HomeMy WebLinkAboutDSHW-2018-003922 - 0901a0688080c67dDiv of Waste Management and Radiation Control Chevron 1%0 IMO John Amato Project Manager MAY 03 2018 7-44 V V-ZI Refining Business Unit Chevron Environmental Management Company 324 W. El Segundo Blvd. (M0-133) El Segundo, CA 90245 (310) 615-5034 John.Amato@chevron.com April 27, 2018 Mr. Scott Anderson Division Director Division of Waste Management and Radiation Control Utah Department of Environmental Quality 195 North 1950 West P. O. Box 144880 Salt Lake City, Utah 84114-4880 RE: Response to Review Comments on Contaminant Transport Model Update Chevron Products Company, Salt Lake Refinery, Salt Lake City, Utah Dear Mr. Anderson: On March 12, 2018, Chevron received comments from The Utah Department of Waste Management and Radiation Control (Department) seeking further clarification on several aspects of the Groundwater Flow and Contaminant Transport Model Update submitted in December 2017. EarthFax Engineering Group, LLCs (EarthFax) was tasked with preparing the responses to the Department's review comments. The memorandum from EarthFax containing both the Departments review comments and their responses is attached. If you have any questions or comments regarding the attached memorandum, please contact me at (310) 615-5034 or via email at John.Amatogchevron.com. Sincerely, JohI Amato Project Manager Chevron Environmental Management Company Cc: Hao Zhu, Utah DEQ Keith Rittle, Trihydro Christina King, Chevron SLR TECHNICAL MEMORANDUM TO: Mr. John Amato, Chevron Environmental Management Company FROM: Richard White, EarthFax Engineering Group, LLC DATE: April 26, 2018 RE: Response to Comment on the 2017 Chevron Salt Lake Refmery Groundwater Flow and Contaminant Transport Model by the Utah Division of Waste Management and Radiation Control In December 2017, Chevron Environmental Management Company ("CEMC") submitted a report to the Utah Division of Waste Management and Radiation Control (the "Division") entitled Chevron Salt Lake Refinery Facility Groundwater Flow and Contaminant Transport Model Update, prepared by EarthFax Engineering Group, LLC ("EarthFax"). The purpose of that report was to update the results of prior modeling of groundwater flow and contaminant transport performed by EarthFax at the site beginning in 1992 and as subsequently updated in 1996, 2012, and 2014. In accordance with a post-closure permit issued to Chevron originally in 1997, the 2017 model also included a Monte Carlo uncertainty analysis. On March 12, 2018 the Division issued comments to John Amato of CEMC concerning the 2017 model. The purpose of this document is to respond to the Division's March 2018 comments. For the sake of completeness, the Division's comments are presented below in bold italics with responses presented in normal text. I) Chapter 2, page 3 and 4. The text mentions that an upward gradient exists between the deeper, confined aquifer and the surface aquifer (the focus of the update). For clariV, please state how many locations this was observed at, and y' any current data exists to confirm these observations which date back to the 1992 and 1996 model reports. Historical groundwater quality data collected from deep monitoring wells at the Salt Lake Refmery consistently indicated a lack of detectable hydrocarbon concentrations. Therefore, in accordance with the facility post-closure permit, all wells monitoring the deep, confmed aquifer were removed from the groundwater monitoring program in 1997. Several of these wells have since been abandoned in accordance with Utah standards to accommodate infrastructure modifications at the refmery. As a result, no local data have been collected since 1997 to confirm the upward groundwater gradient at the Salt Lake Refmery. However, long-term data downloaded from the U.S. Geological Survey Active Water-Level Networki, as summarized in Figure 1, indicate that groundwater levels in 2017 collected from wells completed in the regional confined aquifer near the Salt Lake Refinery are consistent with those collected in the early 1990s when the flow model was first calibrated. Therefore, it is reasonable to conclude that the upward gradient between the deep, confined aquifer and the shallow, unconfined aquifer continues to exist at the Salt Lake Refinery. https://awatenusgs.gov/infodata/groundwater.html Mr. John Amato Chevron SLR 2017 Groundwater Model Chevron Environmental Management Company Response to Comments by Utah DWMRC April 26, 2018 The Classic interface was used during this modeling effort. This interface affects only the screen presentation, not the operation of the model, which was developed and first published in 1984 under the authorship of M.G. McDonald and A.W. Harbaugh of the U.S. Geological Survey, as noted in the 2017 model report. SimLab is a public-domain simulation package used for uncertainty and sensitivity analysis. This software was developed by the European Commission's Science and Knowledge Service, Joint Research Center, and is available at https://ec.europa.eu/jrc/en/samo/simlab. As stated in Section 4.1.1 of the 2017 report, Version 2.2 of Simlab was used for the Monte Carlo analyses. The organization that controls the development of the software and the web address from which this software was downloaded were cited in the text. Since neither the web site nor the Simlab reference manual list authors for the software, this form of citation is considered standard. However, at the request of the Division, a Simlab citation will be added to the list of references in future model update reports. 4) Section 3.1.1, Model Setup, page 6. The text states that it was assumed that principal directions of hydraulic conductivity are collinear with the x and y coordinates of the model grid. While this was the case for the 1992 and 1996 model setups, how was that verified in terms of the current model? As noted in Sections 2.3.1 and 3.2 of the 1992 groundwater model report, the principal direction of hydraulic conductivity for the shallow aquifer beneath the Salt Lake Refinery, based on the results of a single pumping test, is offset 9° from a true east-west line. Given this small variation, prior groundwater modeling efforts were based on a north/south-east/west coordinate system. Given the fact that there have been no changes to the hydraulic conductivity of the shallow aquifer since 1992, together with the minor directional variation from standard coordinates and in order to maintain consistency with past modeling efforts, the 2017 model was also performed based on a north/south-east/west coordinate system. 5) Section 3.1.1, Model Setup, page 6. The text states that hydraulic transmissivities (and therefore also conductivities) are based on pumping and slug test data, presented in Appendix A, but were varied for model input based on professional judgment. Please explain what the professional judgment consisted of A perusal of Appendix A data gives the impression that perhaps early slug drawdown responses were matched, rather than employing the suggested "B-C" fit, as recommended by Bouwer, 1989, The Bouwer and Rice Slug Test - An Update, Groundwater, Vol. 27, Issue 3. Please elaborate. Appendix A of the 2017 model report presents the results of slug tests performed on seven monitoring wells at the Salt Lake Refmery in June 2017. These wells were all installed after the early 1990s when hydraulic testing was conducted in the then-existing facility monitoring wells in support of the 1992 groundwater flow model 3 Mr. John Amato Chevron SLR 2017 Groundwater Model Chevron Environmental Management Company Response to Comments by Utah DWMRC April 26, 2018 The 1992 groundwater flow model utilized the parameter-optimization program MODINV (developed by Doherty [1990]) to improve model calibration. As stated in the 1992 model report, "using MODINV, specific values . . . can be optimized such that model-generated water levels are as well matched as possible to those observed in the field. . . . The objective of MODINV is to minimize the sum of the squared residuals (i.e., differences between simulated and observed water levels). . . . Initially, an automated calibration using MODINV was performed. This allowed the computer to perform the time-consuming trial-and-error iterations to approximate the initial water levels. After a satisfactory initial calibration was obtained by using MODINV, the model was fine-tuned by using manual trial-and-error methods." The software package PMWIN (Processing Modflow for Windows), developed by Chiang and Kinzelbach (1996), was used during calibration of the 1996 groundwater flow and contaminant transport models. This package was used to design the model structure and to create, adjust, and manipulate input and output files, thereby simplifying model setup and interpretation. Given the optimization efforts that went into the original setup of the groundwater flow and contaminant transport models, together with the fact that subsequent updates were conducted primarily to account for changes in site conditions, additional optimization via add-on programs was not considered necessary. Since the base model had been optimized previously using automated methods, manual methods were considered an adequate optimization approach for the 2017 model update. Other calibration-oriented figures beyond those presented in the 2017 model report were not prepared since the model objective functions were met and this effort was intended primarily to update the model to current facility conditions. The use of additional calibration-oriented figure will be evaluated for use during future model updates. 7) Section 3.2.1, Model Setup, page 8. The text mentions that constant concentration cells were used to model sources. This seems to be a valid approach if the intent was to be conservative, but it could be more realistic to model these cells as continuous sources with decaying concentration (provided calibration is successful). The benefit might be that predicted, probabilistic contaminant concentrations would be lower in the model runs for the years 2037 and 2047, as displayed in Appendices C and D (which is what one would expect). The only sources allowed by Visual Modflow are constant concentration, recharge concentration, and point source. Contaminated groundwater at the Salt Lake Refinery exists in a relatively small area and has existed in that small area for several years. Given the length of time that contaminants have existed in this limited area, it is reasonably likely that these contaminants exist as residuals that are sorbed to the soil. Thus, of the available model source settings, constant concentration sources were considered most applicable. However, Visual Modflow does allow the use of first-order irreversible decay downgradient from a constant concentration 5 Mr. John Amato Chevron SLR 2017 Groundwater Model Chevron Environmental Management Company Response to Comments by Utah DWMRC April 26, 2018 10) Section 4.2, Analysis Results, p. 15. The Division recommends adding a short summary discussing lessons learned and recommendations for future groundwater sampling and for future groundwater and transport modeling updates. A brief summary of lessons learned can be added to future reports to discuss recommendations for future groundwater sampling and modeling. The results of the 2017 modeling effort, together with the most recent (future) groundwater sampling results, will be used during discussions prior to the next post-closure permit update to assess the adequacy of the monitoring program (in terms of the number and locations of the wells being sampled and the parameters for which those samples are being analyzed). 11) Appendix B, Comparisons of Converged vs. Non-converged Realizations. While it appears that converged and non-converged distributions are sufficiently similar for the parameters shown in Appendix B, is the presented chart gallery of parameters exhaustive or selective? Please elaborate. The chart gallery of parameters is exhaustive. 12) Appendix C and D, Predictive Probabilities for Benzene and Toluene in Select Monitoring Wells. It appears that all of the probability vs. concentration charts have gaps with probabilities of zero at irregular interval s. Is this a printing artifact or a function of the limited number of runs which converged? Please explain. As in all sampling efforts (whether physical or statistical samples), the goal of sampling is to obtain an understanding of the population with a reasonable degree of confidence. The only way to effectively fill the concentration gaps is to increase the number of Monte Carlo samplings. As noted in Section 4.1.3 of the 2017 report, this evaluation was conducted with 207 converged simulations, compared with a minimum desirable sample size of 130 simulations. Therefore, nearly 60% more converged simulations were evaluated than recommended as a minimum. Performing more simulations would decrease the number of gaps but would not add materially to an understanding of the population. References Cited Anderson, M.P. and W.W. Woessner. 1992. Applied Groundwater Modeling. Academic Press, Inc. San Diego, California. Bouwer, H. 1989. The Bouwer and Rice Slug Test - An Update. Ground Water. Vol. 27, No. 3, pp. 304-309. 7 USGS 404826112062201 (B- 1- 2) 9aca- 1 -9.8 • mmimmmwmaammumm....m.m.414mmumlint.www_ammmintalmo I- 4228.0 4227.8 I- 4226.0 4225.8 „., 4224.8 1- 4223.0 4222.8 o 721 Gr o u n dw a te r le v e l a bo v e NG V D 1 9 2 9 , fe e t ", 1- 4221.0 1964 1970 1976 1982 1988 1994 2800 2886 2812 2018 -17.8 -16.0 -15.0 Period of approved data Period of provisional data USGS 404 6 1523301 D- 1 ) 7abd- 6 ... Period of approved data mmm Period of provisional data 4275 4270 4265 4260 4255 4250 Gr o u n dw a te r le v e l a bo v e N G V D 19 2 9 , fe et c -15 3 O -10 t. 4.) 3 O ea .c 4.) a. 10 1940 1952 1964 1976 1988 2808 2812 A) Well located approximately 8.5 miles WSW of the Salt Lake Refinery B) Well located approximately 5.5 miles SE of the Salt Lake Refinery Graphs downloaded from httos://utwater.usgs.gov/infodata/eroundwater.html FIGURE 1. HISTORIC GROUNDWATER-LEVEL DATA COLLECTED FROM THE REGIONAL CONFINED AQUIFER =AOC -4AZ41 IA, lel • V18mdrA EarthFax