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' Mr.Marty Hartzell <br /> February 16,2001 <br /> Page 3 of 8 <br /> freshwater habitat, wildlife, fish migration, and fish spawning (CRWQCB Water Quality Control <br />' Plan, 1994). <br /> The existing and potential uses of groundwater in the area include irrigation, private and <br /> municipal water supply, stock watering, process water, and service supply (CRWQCB Water <br /> Quality Control Plan, 1994). The "older alluvium" is the most extensively developed geologic <br /> unit in the area and hosts both unconfined and confined zones. The unconsolidated, mostly <br /> ' coarse grained nature of the aquifer material results in high well yields. Specific capacities of <br /> wells completed in the older alluvium average 42 GPM/ft (USGS Professional Paper 1401-D, <br /> 1989). <br /> Regional groundwater flow in the site area is generally in a northwesterly direction, toward the <br /> San Joaquin River Delta and a regional groundwater depression centered about 4 miles east of <br /> Stockton (San Joaquin County Flood Control and Water Conservation District, Fall 1998). City <br /> of Escalon personnel also indicated that groundwater flows northwest. <br /> ' Published data from the San Joaquin Flood Control and Water Conservation District (Fall 1998) <br /> indicate that the current depth to groundwater in the vicinity the site is approximately 65 feet <br /> below grade. <br /> ' According to City of Escalon personnel, the nearest active water supply well is located <br /> approximately 1,200 feet south (generally upgradient) of the subject site. A water supply well <br /> has reportedly been recently installed approximately 3,000 feet northwest (downgradient) of the <br /> subject site. <br /> ' 3.0 INVESTIGATIVE PROCEDURES <br /> On November 20 and 21, 2000 four soil borings were advanced at the site to investigate the lateral <br /> and vertical extent of hydrocarbon contamination. Soil boring locations are shown on Figure 2. <br /> ' Spectrum advanced the borings under the supervision of field geologist Sean Garvey and project <br /> manager John Lane, a California Registered Geologist. Boring SB 1 was advanced to a depth of <br /> approximately 60 feet below ground surface(bgs) within the former 1,000-gallon gasoline tank pit. <br /> ' Perimeter borings SB2, SB3 and S134 were advanced to depths of approximately 50, 55 and 60 feet <br /> bgs, respectively (Figure 2). Spectrum utilized a CME-85 drilling rig equipped with hollow stem <br /> augers to advance the borings and collect soil samples. Soil samples were collected using an 18- <br /> inch long core sampler lined with new 2-inch diameter brass sleeves, affording soil identification <br /> and subjective evaluation for contamination. A flame ionization detector (FID) was used to <br /> ' monitor for the presence of volatile organic compounds in the soil. Subsequent to collection, the <br /> samples were sealed, labeled, and immediately placed in an iced cooler and transported to Argon <br /> Labs under chain-of-custody protocol. Soil samples were selected for analysis based on <br /> observations and field screening results. <br /> ' datalgrounzelgonzaleslsunuptdoc <br />