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t28 December 2005 <br /> • AGE-NC Project No 98-0511 <br />' Page 2 of 4 <br /> approximately 7 gallons of water had been evacuated Ground water temperature, pH, and <br /> conductivity were measured at regular intervals during the purge process using an Oakton water <br /> analyzer Field data sheets are included in Appendix C Purged water was stored on-site in properly <br />' labeled, Department of Transportation (DOT)-approved 55-gallon drums <br />' 23 COLLECTION AND ANALYSIS OF GROUND WATER SAMPLES <br /> Following purging, the depth to ground water was re-measured to ensure that a minimum of 80% <br />' well-volume recharge had been achieved prior to sampling Water samples were collected from each <br /> purged well using dedicated,disposable plastic bailers Each water sample was transferred into three <br /> laboratory-supplied,40-milliliter(ml)volatile organic analysis(VOA)vials containing 0 5 ml 18% <br />' hydrochloric acid solution as a sample preservative After collection, the samples were properly <br /> labeled, placed in a chilled container, and transported under chain of custody to Cal Tech <br /> Environmental Laboratories (CTEL), a California Department of Health Services (DHS)-certified <br />' laboratory, and analyzed for <br /> - Total petroleum hydrocarbons quantified as gasoline (TPH-g) in accordance with EPA <br /> . Method 8015M, <br /> Benzene, toluene, ethylbenzene, and total xylenes (BTEX) and fuel additives di-isopropyl <br /> I ether(DIPE),ethyl tertiary-butyl ether(ETRE),methyl tertiary-butyl ether(MTBE),tertiary- <br /> amyl methyl ether (TAME), tertiary-butyl alcohol (TBA), 1,2-dibromoethane (EDB), 1,2- <br /> dichloroethane(1,2-DCA), ethanol, and methanol in accordance with EPA Method 8260B <br /> f <br /> I3.0. FINDINGS <br /> Ground water elevation and flow direction were determined from field data Hydrocarbon impact <br /> to ground water was inferred from laboratory analysis of ground water samples <br /> 3 1 GROUND WATER GRADIENT AND FLOW DIRECTION <br /> For the June 2005 ground water monitoring event, the elevation of ground water in each well was <br /> calculated by subtracting the depth to ground water from the surveyed casing elevation (Table 1) <br /> Depths to ground water ranged from 14 40 feet to 15 03 feet below the tops of the well casings <br /> Ground water elevations at the site ranged from 2 71 feet below mean sea level(MSL)in well MW-5 <br /> to 3 74 feet above MSL in well MW-1 Ground water at the site was inferred to flow generally <br /> • toward the northwest on-site at gradients ranging between 0 004 foot/foot(ft/ft) and 0 015 ft/ft and <br /> Advanced GeoEnvironmental,Inc <br />