Pentavalent Uranium Enriched Mineral Surface under Electrochemically Controlled Reducing EnvironmentsClick to copy article linkArticle link copied!
- Ke Yuan*Ke Yuan*Email: [email protected]. Phone: 865-576-7003.Chemical Sciences Division, Oak Ridge National Laboratory, Oak Ridge, Tennessee 37830, United StatesMore by Ke Yuan
- Mark R. AntonioMark R. AntonioChemical Sciences and Engineering Division, Argonne National Laboratory, Lemont, Illinois 60439, United StatesMore by Mark R. Antonio
- Eugene S. IltonEugene S. IltonPacific Northwest National Laboratory, Richland, Washington 99352, United StatesMore by Eugene S. Ilton
- Zhongrui LiZhongrui LiDepartment of Earth and Environmental Sciences, University of Michigan, Ann Arbor, Michigan 48109, United StatesMore by Zhongrui Li
- Udo BeckerUdo BeckerDepartment of Earth and Environmental Sciences, University of Michigan, Ann Arbor, Michigan 48109, United StatesMore by Udo Becker
Abstract
Redox reactions of uranium (U) in aqueous environments have important impacts on the mobility and isotopic fractionation of U in the geosphere. Pentavalent U as the cationic uranyl ion, UO2+, is rarely observed in naturally occurring samples because of its limited lifetime, but it may be an important intermediate state controlling the redox kinetics between hexavalent and tetravalent U. Increasing evidence has indicated that U(V) can be stabilized under laboratory conditions. Here, we showed that U(V) is the dominant species on the magnetite (Fe3O4) surface under reducing conditions controlled by electrochemical methods. Cyclic voltammetry reveals coupled redox peaks corresponding to the U(VI)O22+/U(V)O2+ one-electron redox reaction. Magnetite electrodes polarized at a series of potentials to reduce U(VI)O22+ were characterized by X-ray photoelectron spectroscopy (XPS), X-ray absorption spectroscopy (XAS), and Auger electron mapping. The results showed that up to twice the amount of U(V) to U(VI) was present on the magnetite surface. U(V) adopted a typical uranyl-type structure, and the U coverage on the magnetite surface increased with decreasing potentials. The formation of mixed-valence U(V)/U(VI) species on the surface of magnetite may hinder the U(V) disproportionation reaction, thereby eliminating the presence of tetravalent U. These results show that U(V) can exist over short time scales as the dominant U species on mineral surfaces under selected reducing conditions by the controlled polarization of a mineral electrode.
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