Uranium reduction on magnetite: Probing for pentavalent uranium using electrochemical methods. (1st May 2015)

• Record Type: Journal Article
• Authors: Yuan, Ke; Renock, Devon; Ewing, Rodney C.; Becker, Udo
• Is Part Of: Geochimica et cosmochimica acta. Volume 156(2015:May 01)
• Page Start: 194
• Page End: 206
• Publication Date: 2015-05-01
• Subjects: Geochemistry -- Periodicals; Meteorites -- Periodicals; Géochimie -- Périodiques; Météorites -- Périodiques; Geochemie; Astrochemie; Electronic journals; 551.905
• DOI: 10.1016/j.gca.2015.02.014
• Languages: English
• ISSNs: 0016-7037

Abstract

Abstract: Pentavalent uranium is generally treated as an unstable intermediate when uranyl, U(VI)O2 2+, is reduced to U 4+ . However, mineral surfaces have been shown to stabilize pentavalent uranium, thus hindering further reduction (Ilton et al., 2005, 2010). The subject of this study is to identify the kinetic pathways that lead to U(V)O2 + being a metastable species. Electrochemical methods provide an in situ approach for the investigation of the intermediate reaction of U(V)O2 + on the surfaces of magnetite. Redox reactions of uranyl ions on particulate (∼3 μm) and bulk magnetite surfaces were investigated using cyclic voltammetry and potential step chronoamperometry using cavity microelectrodes and bulk (planar) mineral electrodes. The estimated redox potentials are consistent with the standard redox potential of UO2 2+ /UO2 +, indicating UO2 2+ is first reduced to UO2 + on the surfaces of both powder and bulk magnetite. The one-electron reduction of UO2 2+ to UO2 + was further confirmed by directly measuring the number of electrons transferred during the reduction process on the bulk magnetite electrode. Based on the charge conservation analysis and the positive correlation between the pH and the peak current for the UO2 + transformation to UO2 2+, the peak corresponding to the oxidation of U 4+ to UO2 2+ was assigned in the voltammograms of particulate magnetite. The presence of U 4+ indicates that the disproportionation of UO2 + (2U(V) ↔ U(IV) + U(VI)) is occurring on the surface of particulate magnetite within the timeframe of the experiment. The lack of a peak for U 4+ in voltammograms for bulk magnetite suggests that the rate of the UO2 + disproportionation reaction is slower on bulk magnetite than that on particulate magnetite. The catalytic property of particulate magnetite surfaces on the disproportionation reaction is explained by its ability to adsorb and desorb protons, which could facilitate the proton-coupled disproportionation reaction of UO2 + . This increased catalytic activity and related adsorption and desorption kinetics of protons may be related to the increased number of under-coordinated surface sites near step edges on the magnetite powder.