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' 19 January 2004 <br /> S AGE-NC Project No 95-0173 <br />' Page 3 of 10 <br />' 2 3 LABORATORY ANALYSIS OF GROUND WATER SAMPLES <br /> After labeling, each ground water sample was logged on a chain of custody form,placed in a chilled <br />' container,and transported to Castle Analytical Laboratory(CAL),a California Department ofHealth <br /> Services (DHS)-certified laboratory, to be analyzed for <br /> • Total petroleum hydrocarbons quantified as gasoline(TPH-g)by EPA Method 5030/8015M, <br /> • Benzene, toluene, ethylbenzene, and total xylenes (BTEX) and methyl tertiary-butyl ether <br /> (MTBE) by EPA Method 8020, and <br /> • MTBE, tertiary-amyl methyl ether (TAME), tertiary butanol (TBA), di-isopropyl ether <br /> (DIPE), ethyl tertiary-butyl ether (ETBE), 1,2-dichloro ethane (1,2-DCA), and ethylene <br />' dibromide (EDB) by EPA Method 5030/8260 <br /> 24 QUARTERLY GROUND WATER MONITORING AND SAMPLING FINDINGS <br />' . AGE determined ground water flow direction and gradient from the field data collected on 06 <br /> October 2004, the contaminant Impact to ground water was assessed from the laboratory data <br /> collected on 07 October 2004 <br /> 2 4 1 Ground Water Elevation and Gradient <br />' <br /> During the October 2004 ground water monitoring event, the depths to ground water ranged from <br />' 32 25 feet(MW-1) and 35 50 feet (MW-13C) below the tops of the well casings (Table 2), ground <br /> water elevations were calculated to be between 22 89 feet (MW-1) and 25 59 feet (MW-5) below <br /> mean sea level Figure 3 Illustrates the ground water elevations plotted and contoured on a scaled <br />' site map Generally,groundwater flow direction was inferred to be east-northeast at an apploxlmate <br /> hydraulic gradient of 0 006 fl/ft or less (Figure 3), typically, ground water elevation at the site <br /> decreased an average 2 73 feet between the July and October 2004 ground water monitoring events <br />' Based on the historical ground water data collected at the site, it Is likely that the ground water <br />. elevatlolls measured from Vveils lv/ VV -i ar'ld tYl TV-U YY4117 Q �Lrle 111LL<.cur"a e, eitllVl UU%A LV 1aLL1LY L,.L.ILL1V111G11L <br /> and/or technician error Therefore,ground water elevation measurements collected from wells MW-1 <br />' and MW-8 were not utilized In contouring the October 2004 ground water elevations (Figure 3) <br /> GeoTracker confirmation pages of the submitted ground water monitoring electronic deliverable <br /> format (EDF) files are Included In Appendix B <br /> Advanced GeoEnvironmental,Inc <br /> I <br />