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Uranium transport in acidic brines under reducing conditions.


ABSTRACT: The behavior of uranium in environments, ranging from those of natural systems responsible for the formation of uranium deposits to those of nuclear reactors providing 11% of the world's electricity, is governed by processes involving high-temperature aqueous solutions. It has been well documented that uranium is mobile in aqueous solutions in its oxidized, U6+ state, whereas in its reduced, U4+ state, uranium has been assumed to be immobile. Here, we present experimental evidence from high temperature (>100?°C) acidic brines that invalidates this assumption. Our experiments have identified a new uranium chloride species (UCl4°) that is more stable under reducing than oxidized conditions. These results indicate that uranium is mobile under reducing conditions and necessitate a re-evaluation of the mobility of uranium, particularly in ore deposit models involving this metal. Regardless of the scenario considered, reducing conditions can no longer be considered a guarantee of uranium immobility.

SUBMITTER: Timofeev A 

PROVIDER: S-EPMC5902481 | biostudies-literature | 2018 Apr

REPOSITORIES: biostudies-literature

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Uranium transport in acidic brines under reducing conditions.

Timofeev Alexander A   Migdisov Artaches A AA   Williams-Jones Anthony E AE   Roback Robert R   Nelson Andrew T AT   Xu Hongwu H  

Nature communications 20180416 1


The behavior of uranium in environments, ranging from those of natural systems responsible for the formation of uranium deposits to those of nuclear reactors providing 11% of the world's electricity, is governed by processes involving high-temperature aqueous solutions. It has been well documented that uranium is mobile in aqueous solutions in its oxidized, U<sup>6+</sup> state, whereas in its reduced, U<sup>4+</sup> state, uranium has been assumed to be immobile. Here, we present experimental e  ...[more]

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