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' 30 April 2005 <br /> AGE-NC Project No 03-1070 <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) of Paramount, a California Department of Health Services- <br /> certified analytical laboratory, for analysis The samples were analyzed for <br /> • Total petroleum hydrocarbons quantified as gasoline (TPH-g) in accordance with EPA <br /> Method 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(DIPS),ethyl <br /> tertiary-butyl ether (ETBE), tertiary-amyl methyl ether (TAME), tertiary butanol (TBA), <br /> ethylene dibromide (EDB) and 1,2-dichloroethane (1,2-DCA) in accordance with EPA <br /> Method 8260B <br /> 3.0. FINDINGS <br /> • Ground water elevation, flow direction, and gradient were determined from field data collected on <br /> 14 February 2005 The contaminant impact to ground water was quantified from the laboratory <br /> analytical data <br /> 3 1 GROUND WATER GRADIENT AND FLOW DIRECTION <br /> At the time of the February 2005 sampling event,depths to ground water ranged from 30 09(MW-2) <br /> feet to 31 59(MW-1)feet below the tops of the well casings (Table 1) The ground water elevations <br /> Icalculated from the depth to water measurements averaged approximately 19 63 feet below mean <br /> sea level (MSL) The net ground water flow was inferred to be towards the west to southwest at a <br /> calculated hydraulic gradient of 0 034 foot per foot(ft/ft) Figure 3 illustrates the contoured ground <br /> water elevations as measured on 14 February 2005 <br /> During this monitoring event, the ground water level in wells MW-2 and MW-4 were at least <br /> 0 39 feet below the top of the well screens, indicating that the wells are properly screened and <br /> representative of shallow ground water conditions Wells MW-1 and MW-3 were at least 3 48 feet <br /> above the tops of the well screen, however, the ground water samples, although collected from <br /> "flooded" wells, are representative of shallow ground water conditions because the aquifer is <br /> confined by overlying fine-grained materials and the wells are screened in the first encountered <br /> ground water unit ` <br /> IAdvanced GeoEnvironmental,Inc <br /> I <br />