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' 30 July 2002 <br /> AGE-NC Project No 99-0624 <br />' Page 3 of 5 <br /> depicted and contoured in Figure 3 <br /> The general ground water gradient in the area of wells MW-1 through MW-4 was calculated to be <br /> approximately 0 002 ft/ft or less, or approximately 11 feet per mile and inferred to be flowing <br /> towards the south-southwest <br />' 3 2 LABORATORY RESULTS OF GROUND WATER SAMPLES <br /> A total of three ground water samples were submitted to a DHS-certified laboratory TPH-g was <br />' detected in water samples collected from wells MW-2 and MW-3 at concentrations of 800 <br /> micrograms per liter (ug/1) and 61 ug1l, respectively The laboratory indicated that the sample <br />' chromatograms from MW-2 and MW-3 had significant unmodified or weakly modified gasoline <br /> BTEX constituents were detected in ground water samples collected from wells MW-2 and MW-3 <br /> tat concentrations ranging as high as 79 pg/1 (xylene, MW-2) <br /> . MTBE was detected (EPA 8260) in ground water samples collected from wells MW-1,MW-2 and <br />' MW-3 at concentrations ranging as high as 11,000 pg/1 (MW-2) No other constituents of concern <br /> were detected above laboratory reporting limits in the analyzed samples Previous and current <br /> analytical results of ground water monitoring well samples are summarized in Tables 3 and 4 The <br />' laboratory reports (McCampbell Analytical Inc Lab I D No 0203200-1, 2 and 3) and chain-of- <br /> custody forms are presented in Appendix B <br />' 4.0. SUMMARY AND CONCLUSIONS <br />' The implications from the findings of the March 2002 investigation are <br /> • The average depth to ground water and ground water elevation on-10 March 2002 in <br /> monitoring wells on-site was approximately 50 feet below surface grade and 11 feet below <br /> MSL, respectively <br /> • Ground water flow direction 1n the area of wells MW-1 through MW-4 was inferred to be <br /> towards the south-southeast at an approximate gradient of 0 002 ft/ft Due to the low <br /> hydraulic gradient at the site, slight variations in ground water measurements or changes of <br /> recharge/discharge of the local ground water could greatly modify the inferred ground water <br /> flow direction <br /> I • TPH-g was detected in ground water samples from wells MW-2 and MW-3, the highest <br /> • concentration was detected in the sample collected from MW-2 at 800 µg/l,a steady increase <br /> Advanced GeoEnvironmental,Inc <br />