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000052399 084__ $$2WoS$$aEngineering, Environmental
000052399 084__ $$2WoS$$aEnvironmental Sciences
000052399 1001_ $$0P:(DE-HGF)0$$aFischer, A.$$b0
000052399 245__ $$aA multitracer test proving the reliability of Rayleigh equation-based  approach for assessing biodegradation in a BTEX contaminated aquifer
000052399 260__ $$aColumbus, Ohio$$bAmerican Chemical Society$$c2006
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000052399 520__ $$aCompound-specific stable isotope analysis (CSIA) is one of the most important methods for assessing biodegradation activities in contaminated aquifers. Although the concept is straightforward, the proof that the method cannot be only used for a qualitative analysis but also to quantify biodegradation in the subsurface was missing. We therefore performed a multitracer test in the field with ring-deuterated (d(5)) and completely (d(8)) deuterium-labeled toluene isotopologues (400 g) as reactive tracers as well as bromide as a conservative tracer. The compounds were injected into the anoxic zone of a BTEX plume located down-gradient of the contaminant source. Over a period of 4.5 months the tracer concentrations were analyzed at two control planes located 24 and 35 m downgradient of the injection well. Deuterium-labeled benzylsuccinate was found in the aquifer, indicating the anaerobic biodegradation of deuterated toluene via the benzylsuccinate synthase pathway. Three independent methods were applied to quantify biodegradation of deuterated toluene. First, fractionation of toluene-d(8) and toluene-d(5) using the Rayleigh equation and an appropriate laboratory-derived isotope fractionation factor was used for the calculation of the microbial decomposition of deuterated toluene isotopologues (CSIA-method). Second, the biodegradation was quantified by the changes of the concentrations of deuterated toluene relative to bromide. Both methods gave similar results, implying that the CSIA-method is a reliable tool to quantify biodegradation in contaminated aquifers. The results of both methods yielded a biodegradation of deuterated toluene isotopologues of approximately 23-29% for the first and 44-51% for the second control plane. Third, the mineralization of deuterated toluene isotopologues was verified by determination of the enrichment of deuterium in the groundwater. This method indicated that parts of deuterium were assimilated into the biomass of toluene degrading microorganisms.
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000052399 7001_ $$0P:(DE-Juel1)VDB62716$$aBauer, J.$$b1$$uFZJ
000052399 7001_ $$0P:(DE-HGF)0$$aMeckenstock, R. U.$$b2
000052399 7001_ $$0P:(DE-HGF)0$$aStichler, W.$$b3
000052399 7001_ $$0P:(DE-HGF)0$$aGriebler, C.$$b4
000052399 7001_ $$0P:(DE-HGF)0$$aMaloszewski, P.$$b5
000052399 7001_ $$0P:(DE-HGF)0$$aKastner, M.$$b6
000052399 7001_ $$0P:(DE-HGF)0$$aRichnow, H. H.$$b7
000052399 773__ $$0PERI:(DE-600)1465132-4$$a10.1021/es052466t$$gVol. 40, p. 4245 - 4252$$p4245 - 4252$$q40<4245 - 4252$$tEnvironmental Science & Technology$$v40$$x0013-936X$$y2006
000052399 8567_ $$uhttp://dx.doi.org/10.1021/es052466t
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