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1 <br />' 20 January 2005 <br /> AGE-NC Project No 97-0343 <br />' Page 8 of 21 <br />' The soil profile beneath the site is composed dominantly of sands and silts from surface grade to <br /> approximately 96 feet bsg,and finer-grained silts and clays from 96 feet bsg to total depth of 134 feet <br /> bsg Figures 4 and 5 Illustrate subsurface geologic profiles at the site Boring logs are Included in <br />' Appendix A <br /> Since initiation of ground water monitoring in February 2000,depth to ground water measurements <br />' have fluctuated between a 33 feet btoc and 62 feet btoc (Table 1) The Inferred ground water flow <br /> direction generally has been towards the northwest(nine times)at gradients ranging between 0 001 <br /> ft/ft and 0 008 ft/ft, ground water flow was towards the south four times at gradients between 0 01 <br />' ft/ft and 0 05 ft/ft, and twice towards the east or northeast at gradients between 0 001 ft/ft and <br /> 0 04 ft/ft <br />' Releases of petroleum hydrocarbons occurred from the on-site USTs Once released to the <br /> subsurface,the contaminants migrated through the fine grained unit directly below the UST area to <br /> a vertical depth of approximately 15 feet bsg, at which point the contaminants encountered a more <br />' porous sand unit and began to migrate laterally as well as vertically The lateral migration was <br /> further Increased when ground water was encountered(which has been recorded at 33 feet to 62 feet <br /> bsg during the investigation), the direction of lateral migration was dominantly towards the <br /> northwest, in the preferred ground water flow direction <br /> I Significant petroleum-hydrocarbon impact to soil in the vadose zone is present in borings B1, B3, <br /> B5, MW 1, and MW2, in the area of the former USTs (Table 6) TPH-g, TPH-d and MTBE are <br /> present at maximum concentrations of 14,000 mg/kg (B5-25), 12,000 mg/kg (B340 and -15) and <br />' 1,100 mg/kg(B 1-30),respectively Most of the contamination appears to reside above the top of the <br /> fine grain layer, at approximately 50 to 55 feet bsg, currently the extent of the soil contamination is <br /> completely within the vadose zone <br />' The vertical extent of ground water is defined near the UST area by MW-8, ground water <br /> contamination does not extend below 90 feet bsg The lateral extent ofpetro Icum-imp acted ground <br /> water was defined by wells MW-4 through MW-7,but these wells are now intermittently dry With <br /> the exception of two detections of 1,2-DCA in well MW-4,petroleum hydrocarbons have not been <br /> detected in wells peripheral to wells MW-1 through MW-3, located in the UST area, since third <br /> quarter 2001 <br /> 8.0 POTENTIAL IMPACT ON NEARBY SURFACE AND GROUND WATER <br /> Typically, ground water would represent the migration medium for contaminants over significant <br /> horizontal distances However, sites located in up-gradient or cross-gradient directions from the <br /> • subject property are not likely to be negatively impacted by the subject property In addition, first <br /> IAdvanced GeoEnvi ron mental,Inc <br />