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I22 July 2002 <br /> • AGE-NC Project No 99-0592 <br /> IPage 2 of 4 <br /> opened and water was allowed to run until the pump turned on The samples were transferred into <br /> laboratory-supplied 40-m1 EPA-approved VOA vials containing 0 5 ml 18% hydrochloric acid as <br /> a sample preservative and into one 1-liter amber bottle without a sample preservative The sample <br /> containers were then labeled with well designation,date,time of sampling and the sampler's initials <br />' The samples were transported in a chilled container under chain-of-custody to McCampbell <br /> Analytical, Inc (MAI), a California Department of Health Services(DHS)-certified laboratory, for <br /> analysis The samples were analyzed for <br /> • Total petroleum hydrocarbons quantified as gasoline (TPH-g) and diesel (TPH-d) in <br /> accordance with EPA Method 8015 modified, <br /> IBenzene, toluene, ethylbenzene and total xylenes(BTEX) and the oxygenated ether methyl <br /> tertiary butyl ether(MTBE) in accordance with EPA Method 8021B, and <br /> IThe fuel oxygenates MTBE, di-isoproply ether (DIPE), ethyl tertiary butyl ether(ETBE), <br /> tertiarty amyl methyl ether (TAME), tertiary butanol (TBA), methanol, ethanol, and 1,2- <br /> dibromoethane (EDB) and 1,2-dichloroethane (1,2-DCA) in accordance with EPA Method <br /> 8260B <br /> 3.0. FINDINGS <br /> Ground water elevation, flow direction, and gradient were determined from field data collected on <br /> 10 June 2002 Laboratory analysis of ground water samples was used to quantify the impact to <br /> ground water <br /> 3 1 GROUND WATER GRADIENT AND FLOW DIRECTION <br /> 1 <br /> Depth to ground water was measured between 59 60 feet and 60 21 feet bsg on 10 June 2002 <br /> Ground water elevations at the site ranged from 32 42 feet below mean sea level (MSL) in well <br /> MW-I to 33 20 feet below msl in well MW-4 Monitoring data from the site was combined with <br /> monitoring well data collected from the adjacent former Cherokee Truck Stop site (3535 East <br /> Cherokee Road) also collected on 10 June 2002, to determine the approximate ground water flow <br /> direction Ground water elevation data are presented on Table 1 Ground water flow direction was <br /> inferred to be toward the northeast at a very low gradient of approximately 0 0001 ft/ft (Figure 3) ' <br /> I <br /> 3 2 ANALYTICAL RESULTS OF GROUND WATER SAMPLES <br /> IThe ground water sample collected from MW-I contained TPH-g and TPH-d at concentrations of <br /> 330 micrograms per liter (µg/1) and 210 µg/1, respectively In addition, BTEX compounds were <br /> IAdvanced GcoEnVLronmental,Inc <br /> I <br />