Natural attenuation of chlorinated solvents at Area 6, Dover Air Force Base: characterization of microbial community structure

被引:32
作者
Davis, JW
Odom, JM
DeWeerd, KA
Stahl, DA
Fishbain, SS
West, RJ
Klecka, GM
DeCarolis, JG
机构
[1] Dow Chem Co USA, Toxicol & Environm Res Lab, Midland, MI 48674 USA
[2] EI Du Pont Nemours & Co, Wilmington, DE 19880 USA
[3] GE Co, Corp Res & Dev, Schenectady, NY 12301 USA
[4] Univ Washington, Dept Civil & Environm Engn, Seattle, WA 98195 USA
关键词
natural attenuation; biodegradation; chlorinated solvents; microorganisms; bioremediation;
D O I
10.1016/S0169-7722(01)00217-0
中图分类号
X [环境科学、安全科学];
学科分类号
08 [工学]; 0830 [环境科学与工程];
摘要
A polyphasic approach based on cultivation and direct recovery of 16S rRNA gene sequences was utilized for microbial characterization of an aquifer contaminated with chlorinated ethenes. This work was conducted in order to support the evaluation of natural attenuation of chlorinated ethenes in groundwater at Area 6 at Dover Air Force Base (Dover, DE). Results from these studies demonstrated the aquifer contained relatively low biomass (e.g. direct microscopic counts of < 10(7) bacteria/g of sediment) comprised of a physiologically diverse group of microorganisms including iron reducers, acetogens, sulfate reducers, denitrifiers, aerobic and anaerobic heterotrophs. Laboratory microcosms prepared with authentic sediment and groundwater provided direct microbiological evidence that the mineralization of vinyl chloride and cis-dichloroethene as well as each step in the complete reductive dechlorination of tetracloroethene to ethene can occur in the Area 6 aquifer. Enrichment cultures capable of the oxidative degradation of cis-1,2-dichloroethene (cis-DCE) and vinyl chloride (VC) were obtained from groundwater across the aquifer demonstrating the possible importance of direct, non-cometabolic oxidation of cis-DCE and VC in natural attenuation. Culture-independent analyses based upon recovery of 16S rRNA gene sequences revealed the presence of anaerobic organisms distributed primarily between two major bacterial divisions: the delta subdivision of the Proteobacteria and low-G + C gram positive. Recovery of sequences affiliated with phylogenetic groups containing known anaerobic-halorespiting organisms such as Desulfitobacterium, Dehalobacter, and certain groups of iron reducers provided qualitative support for a role of reductive dechlorination processes in the aquifer. This molecular data is suggestive of a functional linkage between the microbiology of the site and the apparent natural attenuation process. The presence and distribution of microorganisms were found to be consistent with a microbially driven attenuation of chlorinated ethenes within the aquifer and in accord with a conceptual model of aquifer geochemistry which suggest that both reductive and oxidative mechanisms are involved in heterogeneous, spatially distributed processes across the aquifer. (C) 2002 Elsevier Science B.V All rights reserved.
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页码:41 / 59
页数:19
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