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• W1557029160 endingPage "852" @default.
• W1557029160 startingPage "846" @default.
• W1557029160 abstract "Iron-oxidizing bacteria are present within the top 2 m (but not always at the surface) and near the water table-capillary fringe of the vegetated Nordic uranium deposit, Elliot Lake, Ontario, Canada. They are distributed uniformly in the top 0.5 m of unvegetated tailings. The locations of these bacteria correlate with zones of pyrite oxidation as delineated in previous studies by the formation of soluble iron and sulfate. Heterotrophic bacteria are also present in the tailings, with greatest concentrations at the surface and near the water table-capillary fringe. Sulfate-reducing bacteria were detected in the soil and peat at the base of the tailings. The results of this study suggest that the establishment of vegetation directly upon the tailings surface does not arrest bacterial pyrite oxidation." @default.
• W1557029160 created "2016-06-24" @default.
• W1557029160 creator A5041075151 @default.
• W1557029160 date "1987-04-01" @default.
• W1557029160 modified "2023-09-25" @default.
• W1557029160 title "Distribution of Iron-Oxidizing Bacteria in the Nordic Uranium Tailings Deposit, Elliot Lake, Ontario, Canada" @default.
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• W1557029160 doi "https://doi.org/10.1128/aem.53.4.846-852.1987" @default.
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