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Stantec <br /> No Further Action Request Report <br /> Chevron and ARCO Commingled Plume No. CP0034 <br /> April 10, 2012 <br /> 2. BACKGROUND <br /> 2.1. SITE DESCRIPTION <br /> The Chevron facility No. 94275 and ARCO Service Station No. 2133 are located at the <br /> intersection of West Benjamin Holt Drive and Plymouth Road in Stockton, California. The site is <br /> located in a light commercial and residential area of Stockton in a relatively flat lying area. <br /> ARCO 2133 is currently comprised of an AM/PM mini-mart that retails gasoline fuel with four <br /> underground storage tanks (USTs), dispenser islands, and associated product lines. Chevron <br /> 94275 features include two double-walled, fiberglass USTs, a station building, six product <br /> dispensers under a common canopy, and a car wash. The site is bound by retail shopping to <br /> the north, residential homes to the south, and Interstate Highway 5 to the west. The site is <br /> bound by Plymouth Road to the east, beyond which are a golf course and residential homes. <br /> According to a United States Geological Survey Map dated 1976, the elevation of the site is at <br /> approximately 3 feet (ft) above mean sea level. The nearest open body of water is the Fourteen <br /> Mile Slough, located approximately 2,000 ft south of the site. A site location map and a site <br /> plan are included as Figures 1 and 2. <br /> 2.2. REGIONAL GEOLOGY AND HYDROLOGY <br /> The City of Stockton is located in the San Joaquin Valley which is underlain by alluvial <br /> sediments up to 1,000 ft thick. The principal source of recharge to the groundwater in the <br /> valley is the Sierra Nevada Mountains to the east. Groundwater historically flowed from the <br /> base of the Sierra Nevada Mountains westward towards the San Joaquin-Sacramento River <br /> delta. However, increased municipal use of groundwater in the Stockton area has developed a <br /> groundwater depression changing the regional gradient away from the delta and towards the <br /> municipal wells. This has caused easterly migration of poor quality saline groundwater from the <br /> delta. Most water wells in the Stockton area draw groundwater sandstone beds at depths <br /> greater than 150 ft bgs (EMCON, 1986). <br /> 2.3. SITE GEOLOGY AND HYDROGEOLOGY <br /> Geologic cross-sections for the site are presented in Appendix B. Historical boring logs are <br /> provided in Appendix C. Soil boring and well construction details are presented in Table 1. The <br /> cross sections and boring logs depict the following conditions: <br /> • A predominantly clay and silt layer encountered from the ground surface to <br /> approximately ten ft below ground surface (bgs). <br /> 94275 NFAR 2012.doc 3 <br />