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Oxidation state and accumulation of uranium in hydrothermal REE minerals
Journal article   Open access   Peer reviewed

Oxidation state and accumulation of uranium in hydrothermal REE minerals

Tobias G. Bamforth, Barbara Etschmann, Joël Brugger, Fang Xia, Udo Becker, Ignacio González-Álvarez, Maryam O. Abdus-Salam, Paul Guagliardo, Andrew Langendam and Jeremy Wykes
Journal of hazardous materials, Vol.500, 140549
2025
PMID: 41289669
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Published7.09 MBDownloadView
CC BY V4.0 Open Access

Abstract

Critical metals Hydrothermal Rare-earth elements Uranium XAS
To meet growing demand for renewable technologies that will mitigate climate change, the world requires a sustainable supply of rare earth elements (REEs). Uranium (U) is a common impurity in REE ores that causes socio-environmental challenges during mining and processing. Sustainable REE extraction thus relies on targeting ores with little U, which necessitates an understanding of the conditions under which U accumulates in REE minerals. Here we show that rhabdophane and monazite – two common hydrothermal REE ore minerals – can incorporate U in its oxidised U(V) and U(VI) forms. Contrary to current understanding, this demonstrates that reducing conditions are not required for U to accumulate in hydrothermal REE minerals. Rather, the higher availabilities of U in oxidising and/or Ce-poor fluids can also drive significant accumulation. Four redox scenarios are consequently theorized for predicting the capacity of aqueous-fluid-affected REE ores for accumulating U. This framework may assist in evaluating the environmental sustainability of various REE deposits, thereby guiding decisions on exploration and extraction. Results also confirm the capacity of both minerals to immobilise fluid-soluble U(VI) during formation, with implications for their application as mineral barriers in U-contaminated systems. [Display omitted]

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