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o» in ao x0viz 'p•51u 64Z 5Z5L CHEVRON PRODUCTS 14004/005 <br /> Comments \\\ <br /> 1) The primary hydrocarbon source area at the site is believed to <br /> have been immediately to the east of the former tank pit, adjacent <br /> to the pump island. Definition of the probable source area is based <br /> on elevated concentrations of dissolved hydrocarbons measured in <br /> MW-3 to -5 (prior to September 1989) , and pre-remediation soil <br /> samples. <br /> 2) Removal of hydrocarbon mass from the subsurface is indicated by <br /> the recovery of the VES, analytical data from confirmation soil <br /> borings, and the reduction in dissolved hydrocarbon concentrations <br /> in downgradient well MW-11. <br /> It should be noted that groundwater has not been sampled from <br /> formerly impacted wells mw-3, -4 and -5 since late 1989, due to <br /> insufficient water. If the trend toward increasing water table <br /> elevation continues, it may be possible to sample these wells <br /> during a future monitoring event. Reduced hydrocarbon <br /> concentrations in groundwater samples collected from these wells <br /> will provide conclusive evidence for the effectiveness of former <br /> remediation activity. <br /> 3) The apparent equilibrium line of dowagradient hydrocarbon <br /> migration which is noted at the site likely developed, at least in <br /> part, to the attenuation and destruction of dissolved hydrocarbons <br /> by a variety of processes. Destructive processes include <br /> biodegradation, abiotic oxidation and hydrolysis. <br /> The process of biodegradation results in the ultimate <br /> transformation of the hydrocarbon compound into the metabolic <br /> byproduct of bacterial activity; water and carbon dioxide. The <br /> limitation on the degree of biodegradation is often the absence of <br /> a suitable electron acceptor Compound available in the subsurface. <br /> By measuring groundwater for the presence of various electron <br /> acceptor compounds, the areal distribution of the dissolved phase <br /> may be explained. <br /> The most common electron acceptor preferred for aerobic bacterial <br /> biodegradation is dissolved oxygen. Alternative electron acceptor <br /> compounds which will facilitate anaerobic bacterial activity <br /> include nitrates, ferric iron and sulfates. <br /> The following electron acceptor data was analyzed at the site (see <br /> attached Laboratory Analysis Data Table) : <br /> (a) Dissolved Sulfate - concentrations are uniformly elevated <br /> at all sampled wells (see attached Site Map/Dissolved Sulfate <br /> Concentrations) . The presence of relatively abundant dissolved <br /> sulfate indicates sufficient concentrations of the anaerobic <br /> electron acceptor to facilitate the biodegradation of dissolved <br /> hydrocarbons both on-site and off-site. <br /> 3 <br />