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After drilling and soil sampling was completed, 2-inch diameter PVC monitoring wells were <br /> constructed within the boreholes through the hollow stem of the augers. The wells were constructed <br /> of 2-inch diameter Schedule 40 PVC casing with flush-threaded connections and PVC well screens <br /> with 0.020-inch slots. Well screens extended 11 to 12 feet below the water table surface and 3 to <br /> 4 feet above the water table surface. A graded sand pack (#2112)was placed adjacent to the entire <br /> length of the well screen and extended two feet above the top of the screen. A two feet bentonite <br /> pellet seal was placed above the sand pack and hydrated with potable water. Levels of the sand <br /> pack and bentonite pellets were confirmed during placement by sounding with a weighted tape. The <br />' annular space above the bentonite pellet seal was filled to the ground surface with neat cement <br /> containing approximately 5 percent bentonite. The wells were completed at grade in traffic-rated <br /> utility vaults with a locking water-tight cap. Well construction details are presented in Table 1 and <br /> shown graphically on the boring logs included in Appendix B. <br /> 2.2 WELL SURVEY AND WATER LEVEL MEASUREMENTS <br /> The two newly-installed wells (MW-2 and MW-3) and the existing well (MW-1A)were surveyed by <br /> a California licensed surveyor for ground-level and top of PVC casing elevations. The reference <br /> datum for all elevations is the City of Lodi Bench Mark #849 (elevation 47.49 feet MSL). Static <br /> water levels were measured to the nearest 0.01 foot in each well on January 15, 1993 using an <br /> electronic water level indicator. Well survey results, depth to groundwater and groundwater <br /> elevations are shown on Table 1. <br /> 2.3 WELL DEVELOPMENT AND GROUNDWATER SAMPLING <br /> The newly-installed wells (MW-2 and MW-3) were developed and sampled on January 15, 1993. <br /> Well development was accomplished by bailing with a clean PVC bailer to remove fine sand and <br /> suspended sediment from the well. Approximately 15 well casing volumes (25 gallons)of water were <br /> removed from MW-2 and MW-3 during development. During development, the discharge water was <br /> measured for pH, temperature, and specific conductance. Stabilization of these physical parameters <br /> was used to indicate that fresh formation water was entering the wellbore. <br /> Following completion of development, groundwater samples from wells MW-2 and MW-3 were <br /> collected using a clean stainless steel bailer. Existing well MW-lA was purged and sampled on <br /> January 15, 1993. Prior to sampling, approximately 3 well casing volumes of water was evacuated <br /> from the well using a clean PVC bailer. During evacuation, pH, temperature, and specific <br /> conductance measurements were recorded as described above. Following purging, a groundwater <br /> sample was collected using a clean stainless steel bailer. Field sampling data sheets for each <br /> monitoring well are included as Appendix C. <br /> Water samples were transferred directly from the bailer into laboratory supplied glassware and <br /> labeled to designate sample location, sample number, and date and time collected. Sample <br /> containers were stored in a cooler containing ice. Water samples were delivered to Superior and <br /> analyzed for TPHg and BTEX in accordance with EPA methods modified 8015 and 602,respectively. <br /> ( <br /> MARDEERPT <br /> 50014-003-01 MD04 6 <br />