We evaluated compound-specific isotope analysis (CSIA) as a tool to assess the coupling of microbial toluene oxidation by Fe(III)-reducing bacteria and abiotic reduction of nitroaromatic contaminants by biogenic mineral-bound Fe(II) species. Examination of the two processes in isolated systems revealed a reproducible carbon isotope fractionation for toluene oxidation by Geobacter metal-lireducens with a solid Fe(III) phase as terminal electron acceptor. We found a carbon isotope enrichment factor, epsilonC, of -1.0 +/- 0.1 per thousand, which corresponds to an apparent kinetic isotope effect (AKIE(C)) of 1.0073 +/- 0.0009 for the oxidative cleavage of a C-H bond. Nitrogen isotope fractionation of the reduction of nitroaromatic compounds (NAC) by mineral-bound Fe(ll) species yielded a nitrogen isotope enrichment factor, epsilonN, of -39.7 +/- 3.4 per thousand for the reduction of an aromatic NO2-group (AKIE(N) = 1.0413 +/- 0.0037) that was constant for variable experimental conditions. Finally, AKIE values for C and N observed in coupled experiments, where reactive Fe(II) was generated through microbial activity, were identical to those obtained in the isolated experiments. This study provides new evidence on isotope fractionation behavior during contaminant transformation and promotes the use of CSIA for the elucidation of complex contaminant transformation pathways in the environment.

The toxicity of electrqphiles, including reactive organochlorines, epoxides, and compounds with an activated double bond was investigated. A set of different bioanalytical assays based on genetically modified Escherichia coli strains was set up to quantify cytotoxicity and specific reactivity toward the important biological nucleophiles DNA and glutathione (GSH). The significance of GSH for detoxification was assessed by cellular GSH depletion as well as by growth inhibition of a GSH-deficient strain. Tests for DNA damage comprised the measurement of induction of DNA repair systems, DNA fragmentation, and growth inhibition of a strain deficient in major DNA repair mechanisms. The most suitable assays for detection of mechanisms that underlie the observable cytotoxicity of the tested electrophiles were two sets of strains either lacking GSH or DNA repair in combination with their corresponding parent strains. Comparison of toxicity observed in those strains suggests three clearly distinguishable modes of toxic action for electrophilic chemicals: "DNA damage", "GSH depletion-related toxicity", and "unspecific reactivity". The class of chemicals causing DNA damage includes the epoxides 1,2-epoxybutane, (2,3-epoxypropyl)benzene, and styrene oxide. The class of chemicals with GSH depletion-related toxicity includes compounds with an activated double bond, like acrylates and acrolein. All reactive organochlorines and some epoxides were classified as unspecifically reactive because their toxicity is initiated by reactions with both biological nucleophiles. The work presented here is a contribution for an alternative hazard and effect assessment of organic pollutants based on mode of toxic action classification.

Microbial oxidation of BTEX compounds under iron-reducing conditions is an important attenuation process for fuel-contaminated sites. We evaluated the use of compound-specific isotope analysis for the identification and quantification of anaerobic toluene oxidation by Geobacter metallireducens. 13C and 2H enrichment of toluene was measured in laboratory batch systems and varied significantly for a solid vs a dissolved Fe(III) phase provided as terminal electron acceptor. 13C enrichment factors (epsilonC) in suspensions of a solid Fe(III) phase were between -1.0 and -1.3% per hundred, whereas epsilonC-values were significantly higher in solutions of Fe(lll) citrate (-2.9 to -3.6% per hundred. The same trend was observed for 2H fractionation. Solid phase reduction resulted in an epsilonH-value of -34.6 +/- 0.9% per hundred, compared to -98.4 +/- 3.0% per hundred for the reduction of dissolved Fe(lll). The linear correlation of delta(2)H vs. delta(13)C during toluene oxidation resulted in nearly identical slopes for both systems, confirming that the reaction mechanism, that is enzymatic methyl-group oxidation, was the same. We hypothesize that smaller 2H and 13C fractionation in suspensions is due to toluene transport limitations to cells of G. metallireducens at surfaces of solid Fe(III) phases. Enrichment factors determined in Fe(III) mineral suspensions should be more representative for anaerobic toluene degradation owing to the abundance of solid Fe(III) in soils and aquifers.

In anoxic environments, the oxidation of organic compounds, such as BTEX fuel components, by dissimilatory Fe(III) reduction can generate reactive mineral-bound Fe(II) species, which in turn are able to reduce other classes of organic and inorganic groundwater contaminants. In this study, we designed and evaluated an anaerobic batch reactor that mimicks iron-reducing conditions to investigate the factors that favor the coupling of microbial toluene oxidation and abiotic reduction of nitroaromatic contaminants. We investigated the influence of different Fe(III)-bearing minerals and combinations thereof on the coupling of these two processes. Results from laboratory model systems show that complete oxidation of toluene to CO2 by Geobacter metallireducens in the presence of Fe(III)-bearing minerals leads to the formation of mineral-bound Fe(II) species capable of the reduction of 4-nitroacetophenone. Whereas significant microbial toluene oxidation was only observed in the presence of amorphous Fe(III) phases, reduction of nitroaromatic compounds only proceeded with Fe(II) species bound to crystalline Fe(III) oxides. Our results suggest that in anoxic soils and sediments containing amorphous and crystalline iron phases simultaneously, coupling of microbial oxidation and abiotic reduction of organic compounds may allow for concurrent natural attenuation of different contaminant classes.

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