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1 <br /> •` A September 2002 <br />' GE-NC Project No. 95-0100 <br /> Page 2 of 9 <br />' 2.3• REGIONAL HYDROGEOLOGIC SETTING <br /> The site is located within the 13,500 square-mile San Joaquin Valley Ground Water Basin[California <br />' Department of Water Resources(CDWR)Basin No. 5-22]. The principal subsurface units that supply <br /> ground water are the Modesto, Riverbank and Turlock Lake Formations and overlying modern <br /> alluvium. This basin is drained primarily by the San Joaquin River. <br /> AGE has installed and monitored six ground water monitoring wells on the subject property. Based <br /> on these wells, the average depth to ground water is approximately 54-feet bsg. The ground water <br /> flow direction beneath the site is to the northwest, however, the flow direction can vary locally due <br /> to pumping of production wells in the area or through seasonal recharge. <br /> A total of three domestic ground water wells were located on the site. One well (DW-1, now <br />' abandoned)was located approximately 150 feet west ofthe UST investigation area.A secondary well <br /> (DW-2) is located approximately 250 feet north of the former UST investigation area. The primary <br /> production water well (DW-3) is located approximately 350 feet northwest of the former UST <br /> investigation area. Based on the Well Completion Report for the domestic well drilled on the site in <br />' 1992, the well was constructed with a sanitary sea] to a depth of 100 feet, and is screened over the <br /> depth interval of 160 to 200 feet bsg. Ground water was measured at a depth of 54 feet below surface <br /> grade (bsg). <br />' Jefferson School is located on the southeast corner ofLinne Road and Chrisman Road a r xi <br /> 600 feet.southeast of the site. The ground water well utilized by the Jefferson School Districteis <br />' located approximately 700 feet southeast of the former UST area. <br /> 3.0. PREVIOUS INVESTIGATIONS <br /> 3.1. UNDERGROUND STORAGE TANK REMOVAL <br /> Two 1,500-gallon USTs,piping and dispensers were removed from the property in September 1993. <br /> Analysis of soil samples collected from beneath the dispenser at a depth of six feet below surface <br /> grade(bsg) indicated that total petroleum hydrocarbons quantified as gasoline(TPH-g) and volatile <br />' aromatics(benzene,toluene,ethylbenzene andlenes:BTE <br /> xy X)were present at concentrations as high <br /> as 48,000 parts per million(ppm,reported as nvlligrams per kilogram). Total petroleumhydrocarbons <br /> quantified as diesel were not detected in the soil sample analyzed. Total lead was detected in the <br /> sample collected from the dispenser area at 270 ppm. Ethylene-dibromide was also detected in the <br /> same sample at 70 parts per billion(ppb,reported as micrograms per kilogram). The analytical results <br /> of the soil samples from the UST removal are summarized on Table 1. <br /> -` - --3.2:`- INJTIAL:SITE'ASSESSMENT <br /> On 12 August 1994, two borings (boring B 1 and boring B2) were drilled under the supervision of <br /> Geological Audit Services, Inc. (GAS) in the area of the former fuel dispenser island. TPH-g was <br /> detected at concentrations as high as 13,000 milligrams per kilogram(mg/kg)and hydrocarbons were <br /> Advanced GeoEnvironmiental,Inc. <br /> t - <br />