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I <br /> l18 February 2003 <br /> AGE-NC Project No 96-0229 <br /> Page 5 of 9 <br /> 3.0. FINDINGS <br /> Soil descnptigns were utilized to construct geologic cross sections of the site Field data was utilized <br /> to select soil samples for laboratory analysis and to determine ground water flow direction and <br /> gradient Hydrocarbon Impact to soil and ground water was assessed and quantified by laboratory <br /> analysis <br /> 31 STRATIGRAPHY <br /> Generally, a dark brown,damp medium dense,clayey sand was encountered at 5 feet bsg and a pale <br /> brown, damp,very stiff,silty clay with some fine sand was encountered at 10 feet bsg at both boring <br /> locations Between 15 and 20 feet bsg, finer-grained clayey sand underlain by clay was Identified in <br /> boring MW-11,whereas brown to red-brown silty sand was Identified in boring MW-12 Below 20 <br /> feet bsg In both borings,the soil consisted of a brown to gray,damp to saturated,medium dense,fine <br /> to coarse sand with some gravel at between 25 and 35 feet bsg, and gray-brown to red-brown, <br /> saturated, dense, clayey fine sand at between 40 and 45 feet bsg Boring logs are included In <br /> r • Appendix B General lithology beneath the site in cross-sectional view is depicted in Figures 5 and 6 <br />` Saturated soil was encountered at approximately 35 feet bsg in both borings, ground water levels <br /> were measured at approximately 32 feet bsg utilizing a Solinst water level meter <br /> 32 FIELD EVIDENCE OF HYDROCARBON-IMPACTED SOIL AND GROUND WATER <br /> I <br /> I No petroleum hydrocarbon odor,petroleum hydrocarbon vapor(using a PID)or discoloration were <br /> observed in soil sample duplicates collected from soil borings MW-11 and MW-12 <br /> 3 3 GROUND WATER ELEVATION AND GRADIENT <br /> During the 25 November 2002 monitoring event, depths to ground water in wells MW-1 through <br /> MW-12 were measured at between 30 87 and 33 17 feet below the tops of the welt casings t I able 2) <br /> Ground water elevations were calculated to be between 20 30 feet(MW-5)and 22 18 feet(MW-12) <br /> below mean sea level (MSL), the ground water elevation decreased an average of 1 35 feet between <br /> the August 2002 and the November 2002 ground water monitoring events The ground water surface <br /> elevation at the site was within the screened Intervals of wells MW-2 through MW-I OA, MW-11 <br /> and M W-12 but was approximately 16 and 18 feet above the screen intervals in wells MW-1 and <br /> MW-IOB,respectively <br /> Advanced GeoE oviren mental,Inc <br />