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dc.contributor.authorBuchanan, DM
dc.contributor.authorNewsome, L
dc.contributor.authorLloyd, JR
dc.contributor.authorKazemian, M
dc.contributor.authorKaulich, B
dc.contributor.authorAraki, T
dc.contributor.authorBagshaw, H
dc.contributor.authorWaters, J
dc.contributor.authorvan der Laan, G
dc.contributor.authorN’Diaye, A
dc.contributor.authorCoker, VS
dc.date.accessioned2022-08-31T09:36:45Z
dc.date.issued2022-05-03
dc.date.updated2022-08-30T14:23:10Z
dc.description.abstractCobalt is an essential element for life and plays a crucial role in supporting the drive to clean energy, due to its importance in rechargeable batteries. Co is often associated with Fe in the environment, but the fate of Co in Fe-rich biogeochemically-active environments is poorly understood. To address this, synchrotron-based scanning X-ray microscopy (SXM) was used investigate the behaviour of cobalt at the nanoscale in Co-Fe(III)-oxyhydroxides undergoing microbial reduction. SXM can assess spatial changes in metal speciation and organic compounds helping to elucidate the electron transfer processes occurring at the cell-mineral interface and inform on the fate of cobalt in redox horizons. G. sulfurreducens was used to reduce synthetic Co-ferrihydrite as an analogue of natural cobalt-iron-oxides. Magnetite [Fe(II)/Fe(III)3O4] production was confirmed by powder X-ray diffraction (XRD), SXM and X-ray magnetic circular dichroism (XMCD) data, where best fits of the latter suggested Co-bearing magnetite. Macro-scale XAS techniques suggested Co(III) reduction occurred and complementary SXM at the nanoscale, coupled with imaging, found localised biogenic Co(III) reduction at the cell-mineral interface via direct contact with outer membrane cytochromes. No discernible localised changes in Fe speciation were detected in the reordered cobalt-iron-oxides that were formed and at the end point of the experiment only 11% Co and 1.5% Fe had been solubilised. The solid phase retention, alongside the highly localised and preferential cobalt bioreduction observed at the nanoscale is consistent with retention of Co in redox zones. This work improves our fundamental molecular-scale understanding of the fate of Co in complex environmental systems and supports the development of biogenic Co-doped magnetite for industrial applications from drug delivery systems to magnetic recording media.en_GB
dc.description.sponsorshipNatural Environment Research Councilen_GB
dc.description.sponsorshipEPSRC studentshipen_GB
dc.format.extent799328-
dc.identifier.citationVol. 10, article 799328en_GB
dc.identifier.doihttps://doi.org/10.3389/feart.2022.799328
dc.identifier.grantnumberNE/M011518/1en_GB
dc.identifier.grantnumber1919159en_GB
dc.identifier.urihttp://hdl.handle.net/10871/130617
dc.identifierORCID: 0000-0002-0283-3001 (Newsome, Laura)
dc.identifierScopusID: 37862010700 (Newsome, Laura)
dc.language.isoenen_GB
dc.publisherFrontiers Mediaen_GB
dc.rightsCopyright © 2022 Buchanan, Newsome, Lloyd, Kazemian, Kaulich, Araki, Bagshaw, Waters, van der Laan, N’Diaye and Coker. This is an open-access article distributed under the terms of the Creative Commons Attribution License (CC BY). The use, distribution or reproduction in other forums is permitted, provided the original author(s) and the copyright owner(s) are credited and that the original publication in this journal is cited, in accordance with accepted academic practice. No use, distribution or reproduction is permitted which does not comply with these terms.en_GB
dc.subjectcobalten_GB
dc.subjectferrihydriteen_GB
dc.subjectpolymetallic nodulesen_GB
dc.subjectmagnetiteen_GB
dc.subjectscanning transmission X-ray microscopyen_GB
dc.titleInvestigating nanoscale electron transfer processes at the cell-mineral Interface in cobalt-doped ferrihydrite using Geobacter sulfurreducens: A multi-technique approachen_GB
dc.typeArticleen_GB
dc.date.available2022-08-31T09:36:45Z
dc.identifier.issn2296-6463
exeter.article-numberARTN 799328
dc.descriptionThis is the final version. Available from Frontiers Media via the DOI in this record.en_GB
dc.descriptionDATA AVAILABILITY STATEMENT: The raw data supporting the conclusion of this article will be made available by the authors, without undue reservation.en_GB
dc.identifier.journalFrontiers in Earth Scienceen_GB
dc.relation.ispartofFrontiers in Earth Science, 10
dc.rights.urihttps://creativecommons.org/licenses/by/4.0/en_GB
dcterms.dateAccepted2022-03-22
rioxxterms.versionVoRen_GB
rioxxterms.licenseref.startdate2022-05-03
rioxxterms.typeJournal Article/Reviewen_GB
refterms.dateFCD2022-08-31T09:33:41Z
refterms.versionFCDVoR
refterms.dateFOA2022-08-31T09:36:50Z
refterms.panelBen_GB
refterms.dateFirstOnline2022-05-03


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Copyright © 2022 Buchanan, Newsome, Lloyd, Kazemian, Kaulich, Araki, Bagshaw,
Waters, van der Laan, N’Diaye and Coker. This is an open-access article distributed
under the terms of the Creative Commons Attribution License (CC BY). The use,
distribution or reproduction in other forums is permitted, provided the original
author(s) and the copyright owner(s) are credited and that the original publication
in this journal is cited, in accordance with accepted academic practice. No use,
distribution or reproduction is permitted which does not comply with these terms.
Except where otherwise noted, this item's licence is described as Copyright © 2022 Buchanan, Newsome, Lloyd, Kazemian, Kaulich, Araki, Bagshaw, Waters, van der Laan, N’Diaye and Coker. This is an open-access article distributed under the terms of the Creative Commons Attribution License (CC BY). The use, distribution or reproduction in other forums is permitted, provided the original author(s) and the copyright owner(s) are credited and that the original publication in this journal is cited, in accordance with accepted academic practice. No use, distribution or reproduction is permitted which does not comply with these terms.