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1 <br /> r19 February 1997 <br /> • AGE-NC Project No 95-0104 <br /> Page 3 of b <br /> r the to the nearest 0 01 foot to determine the elevation relative to existing wells The results of the <br /> monitoring well survey are contained in Table 1 - Relative Ground Water Elevations <br /> r2 1 6 WELL DEVELOPMENT <br /> rOn 11 December 1996, wells MW-5 and MW-6 were developed utilizing a Grundfos Rediflo TI <br /> submersible pump Ground water was purged from each well until each well was essentially sediment <br /> free Approximately 25 gallons of ground water were purged from each monitoring well Purged <br /> rground water was containerized in properly labeled D O T model 17H 55-gallon drums and stored <br /> on-site in an area inaccessible to the general public <br /> r <br /> 2 1 7 SOIL PROFILE <br /> Generally, a brown to gray sandy silt and silty sand were encountered from surface grade to depths <br /> of approximately 87 feet in each boring However, small lenses of fine-grained sand and silt were <br /> encountered throughout the soil profile <br /> Groundwater was encountered during drilling activities at a depth of approximately 72 feet General <br /> r soil conditions are summarized in boring logs contained in Appendix A Cross sections depicting soil <br /> lithology and the approximate extent of hydrocarbon-impacted soil on the site are depicted in Figure <br /> 5 - Cross Section A -A ' and Figure 6 - Cross Section B -B' <br /> r <br /> 2 1 8 FIELD EVIDENCE OF HYDROCARBON-IMPACTED SOIL <br /> r <br /> During drilling activities organic vapors (OVs) were detected at concentrations as high as 1 2 PPm <br /> in MW-5 at 75 feet( hydrocarbon odors were not detected in 1\4W-5) Hydrocarbon odors and OVs <br /> rwere detected in MW-6 at depths between 40 and 65 feet bsg <br /> r2 2 GROUND WATER MONITORING AND SAMPLING <br /> 2 2 1 GROUND WATER DEPTH MEASUREMENTS <br /> On 11 December 1996, the depth to ground water in each monitoring well was measured to the <br /> nearest 0 01 foot utilizing a Sohnst water level meter The relative ground water elevations were <br /> calculated by subtracting the depth to ground water from the relative casing elevations surveyed from <br /> a temporary benchmark assigned an arbitrary elevation (Table 1) Relative ground water elevations <br /> were plotted and contoured on a scaled site map (Figure 7 -Relative Elevation Ground Water Map) <br />