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Bulk Transportation Page 3 <br /> Site Conceptual Model& Closure Report <br /> GPE Project No. 606.3 <br /> August 28, 2009 <br /> The formation of soils in San Joaquin County is dependent on the sedimentary <br /> '- transport path from the primary sediment sources. These sediment sources <br /> are the Coastal Range to the west and the Sierra Nevada to the east of the <br /> County. Generally, the longer the transport path the greater the working of <br /> the sediments prior to deposition as soils. Along the San Joaquin River and in <br /> the delta regions west of Stockton, the low energy river and flood plain <br /> environments deposit layers of silt and clays during seasonal floods. These <br /> ` fine-grained sediments flocculate out of slack water as floodwaters recede. The <br /> erosion of the Coast Range forms portions of far western San Joaquin County <br /> soils and transport of these sediments is facilitated through seasonal run-off of <br /> the minor streams of the Coast Range. These soils are formed in environments <br /> similar to those of eastern San Joaquin county, i.e., alluvial fans, but tend to <br /> be less well worked in comparison to their Sierran derived counterparts due to <br /> the shorter transport path. <br /> +� The USDA Soils Conservation Service Soil Survey of Sari Joaquin County, <br /> California, October 1992 soil survey report classifies soil in San Joaquin <br /> County. The Survey generally classifies the soils in this area of Stockton as <br /> part of the Jacktone-Hollenbeck-Stockton association; a nearly level soil in <br /> basins or basin rims. Somewhat poorly drained to moderately well drained <br /> fine textured soils, moderately deep to deep to a cemented hardpan. The <br /> specific on site soil is classified as Urban Land Complex, meaning it is so <br /> severely disturbed by human activity as to be unidentifiable as to type. It is, <br /> however mostly Jacktone clay, a heavy, dense, clay soil with rapid drainage <br /> and poor permeability. <br /> Observations taken in 2003 by Hygienetics Environmental during the over <br /> excavation of the tank pit indicated that from about 4 to 16 feet below grade, <br /> the soil consists principally of yellow-brown silt. At the 16-foot level, a fine- <br /> grained silty sand was observed. <br /> 2.2 Site History <br /> A former 12,000-gallon diesel UST was operated on the site until it was <br /> removed in 2002. Confirmation soil samples collected from the tank pit <br /> indicated that a leak had impacted the surrounding soil. It appears the <br /> ` source(s) of the diesel release were related to dispenser piping rather than a <br /> defective tank. The San Joaquin County EHD issued a Notice of <br /> Unauthorized Release on November 8, 2002. <br /> In 2003, the pit was over-excavated by Hygienetics Environmental, and the <br /> diesel-impacted soil was removed and stockpiled on the site. The report of the <br /> excavation estimated that 110 cubic yards of soil was removed. Seven <br /> �. 2937 Veneman Ave.,#B240 Geo-Phase Environmental Inc. Phone (209) 569-0293 <br /> Modesto, CA 95356 Fax (209) 569-0293 <br />