Abstract
Uranium is a contaminant of major concern across the US Department of Energy complex that served a leading role in nuclear weapon fabrication for half a century. In an effort to decrease the concentration of soluble uranium, tripolyphosphate injections were identified as a feasible remediation strategy for sequestering uranium in situ in contaminated groundwater at the Hanford Site. The introduction of sodium tripolyphosphate into uranium-bearing porous media results in the formation of uranyl phosphate minerals (autunite) of general formula {X1–2[(UO2)(PO4)]2–1·nH2O}, where X is a monovalent or divalent cation. The stability of the uranyl phosphate minerals is a critical factor that determines the long-term effectiveness of this remediation strategy that can be affected by biogeochemical factors such as the presence of bicarbonates and bacterial activity. The objective of this research was to investigate the effect of bicarbonate ions present in the aqueous phase on Ca-autunite dissolution under anaerobic conditions, as well as the role of metal-reducing facultative bacterium Shewanella oneidensis MR1. The concentration of total uranium determined in the aqueous phase was in direct correlation to the concentration of bicarbonate present in the solution, and the release of Ca, U and P into the aqueous phase was non-stoichiometric. Experiments revealed the absence of an extensive biofilm on autunite surface, while thermodynamic modeling predicted the presence of secondary minerals, which were identified through microscopy. In conclusion, the dissolution of autunite under the conditions studied is susceptible to bicarbonate concentration, as well as microbial presence.






Similar content being viewed by others
Explore related subjects
Discover the latest articles and news from researchers in related subjects, suggested using machine learning.References
Anagnostopoulos, V., Symeopoulos, B., Bourikas, K., & Bekatorou, A. (2015). Biosorption of U(VI) from aqueous systems by malt spent rootlets. Kinetic, equilibrium and speciation studies. International Journal of Environmental Science and Technology,13, 285–296.
Bachmaf, S., Planer-Friedrich, B., & Merkel, B. J. (2008). Effect of sulfate, carbonate, and phosphate on the uranium(VI) sorption behavior onto bentonite. Radiochimica Acta,96, 359–366.
Belli, K. M., DiChristina, T. J., Van Cappellen, P., & Taillefert, M. (2015). Effect of aqueous uranyl speciation on the kinetics of microbial uranium reduction. Geochimica et Cosmichimica Acta,157, 109–124.
Bernhard, G., Geipel, G., Reich, T., Brendler, V., Amayri, S., & Nitsche, H. (2001). Uranyl(VI) carbonate complex formation: Validation of the Ca2UO2(CO3)3(aq.) species. Radiochimica Acta,89, 511–518.
Braet, F., De Zanger, R., & Wisse, E. (1997). Drying cells for SEM, AFM and TEM by hexamethyldisilazane: a study on hepatic endothelial cells. Journal of Microscopy,186(1), 84–87.
Claessens, J., van Lith, Y., Laverman, A. M., & Van Cappellen, P. (2006). Acid-base activity of live bacteria: Implications for quantifying cell wall charge. Geochimica et Cosmochimica Acta,70(2), 267–276.
Donlan, R. M. (2002). Biofilms: Microbial life on surfaces. Emerging Infectious Diseases,8, 881–890.
Ejnik, J. W., Hamilton, M. M., Adams, P. R., & Carmichael, A. J. (2000). Optimal sample preparation conditions for the determination of uranium in biological samples by kinetic phosphorescence analysis (KPA). Journal of Pharmaceutical and Biomedical Analysis,24(2), 227–235.
Gudavalli, R. K. P., Katsenovich, Y. P., Wellman, D. M., Idarraga, M., Lagos, L. E., & Tansel, B. (2013). Comparison of the kinetic rate law parameters for the dissolution of natural and synthetic autunite in the presence of aqueous bicarbonate ions. Chemical Geology,351, 299–309.
Hazrin-Chong, N. H., & Manefield, M. (2012). An alternative SEM drying method using hexamethyldisilazane (HMDS) for microbial cell attachment studies on sub-bituminous coal. Journal of Microbiological Methods,90(2), 96–99.
Katsenovich, Y., Carvajal, D., Guduru, R., Lagos, L., & Li, C.-Z. (2013). Assessment of the resistance to uranium(VI) exposure by Arthrobacter sp. isolated from hanford site soil. Geomicrobiology Journal,30(2), 120–130.
Langmuir, D. (1978). Uranium solution-mineral equilibria at low temperatures with application to sedimentary ore deposits. Geochimica et Cosmochimica Acta,42, 547–569.
Lin, H., Bennett, G. N., & San, K.-Y. (2005). Chemostat culture characterization of Escherichia coli mutant strains metabolically engineered for aerobic succinate production: A study of the modified metabolic network based on metabolite profile, enzyme activity, and gene expression profile. Metabolic Engineering,7(5–6), 337–352.
Lin, X., Kennedy, D., Peacock, A., McKinley, J., Resch, C. T., Fredrickson, J., et al. (2012). Distribution of microbial biomass and potential for anaerobic respiration in hanford site 300 area subsurface sediment. Applied and Environmental Microbiology,78(3), 759–767.
Marshall, M., Plymale, A., Kennedy, D., Shi, L., Wang, Z., Reed, S., et al. (2008). Hydrogenase- and outer membrane c-type cytochrome-facilitated reduction of technetium(VII) by Shewanella oneidensis MR-1. Environmental Microbiology,10(1), 125–136.
McLean, J. S., Pinchuk, G. E., Geydebrekht, O. V., Bilskis, C. L., Zakrajsek, B. A., Hill, E. A., et al. (2008). Oxygen-dependent autoaggregation in Shewanella oneidensis MR-1. Environmental Microbiology,10(7), 1861–1876.
Meshulam-Simon, G., Behrens, S., Choo, A. D., & Spormann, A. M. (2007). Hydrogen metabolism in Shewanella oneidensis MR-1. Applied and Environmental Microbiology,73(4), 1153–1165.
Pinchuk, G. E., Ammons, C., Culley, D. E., Li, S.-M. W., McLean, J. S., Romine, M. F., et al. (2008). Utilization of DNA as a sole source of phosphorus, carbon, and energy by Shewanella spp.: Ecological and physiological implications for dissimilatory metal reduction. Applied and Environmental Microbiology,74(4), 1198–1208.
Pinchuk, G. E., Hill, E. A., Geydebrekht, O. V., De Ingeniis, J., Zhang, X., Osterman, A., et al. (2010). Constraint-based model of Shewanella oneidensis MR-1 metabolism: A tool for data analysis and hypothesis generation. PLoS Computational Biology,6(6), e1000822.
Pinchuk, G. E., Geydebrekht, O. V., Hill, E. A., Reed, J. L., Konopka, A. E., Beliaev, A. S., et al. (2011). Pyruvate and lactate metabolism by Shewanella oneidensis MR-1 under fermentation, oxygen limitation, and fumarate respiration conditions. Applied and Environmental Microbiology,77(23), 8234–8240.
Sánchez, A. M., Bennett, G. N., & San, K.-Y. (2005). Novel pathway engineering design of the anaerobic central metabolic pathway in Escherichia coli to increase succinate yield and productivity. Metabolic Engineering,7(3), 229–239.
Sheng, L., & Fein, J. B. (2013). Uranium adsorption by Shewanella oneidensis MR-1 as a function of dissolved inorganic carbon concentration. Chemical Geology,358, 15–22.
Sheng, L., & Fein, J. B. (2014). Uranium reduction by Shewanella oneidensis MR-1 as a function of NaHCO3 concentration: Surface complexation control of reduction kinetics. Environmental Science & Technology,48(7), 3768–3775.
Smeaton, C. M., Weisener, C. G., Burns, P. C., Fryer, B. J., & Fowle, D. A. (2008). Bacterially enhanced dissolution of meta-autunite. American Mineralogist,93, 1858–1864.
Tang, Y. J., Laidlaw, D., Gani, K., & Keasling, J. D. (2006). Evaluation of the effects of various culture conditions on Cr(VI) reduction by Shewanella oneidensis MR-1 in a novel high-throughput mini-bioreactor. Biotechnology and Bioengineering,95(1), 176–184.
US EPA. (2000). Report 66 FR 37617. Part IV. National primary drinking water regulations (Vol. 65, pp. 37617–37631).
Wellman, D. M., Gunderson, K. M., Icenhower, J. P., & Forrester, S. W. (2007). Dissolution kinetics of synthetic and natural meta-autunite minerals, X3−n(n)+ [(UO2)(PO4)]2 · xH2O, under acidic conditions. Geochemistry, Geophysics, Geosystems,8(11), 1–16.
Wu, C., Cheng, Y.-Y., Yin, H., Song, X.-N., Li, W.-W., Zhou, X.-X., et al. (2013). Oxygen promotes biofilm formation of Shewanella putrefaciens CN32 through a diguanylate cyclase and an adhesin. Scientific Reports,3(1945), 1–7.
Zachara, J. M., Davis, J. A., McKinley, J. P., Wellman, D. M., Liu, C., Qafoku, N., et al. (2005). Uranium geochemistry in vadose zone and aquifer sediments from the 300 area uranium plume. Richland, WA: Pacific Northwest National Laboratory.
Zachara, J. M., Liu, C., Brown, C., Kelly, S., Christensen, J., McKinley, J., Davis, J. A., Serne, J., Dresel, E., & Um, W. (2007). A site-wide perspective on Uranium geochemistry at the hanford site. Richland, WA: PNNL-17031.
Acknowledgements
Funding for this research was provided by the US Department of Energy Office of Environmental Management under cooperative agreement DE-EM0000598. The authors also acknowledge Thomas Beasley at FIU FCAEM for his assistance with the SEM/EDS analysis.
Author information
Authors and Affiliations
Corresponding author
Additional information
Publisher's Note
Springer Nature remains neutral with regard to jurisdictional claims in published maps and institutional affiliations.
Electronic supplementary material
Below is the link to the electronic supplementary material.
Rights and permissions
About this article
Cite this article
Anagnostopoulos, V., Katsenovich, Y., Lee, B. et al. Biotic dissolution of autunite under anaerobic conditions: effect of bicarbonates and Shewanella oneidensis MR1 microbial activity. Environ Geochem Health 42, 2547–2556 (2020). https://doi.org/10.1007/s10653-019-00480-7
Received:
Accepted:
Published:
Issue Date:
DOI: https://doi.org/10.1007/s10653-019-00480-7


