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, <br /> TreadwelEADI D <br /> of 41 samples). In addition, in only 3 % of the results, TPH-kerosene concentrations have been reported <br /> to be greater in magnitude than the corresponding TPH-gasoline result from soil and groundwater (3 out <br /> of 86 samples) . Based on this data and historical evidence indicating that the USTs did not contain <br /> Kerosene, TPH-k does not appear to be a contaminant at the Site. <br /> Based on the age of the release, it is estimated that1 MTBE and fuel oxygenates were not present in <br /> ( '0{th s gasoline released at the site. This is further supported by the general absence of these compounds in <br /> k Site soil and groundwater. Sporadic, low concentrations of MTBE and a few oxygenates have been <br /> r <br /> detected, but not at a frequency or concentration to classify them as contaminants of concern . For <br /> example, MTBE has been detected in six of the fifty-six water samples collected at the Site at <br /> concentrations ranging from 1.5 to 3. B pg/L, which is lower than the Maximum Contaminant Level for <br /> drinking water of 13 pg/L1 j <br /> 7. 2 Extent of Groundwater Impacts. <br /> The lateral distribution of TPHg and benzene in the shallow zone groundwater are shown on ' - - <br /> Figures 5 and 6 respectively. These figures indicate that the shallow source plume is largely located <br /> within the vicinity of the former pump station and distribution lines. The extent of contaminant migration <br /> in the shallow zone does not appear to extend more than 50 feet down-gradient of the former USTs <br /> based on investigations performed thus far. <br /> ( l <br /> Petroleum hydrocarbon impacts are greater within the deep zone. The lateral distribution of TPHg and <br /> benzene in the deep zone groundwater are shown on figures 7 and 8 respectively. Significant <br /> concentrations of TPHg and BTEX appear to be distributed over a larger area than within the shallow <br /> zone. The contaminant distribution suggests that the direction of groundwater gradient in the deep <br /> zone is likely to the north-east, however, no wells have been placed in this zone, so an accurate <br /> groundwater flow direction and gradient has not yet been identified, and therefore the lateral extent of <br /> contamination has not yet been established. % <br /> 8.0 PROPOSED GROUNDWATER MONITORING <br /> This work plan proposes to install six monitoring wells at four locations (MW-5s, MW-5d, MW-6s, MW-6d, <br /> MW-7s, and MW-8d) as shown on Figure 9. The well locations were selected to better characterize the <br /> 12 <br /> 25971201 . DGD 6 February 2008 <br />