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i <br /> i07 February 2005 <br /> • AGE-NC Project No 03-1070 <br /> iPage 2 of 4 <br /> Environmental Laboratories (CTEL) of Paramount, a California Department of Health Services- <br /> icertified analytical laboratory, for analysis The samples were analyzed for <br /> • Total petroleum hydrocarbons quantified as gasoline (TPH-g) in accordance with EPA <br /> iMethod 8015 Modified, <br /> • Benzene,toluene,ethylbenzene and total xylenes(BTEX) in accordance with EPA Method <br /> 8260B, and <br /> • Fuel additives including methyl tertiary-butyl ether(MTBE),di-isopropyl ether(DIPE),ethyl <br /> tertiary-butyl ether (ETBE), tertiary-amyl methyl ether (TAME), tertiary butanol (TBA), <br /> i ethylene dibromide (EDB) and 1,2-dichloroethane (1,2-DCA) in accordance with EPA <br /> Method 8260B <br /> i <br /> 3.0. FINDINGS <br /> iGround water elevation, flow direction, and gradient were determined from field data collected on <br /> 30 August 2004 The contaminant impact to ground water was quantified from the laboratory <br /> i - analytical data <br /> i3 1 GROUND WATER GRADIENT AND FLOW DIRECTION <br /> At the time of the August 2004 sampling event, depths to ground water ranged from 30 90 (MW-2) <br /> ifeet to 3145 (MW-1) feet below the tops of the well casings Ground water elevation at the site <br /> averaged approximately 20 16 feet below mean sea level (MSL)(Table 1), resulting in an average <br /> decrease of 156 feet since the last monitoring event Ground water flow was inferred to be flowing <br /> itowards the southeast with an average hydraulic gradient of 0 003 footifoot Figure 3 illustrates the <br /> contoured ground water elevations as measured on 30 August 2004 <br /> iDuring this monitoring event, the ground water level in wells MW-2 and MW-4 were at least <br /> 1 24 feet below the top of the well screens, indicating that the wells are properly screened and <br /> i representative of shallow ground water conditions Wells MW-1 and MW-3 were at least 3 71 to <br /> 3 55 feet above the tops of the well screen, however, the ground water samples, although collected <br /> from"flooded"wells, are representative of shallow ground water conditions because the aquifer is <br /> i confined by overlying fine-grained materials and the wells are screened in the first encountered <br /> ground water unit <br /> i <br /> iAdvanced GeoEnvironmentsl,Inc <br /> I <br />