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eeologfea(hcklucsinc Page 5 <br /> Groundwater Monitoring Report <br /> Project No 724 2 <br /> August 11, 2003 <br /> • Intennediate wells MW-106 and MW-107 contained trace BTEX concentrations and <br /> low TPH-G and MTBE concentrations <br /> ' • TPH-G was non-detected in water table wells MW-4, MW-5, MW-6 or MW-7 <br /> « A contour diagram illustrating the extent of the TPH-G plume in the shallow aquifer was <br /> not ptepared for this season <br /> ' • TPH-G was detected in intermediate wells MW-2, MW-3, MW-106 and MW-107 <br /> Figure 5 — Intermediate Well TPH-G Concentrations - illustrates the extent of the TPH- <br /> ' G plume in the intermediate aquifer <br /> Benzene was non-detected in water table wells MW-4, MW-5, MW-6 or MW-7 so a contour <br /> ' diagram illustrating the extent of the benzene plume in the shallow aquifer was not <br /> prepared MTBE has been present in well MW-7 (5 2 ug/1), which continues to be the only <br /> water table well that contains MTBE - see Figure 7 — Water Table Well MTBE <br /> Concentrations <br /> Figure 6 -- Intennedtate Well Benzene Concentrations & Figure 8 — Intermediate Well <br /> MTBE Concentrations suggest that a significant plume does not exist below the water table <br /> The presence of TPH-G contamination in well MW-106 and MW-107 suggests that a <br /> submerged plume is being sourced by residual soil contamination beneath the present water <br /> table It is noted that the screened intervals of these wells (55-60 feet bgs) are placed near <br /> the elevation of the groundwater table in 1992 — approximately 54 feet bgs <br /> As indicated in Figure 9 — MW-2 TPH-G vs GW Elevation, with the exception of June 20, <br /> 1997, contaminant concentrations have generally mimicked the pattern of groundwater <br /> elevation changes for the past 10 years in down gradient well MW-2 The June 20, 1997 <br /> test result appears to be an anomalous data point or a point at which the rising groundwater <br /> table encountered residual soil contamination <br /> Oxidation/Reduction Potential (ORP) measurements (Table 5) show that eight of ten wells <br /> have negative values The negative ORP values obseived in the wells show that they are <br />' either within the core of the contamination plume or aie in the reaction/depletion shadow <br /> down gradient of the plume Well MW-4's ORP values fluctuate between positive and <br /> negative values suggesting that the well is on the up gradient edge of the plume Dissolved <br />' oxygen values corroborate with the ORP values measure in these wells <br /> 3.0 CONCLUSIONS & RECOMMENDATIONS <br /> The contamination plume as observed from these wells is stable and does not appear to be <br />' sourcing a significant off site plume In GTI's opinion, the levels of contamination present <br /> do not warrant an engineered clean up <br /> 1 <br />