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' 08 March 2006 . AGE-NC-95-0185 Page 3 of 4 elevation at the site increased approximately 1.86 feet since the previous monitoring event in August 2005. Theg round water flow direction was inferred to be toward the southeast at a gradient of approximately 0.009 foot/foot (ft/ft) near the former UST locations (Figure 3). 3.2. LABORATORY RESULTS OF GROUND WATER SAMPLES ' TPH-g and TPH-d were detected in the samples collected from wells MW-1 and MW-4 during the November 2005 sampling at concentrations as high as 220,000 micrograms per liter (µg11) and 1,300,000 µg/l, respectively,'both from well MW-4. i No other constituents of concern were not detected in the samples taken from wells MW-1 through MW-4. Current and previous analytical results are summarized in Tables 2 and 3. The laboratory reports ' (CTEL Project No. CT214-0511096),quality control/quality assurance(QA/QC)reports and chain of custody forms are included in Appendix C. GeoTracker confirmation pages of the submitted laboratory electronic deliverable format(EDF)files and depth to water measurements are provided ' • in Appendix D. ' 4.0. CONCLUSIONS Based on the data collected during the November 2005 monitoring period, AGE concludes: • not been resent in well MW-4 since October 2005. Free product Visual free product has p monitoring and remediation was initiated in August 2005. Well MW-5 continues to be ' inaccessible this quarter and has not been monitored since June 2004. • The depth to ground water was near 25 feet below casing grade. Ground water elevation ranged between 33.85 feet and 34.67 feet above MSL and was inferred to flow toward the southeast at a gradient of approximately 0.009 ft/ft. • Petroleum hydrocarbons have not been detected in wells MW-2 and MW-3 since the third quarter 2002. High concentrations of dissolved TPH-d were detected in the fourth quarter sampling event. ' Advanced GeoEnvironmental,Inc.