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Title: Combined Effects of Fe(III)-Bearing Clay Minerals and Organic Ligands on U(VI) Bioreduction and U(IV) Speciation

Abstract

Reduction of U(VI) to U(IV) drastically reduces its solubility and has been proposed as a method for remediation of uranium contamination. However, much is still unknown about the kinetics, mechanisms, and products of U(VI) bioreduction in complex systems. In this work, U(VI) bioreduction experiments were conducted with Shewanella putrefaciens strain CN32 in the presence of clay minerals and two organic ligands: citrate and EDTA. In reactors with U and Fe(III)-clay minerals, the rate of U(VI) bioreduction was enhanced due to the presence of ligands, likely because soluble Fe3+- and Fe2+-ligand complexes served as electron shuttles. In the presence of citrate, bioreduced U(IV) formed a soluble U(IV)-citrate complex in experiments with either Fe-rich or Fe-poor clay mineral. In the presence of EDTA, U(IV) occurred as a soluble U(IV)-EDTA complex in Fe-poor montmorillonite experiments. However, U(IV) remained associated with the solid phase in Fe-rich nontronite experiments through the formation of a ternary U(IV)-EDTA-surface complex, as suggested by the EXAFS analysis. Our study indicates that organic ligands and Fe(III)-bearing clays can significantly affect the microbial reduction of U(VI) and the stability of the resulting U(IV) phase.

Authors:
 [1];  [2];  [2];  [3];  [3]; ORCiD logo [3];  [4];  [5];  [6]; ORCiD logo [2];  [7]
  1. China Univ. of Geosciences, Beijing (China); Chinese Academy of Sciences (CAS), Beijing (China)
  2. China Univ. of Geosciences, Beijing (China)
  3. Argonne National Lab. (ANL), Argonne, IL (United States)
  4. Ecole Polytechnique Federale Lausanne (Switzerland)
  5. Fudan Univ., Shanghai (China)
  6. Chinese Academy of Sciences (CAS), Beijing (China)
  7. Argonne National Lab. (ANL), Argonne, IL (United States); Bulgarian Academy of Sciences, Sofia (Bulgaria)
Publication Date:
Research Org.:
Argonne National Lab. (ANL), Argonne, IL (United States)
Sponsoring Org.:
USDOE Office of Science (SC), Biological and Environmental Research (BER); National Natural Science Foundation of China (NSFC)
OSTI Identifier:
1798054
Grant/Contract Number:  
AC02-06CH11357; 41630103
Resource Type:
Accepted Manuscript
Journal Name:
Environmental Science and Technology
Additional Journal Information:
Journal Volume: 55; Journal Issue: 9; Journal ID: ISSN 0013-936X
Publisher:
American Chemical Society (ACS)
Country of Publication:
United States
Language:
English
Subject:
37 INORGANIC, ORGANIC, PHYSICAL, AND ANALYTICAL CHEMISTRY; redox reactions; uranium; ligands; minerals; clay

Citation Formats

Zhang, Limin, Chen, Yu, Xia, Qingyin, Kemner, Kenneth M., Shen, Yanghao, O’Loughlin, Edward J., Pan, Zezhen, Wang, Qihuang, Huang, Ying, Dong, Hailiang, and Boyanov, Maxim I. Combined Effects of Fe(III)-Bearing Clay Minerals and Organic Ligands on U(VI) Bioreduction and U(IV) Speciation. United States: N. p., 2021. Web. doi:10.1021/acs.est.0c08645.
Zhang, Limin, Chen, Yu, Xia, Qingyin, Kemner, Kenneth M., Shen, Yanghao, O’Loughlin, Edward J., Pan, Zezhen, Wang, Qihuang, Huang, Ying, Dong, Hailiang, & Boyanov, Maxim I. Combined Effects of Fe(III)-Bearing Clay Minerals and Organic Ligands on U(VI) Bioreduction and U(IV) Speciation. United States. https://doi.org/10.1021/acs.est.0c08645
Zhang, Limin, Chen, Yu, Xia, Qingyin, Kemner, Kenneth M., Shen, Yanghao, O’Loughlin, Edward J., Pan, Zezhen, Wang, Qihuang, Huang, Ying, Dong, Hailiang, and Boyanov, Maxim I. Tue . "Combined Effects of Fe(III)-Bearing Clay Minerals and Organic Ligands on U(VI) Bioreduction and U(IV) Speciation". United States. https://doi.org/10.1021/acs.est.0c08645. https://www.osti.gov/servlets/purl/1798054.
@article{osti_1798054,
title = {Combined Effects of Fe(III)-Bearing Clay Minerals and Organic Ligands on U(VI) Bioreduction and U(IV) Speciation},
author = {Zhang, Limin and Chen, Yu and Xia, Qingyin and Kemner, Kenneth M. and Shen, Yanghao and O’Loughlin, Edward J. and Pan, Zezhen and Wang, Qihuang and Huang, Ying and Dong, Hailiang and Boyanov, Maxim I.},
abstractNote = {Reduction of U(VI) to U(IV) drastically reduces its solubility and has been proposed as a method for remediation of uranium contamination. However, much is still unknown about the kinetics, mechanisms, and products of U(VI) bioreduction in complex systems. In this work, U(VI) bioreduction experiments were conducted with Shewanella putrefaciens strain CN32 in the presence of clay minerals and two organic ligands: citrate and EDTA. In reactors with U and Fe(III)-clay minerals, the rate of U(VI) bioreduction was enhanced due to the presence of ligands, likely because soluble Fe3+- and Fe2+-ligand complexes served as electron shuttles. In the presence of citrate, bioreduced U(IV) formed a soluble U(IV)-citrate complex in experiments with either Fe-rich or Fe-poor clay mineral. In the presence of EDTA, U(IV) occurred as a soluble U(IV)-EDTA complex in Fe-poor montmorillonite experiments. However, U(IV) remained associated with the solid phase in Fe-rich nontronite experiments through the formation of a ternary U(IV)-EDTA-surface complex, as suggested by the EXAFS analysis. Our study indicates that organic ligands and Fe(III)-bearing clays can significantly affect the microbial reduction of U(VI) and the stability of the resulting U(IV) phase.},
doi = {10.1021/acs.est.0c08645},
journal = {Environmental Science and Technology},
number = 9,
volume = 55,
place = {United States},
year = {Tue Apr 06 00:00:00 EDT 2021},
month = {Tue Apr 06 00:00:00 EDT 2021}
}

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