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U <br /> Ms.Lori Duncan,REHS Page 3 of 8 <br /> San Joaquin Environmental Health Department <br /> June 9,2005 <br /> Groundwater Monitoring <br /> The site has been on a quarterly groundwater monitoring schedule since February 1995. Groundwater <br /> concentrations during the first quarter 2005 included gasoline range organics (GRO) up to 29,000 <br /> micrograms per liter(µg/L)(MW-4), benzene up to 12,000 gg/L(MW4), and methyl tert-butyl ether up <br /> to 23 µg/L(MW-1). Groundwater is currently approximately 20 feet below the ground surface (bgs)and <br /> flowing in an easterly direction. <br /> Soil Remediation <br /> Approximately 300 cubic yards of hydrocarbon-impacted soil were removed from the site during the <br /> UST-and dispenser-removal activities. <br /> SVE was conducted from January 1997 through February 1998 to remediate vadose zone soil impacts. <br /> SVE was terminated after an estimated mass of approximately 10,000 pounds (approximately 1,600 <br /> gallons) of total petroleum hydrocarbons as gasoline (TPHg) was removed and influent benzene <br /> concentrations were less than laboratory reporting limits of 0.5 milligram per cubic meter(mg/m3). <br /> t--�ite Geology and Hydrogeology <br /> Based on observations during drilling, the subsurface beneath the site is dominated by silt. The upper 40 <br /> feet of soil beneath the site consists of clayey silt and silty clay. Below 40 feet bgs, sand and silty sand <br /> dominate to approximately 55 feet bgs. From 55-feet bgs to approximately 85 feet bgs, the primary <br /> material is sand. Below 85 feet bgs to the maximum depth explored (120 feet bgs), the lithology is silt <br /> with variable sand and clay fractions. A generalized geologic cross-section is provided as Figure 3. <br /> Investigations at the site have concluded that soil impacts are confined to the soils above 41.5 feet bgs in <br /> the shallow silt zone. The deepest soil impact was located in boring B16/MW-5 at 41 feet bgs in a stiff <br /> silt with TPHg and benzene concentrations reported at 1,700 milligrams per kilogram (mg/kg) and 6.9 <br /> mg/kg, respectively. Typically, the elevated TPHg concentrations are reported in soils located in the <br /> area of 25 feet bgs as seen with samples collected from boring SB-24 (440 mg/kg) and VW-9 (130 <br /> mg/kg) at 25 feet and 26.5 feet,respectively. <br /> Depth-to-water measurements at the site have ranged from approximately 20 to 47 bgs. Monitoring data <br /> from March 30, 2005, indicate that the dominant inferred groundwater flow direction is northeast to <br /> southeast, with average hydraulic gradients from 0.003 to 0.006 feet per foot. Historical data show <br /> groundwater direction and hydraulic gradient to be variable. The direction of flow and gradient will <br /> change between sampling events. <br /> K\WpmcmV5 BP ARCO\02168\2005 System Installation\SVE-AS Workplan Am <br />