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developed and sampled monitoring wells MW-1, MW-2 and MW-3. Analytical results of the soil <br /> and groundwater samples collected indicated elevated concentrations of petroleum hydrocarbons <br /> were present in the soil and groundwater downgradient of the former gasoline UST locations. <br /> On September 24 and October 2, 1996, Smith Technology conducted an additional subsurface <br /> investigation at the site. A total of 9 soil borings were advanced to depths up to 15 feet below <br /> ground surface. Soil, soil vapor, and groundwater samples were collected from the borings. <br /> Analytical results of the soil and groundwater samples collected indicated the general extent of <br /> total petroleum hydrocarbons as gasoline (TPHg), benzene, toluene, ethylbenzene, and xylenes <br /> (BTEX), and methyl tertiary butyl ether (MTBE) in soil and groundwater under the site. <br /> Analytical results for geochemical parameters in soil and groundwater indicated bioremediation <br /> is occurring in the plume of petroleum hydrocarbons in groundwater beneath the site. <br /> Analytical results of soil vapor samples indicated the availability of oxygen, carbon dioxide, <br /> nitrogen and methane in the vadose zone. Also, results of laboratory geophysical testing on <br /> soil samples from the site indicated that the potential receptor on-site, the water supply well, <br /> would not be affected by the plume of petroleum hydrocarbons in groundwater within the next <br /> 20 years, in the worst case. <br /> INTRINSIC BIOREMEDIATION OF GROUNDWATER <br /> Several detailed field studies have been performed examining indicators of intrinsic bioremediation <br /> and identify factors which significantly effect the rate and extent of bioremediation (Buscheck and <br /> others, 1993; McAllister and Chiang, 1994; Borden and others, 1995; Buscheck and Alcantar, <br /> = _l 1995). Through these studies and ongoing research of the factors which control biodegradation, <br /> it is now understood that dissolved petroleum hydrocarbons in groundwater will biodegrade, <br /> without artificial enhancement, due to the presence of naturally occurring (indigenous) <br /> microorganisms. Technical protocols for implementing and monitoring intrinsic bioremediation <br /> studies in groundwater have been developed by the US Air Force and Chevron Corporation. <br /> Intrinsic bioremediation in brief, is the use of indigenous microorganisms to degrade contaminants <br /> which have been released into the subsurface. The biodegradation of the contaminants is <br /> essentially an oxidation-reduction (redox) reaction where the hydrocarbon is oxidized (donates an <br /> electron) and an electron acceptor is reduced (accepts electrons). There are several compounds <br /> that can serve as electron acceptors including oxygen, nitrate, iron oxides (Fe III), sulfate, water, <br /> and carbon dioxide(Borden and others, 1995), and also manganese (Mn IV) and sulfide. Aerobic <br /> microorganisms use oxygen as the electron acceptors. Anaerobic microorganisms use other <br /> compounds such as nitrate, iron oxides (ferric iron), manganese oxide (Mn IV), sulfate and carbon <br /> dioxide as electron acceptors. <br /> Oxygen is the most preferred electron acceptor in groundwater because microorganisms gain <br /> more energy from these reactions, however, this process usually results in the depletion of oxygen <br /> with an increase in carbon dioxide in the subsurface. Therefore low concentrations of dissolved <br /> oxygen and corresponding high concentrations of carbon dioxide within hydrocarbon plume <br /> indicate biodegradation is taking place (Borden and others, 1995). <br /> : i <br /> w:1951221Reporisl4QMR1996.doc 2 <br /> • <br /> smTH <br />