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r , <br /> 10 September 1996 <br /> AGE-NC Project No. 95-0106 <br /> Page 7 of 8 <br /> monitoring well MW-1 at concentrations of 1,500 ppm, 8.3 ppm, 8.4 ppm, 28 ppm, 15 ppm and 55 <br /> ppm, respectively. Analytical results of soil boring samples are summarized on Table 2. The <br /> laboratory report(MAI Laboratory ID 66514 through 66517) and chain-of-custody are in Appendix <br /> F. <br /> 4.5. GROUND WATER ELEVATION AND GRADIENT <br /> The ground water elevation in each well was calculated by subtracting the depth to ground water <br /> from the surveyed casing elevation (Table 3). Monitoring well casing elevations were surveyed <br /> relative to monitoring well MW-1. Ground water gradient on 09 July 1996 was calculated to be <br /> 0.0045 ft/ft(23.76 feet per mile) directed N 16° E. The relative ground water elevation at the site is <br /> illustrated in Figure 3 - Relative Ground Water Elevation. <br /> 4.6. LABORATORY RESULTS OF GROUND WATER SAMPLES <br /> The highest concentrations of hydrocarbons were detected in wells MW-1 and MW-4, located down- <br /> gradient (north) of the former UST excavation; TPH-g was detected at concentrations as high as <br /> 18,000 ppb (TPH-g, MW-4). Benzene was detected at concentrations of 190 ppb and 590 ppb in <br /> MW-1 and MW-4, respectively. The maximum toluene concentration detected was 960 ppb, <br /> encountered in MW-1. The maximum ethylbenzene and total xylenes concentrations of 700 ppb and <br /> 2,100 ppb, respectively, were encountered in MW-4. Neither TPH-g nor BTE&X were detected in <br /> the ground water samples from MW-2 and MW-3. <br /> MTBE was detected in samples collected from wells MW-1, MW-2 and MW-4,at concentrations <br /> of 41 ppb, 16 ppb and 100 ppb, respectively. Analytical results of ground water samples are <br /> summarized on Table 4. The laboratory report (MAI Laboratory ID 66629 through 66632) and <br /> chain-of-custody are in Appendix G. <br /> 5.0. CONCLUSIONS AND RECOMMENDATIONS <br /> 5.1. CONCLUSIONS <br /> The following conclusions were drawn from the results of this investigation: <br /> • Hydrocarbon-impacted soil has been encountered at depths of 6 to 10 feet bsg, coinciding <br /> with the capillary fringe or saturated zone. <br />