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6.. SECTION 2 <br /> Site Setting and Background <br /> L <br /> This section summarizes the site setting and background for the Disco site. This summary is <br /> �- not intended to provide a definitive description of what is known about this site,but is <br /> included to provide the reader with a brief synopsis of the site as it is currently understood by <br /> Del Monte,CH2M HILL,PHS/EHD,and the RWQCB. <br /> 2.1 Site Setting <br /> The Disco site is located near the intersection of Myrtle Street and Filbert Street in Stockton, <br /> California (Figure 1).The site is a former underground storage tank (UST) site that consisted of <br /> three 10,000 gallon gasoline tanks that were removed in 1985. Currently the site is vacant, <br /> unpaved,and fenced. Access to the site is limited to Del Monte employees. <br /> •- 2.2 Site Background <br /> The Disco site is currently owned by Del Monte. Parmaceast owned the site from mid-1960s to <br /> 1976,and operated the USTs that were associated with a former gasoline station. Del Monte <br /> purchased the property from Parmaceast in 1976, and never operated or used the USTs. <br /> In October 1985,Del Monte removed the USTs under the supervision of PHS/EHD. The tanks <br /> were filled with water at the time of removal. Soil beneath the tanks contained gasoline <br /> constituents. The soil was aerated on site to reduce the levels of volatile hydrocarbons below <br /> 1,000 mg/kg and was backfilled into the excavation (Exceltech, 1985). <br /> In 1991,under the direction of the PHS/EHD,Del Monte conducted soil and groundwater <br /> investigation in the vicinity of the Disco site that included a soil-gas survey,seven soil borings <br /> and eight monitoring wells. The results indicated gasoline constituents in soil at depths <br /> between 55 and 75 feet below ground surface (bgs),and in groundwater. <br /> The site is underlain by alluvial sediments.The soil types include clay,silt,sand,and gravel. <br /> The predominant soil types are interbedded sandy clay and silty sand. The depth to <br /> groundwater is currently approximately 47 feet bgs. <br /> w Since 1991,groundwater levels have risen approximately 30 feet (from 77 ft bgs to 47 It bgs), <br /> and the direction of groundwater flow has changed directions by almost 180 degrees. Between <br /> 1991 and July 1994, the groundwater flow direction was predominantly towards the northwest <br /> and an average groundwater flow direction and magnitude of 312°and 0.0006 ft/ft. From <br /> October 1995, through today, the groundwater flow direction has been consistently towards <br /> the southeast, at an average direction and magnitude of 143°and 0.001 ft/ft. <br /> r <br /> Prior to the switch in groundwater flow directions, the extent of the plume was defined <br /> horizontally by monitoring wells MW-DIS-3,MW-DIS-8S,MW-DIS-9,and MW-DIS-10;and <br /> ` vertically by monitoring well MW-DIS-7D and-8D. <br /> Since 1991,Del Monte has conducted quarterly groundwater monitoring and reported results <br /> to PHS/EHD. In February 1995,Del Monte initiated remediation at the Disco site by installing <br /> SFO/CADERNET/GROUPS/EBGIDELMONTE/PLANi_33A40RKPLAN-CPT.DOC 3 <br />