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I <br /> 27 September 2004 <br /> • AGE-NC Project No 01-0827 <br /> Page 3 of 5 <br />' 2 2 2 Ground Water Sample Collection and Analysis <br /> After allowing wells to achieve a minimum 80% recovery of the pre-purge water volume, a water <br /> sample was collected using the disposable bailer The sample was transferred into three 40-m1 EPA- <br /> approved volatile organic analysis (VOA)vials and a 1-liter amber container without preservative <br /> The samples were stored in a chilled container and transported under chain of custody to Cal Tech <br />' Environmental Laboratories (CTEL) a Department of Health Services (DHS)-certified analytical <br /> laboratory The samples were analyzed for <br />' • Total petroleum hydrocarbons quantified as gasoline and diesel (TPH-g/d) in accordance <br /> with EPA Method 8015 Modified, <br />' • Benzene, toluene, ethylbenzene and total xylenes (BTEX), and the fuel oxygenated <br /> compounds tertiary butanol (TBA), di-isopropyl ether (DIPE), ethyl tertiary-butyl ether <br /> (ETBE), tertiary-amyl methyl ether (TAME), methyl-tertiary-butyl ether (MTBE), <br />' 1,2-Dichloroethane (1,2-DCA) and ethylene dtbromide (EDB) by EPA Method 8260 <br />' 30. FINDINGS <br />' Ground water flow directions and gradients were inferred from the field data collected on <br /> 10 August 2004 Contaminant impacts to ground water were assessed from the laboratory analysis <br /> of the ground water samples collected The DO concentrations and ORP were determined from field <br />' data collected on 10 August 2004 (Appendix A) <br />' 3 1 GROUND WATER GRADIENT AND FLOW DIRECTION <br /> On 10 August, depths to ground water in monitoring wells MW-1 through MW-6 and vapor wells <br />' VW-1, VW-2d, VW-3 and VW-5d ranged from 23 25 to 24 91 feet below the tops of the casings <br /> (btoc) (Table 1) The ground water elevations and gradient were calculated and determined from <br /> depths to ground water data from monitoring wells MW-I through MW-5 The August ground water <br />' elevations at the site ranged from 13 35 feet (MW-5) to 14 38 feet (MW-2) below mean sea level <br /> (MSL) The ground water flow direction at the UST release was inferred to be towards the southeast, <br /> at a gradient of approximately 0 01 foot per foot (ft/ft) on-site (Figure 3) <br /> I <br /> I <br /> Advanced GeoEnvironmental,Inc <br /> I <br />