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INTRODUCTION <br /> UNOCAL Corporation petitioned the Underground Storage Tank Cleanup Fund <br /> manager seeking review of the decision of the San Joaquin County Public Environmental <br /> Health Division (County) not to close their UST release site located at 1665 Pacific <br /> Avenue, Stockton, California. This report presents a summary of the site's history, its <br /> hydrogeologic setting and associated groundwater impacts. This report also addresses the 7 <br /> potential for current site conditions to adversely affect beneficial uses of groundwater. <br /> BACKGROUND <br /> The site is located in a commercial/residential area of Stockton and was an ! <br /> operating service station from about 1947 to 1988; gasoline was dispensed from two ! <br /> 10,000 gallon capacity USTs. Since demolition of the station and removal of the USTs in <br /> 1988, the site has remained vacant. <br /> The site is underlain by flood plain sediments (clay, silt and sand) of the <br /> Pliestocene Victor Formation. In the vicinity of the site, groundwater in the more <br /> permeable strata of Victor Formation is generally of inferior quality and is not viewed by <br /> local water purveyors as a source of drinking water. Underlying the Victor Formation are <br /> the alluvial sediments (clay, silt, sand, and gravel) of the Plio-Pliestocene Laguna <br /> Formation. Groundwater in the Laguna Formation is used extensively throughout the area <br /> for municipal, industrial, and agricultural supply. There are no water supply wells within <br /> 800 feet of the site and those municipal wells located in the general area are routinely <br /> constructed with annular seals which extend to depths of 150 to 200 feet so as to exclude <br /> the shallower poor quality groundwater in the Victor Formation. The nearest surface <br /> water, a canal which extends easterly from the Port of Stockton, is about 2,000 feet to the <br /> west. Shallow groundwater at the site flows in a general easterly direction with a gradient <br /> of about 0.002. <br /> In January 1988, analyses of soil samples from five soil borings drilled to depths of <br /> 20 to 30 feet indicated that a release had occurred at the site. In February 1988, three <br /> groundwater monitor wells were installed to assess site groundwater conditions. The <br /> initial groundwater samples from the three wells revealed an absence of gasoline <br /> constituents in groundwater near the location of the two gasoline USTs, high <br /> concentrations (99,000 ppb TPH-g and 5,700 ppb benzene) in the vicinity of the easterly <br /> pump island, and low concentrations (170 ppb TPH-g and 1 ppb benzene) in the vicinity <br /> of the waste oil UST. Data gained from the well installations also indicated that the <br /> groundwater was confined and that it flowed in an easterly direction. <br /> In March 1988, the two 10,000-gallon capacity gasoline USTs, the waste oil UST, ! <br /> and the dispensers and associated piping were removed from the site. Visual inspection of <br /> the bottom and side-walls of the gasoline UST excavation revealed that soil was affected <br /> by a release prompting UNOCAL to over-excavate an estimated 850 cubic yards of soil to <br /> a final depth of 28 to 30 feet'. Soil samples collected from the bottom and side wall of the <br /> ' The volume of soil excavated is a point of contention with the County. UNOCAL indicates in its Site <br /> Closure Summary report that an estimated 1,100 cubic yards of soil were excavated while the County,in I <br /> response to the report, contends that only 350 cubic yards are documented to have been excavated. <br /> However, in a March 12, 1991 letter to UNOCAL, the County states that;"...approximately 1300-1400 <br /> 1 <br />