Abstract

BackgroundRadionuclide- and heavy metal-contaminated subsurface sediments remain a legacy of Cold War nuclear weapons research and recent nuclear power plant failures. Within such contaminated sediments, remediation activities are necessary to mitigate groundwater contamination. A promising approach makes use of extant microbial communities capable of hydrolyzing organophosphate substrates to promote mineralization of soluble contaminants within deep subsurface environments.Methodology/Principal FindingsUranium-contaminated sediments from the U.S. Department of Energy Oak Ridge Field Research Center (ORFRC) Area 2 site were used in slurry experiments to identify microbial communities involved in hydrolysis of 10 mM organophosphate amendments [i.e., glycerol-2-phosphate (G2P) or glycerol-3-phosphate (G3P)] in synthetic groundwater at pH 5.5 and pH 6.8. Following 36 day (G2P) and 20 day (G3P) amended treatments, maximum phosphate (PO4 3−) concentrations of 4.8 mM and 8.9 mM were measured, respectively. Use of the PhyloChip 16S rRNA microarray identified 2,120 archaeal and bacterial taxa representing 46 phyla, 66 classes, 110 orders, and 186 families among all treatments. Measures of archaeal and bacterial richness were lowest under G2P (pH 5.5) treatments and greatest with G3P (pH 6.8) treatments. Members of the phyla Crenarchaeota, Euryarchaeota, Bacteroidetes, and Proteobacteria demonstrated the greatest enrichment in response to organophosphate amendments and the OTUs that increased in relative abundance by 2-fold or greater accounted for 9%–50% and 3%–17% of total detected Archaea and Bacteria, respectively.Conclusions/SignificanceThis work provided a characterization of the distinct ORFRC subsurface microbial communities that contributed to increased concentrations of extracellular phosphate via hydrolysis of organophosphate substrate amendments. Within subsurface environments that are not ideal for reductive precipitation of uranium, strategies that harness microbial phosphate metabolism to promote uranium phosphate precipitation could offer an alternative approach for in situ sequestration.

Highlights

  • Within sediments, the mobility of phosphate (PO432) is controlled by pH, coprecipitation reactions with metals and radionuclides, adsorption/desorption, and ion-exchange reactions [1]

  • Harnessing microbial phosphatases expressed by extant microbial communities within uranium (U)-contaminated environments represents an approach to leverage microbial phosphate acquisition phenotypes to promote in situ sequestration of U as insoluble phosphate minerals

  • This study examined the extant Oak Ridge Field Research Center (ORFRC) prokaryotic community that could promote in situ sequestration of U as geochemically stable autunite-type minerals (Figure 1) through hydrolysis of organophosphate substrates (i.e., G2P and G3P)

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Summary

Introduction

The mobility of phosphate (PO432) is controlled by pH, coprecipitation reactions with metals and radionuclides, adsorption/desorption, and ion-exchange reactions [1]. Harnessing microbial phosphatases expressed by extant microbial communities within uranium (U)-contaminated environments represents an approach to leverage microbial phosphate acquisition phenotypes to promote in situ sequestration of U as insoluble phosphate minerals. Radionuclide- and heavy metal-contaminated subsurface sediments remain a legacy of Cold War nuclear weapons research and recent nuclear power plant failures. Within such contaminated sediments, remediation activities are necessary to mitigate groundwater contamination. A promising approach makes use of extant microbial communities capable of hydrolyzing organophosphate substrates to promote mineralization of soluble contaminants within deep subsurface environments

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