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a <br /> �} <br /> 04 August 2006 <br /> AGE-NC Project No 96-0263 <br /> Page 2 of 4 <br /> water sample was transferred Into three 40-m1 volatile organic analysis (VOA) vials containing <br /> 0 5 milliliters (ml) 18% hydrochloric acid as a sample preservative After collection, the samples <br /> were properly labeled, placed In a chilled container and transported under chain of custody to Cal <br /> Tech Environmental Laboratories (CTEL), a State of California Department of Health Services <br /> (DHS)-certified analytical laboratory The samples were analyzed for <br /> • Total petroleum hydrocarbons quantified as gasoline (TPH-g) In accordance with EPA <br /> Method 5030/8015 Modified, and <br /> • Benzene,toluene,ethylbenzene and total xylenes(BTEX), fuel additives di-isopropyl ether <br /> (DIPS),ethyl tertiary-butyl ether(ETBE),methyl-tertiary-butyl ether(MTBE),tertiary-amyl <br /> methyl ether (TAME), tertiary butanol (TBA), 1,2-dlchloroethane (1,2-DCA) and 1,2- <br /> dlbromoethane(EDB) In accordance with EPA Method 8260B <br /> 3.0. FINDINGS <br /> Ground water elevation, flow direction, and gradient were determined from field data collected on <br /> ' 14 March 2006, the contaminant Impact to ground water was quantified from the laboratory <br /> analytical data <br /> 3 1 GROUND WATER GRADIENT AND FLOW DIRECTION <br /> The elevation of ground water In each well was calculated by subtracting the depth to ground water <br /> from the surveyed well casing elevations(Table 1) For the March 2006 sampling event, depths to <br /> ground water ranged from 7 11 feet to 8 27 feet below the tops of the well casings Ground water <br /> elevations at the site ranged from 28 59 feet above mean sea level(MSL)In well MW-9 to 29 46 feet <br /> above MSL In well MW-1 I <br /> The ground water flow direction was determined by contouring the ground water elevation data The <br /> ground water at the site was Inferred to be flowing north-northwest at an gradients ranging from <br /> 0 003 foot/foot(ft/ft) on the southern portion of the property to 0 008 ft/ft on the northern portion <br /> The groundwater contours are depicted on Figure 3 Elevation data from deep-screened well MW-6 <br /> (screened between 27 and 32 feet bsg) was not used to determine ground water flow direction <br /> 32 ANALYTICAL RESULTS OF GROUND WATER SAMPLES <br /> TPH-g was detected In water samples MW-1, MW-2, MW-7, and MW-8 at concentrations of <br /> Advanced GeoFnvironmental,Inc <br />