Inhibitory effect of silicate on the Fe(II)-catalysed sequestration of U by Fe(III) oxides

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dc.contributor.authorBoland, DDen_AU
dc.contributor.authorCollins, RNen_AU
dc.contributor.authorPayne, TEen_AU
dc.contributor.authorWaite, TDen_AU
dc.date.accessioned2011-01-28T04:23:56Zen_AU
dc.date.available2011-01-28T04:23:56Zen_AU
dc.date.issued2010-06-17en_AU
dc.date.statistics2010-06-17en_AU
dc.description.abstractIt has recently been reported that the natural Fe (II)- catalysed transformation of Fe (III) minerals to more crystalline forms can result in the sequestration of uranium [1], thus potentially leading toward a solution to the universal and emotive problem of uranium contamination. While this process may reduce uranium migration, there is no clear knowledge of its viability in conditions which inhibit the transformation of iron oxides. Here we present XAS results of Fe (II)-catalysed transformations in systems containing 2-line ferrihydrite, silicate and uranium as U (VI). The chemical environment of both co-precipitated and adsorbed U (VI) bound by 2-line ferrihydrite was initiallyidentical, in both cases being associated with the iron oxides as a surface complex. Upon addition of aqueous Fe (II) in anoxic conditions, 2-line ferrihydrite with associated U (VI) transformed to goethite. Ab initio modelling of EXAFS data indicated that U (VI) associated with 2-line ferrihydrite was incorporated into the newly formed goethite mineral structure. In contrast, silicate-ferrihydrite only transformed to ferrihydrite with the associated U (VI) remaining in a form similar to its initial state. The adsorbed U (VI) did however become more resistant to reductive dissolution indicating at least a partial reduction in mobility. These results demonstrate that the Fe (II)-catalysed crystallisation of iron oxides may not always induce uranium reduction or immobilisation in relevant environmental conditions. The precise mechanism of the inhibitory effect of silicate, with a focus on how to control conditions to reduce this effect, must be resolved before this process may be considered a reliable means of preventing sub-surface uranium transport. © 2020 Elsevier B.V.en_AU
dc.identifier.citationBoland, D. D., Collins, R. N., Payne, T. E. & Waite, T. D. (2010). Inhibitory effect of silicate on the Fe(II)-catalysed sequestration of U by Fe(III) oxides. Presentation to the 20th Annual V.M. Goldschmidt Conference (Goldschmidt 2010) - "Earth, Energy and the Environment", 13th - 18th June 2010. Knoxville, Tennessee: Knoxville Convention Center. In Geochimica et Cosmochimica Acta, 74(12), A101. doi:10.1016/j.gca.2010.04.027en_AU
dc.identifier.conferenceenddate18 June 2010en_AU
dc.identifier.conferencename20th Annual V.M. Goldschmidt Conference (Goldschmidt 2010) - 'Earth, Energy and the Environment'en_AU
dc.identifier.conferenceplaceKnoxville, Tennesseeen_AU
dc.identifier.conferencestartdate13 June 2010en_AU
dc.identifier.govdoc3174en_AU
dc.identifier.issn0016-7037en_AU
dc.identifier.issue12en_AU
dc.identifier.journaltitleGeochimica et Cosmochimica Actaen_AU
dc.identifier.paginationA101en_AU
dc.identifier.urihttp://dx.doi.org/10.1016/j.gca.2010.04.027en_AU
dc.identifier.urihttp://apo.ansto.gov.au/dspace/handle/10238/2961en_AU
dc.identifier.volume74en_AU
dc.language.isoenen_AU
dc.publisherElsevier; Cambridge Publicationsen_AU
dc.subjectUraniumen_AU
dc.subjectIronen_AU
dc.subjectSilicate mineralsen_AU
dc.subjectCrystallizationen_AU
dc.subjectGoethiteen_AU
dc.subjectTransformationsen_AU
dc.titleInhibitory effect of silicate on the Fe(II)-catalysed sequestration of U by Fe(III) oxidesen_AU
dc.typeConference Presentationen_AU
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