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Depth to Groundwater(deep wells) _ 49 70 to 50 66 feet below top of well casing <br /> Groundwater Flow Direction/Gradient (deep wells) Northeast/0 0011 ft1ft <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 Deeper <br /> screened wells are 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 fourth quarter 2005 monitoring event, groundwater was encountered in the shallow <br /> monitoring wells at depths ranging from 48 91 to 51 10 feet bgs Well MW-3 is obstructed Groundwater <br /> elevations had decreased between 0 06 and 0 34 feet in all shallow wells except for MW-2, which <br /> increased 0 01 feet since the previous monitoring event (August 15, 2005) Groundwater monitoring data <br /> were normalized to mean sea level (MSL) and used to prepare a groundwater elevation contour map <br /> (Figure 2) The groundwater flow direction was generally to the east at an average gradient of 0 0006 <br /> Rift Since 1995, groundwater flow in the shallow wells has consistently been toward the east and <br /> southeast(except for the first quarter 2005, flow was toward the east-northeast) <br /> TPHG and benzene were reported in wells VEW-land VEW-2 Benzene was also reported In well MW-2 <br /> The highest concentration of TPHG (110,000 pg/L) was reported in well VEW-2 and the highest <br /> concentration of benzene (2,500 pg/L) was reported in well VEW-1 1,2-DCA was reported in wells MW-2 <br /> (57 }µg1Q, MW-5 (1 4 pg/L), and MW-6 (29 uglL) MTBE, DIPE, ETRE, TAME, TBA, or EDB were not <br /> reported in any of the shallow wells The laboratory noted that the pH levels reported in wells VEW-1, <br /> VEW-2, and MW-5 were above the EPA recommended limit of 2 As the reported results appear to be <br /> consistent with historical data, it appears that the elevated pH has not affected data quality These <br /> analytical results are generally consistent with historical data TPHG, benzene, and MTBE concentrations <br /> for samples collected and analyzed during the fourth quarter 2005 are summarized on Figure 3 <br /> Mid-Depth Wells <br /> At the time of the fourth quarter 2005 monitoring event, groundwater was encountered in the mid-depth <br /> monitoring wells at depths of 49 60 and 50 12 feet bgs Groundwater levels had decreased 0 17 feet In <br /> well MW-16 and increased 0 06 feet in well MW-18 since the previous sampling event (August 15, 2005) <br /> Depth-to-water measurements have been summarized on Figure 4 <br /> TPHG (530 gg/L), benzene (11 µg&), 1,2-DCA(11 µg/L), and TBA(52 µg/L)were reported In well MWA8 <br /> MTBE, DIPE, ETBE, TAME, or EDB were not reported in any of the mid-depth wells TPHG, benzene, <br /> and MTBE concentrations for samples collected and analyzed during the fourth quarter 2005 are included <br /> on Figure 5 <br /> • <br /> K(Apache PlasticslQuarterly repons12005\Apache_4Q05 DOC STRATUS <br />