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Site Background <br /> canepa's Car Wash,Park Sweet <br /> page 4 of 8 <br /> eater m elevation) as the <br /> well collar measuring Points on April 4, 2403, approximately 0 25 feet less (greater <br /> gradient was <br /> previous quarter The groundwater elevation contours sgradintshe � <br /> generally toward the northeast, consistent with historical groundwateranal ical <br /> MW-4, MW-6, and MW-7 indicated <br /> groundwater monitoring activiries were con�ci d��J3lY 10, 2QQ3 The laboratory in those <br /> Quarterly gr collected from M <br /> results for the groundwater samplesreported detection limits <br /> or 1e collected from MW- <br /> that BTEX constituents we were ddetected <br /> ected at a modebate conbcentrat on m the -6 was detected in MW-2, <br /> samples BTEX constituents le from MW-5 TPH-G <br /> p Q$3, and 49 mg/L respectively Laboratory analytical <br /> 2, and at relatively elevated concentrations in the samp L to MW-2 and that MTBE was <br /> MW-3, and MW-5, at concentrations of 6 25 le collected from <br /> tection limit of 500 49/L in the groundwater sample <br /> results Indicated that MTBE was detected at a concentration of 400 � al results and the detection <br /> not detected at or above an elevate 2 sample was inconsistent with historic EPA Method <br /> MW-S Because the result for the MW- les were re-analyzed for MTBE by <br /> limit for the MW-5 sample was elevated, the samp wasL The <br /> 8260B The results o <br /> f the EPA Method 8260B analyses indicated�tehdaaM�Ban limit ofd5 0cµ91 int e <br /> of the groundwater samples collected on July 1Q, 2003, `were generally <br /> samples from MW-2 and <br /> MW-5 at or above the laboratory rep <br /> laboratory analytical results <br /> consistent with historical monitoring results the July 2003 monitoring event <br /> The r in the monitor wells was approximately 26 98 feet below the surveyed <br /> oundwater table remained <br /> e hove the top of all well screens wring previous quarter The <br /> The average depth to ground 2403, l 37 feet deeper than the p <br /> well dwat measuring Points on July 10, groundwater gradient was generally toward the <br /> groundwater elevation <br /> with historical groundwater gradients the <br /> northeast, consistent2003 The laboratory <br /> Quarterly groundwater collected from MW-1, MW-4, MW 6, and MW-7 indicated <br /> y oundwater monitoring activitles c were conducted an November � on limits m those <br /> Q groundwater samp reported detects <br /> analytical results for the gr or above collected from MW-3, at <br /> that BTEX constituents were not <br /> ted at a low concentrationinthesample elevated concentrations in <br /> samples BTEX constituents w <br /> le collected from MW-2, and at relatively <br /> e ati y <br /> moderate concentrations <br /> TPH-G was detected in MW- <br /> the 2 MW-3, and MW-5, at concentrations of 11, 0 14, <br /> the sample from M analytical results indicated that MTBE was detected at a <br /> respectively Laboratory <br /> and 50 mg[-, pec in MW-2 and that MTBE was not detected at or above an elevated detection <br /> concentration of 1, µ� <br /> he oundwater sample collected from MW-�oB�he MW 5 sample was elevated,ause the result for the <br /> limit of 1,OOQ µg1L int gi <br /> EPA Method 8260B The results of he EPA <br /> 5 at thabovebthe <br /> 013 <br /> sample was inconsistent with dor MTBE by is and the detection limit <br /> the samples were re-analyzed <br /> les from <br /> i n limits of 0 S and 5 0 µgfL, respectively The laboratory analytical results of <br /> analyses indicated thateMtTaBE was not detected in the samples were generally consistent with historical <br /> laboratory reported <br /> the groundwater samples collected on November 6, 2003 <br /> monitoring results <br /> s during the November 2003 monitoring28 27 feet below the <br /> The groundwater table remaineQundwe <br /> atereiri the top monitoall r wells nwas approximately revious quarter <br /> event The average depth to gr <br /> well collar measuring pointt deeper than the P <br /> s on November 6, 20 groundwater gradient was generally toward the <br /> surveyed <br /> The groundwater elevation contours indicated that the <br /> gr <br /> northeast, consistent with historical groundwater gradients <br /> water monitoring activities were conducted on January 28, 2004 The laboratory <br /> Quarterly ground MW-6, and MW-7 indicated that <br /> analytical results for the groundwater samples collected from MW-4, <br />