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Technical Memorandum <br />April 7, 2017 <br />Page 4 <br />Following completion of the work, the boreholes were backfilled with neat cement via tremie <br />grouting under oversight of the San Joaquin County Environmental Health Department. The <br />surface of the boreholes were patched with concrete to match existing surface conditions. <br />DISCUSSION OF RESULTS <br />The results of the CPT activities indicate that the higher PCE concentrations in the LCP, as <br />represented by the 500 }tg/1 contour on Figure 1, does not extend south of Tokay Street. However, <br />PCE concentration at monitoring well G-25A, an upper intermediate zone well screened from 89 to <br />99 ft-bgs, was observed to be 1,100 Itg/L in November 2017. These data suggest that the leading <br />edge of the 500 gAg/L contour in the intermediate zone is located between G-25A and CPT-38. <br />Langan performed a step-drawdown test at G-25A on October 17, 2016 to estimate the production <br />capacity of the upper intermediate zone and whether an extraction well installed near G-25A would <br />produce the required pumping rate to attain capture of the LCP in that area. The results of the <br />step-drawdown test indicated that groundwater levels decreased a total of 3.6 feet and stabilized <br />within 15 minutes from the start of each step test. With a 2-inch diameter well casing, the <br />maximum pumping rate from G-25A was 8 gpm. These data suggest that an extraction well <br />screened in the upper intermediate zone near G-25A could pump at a stable rate of 8 gpm. <br />The step-drawdown data was evaluated using AQTESOLV, a curve fitting software that <br />incorporates various commonly used aquifer-testing models, to estimate the hydraulic conductivity <br />of the upper intermediate zone. Using the Jvandel and Tsang formula for estimating capture zones <br />(Jvandel and Tsang, 1986, Capture-Zone Type Curves: A Tool for Aquifer Cleanup, in <br />Groundwater, Vol. 24 Issue 5, September 1986), the maximum step-drawdown test pumping rate <br />of 8 gpm, a hydraulic gradient of 0.0035 feet per foot for the upper intermediate zone (see Figure 3, <br />Fourth Quarter and Annual 2016 Groundwater Monitoring Report — Central, Western, Southern, <br />and Northern Plumes, Lodi, California, Stantec, January 31, 2017), and the estimated average <br />hydraulic conductivity value of 10 feet per day, the width of the capture zone at G-25A was <br />estimated to be approximately 870 feet. This indicates the higher PCE concentrations in the LCP <br />in the upper intermediate zone can be captured and contained by an extraction well located near <br />G-25A and screened from 89 to 99 ft-bgs. <br />RECOMMENDED EXTRACTION WELL LOCATION <br />Based on the analysis of currently-available data, results of the step-drawdovvn test at G-25A, <br />results of the CPT investigation, and capture zone analysis, we recommend that a 6-inch diameter <br />replacement extraction well EW-7R be located approximately 20 feet north of monitoring <br />well -25A (see Figure 1). The recommended extraction rate is 8 gpm and the recommended screen <br />interval is from 75 to 100 ft-bgs. Final depth and screen interval will be based on location-specific <br />data collected during drilling. Final extraction rate for EW-7R will be determined during the <br />GWET system startup activities, which will include performing a step-drawdown test at EW-7R. <br />WEST YOST ASSOCIATES <br /> cAA21 3 \ 17-17-37 \wp \LPEDW-7RLocation \ 040517_2M