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27 February 2007 <br /> AGE-NC Project No. 07-1514 <br /> Page 2 of 6 <br /> alluvium. lake, playa and terrace deposits of Quaternary age (California Division of Mines and <br /> Geology, 1977). Rocks cornposing the basement complex of the Province have not been completely <br /> defined but are believed to be metamorphic and igneous in origin. <br /> The Modesto, Riverbank and Turlock Lake Formations and overlying Recent alluvium are the <br /> principal sources of domestic ground water in the 13,500-square mile San Joaquin Valley Ground <br /> Water Basin (Basin 5-22). <br /> The closest surface water feature to the site is the confluence of the Little John Creek and Lone5�ree <br /> Creek, located approximately one mile to the north of the site and the San Joaquin River, located <br /> approximately live miles to the west of the site. Based upon previous environmental assessments <br /> conducted at the site,ground water depth occurs at approximately 38 to 42 feet below surface grade <br /> (bsg); ground flow direction at the site has not been determined. <br /> 2.2. UST UPGRADES AND SITE ASSESSMENT ACTIVITIES <br /> According to the Wright Environmental Services, Inc. (Wright) prepared - Preliminary Soil anct <br /> Groundwater Site Assessment dated 21 December 2004,during dispenser upgrades in January 2004. <br /> 5.54 tons of hydrocarbon-impacted soil was removed from around the UST fill buckets and <br /> dispensers and disposed at Forward Landfill in Manteca, California. In their letter- dated 14 April <br /> 2004,EHD directed the assessment of impact to ground water and to delineate the vertical and lateral <br /> extent of hydrocarbon-impacted soil. <br /> In October 2004, Wright advanced four soil borings at the site and collected soil and ground water <br /> samples. Low concentrations of total petroleum hydrocarbons quantified as diesel (TPM-d) were <br /> reported in the soil sample collected from boring B-2 at 36 ft bsg at 1.1 milligrams per kilogram. No <br /> other constituents of concern was reported in the soil samples collected. TPH-d was reported in the <br /> ground water samples collected from borings B-1, B-2 and B-4 at a maximum concentration o1-79 <br /> micrograms per liter(pg/1)(B-2). TPfI-gasoline(TPI I-g)was reported in the ground water samples <br /> collected from borings B-2 and B-3 at a maximum concentration of 270 µg/1. Additionally, ethanol <br /> was reported in the samples collected from borings B-2 and B-3 at a maximum concentration of 43 <br /> ftg/l (B-2). Kiff Analytical LLC (Kiff) reported that the TPI1-d and TPI I-g did not demonstrate the <br /> typical TPI I-d and TPI -g gas chromatographic patterns for both the soil and ground water analytical <br /> results for the samples collected frorn borings B-1 through B-4. Wright recommended Kiff further <br /> evaluate the analytical results of the soil and ground water samples collected from borings B-1 <br /> through B-4; EHD concurred in their letter dated 16 March 2005 and further requested Kif-freview <br /> the results by EPA method 9260. On 17,luly 2006, Kiff issued a supplementary laboratory report and <br /> reported: <br /> Advanced GeoEnvironmcntal,Inc. <br />