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+«. Gealagkaf Tecluucs Ina Page 6 <br /> Groundwater Monitoring Report <br /> Project No.724.2 <br /> May 16,2005 <br /> 1. TPH-G <br /> • Only MW-2 (63 Vg/L TPH-G) was the only well found detected for TPH-g <br /> contaminants above the laboratory reporting limits. A contour diagram was not <br /> plotted because of the limited data. <br /> • Figure 6 illustrates the distribution of TPH-G in the intermediate wells. A localized <br /> high is centered in well MW-106 and the concentrations attenuate to the locations of <br /> MW-107 &MW-108. <br /> • Figure 7 illustrates the distribution of TPH-G in the deep wells. Only MW-208 shows <br /> the elevated TPH-g concentration. MW-202, MW-209 and MW-210 were non-detect <br /> above the laboratory detection limits for TPH-g. <br /> 2. MTBE <br /> +-� • Figure 8 illustrates the distribution of MTBE in the intermediate wells. A localized <br /> high of 19 µg/1 is present in well MW--106 that attenuates west to the location of MW- <br /> 107. <br /> `" • Figure 9 illustrates the distribution of MTBE in the deep wells. A node of MTBE (15 <br /> [tg/l) is present in well MW-208 that attenuates to the southeast to the location of <br /> MW-209. <br /> 3. Benzene <br /> • Figure 10 illustrates the distribution of Benzene in the intermediate wells. Trace <br /> concentration is present in MW-106 and MW-108. <br /> • Figure 11 illustrates the distribution of Benzene in the deep wells. A node of elevated <br /> Benzene concentration (6.1 [,g/l) is present in well MW-208 that attenuates to non- <br /> 4.6 detectable levels in the southeast, south and southwest locations of MW-209, MW- <br /> 210 &MW-202, respectively. <br /> 4, Oxidation/Reduction Potential (ORP) and dissolved oxygen (DO) measurements (Table 6) <br /> show that all of the sampled wells have a mixture of a couple of positive and mostly negative <br /> ORP values and low DO readings. The negative ORP values observed in the wells show that <br /> 4� they are either within the core of the contamination plume or are in the reaction/depletion <br /> shadow down gradient of the plume. Dissolved oxygen values generally corroborate with the <br /> ORP values measured in these wells and suggest that the plume is relatively stable. <br /> V <br /> As indicated in Figure 12—MW-2: TPH-G vs. GW Elevation, with the exception of rune 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. <br /> 3.0 CONCLUSIONS & RECOMMENDATIONS <br /> Based on our interpretation of the data collected over the course of this subsurface <br /> Lam.- investigation, GTI has reached several conclusions. These conclusions assume that the <br />