Beam-induced oxidation of monomeric U(IV) species

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Abstract

Uranium L III-edge X-ray absorption spectroscopy is often used to probe the oxidation state and coordination of uranium in environmental samples, and micrometre-sized beams can be used to spatially map the distribution of uranium relative to other elements. Here a variety of uranium-containing environmental samples are analyzed at both microbeam and larger beam sizes to determine whether reoxidation of U(IV) occurred. Monomeric U(IV), a recently discovered product of U(VI) reduction by microbes and certain iron-bearing minerals at uranium-contaminated field sites, was found to be reoxidized during microbeam (3 m 2 m) analysis of biomass and sediments containing the species but not at larger beam sizes. Thus, care must be taken when using X-ray microprobes to analyze samples containing monomeric U(IV). © 2013 International Union of Crystallography Printed in Singapore-all rights reserved.

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Alessi, D. S., Uster, B., Borca, C. N., Grolimund, D., & Bernier-Latmani, R. (2013). Beam-induced oxidation of monomeric U(IV) species. Journal of Synchrotron Radiation, 20(1), 197–199. https://doi.org/10.1107/S0909049512041763

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