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CLEARWATER <br /> G a o u r <br /> Enwronmenta! Scrorces <br /> (DO) In anaerobic degradation, compounds other than DO are used as electron acceptors The <br /> reactions that yield the most energy take precedence over those reactions that yield less energy <br /> (except for denitrification which yields the most free energy but will not occur of DO <br /> concentrations are >0 5 mmllngrams per liter (mg(L)) This results in electron acceptors being <br /> used up in the following preferential order DO, nitrate, ferric-iron oxides, sulfate, and carbon <br /> dioxide (methanogenesis) Since DO and nitrate are toxic to sulfate-reducing organisms, sulfate <br /> cannot be used as an electron acceptor until DO and nitrate have been sufficiently depleted4 <br /> Metabolism through iron reduction uses femc-iron oxides and produces ferrous iron (dissolved) <br /> as a byproduct <br /> Reduction-oxidation potential (Eh) is a measure of the electron activity in a solution As electron <br /> acceptors are consumed within the plume during biodegradation, Eh will drop within the plume <br /> Each biochemical pathway has an associated range of Eh values, depending on the influx of <br /> electrons to the system by groundwater recharge Eh values can thus be used to confirm the <br /> active biochemical pathway(s) determined on the basis of electron acceptor depletion <br /> Alternatively, when electron depletion data is inconclusive due to high groundwater recharge, <br /> biodegradation can be confirmed and the active bmochenucal pathway can be assessed by <br /> evaluating Eh values Approximate Eh ranges for each biochemical pathway are <br /> Method of Metabolism Eh Range in millivolts5 <br /> _ Aerobic Degradation +150 to+800 <br /> Denitrification -100 to+750_ <br /> y-.-........................... �-gyp�-�� .................. ...«.....»........_........� y <br /> Sulfate Reduction -770 to-220 <br /> Iron reduction r -470 to+100 <br /> Alkalinity in the groundwater reacts with organic acid byproducts of biodegradation and thus <br /> acts as a buffering agent to maintain pH levels suitable for microbes This reaction causes <br /> alkalinity to decrease in the presence of biodegradation With sufficient alkalinity present to <br /> buffer the products of biodegradation, pH values remain constant inside and outside of the <br /> plume If the groundwater does not contain sufficient alkalinity, the organic acids may build up, <br /> reducing the pH and eventually creating an environment inhospitable to the hydrocarbon- <br /> utilizing microbes <br /> Results of Monitored Natural Attenuation Evaluation <br /> The monitored natural attenuation (MNA) study focused on aerobic and anaerobic <br /> biodegradation processes Positive results for some or all natural attenuation pathways were <br /> anticipated because contaminant concentrations appear to be declining based on determination of <br /> first-order decay rates The results of this study suggest that both aerobic and anaerobic <br /> 4Wiedemeier,T H, Wilson,J T,Kampbell,D R,Miller,RN and Hansen,J H (1995) Technical Protocol for <br /> implementing Intrinsic Remediation with Long-Term Monitoring for Natural Attenuation of Fuel Contamination <br /> Dissolved in Groundwater Vol 1 AFCE,Technology Transfer Division,Brooks AFB, San Antonio,TX <br /> 5Cookson,J T,Jr, 1995 Bioremediation Engineering Design and Application (Ed. Nalven, G) McGraw-Hill, <br /> Inc,New York,NY <br /> ZB178C/3Q03 Momtonng Rpt 7 October 14,2003 <br />