct-99 ND<1 ND<1 ND<1 3.J 700 49 ZM 340 ND<1 Labded inv-g
17-Jan{0 ND<1 ND<1 ND<1 AJ 1,000 na 4800 520 ND<1
17-ran{0 ND<1 ND<1 ND<1 lJ 1,100 fia 2'800 560 ND<1 l-$ded tuMr-g
1&Ar{0 ND<l0 ND<5 ND<5 ND<5 910 97 1/l{X,an ND<l0
1&Apr{0 ND<10 ND<5 ND<5 ND<5 7fi q,1r20,,210 NE)<10 tabded m r-9
'ilIii;t:t*i L-------i Noct 'N'd:i'-ft-d:i'-iid:i'-iifri'-itb.i';.,5:r','ili6:i- -
ND<1
17-Jan{0 NE}<1 ND<1 NB1 ND<1 ND<1 ND<1 u ND<1 ND<1
1&Apr{O ND<10 ND<5 ND<5 ND<5 ND<5 NE}<5 ND<5 ND<10
'ririli--irili''ft-d:i-l'ND.i'-N'6.i''trb:i'x-ci:1-,-------
ND<1
17{an{0 ! ND<1 ND<1 ND<1 ND<1 ND<1 ND<1 u ND<1 ND<1
18rApr{0 i ND<10 ND<5 ND<5 ND<5 ND<5 ND<5 i0<5 ND'<s ND<10
tvTW€ 2GOd-99
1zJafrco
IAAorfl
'ttb':i''frrili''irili''ir6ii''N'D.i''tifri-'5:i'2 iiD:T''Nt5.i-
ND<1 ND<l NE}<1 ND<1 ND<1 ND,<Nf,Fl.2 ND<1 ND<1
ND<l0 ND<5 ND<5 ND<5 Ntxs ND<5 i0<5 ND<5 ND<10
9r-?l.i$Ascuran_q{-Q93!-ity-9-qtEB lSFMalbgB ! ND<1
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ttrol San"ft'#i'l ob Ana
forr---a
Nt)<1 I
!igF---
ND<1 NE}<1 ND<1 iD<1 ND<1 ND<1
RE€P 26-Jum98
EB A-po*
E-gg1a;irc2ffi
17-ram0
1&Aom'
r{D<2-3 ND<1.6 BlankPCE/TCE screen
-iD<s ND<5 Equipment Bhnk#CE/TCE scren
ND<1 ND<1 ND<1 ND<1 ND<1 NE}<1 i1g<l.2 ND<1 ND<1 Blank
ND<1 ND<1 ND<1 ND<1 ND<1 ND<1 nD-f .2 ND<1 ND<1 Blank
ND<1 ND<1 ND<1 ND<1 x,,ND<1 u u Ntxl Equlprnert Blenk
ND<1
t\iEm
ND<1 ND<1 ND<1 ND<1 ND<1 l.D<1.2 ND<1 ND<1 Equiprnent Blank
ND<5 ND<5 ND<5 ND<5 ND<5 r€<5 ND<5 ND<10
P4e3cf4 oTsi/A7m8 u4100
I
TABLE 2. GROUND WATER SAMPLING AMLYSES
I Laundry Supply Company
I Salt Lake City, t tah
Frrd lnfiormdion Vdatile Orqanics 15yy-${$ lUethod 8260 q auivaler I
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Comments
TB 2fiJur98 NE)<2.3 ND<1.6 iTrip Blank rcgTCE scrsr
s{rar-99 ND<1 ND<1 ND<1 ND<1 ND<1 ND<1 NE'<12 ND<1 ND<1 lTrio Blank
24^Jun-99 ND<1 ND<1 ND<1 ND<1 Ntxl ND<1 ND<1.2 ND<1 NE)<1 lTrip Blank
20.oct-99 Ntxl ND<1 ND<1 ND<1 Ntxl ND<1 5,6 ND<1 ND<l iTrip Blank
18rADr{O ND<10 ND<5 ND<5 ND<5 Ntxs ND<5 ND<5 ND<5 ND<10
NGs: pyl = Micrograns per Kilogran
udkg = Microg rs Per Liter
ND = Nd Hected (d laboratory reporting limit)
- = Not Anallzed or Reported
J = Andfe deteded bdor practical quarilitdim limit
1,1OCA = 1, l-Dichloroefhane
1,1OCE = l,l0ichloroethene
cis-1,2-DCE = Cis-1,2-Didllolrethene
Trals-l,2-DCE = Trans-1,2-Dichlsoethene
PCE = Teiraclrlaoeihene
TCE = Trichloroe$ene
BGS = Bdor Grcund Surfae
ndtPrriectsUscAT0OS\
SPM tSle.ns.T$le2
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Srfe Remediation Plan
Laundry Supply Company
APPENDIXA
HRC GRID DESIGN
SPREADSHEET
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I,^'ERIAL SAFETY DATA SHEET
Jast
Revised: January 27,1998
MSDS
-ection I - ilaterial ldentification
!**-ffi*sffi*ffi***
upplien Applied Pouer Concepts, lnc.
411 East Julianna St.
furaheim, CA 92801
Jr"rhone: (714) 502-1150Tacsimile: (714) 502-2450
hemicalName: Propanoicad,td,2l2l2{2+ydoxy-1-oxopropory)-1-oxoproporyl
-1 -oxoproporyl-1,2,}propanetriyl ester
Jnemical
Family: Organic Chemical
Trade Name: Glycerol tripolylactate
*ffi
Jot * za.n6z-22-o
lQne should anticipate the potential for eye initation and skin initation with large scale
]nosure or in sensitive individuals.
lection 3 - Physical Data
Si ffi*ffi*
Ilelting Point: NIA
loiling Point: ND
Flash Point ND
fensitV: 1.YT g/cc
lolubility: Acetone and DMSO
frp"rrance: Pale white liquid
{fdot: Not detectable
faeor Pressure: None
I**"**ffitffiffi*ffiffi
l*,on 4 - Fire and Explosion Hazad Data
Jtinguisfring Media: Carbon Dioxide, Dry Chemical PorderorAppropriate Foam.
J*r
mry be used to keep exposed containerscml.
I Page 1
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For large qmntities involved in a fire, one should uearfull protr{ive clothing and a NIOSH
approved self cortained breathing apparatus with full face piece operated in the pressure
demaM or positive pressure mode as for a situation vrfiere lack of orygen and excess heat are present.
Section 5 - Toxicological Informatlon
I
Acute Effeds:
T
I
RrEcB[Hlosoooo
lnitation data:
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t
Toxicity data:
T
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RTECSilT OD2800000
1,**":::o
I roxicity data:
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May be harmful by inhalation, ingestiolr, or skin absorption.
May cause initation. To the best of our kno$dedge, the chemical,
physical, and toxicological properties of the glycerol tripolylactate have
not been investigated. Listed belor are the toxicological information
for glycerol and lactic acid.
t
t
Target Organ datia: Behavioral (headache), gastrointestinal (nausea or vomiting), Patema! effects
(spermatogenesis, testes, epididymis, sperrn duct), effects of fertility (male fertility index, post-
implantation mortality).
SKN.RBT 5OO MGI?4H MLD
EYE.RBT 126 MG MLD
EYE-RBT 5OO MG/24H MLD
ORL-MUS LD50:4090 MG/KG
SCU-RBT LD50:100 MG/KG
ORL-RAT LD50: 1 2600 MG/KG
IHL-RAT LC50: >570 MG/M3I1H
IPR-RAT LDSO: I I2O MG/KG
IVN-RAT LD50:5566 MG/KG
IPR-MUS LD50: 8700 MGIKG
SCU-MUS LD50:91 MG/KG
IVN-MUS LD50: 4250 MG/KG
ORL-RBT LD50: 27 GMIKG
SKN-RBT LDSO: > 1 OG]vUKG
IVN-RBT LDSO: 53 GT',UKG
ORL€PG LD50: T75A MG/KG
SKN.RBT 5MGT24H SA/
EYE-RBT 750 UG SEV
ORL-FUAT LD50:3543 MG/KG
SKN-RBT LD5O:>ZGIIUKG
ORL-MUS LD50: 4871MG/KG
ORL-GPG LD50: 1810 MG/KG
ORL QAL LD50:>2250 MG/KG
SaJCAE-,^A7,1986
BIOFX.94t1970
85JCAE-,2A7,1986
FRZKAP (6),56,1977
NIIRDN 6,215,1982
FEPRAT 4,142,1915
BIOFp 9<;1920
RCOCB8 56,125,1997
AMNAD 26,1581 ,1976
AMf.lAD 26,1579,1978
NIIRDN 6,215,1992
JAPMAS 39,593,1950
DMDJAP 31 ,276,1959
BloFr 94t1970
NIIRDN 6,215,1982
JIHTAB 23,259, ffN1
SaJCAE -,656,96
A"JOPAA 29,1363,46
FMCHAz-,C252,91
FMCHA2-,C252,91
FAONAU 40, 14,67
JIHTAB 23,259,41
FMCHM-,C252,91
Page2
I
I M.DS
I Or, selected registry of toxic effects of chemical substances (RTECS) data is presented here.
See actual entry in RTECS for complete information on lactic acid ard glycerol.
T
Secdon 6 - Health Hazad Data
Handling: Avoid continued contactwith skin.
I
'n "ro
me or "", "rJ":ffiJ;,-", a prrysicianstroutd be oonsutted immediately.
I ,,*Aid Procedures:
I lnhalation: Removeto fresfr air. lf not breathing give artificial respiration. ln caser of labored breathing give orygen. Call a pirysician-
I lngestion: No effects expected. Do not give anything to an unconscious person.
I Calla physician immediately.
I Skin Contact: Flush with plenty of water. Contaminated clothing mry bewashed or
E dry cleaned normally.
I Eye contact: Wash eyeswith plenty of uraterforat led 15 minutes lifting both upper
I and lorver lids. Calla physician.
Section7 - Reactivity Data
Conditions to Avoid: Strong oxidizing agents, bases and acids
I Ha.ardous Pdymerizati<None knolrr
I Further lnformation: Hydrolyses in vyderto form Lactic Acid and Gtycerol.
I ;;T g: spill,t?lf o,esglo:T lrog"dy,"s
tAft erspi'aseorLeakasi:"ffiffi1,i""::,i,5:l's;J*",ffr#-HT#:lxg.T#:*
I Disposal: Laursandregulationsfordisposalvarywidefybylocallty. ObserveE :i;'$;Tffii;1$:,f,ff;J#,"ffi,:1,ffi.5,ffiera,hours
I No rcquirenrent for a reportable quantity (CERCIA) of a spill is knom.
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MSDS
Section 9 - Special Protection or Handllng
Should be snored in plastic lined $eel, pla$ic, glrc, aluminum, stainless $eel, or
I
reinforced ftberglass containers.
Protective Gloves Mnylor Rubber
I Eyes: Splash Croggle or Full Face Shield
I Area should hane approred rneans of nvastring
r Ventitation: 3ff;o,eNhaust.
I Storage: Store in coo|, dry, ventilated area.
Protect from imcompatible materials.
Section {O - Other lnformationII This material will degrade in the environment by hydrolysisto lactic acid and glycerol.
Materials containing reaetive chemicals should be used only by personnel with appropriate
I chemicalhaining.
T
The infonnation contained in this document is the best available to the supplier as of the time of writing.
I Some possible hazads have been determined by analogy to similar classes of material.
I No separate tests have been performed on the toxicity of this material. The ilems in this document
are subject to change and clarification m more information becones anaifable.
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NAMOHC BOREVIEDIATION USNG HRC
ic bioremdiaim has been rcognized in recat yeanl iN ore of the primry at&nuatim
isns blt uthich a rnlmher of onhmimns can be coAined adfu remdi4ed- Codamients
e b anaercbic biaercdiation irchrde chlainated sdrrcne srch as PCE and TCE, meals
as hexa\raleff chrcmiuq and pesticides nrch as chludane.
C ders a passivg lour-cost apporch to in-sinr aaerobic bioremediatim- Applicatim is fast and
cient ad gliminat€s visible siglrs of on-gciry rdiatio- The use of HRC significafly re&tcs
ign oss md fte need fc capital md operation-inrensirrc rcchmical systec.
is a prqrieary polylaaa;e ester specially famulated for &e slow release of lactic acid upm
dratim. \ilhen HRC is introducd to fte sr$surface, varicus irxrigmw organism help urcorple
rctic acidfromHRC Tben, ferrrsrtative maerobic microbes w&oliz.e tbe lactic acid, driviry an
uifer amerobic and prodrcing hydrcgen in tb praess. lvficrcbes capable of bidqgical
enation (in uifui&' halqgens, typrcally cHcine, are rerrD\red from fte pareil cotrmioant)
can rr;e tb laydrogeo. Sirce most of the cmamination problems invdve &lorinatd
y&ocarbons, refererce is usrnlly made to fte process d "rdrrtive dchlorinaticn" and i8
iationby redu<tive dschlorinr6s. In fte term of oxidaion/re&rction chemistry, bdrogenc m dectron donor md fte chlorinard hy&ocarbon serves as tbe eletron rccepc.
eforg HRC shorfld be onsidered a tircreleas elatron dmor m*erial (sinc fudrcg€n is tbe
Etrorr donor in the dechlsination reaction).
is a moderdely flowatte rrwterizl ftat can be injeced ld€r presflne into an aquifer rciry
rious direct-push techologies. It can maintein dedlorinaing onditions in tbe aryifer for six
to one year or mae dependiry on sie cmditios. UIh marnrfactured as a thicker, fudgel,
1 crn !g applid tsrry a bllcn-stentt alger ils a slowly dissolving "irylant" This larer optbn may
fer mauy years of cominrnus rdease, Aeeeoaing m sie codi6oc. In eifrer fcmulaiom, HRC
ovi&s a time-released fudrcgen soure to aaelerate fte reductircn cf anrrcbically degndfule
are a ntmber d advatages to tsiry time-release starcgies. Irylemetaion cf the appropriare
rdease sysmcanelirninaE *1jor apitd, ard operatirn:l oss associaedwi& rcchznical
, becarse it is delivercd into fte aquifer ody orce or trie a )'ear. The rlse d siryle,
iquions push-poid idectiontechmlogyma&es apflicationfasg dircce4 ad uinimally disnrytive
sie operatios. Project design is siryIified sire tbre is m need for fte design of abovegrouod
process md equipt HRC wifl remaia urhere injeced ad slcmly g€nerafe hi&ly
le organic aci& md hydrogen Since chlcrinated Sdrocaftcr scrc€s are difficult b lea,E,
cudinrDus, higbly diffnsible series of cgmic subst*es rzn imease tb effectiveness d cmtact
biod€radatim.
HRC.{s lnfro to HRC
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RC Design Software
enesis has developed ad distribued the HRC Desrgn Softrvare b aid experienced emrironmenal
rofessionals in tbe proper dcign of cceleraed natural temrationztioremediaion projects. One of
e irryortmt faces of the software is &a it enables the user b perfom muldple iterations of th
ie design with litle effut and to easily evaluaE a nrmber of "what if' scenarios. By aldng ltis
roach, an HRc-based bioremedidion strdqy can be optimd.rnd.
esigns for HRC-based biaemediation prdects are based on delivering IflC inb conaminted
orndrvaEr plumes in a grid or brrier patern, or a combinatim of boft. The selection of the
ropriate design depends pimarily on the siz of &e plum requiring remediatim, groundwder
elocity, sie accessibility to injectbn equipnefr, and desired time frame for remediation. Grid-
ased designs are typically recmmended for small- b mediutrr-sized contaminar plumc in which a
elatively shct remediation period is desired. In comast, barrier-based desigu are rcommendcd
sies with widely distribued high oncentation plumes, seyer€ acces limitations, or long-term,
ume qrt-off remediation stcqies. The primary design issues are (1) amouut of HRC required o
uppoil biodegradation of a given amoud of contaminant md (2) number of delivery locatims
eeded O effectively distribue electm dppl wirhin the coduninantplume. Design approrhes and
amples for bodr HRC grid and barrier approaches are described in the following sectims.
ile we have designed the HRC Desigu Software b be user-friendly md self-explanabry, from
b time &e user may have questions relating to softryare input paraneers or to the
ppropriateress of the sie for the tse of this technology. These facb$ may have a direct bearing on
e feasibility, performancg and cost of a rerrediation project Therefore, Regeaesis stotrgly
eommends that fte user coffact us direcdy for assistance in &veloping an effective HRC-based
ioremediation design for a specific site of concern.
ume Area Treatment H RC Grid Design
C cm be the most cct-effective alemative for treating a contaminad plume area. HRC is
Ljeced ino tbe aquifer mmix in a grid pa&rn over lte areal exEnt and acros tte vertical zme of
contaminant plurr. The shape of the area to be trcaed is deermined primarily by the shrye of
e contaminent plume or tte accessible area wittin the plume. For exmple, long narrow HRC
ids are constructed for long narrow @naminmt plumes.
the event frat &e plume is very lrge and an HRC injection grid is not cost effective, tten m
ErnaE approrch is b we a series of HRC bariers. These HRC barriers are installed perpendicular
the groundwder flow directim at rqular inervals &rougtort the leng& of the plume. In fris
ign approacb, a unit volume of codamiraEd watsr moving in &e plume is subjectto sequetrial
of hydrogen to fuel the reductive dechlorination reirtions.
pr*. cutoff Treatment: H RC Barrier D esign
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ume CutO ff Treatment: H RC Barrier D esign
C can be injeced in one or rmre rcms of, ddivery poins to form an HRC barrier, ttereby
ating m maerobic treatrrEnt zone orientsd b inErcep tte dowagradient migration of
taminanB. The HRC barrier eclnology can be considered a "permeable barrier" echnology;
owever, with HRC there is no need for slurry walls or *gaEs," as required with cber more cosdy
able barrier tahnolqgies .
n aeas of high groundwaEr velocity or ontaminmt loading, it rnay be neessry to insall multiple
s of application points. The locatioas of delivery poins in erh row are staggered with respct o
oinr in other rows to minimize fte effective sprcing perpendicular b grqrndTvaEr flmr. Barriers
y also be cmstructed in an iterative fashion so tht barrier arays ine installed over time o satisfy
egulabry criteria, remediatim budget, and the overall enviromrenal sEaEgy for a given sie.
t should be notd 6at HRC permeable barrier-bued designs are typically asscided wifr a
onteminant cotrainment straEgy ard do not proride for souce area remdiation. If remediation of
e cortaminant source area is not performd, then the HRC barrier will need to be mairaired over
e via re-injection evenB.
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lssolved-phaEo e roundwater G oncsntratlons
nder this cdegory of input paramet€rs, reprcsentative cmtaminaut conceffrations are spcilied for
e area where IIRC will be &Iivered. Specifically, disscflved-phase conceffrations that are
ermined by groundwter well sampling and analysis are enered here. While it is imporant o
nsider tte mostrec€nt daa available, fre inpu values should represetr the conentrdion frat the
er judges b be indictive of acurd subsurfre conditions over the course of an entire hydrogeologic
cle.
geuesis has included input eaces for fte mct cornmonly ercountered dlorinatod solven6;
owever, HRC will stimuliae the degradatim of a myriad of polluas. If the contaminad tte user
erned with is notlised for inpuq pleae contact Regenesis direcdy. We will be glad b assist in
rmining thc amount of HRC required b treat otter less commn coutanrinanB.
orbed Phass C ontamlnant t 8Er
or HRC grid designs, there is usually a multiple of the total dissolved contaminant mass that is
uod to tte saoraEd soil zone matrix. This is called hy&ophdically sorbed coilanination and can
visualized as a thin layer of conhminant that is reaird by clem aquifer maerials whcn they
ome inb coftrt with a dissolved coil@inant flom. Thc mass of ontarninant ssbed to tbe aquifer
trix is a functim of &e bulk density of tte aquifer marrix, the fraction of organic carbon in thc
nput and O utput Parameters for H RC Dcxrign Software
qnorEl Inf ormatlotr 0n Soltraro U so
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ser inpu pdamet€rs are shwn inblue, whereas cells onaining the results of caloilations are
hown inblaclc Red warnings or guiding co@ts may b€ generaed in resporee to the sprrea&hea
ios. Dialog bores "nd point md click butore ae available to asist wift d*a emy ,nd b
vigate the softnrare.
rslo Slto (! harrotsrlrtlcs
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asic site cbaracteristic pa'rmetenr are nee&d to specify tb physical site characgistics. The width
deph of the cotrminant plume refer to the plamed treaiment area, ufiich can vary depending o
ial goals aod clemup strategy.
iof the Contaminaed Saturaed Zone specifies the vertical ifiickness ircross which HRC will
delivered. Tb vertical thicloess is dictaedby the estimatd frickness of the onaminat flume.
or instane, if a siE hac a cmtaminat plurc spannirg tb saftratrd ane abore an aquitard, the"r
desrgn sbuld trea tbe aquifer dourn to fte aquiard. If th ontaminant plume is limied o a
ealized depth iterval or lithdogic layer, ften HRC iqiection canbe limied to tbe onaminad
intenral.
HRC rmterial ost is proportional to th ftidrness specificatim. Therefore, it is impor"rrrt to
ine the vertical @ntaminmt distibutim as acctrrately as possfrle. If only moderate
tims of cpnta'minant ae present, md no vertical profile of the pluae hac ben dme,
gresis suggeils &at tb urcr as$Ere a 6icbss of ryproximtely 2O feet. Porosity refers to the
pacity of the aquifer soil matrix. Using the above inprt paa'rFErs, the oftwae will calculae
treament zorE pore Yolume.
idormdion rcgading aquifer tra$port properties are reqrcsEd. Tbe hy&aulic gradient errl
ivity ae used to calculate the groundwater seepage vdaity, which cm be used b select
ivery poitr spircing and evaluate flow dynamics \iliftin tb grid.
ix (fJ, and fre contaminad-partitiming ccffrcient QQ). An estimaE of the mass of sorbed
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x (fJ, and the conaminant-partitiming ccfficient (IGJ. An estimat of the mass of sorbed
ontasrination is calculated in ftis setim by enrring the facbrs mentioned aborre. Input yalues ftr
he soil, fre bulk density, and the fraction of organic carbon (fJ can be measured or estima,Ed based
soil type. The Ko"valrc can be obained fu each contaminant frm any number of published
efererrces.(
dd ttlon al Il om ul d F act or
Additional Demand Fror is usd to aocourt for uncertafury abort 6e potetial sinks for electrcn
. This factor can be ftought d as a cotingency c safety factor, which is rsed b rccornt fcr
many unertainties intrerrerrt in a subsurfaa investigaticn and in-sitr remediatim project. Poecial
ources of additional HRC &marrl irlude highr thap eryeced @ntaminant mass (i1the form of
esi&nl phase DNAPL ad/ot high onentraioahot spos), microbial demand in ercess of the
timted 3x, and urnertainty abqrt the quantity of HRC regrired for 6e reduction of iron and
ganere. The siryle rasurcmetrt of th onmtrtior of frese cmpeting electun acc€pbrs in
orndraEr samples does not give an accuraE repres€natian d the iron 6fl manganes€ redrction
sine these ryecies may be pres€d either as colloids or attrhed o the soil matrix Regenesis
ecomm€nds an additional demand faorr of 2 to 3 fa a fnst appliction at a sie.
lfe Span lor 0 ne A pplloe[on (lor barrler ilodgtrs)
or IIRC ba:rier desigre, fte life spa fu one application shotild be input in this field. This value is
flornr of contaminar urass into the barriered with the groundwder seep age velocity to estimate the
ing this perid of time.
B C Il eltvery Polnt SD eclng 8nt f, B G I! odng B ets
or grid &signs, thercommendod spacing for HRC deliverS; points raqges from 5 feet-on-mffi b
15 feet-oa'cemer. Sprcing is a function of soil type, grfindrraEr velocity, and ncessay HRC
ing. Gcrally, the lower tbe hy&adic eoductivity of the soil matrix, th dcer &e sprirg.
or siEs wift silts and clay, delivery point spacing should be 5 b 8 feet-on-eng, while a site with
and gravels may have a spaciqg up to 15 fet-m-center. The Delivery Poit Spacing section of
Grid Desigo worlshee allows tb desig!€r to calorlae the required number of points and HRC
rfre for a given plume siu nd sprcing.
or barrier dgsigns, a series of staggered HRC injection point rows are typically constnrcrcd ihe
0rDotlrg BlooEol A GoeDtor C oncatrrtlou
he conentrations of coryeting electo accepttrs (CEAs) such as dissdved orygen, niratg ferric
on, and sulfaE have an dfect on the ammnt d HRC required for enhancing in-situ bicemediatim.
ydrogen"from fre HRC is used to redua tkse CEAs b create redu oonditions frat are conducive
re&rctive dedilorintim procsses. As a result, the CEA- demand for hydrogen (md conseqrendy
RC) must be considered in fte specification of fte amount of HRC rquired fc a project
undwaEr data indic*ing the actual siE values for these paramet€rs arc irrportmt in deermining
accuraE final design fu HRC application However, in tte absence of ttese data, reasonable
timaEs of these values cm be made to getrene a preliminary design and cct estimaE.
lcroDld Demm0 Pactor
addition to cotrryninant and CEA demand for HRC, subsurface microbes will rse some of the
tic acid as a source of energy or strctural carbon. Thereforg in desigring an HRC applicatim,
ese competing microbial p(ocesscr must be taken into accouff. Regenesis' experience indicaes
t a value of 3 suffices under most cmditions. However, if sie-specifrc laboraory microcosm data
arrailable, fre designer rzn input the appropriate value direcdy.
bctive sprcing of delivery points perpendiqrlar to the grroundwaE flow should be rn Ex)re trzn l0
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'ective spacing of &livery points perpendicular to the goundwater flow shouldbe il) trxlre fra 10
-on-cent6. The Delivery Poir Spacing sctim d &e Brrier Design wortshet allows the
igner to estimae tb required nunber d poits aod HRC dce rae fa a given barrier length ad
inatr flow ratg.
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roposod InC 0rtd Spclllcatlons
this secion d the workshet, the desigg may adjust fre btal nrmber d injecioa points ad the
C dosing ra& c leave it as calculaed. Tb softwae wiII then calculae the ost d HRC magial
e*imae tte cost of shipping aod trxes fa th given scqe of the project (i.e., rumber of poinB,
eatnent thickness, and HRC dmiry rate).
v
BG Ingtallatloh C ost Esttnate and Totat Profect C ost --
:
tbugh Regenesis das not perfcm irtallation serrriceq our experience on may apflicaior has
iven us an understmding d the costs assciared wift iratling the HRC. This secion offers tb
igner ar opeortmity to estimde hcff rnuch the HRC gid a barrier apflication will cosl Tb
ested iqutparameenr required are based o Rqerqis' eryerieoce. The result of this section is
estimaed subcoffiacbr installatim cost This estim*e shorld be adjusted based on local cmtr
. The Toal Project Cost prodded represenB tb sum of the IIRC Insallation Cost Estimate and
HRC M*erial Costs. ft does not indude the costs associaed wift groundrrarr monitoriry,
irg, or coiliulting oveffiight
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RC Grid Dedgn Erample
RC injection grids are cmrmonly eryloyed d siEs where a loolized area of a ontrminant phme
be c6st-effecively remediated. The design process fc this treatuent sr.d;q.y is dccribed below
r a hypofreticd sit as a two-sEp prccess, with fre compleed spreadsheetfollm,itrg.
tep l; 0 athsr Belevutt Stts A srorsmmt Il ats
wift any remediatioa design, fte first step is to gafrer the relcrant siE assesment data. For
urple, consider tbe followirg sire:
Y t
Litholqgical data: Groundwaer is locaed 10 feetbelow tbe groirnd surface (bgs) and exends b a
depth of 4(l feet bgs at which point a clay aquitard is encounEred. Aquifer sediments consist
primaily of silty sands.
Contaminant concentrations: PCE concentration ranges from 0. I @ 5 m;grt-. Daryhter products of
the biological degradation of PCE are identified at the following cmcentrations: TCE at0.5 mgtl-
and cis-I,2-DCE at 0.5 mgzl.
Extent of impacted groudrvaer:
. The areal extent of the conaminant plume is estimaed o be 50 feet wide by 100 feet
long.
. Most grormdwater monioring wells comain scre€[ inervals tbat extend to a depth of 20
feet bgs. Vertical profiling of tbe contamimnB is accornrplished by (1) insalling several
groundwater wells with screened imervals locaed from 25 to 30 feet bgs and (2) by
collecting groundwaEr samples rsing directpush equipmenr This result in tk
cmclusion &t fte cofitaminenB are limied b the Wp€r 15 feet of the aquifer.
Aquifer redox conditions: ORP = 100 mV, DO = 2 ^gL, nitraE = | mgtl-, dissolved iron =
t0 mgtL, slfce = 50 mgtl-
Additional aquifer paameters: The follcmiag parrmeErs were collected through soil and
groundwatr investigatims or estimaEd or cdculaed using indutry standad procedures: fraction
of uganic carbon (0.005), porosrty (0.3), hydraulic gradient (0.005 ftzfQ, hydraulic conductivity
(10 ft/day u 3.5x10-3 cm./sec), groundwd€r velocity (60 ftlr).
tep 2:Sveluate $lte Ilata atrd Spedfy E BC Ertd Il eCgn ard G ost
he next sep is o deermine the scope of the remediatim. Afur evaluating healfr risks and
oundwaEr quality thresholds, the desigrer sp*ifies a cleanup goal and the extem of the
onrrminant plume requiring remediatim. Fc this example, assurrE ftattbe following decisions are
conerniry the remediation design:
Areal md vertical exEnt of aquifer requiring remedidion 50 fea x 100 feet x 15 feet
Conservative estimae of cmtaminant cmceffiatios to be biuemdiaed: 5 myL PCE, 0.5
mgzl TCE, md 0.5 mgzl cis-I,2-DCE
pres€nce of daugher prodrrs from the reductive dechlcination of PCE indicaEs that the
iodegradation of PCE is ocorring to a limiEd ext€nt Geochcmical parameers (ORP, DO, ee.)
dicate fratthe aquifer redox cmditions are not yet in the o6imrm range for th redrctive
hlorination of chlorinaEd hy&ocarbons. As a resulg the remediatim designer decides that HRC
m be used b drive the aqpifer more anaerobic and aceleraE tb redrrctive dechloination of PCE
d its daugher products.
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he quantity of IIRC needed to firel the reductive dchlorination process is estimated wing the siE
.rrFro.r.t.ryioaf Ia}rr .r*r,L,a.'rorl.tt ,far.i.=tr crtiJali.rc. TLa IJIDn a-iA iacirrr i.. .'it+rol if|a,l trt, rrr.i*t.=
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r Irts qu4[u]y or rr (r- Itccucu u, r r.Et ute reuucuvc uec[rufrEtuu[ Proues$ r,s tsurllalcu utlllt ut€ $rll
sessment daa and general design guiddines. The HRC grid design prccess is simptified by usitrg
HRC Grid Design worksheet md consists of specifying lte following design variables:
Site inforrratim: Plurre dircnsions, aquifer tansport paam€ters, ad cofaminant and CEA
conccffiations are entered inb the wrksheet
Demand factos: A microbial &mand fror of 3x is used, aod an additional demand factor of 3x
is cbosen sine tte edire soure df thg g6ilt minantplume is targeed for remediation with one
applic*ion of HRC.
HRC delivery goid spring: A delivery poim spaciry of 10 feet on cenEr is sdected o provide a
reasonable distribution of HRC iro &e conaminatr plum. This resule in an HRC grid of 10
rows of,S poim per row, for a tdal of 50 delivery poins.
HRC injection amounf : The cotamimnt and competing eleqtron accpbr concentations,
adsorberl phase concentratioro, md demad facbrs arc used b.estimde fre required arnouft of
hy&ogen end orresponding HRC reqpired for the rcdrctive dechlcination reactions. For a 10
feet-m-center spacing (and 50 toal injection poins a determineil above), a vertical HRC
applicCtion rde d 6.8 lbsft is calculaEd by fre softrrare. Therefore, a total of 5, 107 pounds of
HRC ae required (50 poins wifr 15 feet of injection per point at 6.8 ponds of HRC per vertical
foot).
Coet estimae: The HRC maedal c6t is $6/b for a btal of approximatly $30,640. CosB fa
shrpping md applicable taxes yary from site b sie and should be requesEd from Regenesis' sales
or techdcal suppofi saff if a detailed ost estimaE is needed. HRC installaion ccts cm be
ctimaEd rsing a daily rate for the injection subcomracbr ad an estimaE of the production raE
for the sit. For ttis exmple, it is assumd tbat two injection point can be ompleed per hour
md that a Geopr&e rig coss $2,000 per day and is mbilizdfor $1,000. The insallatim cost
for 50 iqiectim pohiB to a dep6 of 25 feet is ften $9,000, resulting in a oal installation and
HRC maerid cct of approximately $,10,700.
o summarize, the following issrrcs should be onsidered during fte HRC grid design and cost
stimatim procss:
Injection point spacing typicdly ranges from 5 to 15 feet-on-ceffer, md its specificdion depends
on groundwa&r velocity, sediment permeability, required HRC i4iection amoun6, md HRC grid
size.
The HRC injection rae for each poitr typically rrnge:r frorr 4 b l0 lb/ft, and is specification
depends @ the aonaminant oncentations, coryeting electron accepbr concentratims,
competing microbial demand, and soil type. It should be noed frat using fewer poiffs and higher
66ss might not provide suffrcient di*ribution of HRC and lactic acid frroughort tte coffarrinen
plurre.
For larger plums nd/ot large ranges of contaminant onentrations, tte HRC dose raE should
be adjused as appropriae (i.e., tb plume can be divided itro high-, mdirmr-, and low-
sonf,amin6f concentration areas, each with a specific HRC dose rae).
Th nced for reapplication of HRC will depend on achbvable biodqradation raEs, remedial
goals for lte site, prcximity of downgradient receptas, ad otter eeinical/regulaory issues.
Some sies will require only one application d HRC, while otters may require multiple
reapplications; however, &e reapplications qrpically will be done at lower HRC dses and in a
smaller grid area.
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Aqulfer tatrb( Dry Butk Density Tohl Porosity Effective Porcsity llyd. Conducilvity(gm/cm3) (dimless) (dimless) (filderyl
CIay 1.00 - 2.40 0.34 - 0.60 0.01 - 0.2 1t' - 1oo
Peat 0.3 - 0.5
Glacial Sediments 1 .15 - 2j0 -0.05 - 0.2 10t - 1o'
Sandy Clay -0.03 - 0.2 -
sirt t -0.34 - 0.61 0.01 - 0.3 0.001 - 10
Loess 0.75 - 1.60 -0.15 - 0.35 0.001 - 10
Fine Sand 1.37 - 1.81 0.26 - 0.53 . 0.1 - 0.3 5
Medium Sand 1.37 - 1.81 -0.15 - 0.3 50
Coarse Sand 1.37 - 1.81 0.31 - 0.46 0.2 - 0.35 100
Gnavely Sand 1.37 - 1.81 0.2 - 0.35 250
Fine Gnavel 1.36 - 2.19 4.25 - 0.38 0.2 - 0.35 500
Medium Gravel 1.36 - 2.19 0.15 - 0.25 5,000
Coarse Gravel 1.36 - 2.19 0.24 - 0.36 0.1 - 0.25 10,000
Sandstone 1.60 - 2.68 0.05 - 0,30 0.1 - 0.4
Siltstone -0.21- 0.41 0.01 - 0.35
Shale 1.il -3.17 0.0 - 0,10
Limestone 1.74 - 2.79 0.0 - 50 0.01 - 0.24
Gnanite 2.24-2.#
Basatt 2.OO - 2.70 0.03 - 0.35
Volcanic Tuff 0.02 - 0.35
Page 1
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a From Knox et al, 1993
b From Jeng et al, 1992; Temperature = 20"C
c From Houard, 1990; Temperature = 25oC
d From Horard, 1989; Temperature = 25"C
e From Horard, 1989; Temperature = 20"C
f ATSDR, 1990; Temperature = 20"C
g From Houard, 19901 Temperature = 20"C
Koc Values
Gompound Solubility (mgrL)Koc (UKg)
Tetrdrloroethene 150', 1503"263', 35f ,2H23gt
Trichloroethene '1 100''t 10f,137-,97-150t
l,l0ichloroethene 225A', 25000 e[.6t, 90.2b, 150tI
cls -1,2-Dichloroethene 35(p"90.2D, 4gc
tmns -1,2-Di ch I oroethene 63od''5g.9", 90./, 36"
Mnyl Chloride 110f, 26730 2.45t, O.+56d
1,1,1 -Trichloroethane 1495c 1 93"
1,1,z-Trichloroethane't 4/i2a"7A"
1 ,1-Dichloroethane 5060d 40'
1 ,z-Dachloroethane 9520"33 to 152"
Chloroeffiane 5710"33 to 1#1"
Hexachlorobenzene 0.006t
1,z-Achloroberzene 1 56t 272to 1466c
1 ,3-Dichlorobenzene 111s 293 to 31 ,600s
1 ,4-Dichlorobenzene 74to 8t'273 to 1833o
Chlorobenzene 4720,83 to 3890
Carbon Tetrachloride g05s 1 10s
Chloroform 7950"< 34"
llethtlerie Chloride-13000"4g'
Page 1