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■ <br /> ■ except those acquired from EB11 (currently on hold pending <br /> analysis) . Analysis conducted to date revealed that all samples <br /> were free of detectable concentrations of Total Lead (detection <br /> limit 2 .5 ppm) . <br /> ' Each of the soil borings was advanced to a depth of 59 feet <br /> bgs, with the deepest soil samples acquired from 59 .0--60 . 5 feet. <br /> Groundwater was encountered at 59 feet in EB-8 and 58. 5 feet <br /> in FB-11 . The borings were se ed with bentonite from the bottom <br /> ' of the borehole to one foot belo the water level and then filled <br /> with grout cement to the ground surface. <br /> 7 <br /> ' The borings advanced on June 22-25 and 29, 1992 were converted <br /> to 2" inside-diameter groundwater monitoring wells constructed <br /> of threaded, Schedule 40 PVC risers attached to 0 . 020" slotted <br /> ' PVC well screen. The screened interval was extended five feet <br /> above the water table and the annular space around the screen <br /> was filled with ##3 Monterey Silica Sand. The annular pack was <br /> then covered by a two foot thick bentonite seal to protect <br /> groundwater from surface water infiltration. Cement was added <br /> from the top of the bentonite seal to 0 . 5 feet bgs followed <br /> by concrete aggregate to grade. Each well was then covered <br /> with a locking traffic box. Construction details for each well <br /> are presented graphically in Appendix A. <br /> Following construction of the monitoring wells, each was allowed <br /> to equilibrate for a period of at least 48 hours. Following <br /> this period, the depth to water and total well depth were <br /> measured with an electric water level meter and the volume of <br /> water contained in each well casing was computed. Each well <br /> was developed using a vented surge block to release and draw <br /> fines ( silts, clays, and fine sands ) into the well by forcing <br /> water in and out of the screen slots and adjacent annular pack. <br /> Each well was then purged using a clean bailer until the ground- <br /> water was free of sediment and other grit material, and the <br /> pH, conductivity, and temperature were stabilized. Measurements <br /> of pH, conductivity, and temperature were recorded and are <br /> presented in Appendix A. <br /> Samples from each developed well were obtained in a clean, <br /> disposable, polyethylene bailer lowered into the well to a point <br /> immediately below the water surface. Each water sample was <br /> transferred into three ( 3 ) amber glass sample bottles and two <br /> ( 2 ) Volatile Organic Analysis (VOA) vials . Each container was <br /> promptly sealed with a teflon-lined screw cap, labeled, placed <br /> on blue ice, and transported to a California--state certified <br /> hazardous waste analytical laboratory under chain of custody. <br /> Subsequent analyses were conducted for TPH-G and BTEX using <br /> EPA Methods 5030/8015-8020 (602) ; TPH-D using EPA Methods 3510/ <br /> 8015, HVOs using EPA Method 601 ; and Total and Fecal Coliforms . <br /> The report of laboratory analyses appears in Appendix B. These <br /> 6. <br /> ■ <br />