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I19 October 2004 <br /> . AGE-NC Project No. 97-0343 <br /> Page 2 of 4 <br /> labeled, placed in a chilled container, and transported under chain-of-custody to Cal Tech <br /> Environmental Laboratories(CTEL),aDepartment of Health Services-certified analytical laboratory. <br /> The ground water samples were analyzed for: <br /> • Total petroleum hydrocarbons quantified as gasoline (TPH-g) and as diesel (TPH-d) in <br /> accordance with EPA Method 8015 Modified; <br /> r • Benzene, toluene, ethylbenzene, and total xylenes (BTEX) and the fuel additives methyl- <br /> tertiary butyl ether (MTBE), di-isopropyl ether (DIPE), ethyl tertiary-butyl ether (ETBE), <br /> tertiary-amyl methyl ether (TAME), tertiary butyl alcohol (TBA), 1,2-dichloroethane <br /> (1,2-DCA), and 1,2-dibromoethane (EDB) in accordance with EPA Method 8260B. <br /> 2.3. WASTE DISPOSAL <br /> On 22 April 2004, Slaby Sales of Borrego Springs, California collected 8 soil drums from the site. <br /> The soil was transported under non-hazardous waste manifests to Filter Recycling Services in Rialto, <br /> California, an EPA-approved disposal facility. A copy of the non-hazardous waste manifest can be <br /> found in Appendix C. <br /> 3.0. FINDINGS <br /> Ground water elevation, flow direction, and gradient were determined from field data collected on <br /> 30 June 2004.The contaminant impact to ground water was quantified from the laboratory analytical <br /> data. <br /> 3.1. GROUND WATER GRADIENT AND FLOW DIRECTION <br /> At the time of the June 2004 sampling event,depths to ground water in wells MW-4 through MW-8 <br /> ranged from 58.45 feet to 60.06 feet below the tops of the well casings; ground water elevations <br /> I ranged from 30.18 feet below mean sea level(MSL)in well MW-4 to 31.87 feet below MSL in well <br /> MW-5 (Table 2). The average ground water elevation at the site this quarter was 31.34 feet below <br /> MSL. The average groundwater elevation at the site decreased 5.34 feet between the March 2004 <br /> and June 2004 sampling events. <br /> Based on depth to ground water measurements, ground water at the site appeared to be flowing in <br /> a northeast plunging trough. The southeast and northwest limbs of the trough were flowing under <br /> • an average hydraulic gradient of approximately 0.03 8 foot/foot north-northwest and 0.006 foot/foot <br /> Advanced GeoEnvironmental,Inc. <br />