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1 <br /> from the welts and equipment decontamination water was placed in Department of Transportation (DOT) <br /> ' approved I7H drums. The contents of the drums were transported by a licensed hauler for disposal at a <br /> licensed waste treatment site. The volume of groundwater removed from the wells and other measured <br /> sampling parameters are noted on the water sampling togs included in Appendix B. <br /> ' 3.0 LABORATORY ANALYSIS <br /> The groundwater samples were transported to STL Chromalab Analytical Labs, Inc., a state-certified <br /> laboratory, located in Pleasanton, California. The groundwater samples were analyzed for the presence <br /> of TPH-G, BTEX, the five fuel oxygenates, and 1,2 DCA and EDB in accordance with USEPA Method <br /> 8260B. Copies of the laboratory analytical report and chain of custody record are in Appendix C. <br /> 4.0 SUMMARY OF RESULTS <br /> A summary of the analytical results from current and past well sampling is presented in Table 1. Based <br /> on the groundwater-level data for August 30, 2002, ATC has interpreted the groundwater gradient and <br /> flow direction for the upper aquifer as shown on Figure 3. In the upper aquifer monitoring wells MW-5, <br /> MW-6, MW-7 and MW-10, the groundwater elevation decreased from the previous quarter an average of <br /> ' 0.875 feet, ranging from 0.81 feet in monitoring well MW-5 and MW-6 to 0.95 feet in monitoring well <br /> MW-10. The apparent groundwater flow direction in the upper aquifer was generally southeasterly at a <br /> gradient of approximately 0.003 (Figure 3). <br /> Based on the groundwater-level data for August 30, 2002 (Table 1), ATC has interpreted the <br /> groundwater gradient and flow direction for the lower aquifer as shown on Figure 4. In the lower aquifer <br /> monitoring wells MW-IR, MW-2, MW-3, MW-4 and MW-8, the groundwater level decreased from the <br /> ' previous quarter an average of 0.83 feet, ranging from 0.79 feet in monitoring wells MW-2 and MW-3 to <br /> 0.98 in MW-9. The apparent groundwater flow direction in the lower aquifer was generally southeasterly <br /> at a gradient of approximately 0.003 (Figure 4). <br /> ' Laboratory analysis of the water samples collected on August 30, 2002 indicates TPH-G, BTEX, and <br /> MTBE were not detected in groundwater samples collected from MW-31—MW-8 and MW-9 in the local <br /> ' lower aquifer, or MW-10 in the local upper aquifer.TPH-G and BTEX were not detected in any of the <br /> groundwater samples during this sampling event. MTBE was detected in groundwater samples collected <br /> from MW-IR (42 micrograms per liter (µg11)), MW-2 (4,000 µg11), and MW4 (7.9 µg11) in the lower <br /> ' aquifer; and MW-5 (2,200 µg11), MW-6 (0.61 µg/1) and MW-7 (1.1 µg11) in the upper aquifer. Fuel <br /> oxygenates other than MTBE (TBA, DIPS, ETBE, TAME), and 1,2-DCA and EDS were not detected in <br /> the groundwater samples collected from the ten wells sampled this quarter. The next quarterly <br /> ' groundwater sampling is scheduled for the fourth quarter of 2002. i <br /> 1 <br /> MATC <br /> Quarterly GW Monitoring Report-3rd Qtr 2002 <br /> Quik Stop 132 <br /> Quik Stop Markets, <br /> Inc. <br /> j,kPROJECMQVIK STOP MKTS%GS 13Z A pon.t2002N3rdO1r2002Rpt ATC Project No.75.62503.3203 <br /> November 11,2002 <br /> Page 2 of 3 <br />