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GEORGE AND MEI TERANISHI • <br /> 1600 Durham Ferry Rd. <br /> Page 3 of <br /> to augment the excavation remedial effort by installing a low-flow blower and <br /> carbon canisters to initiate bio-venting and vapor extraction to address <br /> hydrocarbons impacting the excavation backfill that are thought to have been <br /> introduced via migrating impacted ground water. <br /> EHD cannot approve this portion of the work plan at this time for the following <br /> reasons: <br /> • There has been no demonstration that the excavation backfill has been <br /> significantly impacted by fuel components; <br /> • There has been no presentation of data or a calculation of the <br /> contaminant mass impacting the backfill; and <br /> • The planned scope of work will not directly address the contaminant mass <br /> impacting soil, and therefore ground water; that was left in place; <br /> • Other than the redox potential data, there has been no demonstration that <br /> bioremediation is a viable process that could be stimulated through the <br /> introduction of supplemental oxygen, or that such biological processes <br /> that may be currently operating in the area of concern will address <br /> hydrocarbons and/or fuel additives; <br /> EHD notes that the 1QR02 proposed to collect "natural attenuation parameters" <br /> from water samples from the 12 monitoring wells and three domestic wells to <br /> ascertain that natural attenuation is occurring at the site. This data will help <br /> address the fourth point above and EHD will approve its collection, but requests <br /> specification of the parameters to be collected and a brief justification for each <br /> monitored point to be so assessed. Soil samples from the impacted area should <br /> also undergo the analyses. <br /> EHD's analysis of the site data has identified two concerns that should be <br /> addressed. EHD notes that the vertical extent of impacted soil east of the <br /> probable release point has been delineated by samples from borings MW-102 <br /> and MW-202, but the area that appears to have been most impacted, near SE <br /> sidewall 9.5, SB-1 , HBA SW sidewalls, and MW-1 (concentrations increasing <br /> with depth) does not have a delineated vertical extent. Shallow ground water <br /> conditions and the previously mentioned vertical gradients have probably limited <br /> the vertical extent of impacted soil in this area of concern to depths similar to the <br /> MW-102 area, but EHD recommends a boring between the former pump island <br /> and the building near the edge of the excavation to delineate the vertical extent <br /> of impacted soil. <br /> Of greater concern is the potential lateral extent of impacted ground water. <br /> Monitoring wells MW-6, MW-7 and MW-107 appear to provide down gradient <br /> limits to the plume of impacted ground water, but EHD notes that MW-6 and <br /> MW-7 are completed in the shallow soil with calculated ground water velocities of <br /> 0.1 to 1.03 feet per year, so an impact in these wells is not likely to occur until <br />