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Mineralization Of PAHs In Coal-Tar Impacted Aquifer Sediments And Associated Microbial Community Structure Investigated With FISH
Citation:
ROGERS, S. W., S. K. ONG, AND T. B. MOORMAN. Mineralization Of PAHs In Coal-Tar Impacted Aquifer Sediments And Associated Microbial Community Structure Investigated With FISH. L. L. Needham, H. Fiedler (ed.), CHEMOSPHERE. Elsevier Science Ltd, New York, NY, 69(10):1563-1573, (2007).
Impact/Purpose:
The objectives were (1) to determine whether changes in the aqueous geochemical environments exhibited in situ may be related to oxygen-, nitrate-, iron-, or sulfate-limited degradation of PAHs as evidenced by laboratory microcosms under defined oxidation-reduction conditions, and (2) identify whether shifts in the structure of the intrinsic microbial community relative to nearby pristine conditions (a) reflected the aqueous geochemistry observed in groundwater measurements and (b) were related to growth of microbial taxa in laboratory microcosms with site sediments under the dominant redox processes related to PAH mineralization.
Description:
The microbial community structure and mineralization of polycyclic aromatic hydrocarbons (PAHs) in a coal-tar contaminated aquifer were investigated spatially using fluorescence in situ hybridization (FISH) and in laboratory-scale incubations of the aquifer sediments. DAPI-detected microbial populations in the contaminated sediments were three orders of magnitude greater than nearby uncontaminated sediments, suggesting growth on coal-tar constituents in situ. Actinobacteria, β- and γ-Proteobacteria, and Flavobacteria dominated the in situ aerobic (>1 mg l-1 dissolved oxygen) microbial community, whereas sulfate-reducing bacteria comprised 37% of the microbial community in the sulfidogenic region of the aquifer. Rapid mineralization of naphthalene and phenanthrene were observed in aerobic laboratory microcosms and resulted in significant enrichment of β- and γ-Proteobacteria potentially explaining their elevated presence in situ. Firmicutes, Flavobacteria, α-Proteobacteria, and Actinobacteria were also enriched in the mineralization assays, but to a lesser degree. Nitrate- and sulfate-limited mineralization of naphthalene in laboratory microcosms occurred to a small degree in aquifer sediments from locations where groundwater chemisty indicated nitrate-and sulfate-reduction, respectively. Some iron-limited mineralization of naphthalene and phenanthrene was also observed in sediments originating near groundwater measurements of elevated ferrous iron. The results of this study suggest that FISH may be a useful tool for providing a much needed link between laboratory microcosms and groundwater measurements made in situ necessry to better demonstrate the potential for natural attenuation at complex PAH contaminated sites.
