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1 a <br /> L 20 March 2001 <br /> AGE NC Pro}ectrNo 96-0235, <br /> page 3 of 5 T yvithln the screened M <br /> " e dee r water data set Ground water was <br /> the, Pe _7 M�7�T_8A, -10, MW-11A, MW-12A,, - <br /> 13B comprising MW tel 12 44 feet <br /> 12B and MW` 5 MW-6A, MSN ' water was appro� y' <br /> intervals for wells MWA4 MN- ' 3 and EW-2 are <br /> 1, comprising the shallow water 3 d,respectively <br /> and EW , ©undwater elevations <br /> screened ound,watex Figure 3 illustrates the gY <br /> and 1139 feet above the llow and deep Sx m was inferred to be toward the southwest. ta <br /> screenedbetweei the shallow ection based up <br /> d water elevations, <br /> based on the two datasets n d chin the lo-We"interval the north to northeast <br /> using data from wells scree from t <br /> from the shallow wells indicate a radial flow varyl <br /> 'RESU rS OF WATER SALES r" <br /> 3 2 ANAi_,YTICAL 3,MW-8A,N1W-14, MW_ <br /> "2" � Per ltter (µ�) <br /> les collected from Whi h as 63,004 rriicrogralns 3A?MW-13B <br /> TPH-g was detected;n the samP2 at concentrations as high, <br /> MW-12B,lr fW- <br /> ples <br /> 11 B, MW-128, ,W--1 and EW-- 9, MW-10, <br /> tected in MW- MW 0 /1 BTEC compounds were detected m oluene), <br /> TPH-d was de as 18,00 µg 304 µg/1 {benzene), 14,044 µ9 t <br /> , and EW-1 at concentrations as high iii h as 2, ^ <br /> from 19 of the 20 welts at concentrations 1 nes) <br /> 2,300 µg/l (ethyl benzene) and 11,000 4911 (XY 11B, MW.-12B, <br /> g, MW-10) MW- 1 TBA was <br /> r MTBE,was detected m the water same <br /> les collected from MW 5 5 µgfl to 200 µg/ <br /> -13B and FW-1 at concentrations rang g /l Ethanol was detected at s <br /> MW-13A, MW 11B ata concentration of 6 8 µg _ <br /> samples from M�- MW-128 1,2-OCA was detected m`Fater samP3B AY <br /> detected In waterles from -11B, MW-12S,,MW` <br /> ll lnwater camp 6B, MW_�7, MW--8A, MW- <br /> concentration of 170'µmW-5, <br /> g�W 5, W-6A, MW_ 1 Analytical results,of water samples <br /> from MW-13 in from 1 2 µgll to 28 µ d 3 analytical results from <br /> quarter of 2000 are surrimarized on Table 2 y <br /> and EW-2 at concentrations ranging, ores 4 and 5 illustrate the ground <br /> collected during the fourth q ized on Tables 4,and 5 Ftg The laboratory report(MAl <br /> events are sunimar ound water Intervals QA/QC <br /> report are <br /> pxeviaiis monitoring lumen in upper and 10 gr and the faboratdry Q <br /> water cont anon p of-custody forms <br /> Sample Nos 56287 through 56346) cij,luded in Appendix$ <br /> AND CONCLUSIONS _ <br /> i <br /> 4.0. SUMMARY - 3 area, AGE finds <br /> I , <br /> Based on the data collected from the former UST No s to have been toward the <br /> Basvariably <br /> ears to have been flowing <br /> d v'vater flow -within the lower,i�ci,ei,j�erv�PP aPpe <br /> • Grotto , <br /> southwest, ground water flow in t e'u'P wells <br /> EW-2' <br /> toward the north to northeast <br /> t i ground <br /> The <br /> were detecte in <br /> hydrocarbons m gr <br /> • The greatest concentrations of by` Advanced C,e0Rnv1r0-F1 je1tai,Inc <br /> , <br /> 5 j <br />