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ASS O C I ATE S I N C. <br />The Theis type -curve solution for a confined aquifer, <br />-results are presented in Table 3. The calculated stora <br />confined condition. The storage coefficients for uncoi <br />0.3, while those for confined aquifers are typically be <br />1986). The average storage coefficient calculated <br />average hydraulic conductivity value (0.00012 meters <br />Table 3, fall within the average range for fine to cc <br />1986). A distance versus drawdown plot is shown on <br />334 Groundwater Sampling and Analysis <br />Grab groundwater samples were collected from well <br />at the completion of the pump test after the groundw <br />Groundwater samples were transferred to appropriate <br />bailers with bottom emptying devices to reduce vc <br />labeled with sample identification, placed on ice, ar <br />certified Argon Laboratories for chemical analysis. <br />hydrocarbons as gasoline (TPHg) by EPA method <br />xylenes (BTEX) by EPA method 8020; and methyl <br />butyl ether (ETBE), di -isopropyl ether (DIPE), tertia <br />(TAME), 1,2-dichloroethane (1,2 -DCA), and ethyl <br />Groundwater analytical results are summarized in <br />presented in Appendix C. <br />335 Results of Groundwater Pumping Test <br />The observed maximum drawdown in each of the <br />distance of each well from well EW -1. Based on A <br />.. sites, the radius of influence is typically the point whet <br />— - least 0.10 feet. The maximum drawdown in well M' <br />influence (ROI) for groundwater extraction at the site <br />Laboratory results of the groundwater samples Indic <br />.. the samples collected from well EW -1 before and a <br />of groundwater was extracted from well EW -1, <br />concentrations of TPHg and BTEX from the t <br />® approximately 0.135 pounds of TPHg and 0.04 F <br />groundwater extraction pilot test as shown below: <br />r <br />r <br />wA259571reportslpumptest.doc 4 <br />used to estimate aquifer parameters. The <br />coefficient indicates the aquifer exists in a <br />ied aquifers are typically between 0.01 and <br />.-en 0.00005 and 0.005 (Driscoll page 210, <br />.ng the Theis solution was 2.4E-3. The <br />r second [m/s]) calculated and presented in <br />ie sand (1 to 105 m/s) (Driscoll page 74, <br />Lure 4. <br />EW -1 prior to beginning the pump test and <br />Iter elevation had been allowed to recharge. <br />sample containers, using clean, disposable <br />latilization. Sample containers were then <br />d shipped under chain -of -custody to State - <br />Samples were analyzed for total petroleum <br />015; benzene, toluene, ethyl benzene, and <br />tertiary butyl ether (MTBE), ethyl tertiary <br />.y butyl alcohol (TBA), tertiary amyl ether <br />dibromide (EDB) by EPA method 8260. <br />Table 2, and laboratory data sheets are <br />bservation wells was plotted against the <br />"s experience at groundwater remediation <br />3�0 <br />the drawdown in the observation well is at <br />0.15 feet <br />l <br />-4 was which yields a radius of <br />f approximately 90 feet (Figure 3). <br />I that TPHg and BTEX were detected in <br />the pump test. Assuming 5,280 gallons <br />stated in Section 3.2, and averaging <br />.ning and ending pump test samples, <br />is of BTEX were removed during the <br />