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,• 11 March 2002 <br /> AGE-NC Project No. 95-0130 <br /> ' Page 5 of 13 <br /> Jackson-Hallenbeck-Stockton (JHS) association. The JHS soils are located within basins, and <br /> generally consist of moderate to poorly drained fine textured soils. The soils are generally derived <br /> from both marine and non-marine sediment, and are generally formed in alluvium derived from <br /> mixed rock sources. <br /> The Modesto,Riverbank,Turlock Lake Formations and overlying recent alluvium are the principal <br /> ' source of domestic ground water in the 13,500 square-mile San Joaquin Valley Ground Water Basin <br /> (Basin 5-22). This basin is drained primarily by the San Joaquin River. The nearest surface water <br /> feature in the vicinity of the property is the Stockton Deep Water Channel, located approximately <br /> ' 3,000 feet west of the property. <br /> ' 2.5.' GROUND WATER DEPTH AND FLOW DIRECTION <br /> ' The estimated depth to ground water at the site is approximately 40 feet below surface grade(bsg) <br /> based on information from Lines of Equal Depth of Water Wells Spring 1999, published by the San <br /> Joaquin CountyFlood Control District and Water Conservation District(SJCFCD).Based onreview <br /> '• of a regional ground water elevation map published by the SJCFCD, the prevailing ground water <br /> flow direction in central Stockton is generally toward the northeast, although flow directions may <br /> be both locally and seasonably variable. <br /> ' Based on data collected during the December 2001 ground water monitoring event,first observed <br /> ground water was approximately 42 feet bsg; the ground water flow direction was inferred to be <br /> towards the northeast at a calculated gradient of 0.002. Ground water flow direction at the site was <br /> inferred towards the northeast from sixteen consecutive quarterly ground water monitoring events <br /> between September 1997 and December 2001. <br /> 3.0. SCOPE OF WORK <br /> AGE proposes to drill and install nine wells screened through Vadose Zone(located between <br /> surface grade and 40 feet bsg)and Hydrologic Unit 1 (located between 40 and 57 feet bsg):one <br /> 6-inch diameter ground water extraction well(EW-1)will be screened between 35 feet and 55 <br /> feet bsg; one 4-inch diameter SVE well (VW-4)will be screened between 10 and 40 feet bsg; <br /> one 2-inch diameter IAS well(AW-1)will be screened between 50 and 55 feet bsg;two 2-inch <br /> diameter ground water monitoring wells (MW-8 and MW-9)will be screened between 35 and <br /> 55 feet bsg (Figure 2). AGE proposes to advance four additional multi-level ground water <br /> ' monitoring wells to depths of 145 feet bsg to characterize and delineate the off-site vertical extent <br /> of petroleum hydrocarbon-impacted ground water. Mw 10- Kw 13 <br /> '• Following installation of the above referenced wells, a series of pilot tests will be performed <br /> Advanced G"Environmental,Inc. <br />