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Bacterial production of vanadium ferrite spinel (Fe,V)3O4 nanoparticles

Published online by Cambridge University Press:  01 July 2020

Victoria S Coker ,
Gerrit van der Laan ,
Neil D Telling ,
Jonathan R Lloyd ,
James M Byrne ,
Elke Arenholz  and
Richard AD Pattrick Open the ORCID record for Richard AD Pattrick [Opens in a new window]
Victoria S Coker*
Affiliation:
School of Earth & Environmental Sciences, University of Manchester, ManchesterM13 9PL, UK
Gerrit van der Laan
Affiliation:
School of Earth & Environmental Sciences, University of Manchester, ManchesterM13 9PL, UK Magnetic Spectroscopy Group, Diamond Light Source, Didcot, OxfordshireOX11 0DE, UK
Neil D Telling
Affiliation:
Institute for Science and Technology in Medicine, Keele University, Thornburrow Drive, Hartshill, Stoke-on-TrentST4 7QB, UK
Jonathan R Lloyd
Affiliation:
School of Earth & Environmental Sciences, University of Manchester, ManchesterM13 9PL, UK
James M Byrne
Affiliation:
School of Earth Sciences, Wills Memorial Building, Queens Road, Clifton, BristolBS8 1R, UK
Elke Arenholz
Affiliation:
Advanced Light Source, Lawrence Berkeley National Laboratory, Berkeley, CA 94720, USA
Richard AD Pattrick
Affiliation:
School of Earth & Environmental Sciences, University of Manchester, ManchesterM13 9PL, UK
*
*Author for correspondence: Victoria S Coker, Email: vicky.coker@manchester.ac.uk
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Abstract

Biogenic nanoscale vanadium magnetite is produced by converting V(V)-bearing ferrihydrites through reductive transformation using the metal-reducing bacterium Geobacter sulfurreducens. With increasing vanadium in the ferrihydrite, the amount of V-doped magnetite produced decreased due to V-toxicity which interrupted the reduction pathway ferrihydrite–magnetite, resulting in siderite or goethite formation. Fe L2,3 and V L2,3 X-ray absorption spectra and data from X-ray magnetic circular dichroism analysis revealed the magnetite to contain the V in the Fe(III) Oh site, predominately as V(III) but always with a component of V(VI), present a consistent V(IV)/V(III) ratio in the range 0.28 to 0.33. The bacteriogenic production of V-doped magnetite nanoparticles from V-doped ferrihydrite is confirmed and the work reveals that microbial reduction of contaminant V(V) to V(III)/V(IV) in the environment will occur below the Fe-redox boundary where it will be immobilised in biomagnetite nanoparticles.

Keywords

vanadiumbiomagnetiteGeobacter sulfurreducensL2,3-edge XASXMCD
Type
Article
Information
Mineralogical Magazine , Volume 84 , Issue 4 , August 2020 , pp. 554 - 562
Copyright
Copyright © The Mineralogical Society of Great Britain and Ireland, 2020

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Footnotes

†

Current address: CHESS/Wilson Lab, 161 Synchrotron Drive, Ithica, NY 14853, 607-255-7163, USA.

Associate Editor: Janice Kenney

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