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3� <br /> Groundwater Flow Direction/Gradient (mid-depth wells) NA <br /> Depth to Groundwater(deep wells) 48 68 to 50 53 feet below to of well casin <br /> Groundwater Flow Direction/Gradient (deep wells) East to 012 ft/ft <br /> DISCUSSION <br /> As discussed in the Site Conceptual Model (SCM), review of the subsurface geology and groundwater well <br /> elevation data indicate that although different transmissive (i a sandy) zones have been Identified at <br /> various depths at this site, these zones appear to be hydraulically connected and likely form one <br /> continuous water-bearing zone Groundwater monitoring wells have been screened at three distinct <br /> intervals Shallow screened wells VEW-1, VEW-2, MW-2 through MW-7, and MW-15 were screened at <br /> various depth intervals between 40 and 70 feet below ground surface (bgs) Samples collected from <br /> these wells currently represent groundwater concentrations at first encountered groundwater <br /> Deeper screened wells intended to target sandy, more transmissive zones that may represent preferential <br /> pathways for petroleum hydrocarbon migration Mid-depth wells MW-16 and MW-18 are screened in <br /> sandy zones between 85 and 90 feet bgs Deep wells MW-8 through MW-11 and MW-17 are screened <br /> between 94 and 120 feet bgs, within a laterally continuous sandy unit first encountered at approximately <br /> 95 to 105 feet bgs <br /> Shallow Wells <br /> At the time of the second quarter 2004 monitoring event, groundwater was encountered in the shallow <br /> monitoring wells at depths ranging from 47 82 to 49 35 feet bgs Well MW-3 is obstructed Groundwater <br /> elevations had increased between 0 11 and 0 28 feet in the shallow wells since the previous monitoring <br /> event (February 23, 2004) Groundwater monitoring data were normalized to mean sea level (MSL) and <br /> used to prepare a groundwater elevation contour map (Figure 2) The groundwater flow direction on May <br /> 24, 2004, was toward the east-northeast at a gradient of 0 001 ft/ft Since 1995, groundwater flow in the <br /> shallow wells has consistently been toward the east and southeast <br /> In the shallow wells, THPG and benzene were reported in wells VEW-1, and VEW-2 The highest <br /> concentrations of TPHG (120,000 µg/L) were reported In both wells VEW-1 and VEW-2, and the highest <br /> concentrations of benzene (1,100 µg/L) were also reported in both wells VEW-1 and VE 1 2-DCA <br /> , <br /> (4 2 µglL) was reported in well MW-2 MTBE, D1PE, ETBE, TAME, TBA, or EDB were not repoed in any <br /> of the shallow wells These analytical results are generally consistent with historical data TPHG, <br /> benzene, and MTBE concentrations for samples collected and analyzed during the second quarter 2004 <br /> are summarized on Figure 3 <br /> Mid-Depth Wells <br /> At the time of the second quarter 2004 monitoring event, groundwater was encountered in the mid-depth <br /> monitoring wells at depths of 48 53 and 49 34 feet bgs Since only two mid-depth monitoring wells have <br /> been installed, groundwater flow direction and gradient cannot be calculated at this time Depth-to-water <br /> measurements have been summarized on Figure 4 <br /> TPHG (450 µg/L), benzene (19 µg/L), TBA (110 µg/L), and 1,2-DCA(210 µg/L)were reported in well Mw_ <br /> 18 Petroleum hydrocarbons or fuel additives were not reported in the sample collected from well MW-16 <br /> TPHG benzene and MTBE concentrations for samples collected and analyzed during the second quarter <br /> 2004 are included on Figure 5 <br /> P wache Plastics\Quarterly reportsQ00AApache_2Q04 DOC <br /> snegrus <br />