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r The following is a brief historical summary of Petitioner's site at 1665 Pacific Avenue in <br /> the City of Stockton. The site is located in a commercial/residential area of the city 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 I988, <br /> the site has remained vacant. <br /> The site is underlain by flood plain sediments (clay, silt and sand) of the Pliestocene <br /> Victor Formation. In the vicinity of the site, groundwater in the more permeable strata of the <br /> Victor Formation is generally of inferior quality (concentrations of nitrate greater than <br /> 45,000 ppb, chloride greater than 300,000 ppb, and TDS greater than 1,000,000 ppb) and is not <br /> viewed by local water purveyors as a source of drinking water. Underlying the Victor Formation <br /> are the alluvial sediments (clay, silt, sand, and gravel) of the Plio-Pliestocene Laguna Formation. <br /> Groundwater in the Laguna Formation is used extensively throughout the area for municipal, <br /> industrial, and agricultural supply. There are no active municipal water supply wells within <br /> 2,500 feet of the site. There is an emergency backup well 800 feet to the northeast of the site <br /> which is screened between 200-400 feet and which has a 96-foot seal. This well, owned by the <br /> California Water Service (CWS), was taken out of service in 1991 because of a sanding problem. <br /> The CWS has indicated that it has no intention of using this well for municipal supply purposes . <br /> and intends to use it only in the event of a local disaster or fire. An additional CWS well is <br /> located 2,200 feet north of the site and has a 72-foot seal. This well is listed as a backup well. <br /> The nearest surface water, a canal that extends easterly from the Port of Stockton, is about <br /> 2,000 feet to the west. Shallow groundwater at the site flows in a general easterly direction with <br /> a gradient of about 0.002. <br /> In January 1988, analyses of soil samples from five soil borings drilled to depths of 20 to <br /> 30 feet indicated that a release had occurred at the site. In February 1988, three groundwater <br /> monitor wells were installed to assess site groundwater conditions. The initial groundwater <br /> samples from the three wells revealed an absence of gasoline constituents in groundwater near <br /> the location of the two gasoline USTs, high concentrations (99,000 ppb TPH-g and 5,700 ppb <br /> benzene) in the vicinity of the easterly pump island, and low concentrations (170 ppb TPH-g and <br /> 1 ppb benzene) in the vicinity of the waste oil UST. Data gained from the well installations also <br /> indicated that the 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, and <br /> the dispensers and associated piping were removed from the site. Visual inspection of the <br /> 4 <br />