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07 September 2005 <br /> AGE-NC Project No 98-0540 <br /> Page 7 of 9 <br /> toluene, and 34 µg/1 xylenes <br /> The fuel additive 1,2-DCA was detected in the ground water samples from wells MW-1 and MW-3 <br /> through MW-5 at concentrations of 190 µg/1, 310 µg/l, 9 7 µg/1, and 9 5 µg/1, respectively <br /> No other target analytes were detected at or above laboratory reporting limits in the samples <br /> analyzed Analytical results of ground water samples are summarized in Table 4 Maps depicting the <br /> estimated lateral extents of dissolved TPH-g and 1,2-DCA are illustrated on Figures 6 and 7, <br /> respectively Copies of the laboratory report(CTEL Project No CT214-0506135), QA/QC reports, <br /> and chain of custody forms are included in Appendix H <br /> I3 5 GROUND WATER GRADIENT AND FLOW DIRECTION <br /> During the June 2005 ground water monitoring event, depths to ground water ranged between <br /> 78 58 feet (MW-2) and 8145 feet (MW-5) below the tops of the well casings By subtracting the <br /> depths to ground water from the surveyed relative casing elevations in monitoring wells MW-1 <br /> through MW-3, the average ground water elevation was calculated to be approximately 2197 feet <br /> below mean sea level (MSL), indicating an increase in ground water elevation of approximately <br /> 2 77 feet since the last ground water monitoring event in December 2004 (Table 1) Since a well- <br /> head elevation survey has not been completed for wells MW-4 and MW-5,these wells were not used <br /> to determine the average elevation <br /> At the time of the June 2005 ground water monitoring event, ground water was inferred to be <br /> flowing toward the southwest under a hydraulic gradient of approximately 0 007 foot/foot (ft/ft) <br /> During this monitoring event, ground water elevations were within the screened intervals of the <br /> I wells, indicating that the wells are properly screened to yield samples representative of shallow <br /> ground water conditions Figure 8 illustrates the contoured ground water elevation as measured on <br /> 14 June 2005 <br /> I ' <br /> 36 GEOTRACKER CONFIRMATIONS <br /> Documents confirming the upload of laboratory electronic deliverable format(EDF)files and depth <br /> to water measurements to GeoTracker are included in Appendix I <br /> I <br /> 4.0. SUMMARY AND CONCLUSIONS <br /> I Based upon the findings investigation, <br /> s of this AGE concludes <br /> • P g <br /> Advanced GeoEonronmental,Inc. <br />