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Table 1 - Results of Certified Laboratory Analyses of <br /> Soil Samples Acquired from Boring S-3 <br /> March, 1991 <br /> Ethyl- <br /> Sample TPH-D TPH-G Benzene Toluene benzene Xylenes <br /> Number (Rpm) (Ppm) (]RPM) (ppm) ( m) ( m) <br /> ' S3-15 ' 75 1400 N.D. 6 . 5 14 120 <br /> S3-20 ' 54 1200 N.D. 16 14 95 <br /> ' --------r <br /> Method <br /> Detect 10 1 . 003 . 003 . 003 . 003 <br /> Limit <br /> ------------------------------------------------------------- <br /> TPH-D. . .Total Petroleum Hydrocarbons as Diesel <br /> TPH-G. . .Total Petroleum Hydrocarbons as Gasoline <br /> ' <br /> ppm. . . Parts per million <br /> N.D. —Not detected at or above laboratory detection limits <br /> To further define the vertical and horizontal extent of <br /> hydrocarbon contamination, three additional soil borings were <br /> dvanced and sampled during December, 1991 . The data acquired <br /> during December revealed detectable concentrations of fuel <br /> ydrocarbons in soil samples acquired from borings EB-5 and <br /> EB-6 (Figure 2 ) . Concentrations of TPH-G between 40 and 150 <br /> ' ppm were present in EB--5 at 21 and 22 . 3 feet. TPH-D was present <br /> in these samples (at 29 and 200 ppm, respectively) . Low levels <br /> of benzene, toluene, ethylbenzene, and xylenes (BTEX) were also <br /> present in EB-5 at 22 . 3, 31 , 36, 41 , and 46 feet. <br /> Concentrations of TPH-G and TPH-D in boring EB-6 did not exceed <br /> ' 1 . 1 ppm and BTEX was detected in the samples from 36 and 41 feet. Total lead was present in all samples, ranging from 1 . 4 <br /> to 4 . 4 ppm (well below the 16 ppm average for the Earth' s crust) . <br /> Grab water samples collected from borings EB-4 and EB-5 contained <br /> 170-200 parts per billion (ppb) TPH-G and 82-98 ppb TPH-D. <br /> The Halogenated Volatile Organic (HVO) compounds 1 , 2 Dichloro- <br /> ethane ( 1 , 2 DCA) and Perchloroethene ( PCE) were present at 33-100 <br /> ppb and N.D. -11 ppb, respectively. <br /> ' GEOLOGICAL AND HYDROGEOLOGICAL SETTING <br /> The site is located on an alluvial plain and is underlain by <br /> ' Quarternary alluvium of the Great Valley or Central Valley <br /> that consists of generally horizontal, interbedded clay, silt, <br /> 2 . <br />