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Marshall, Timothy A., Morris, Katherine, Law, Gareth T.W., W. Mosselmans, J. Frederick, Bots, Pieter, Roberts, Hannah, Shaw, Samuel (2015) Uranium fate during crystallization of magnetite from ferrihydrite in conditions relevant to the disposal of radioactive waste. Mineralogical Magazine, 79 (6) 1265-1274 doi:10.1180/minmag.2015.079.6.02

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Reference TypeJournal (article/letter/editorial)
TitleUranium fate during crystallization of magnetite from ferrihydrite in conditions relevant to the disposal of radioactive waste
JournalMineralogical Magazine
AuthorsMarshall, Timothy A.Author
Morris, KatherineAuthor
Law, Gareth T.W.Author
W. Mosselmans, J. FrederickAuthor
Bots, PieterAuthor
Roberts, HannahAuthor
Shaw, SamuelAuthor
Year2015 (November)Volume79
Issue6
PublisherMineralogical Society
DOIdoi:10.1180/minmag.2015.079.6.02Search in ResearchGate
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Mindat Ref. ID244704Long-form Identifiermindat:1:5:244704:3
GUID0
Full ReferenceMarshall, Timothy A., Morris, Katherine, Law, Gareth T.W., W. Mosselmans, J. Frederick, Bots, Pieter, Roberts, Hannah, Shaw, Samuel (2015) Uranium fate during crystallization of magnetite from ferrihydrite in conditions relevant to the disposal of radioactive waste. Mineralogical Magazine, 79 (6) 1265-1274 doi:10.1180/minmag.2015.079.6.02
Plain TextMarshall, Timothy A., Morris, Katherine, Law, Gareth T.W., W. Mosselmans, J. Frederick, Bots, Pieter, Roberts, Hannah, Shaw, Samuel (2015) Uranium fate during crystallization of magnetite from ferrihydrite in conditions relevant to the disposal of radioactive waste. Mineralogical Magazine, 79 (6) 1265-1274 doi:10.1180/minmag.2015.079.6.02
Abstract/NotesAbstractUranium incorporation into magnetite and its behaviour during subsequent oxidation has been investigated at high pH to determine the uranium retention mechanism(s) on formation and oxidative perturbation of magnetite in systems relevant to radioactive waste disposal. Ferrihydrite was exposed to U(VI)aq containing cement leachates (pH 10.5–13.1) and crystallization of magnetite was induced via addition of Fe(II)aq. A combination of XRD, chemical extraction and XAS techniques provided direct evidence that U(VI) was reduced and incorporated into the magnetite structure, possibly as U(V), with a significant fraction recalcitrant to oxidative remobilization. Immobilization of U(VI) by reduction and incorporation into magnetite at high pH, and with significant stability upon reoxidation, has clear and important implications for limiting uranium migration in geological disposal of radioactive wastes.


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