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17 June 1996 <br /> AGE-NC Project,No 95-0121 <br /> Page 4 of 6 <br />' 4 0. FINDINGS <br /> 41 RELATIVE GROUND WATER ELEVATION AND GRADIENT <br /> 1 <br /> The depths to ground water in wells MW-1 through MW-9 ranged between 20 40 and 22 03 feet <br />' below the top of each well casing, and on the average rose approximately 129 feet between February <br /> 1996 and May 1996 <br /> Currently, ground water is between 2 to 11 feet above the top of the screen intervals in the nine <br />' ground water monitoring wells <br /> t <br />' Ground water flow direction at the site is generally toward the northeast at a, gradient of <br /> approximately 0 0016, or 9 feet per mile (Figure 3 -Surface Ground Water Elevation Contour Map) <br /> 42 LABORATORY RESULTS OF GROUND WATER SAMPLES <br /> TPH-g was detected in water samples from MW-1 through MW-4, MW-6, and MW-7 at <br /> concentrations as high as 29,000 ppb(parts per billion reported as micrograms per liter), TPH-d was <br /> detected in samples from MW-1 through MW-4,and MW-6 through MW-9 at concentrations as high <br />' as 34,000 ppb <br /> Benzene was detected in samples from MW-1 through MW-7 at concentrations up to 7,800 ppb <br /> Toluene was detected in samples from MW-1 through MW-3, MW-6, and MW-7 at concentrations <br /> up to 1,300 ppb Ethyl benzene was detected in water samples from MW-i through MW-5, and MW- <br /> 7 at concentrations as high as 1,400 ppb Xylenes were detected in water samples from MW-1 <br /> through MW-7 at concentrations up to 1,600 ppb <br /> The analytical results for soil samples are summarized in Table 2 The laboratory report (CAL, <br /> Laboratory Batch Nos 764-1) and chain-of-custody forms are included in Appendix B <br /> f <br /> 5.0. CONCLUSIONS & RECOMMENDATIONS [ <br /> 51 CONCLUSIONS <br /> I Ground water flow direction has remained relatively constant at the site over the past two years <br /> Monitoring wells MW-6 and MW-9 continue to be up-gradient of the former UST area, while <br /> monitoring wells MW-8 and MW-5 continue to be down-gradient <br /> r <br /> I <br />