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Lk4l KLEINFELDER' <br /> File No. 20-3937-01 <br /> September 3, 1996 <br /> L <br /> ti EXECUTIVE SUMMARY <br /> L This is a revised report of Kleinfelder's limited soil and groundwater assessment conducted on <br /> p <br /> the proposed Schaeffer Industries facility at 1265 North Shaw Road in Stockton, California <br /> L (APN # 143-270-041). Mr. Clark Taylor of the Schaeffer Industries retained Kleinfelder to <br /> conduct the assessment in accordance with our proposal dated June 21, 1996, and our <br /> subsequent additional authorization dated July 29, 1996. <br /> On July 22 to July 24, 1996, four soil borings were advanced on site and a monitoring well was <br /> subsequently constructed in each boring. During our field work, Kleinfelder collected a total of <br /> thirty-six (36) soil samples from three (3) soil borings. Nineteen of the 36 samples were <br /> subsequently analyzed based on field indications and the approved scope of work. Groundwater <br /> samples were collected from the three monitoring wells (MW-1, MW-2, MW-3) and <br /> submitted for analyses. The nineteen soil samples and three groundwater samples were <br /> analyzed for the following analytes: <br /> • Volatile Organic Compounds (VOCs) including Benzene, Toluene, Ethylbenzene, <br /> Xylenes (13TEX) by EPA Method 8260: <br /> 0 Total Purgeable Petroleum Hydrocarbons as Referenced to Gasoline in the approximately <br /> C6 to C,Zcarbon range (TPH-G) by EPA Method 8015M/5030 <br /> • Total Extractable Petroleum Hydrocarbons (Fuel Fingerprint) in the approximately C8 to <br /> Cz; carbon range by EPA Method 8015M/3550 <br /> • Sulfate by EPA Method 375.4 <br /> A groundwater gradient and direction was calculated based on depth-to-water data collected <br /> on July 30, 1996, by Kleinfelder representatives and by data collected during a survey by our <br /> firm on August 20, 1996. The groundwater flow direction is estimated to be towards the <br /> southwest at a relatively flat gradient of 0.003 ft/ft. In areas of flat groundwater gradients <br /> such as this site, groundwater flow directions may significantly fluctuate due to rainfall, <br /> groundwater recharge, groundwater pumping, etc.... Therefore, changes in groundwater flow <br /> directions may vary at this site with time. <br /> Four (4) additional surface soil samples were obtained from the northern portion of the site for <br /> asbestos analysis. <br /> Based on the data obtained during our assessment, the following conclusions and <br /> recommendations have been formulated: <br /> 20-3937-01/MR960189 Page 1 of 18 01996. Kleinfelder, Inc. <br />