Laserfiche WebLink
I • i <br /> I04 October 2000 <br /> • AGE-NC Project No 97-0326 <br /> Page 2 of 4 <br /> placed in a chilled container and transported under chain-of-custody to Alpha Analytical <br /> Laboratories, Inc (Alpha Analytical), a State of California Department of Health Services (DHS)- <br /> certified analytical laboratory Each sample was analyzed for <br /> I • Total petroleum hydrocarbons quantified as gasoline (TPH-g) in accordance with EPA <br /> method GCFID 5030 <br /> I • Volatile aromatic hydrocarbons -benzene,toluene, ethylbenzene and total xylenes(BTEX) <br /> with methyl tertiary-butyl ether (MTBE) in accordance with EPA Method 8020 <br /> I • Oxygenated compounds - di-isopropyl ether (DIPE), ethyl tertiary-butyl ether (ETBE), <br /> MTBE, tertiary-amyl methyl ether(TAME) and tertiary butanol (TBA) in accordance with <br /> I EPA Method 8260B <br /> • Ethylene Dibromide (EDB) and 1,2 Dichloroethane (1,2 DCA) in accordance with EPA <br /> Method 8260 <br /> I <br /> lie3.0. FINDINGS <br /> From the field data,AGE was able to infer the ground water flow direction and gradient Laboratory <br /> I analysis of three ground water samples detected petroleum hydrocarbons and volatile aromatic <br /> hydrocarbons in all three samples, oxygenated fuel additives were found in two of the samples <br /> (MW 1 and MW3) <br /> 3 1 GROUND WATER GRADIENT AND FLOW DIRECTION <br /> Ground water was measured at a depth of approximately 32 feet below the tops of the well heads <br /> during the September 2000 monitoring event,within the screened interval of MW2 and MW3,but <br /> approximately 3 feet above the screened interval in MW 1 The elevation of ground water in each <br /> well was calculated by subtracting the depth to ground water from the well head elevations Ground <br /> water elevations ranged from 16 76 to 16 89 feet below mean sea level (MSL) Ground water data <br /> Iis summarized on Table 1 <br /> Ground water elevation contours based on the data for the September 2000 monitoring event are <br /> illustrated on Figure 3 The ground water flow direction was very nearly due south with a gradient <br /> of 0 0065 ft/ft <br /> Advanced GeoEnvironmental,Inc <br /> I <br />