Groundwater contamination presents challenges across world, yet remediation solutions in variably oxidized regions are limited and many co-interactions between contaminant metals and microbial reactions occur. Here we present a genomic and metabolic study into the biogeochemistry of a uranium-contaminated surficial aquifer site in Riverton, WY. We identified unique communities that varied based on geochemistry, geography, and compartment, matching microbial subsurface studies. Cross-site metabolism tests showed communities had functional capabilities of nitrogen respiration, manganese reduction, iron reduction, and sulfide oxidization. No sites showed evidence of microbial U-bioreduction nor ammonium oxidation. Only former tailings area groundwater and ditch surface water sites nearest a retention pond, and a downgradient oxbow lake exhibited sulfate reduction metabolisms. This was contrary to our hypothesis of near-river downgradient groundwater sites having U and S reduction capability. Most communities which showed S reduction capacity exhibited Fe oxidation capacity. Modeling demonstrated U as calcium uranyl carbonates. Based on our metabolism tests and known mineral and microbial metabolism reduction potentials, this suggests U reduction could only be achieved via abiotic reaction with biogenic sulfide. Of eleven sites tested, it is possible in four. This has impact on future site-specific remediation plans and understanding of microbial reactions in variably reduced zones.
Pettinger, C., Woods, A., Johnson, R., Paradis, C., Majumder, E. L.- W.
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