Reduction of Vanadium(V) by Iron(II)-Bearing Minerals

O’Loughlin, Edward J.; Boyanov, Maxim I.; Kemner, Kenneth M.

doi:10.3390/min11030316

Reduction of Vanadium(V) by Iron(II)-Bearing Minerals

Journal Article · Thu Mar 18 00:00:00 EDT 2021 · Minerals

DOI:https://doi.org/10.3390/min11030316· OSTI ID:1798316

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Argonne National Lab. (ANL), Argonne, IL (United States)
Argonne National Lab. (ANL), Argonne, IL (United States); Bulgarian Academy of Sciences, Sofia (Bulgaria)

Fe(II)-bearing minerals (magnetite, siderite, green rust, etc.) are common products of microbial Fe(III) reduction, and they provide a reservoir of reducing capacity in many subsurface environments that may contribute to the reduction of redox active elements such as vanadium; which can exist as V(V), V(IV), and V(III) under conditions typical of near-surface aquatic and terrestrial environments. To better understand the redox behavior of V under ferrugenic/sulfidogenic conditions, we examined the interactions of V(V) (1 mM) in aqueous suspensions containing 50 mM Fe(II) as magnetite, siderite, vivianite, green rust, or mackinawite, using X-ray absorption spectroscopy at the V K-edge to determine the valence state of V. Two additional systems of increased complexity were also examined, containing either 60 mM Fe(II) as biogenic green rust (BioGR) or 40 mM Fe(II) as a mixture of biogenic siderite, mackinawite, and magnetite (BioSMM). Within 48 h, total solution-phase V concentrations decreased to <20 µM in all but the vivianite and the biogenic BiSMM systems; however, >99.5% of V was removed from solution in the BioSMM and vivianite systems within 7 and 20 months, respectively. The most rapid reduction was observed in the mackinawite system, where V(V) was reduced to V(III) within 48 h. Complete reduction of V(V) to V(III) occurred within 4 months in the green rust system, 7 months in the siderite system, and 20 months in the BioGR system. Vanadium(V) was only partially reduced in the magnetite, vivianite, and BioSMM systems, where within 7 months the average V valence state stabilized at 3.7, 3.7, and 3.4, respectively. The reduction of V(V) in soils and sediments has been largely attributed to microbial activity, presumably involving direct enzymatic reduction of V(V); however the reduction of V(V) by Fe(II)-bearing minerals suggests that abiotic or coupled biotic–abiotic processes may also play a critical role in V redox chemistry, and thus need to be considered in modeling the global biogeochemical cycling of V.

View Accepted Manuscript (DOE)

Research Organization:: Argonne National Laboratory (ANL), Argonne, IL (United States)

Sponsoring Organization:: USDOE Office of Science (SC), Biological and Environmental Research (BER)

Grant/Contract Number:: AC02-06CH11357

OSTI ID:: 1798316

Journal Information:: Minerals, Journal Name: Minerals Journal Issue: 3 Vol. 11; ISSN 2075-163X

Publisher:: MDPICopyright Statement

Country of Publication:: United States

Language:: English

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BIOGEOCHEMICAL AND ENVIRONMENTAL FACTORS IN Fe BIOMINERALIZATION: MAGNETITE AND SIDERITE FORMATION Roh, Y.; Zhang, C. -L.; Vali, H. Clays and Clay Minerals, Vol. 51, Issue 1 https://doi.org/10.1346/CCMN.2003.510110	journal	February 2003
Orthominasragrite, v4+o (So4) (H2o)5, a new Mineral Species from Temple Mountain, Emery County, Utah, U.S.A. Hawthorne, F. C.; Schindler, M.; Grice, J. D. The Canadian Mineralogist, Vol. 39, Issue 5 https://doi.org/10.2113/gscanmin.39.5.1325	journal	October 2001
Schubnelite, [Fe (super 3+) (V (super 5+) O ₄ )(H ₂ O)], a novel heteropolyhedral framework mineral Schindler, Michael; Hawthorne, Frank C. American Mineralogist, Vol. 84, Issue 4 https://doi.org/10.2138/am-1999-0419	journal	April 1999
The reduction of aqueous Au ³⁺ by sulfide minerals and green rust phases Heasman, D. M.; Sherman, D. M.; Ragnarsdottir, K. V. American Mineralogist, Vol. 88, Issue 5-6 https://doi.org/10.2138/am-2003-5-602	journal	May 2003
Ferrous hydroxy carbonate is a stable transformation product of biogenic magnetite Kukkadapu, R. K. American Mineralogist, Vol. 90, Issue 2-3 https://doi.org/10.2138/am.2005.1727	journal	February 2005
Reaction of Uranium(VI) with Green Rusts: Effect of Interlayer Anion Latta, Drew; Boyanov, Maxim; Kemner, Kenneth Current Inorganic Chemistry, Vol. 5, Issue 3 https://doi.org/10.2174/1877944105666150420235350	journal	July 2015
Vanadium Kelley, Karen D.; Scott, Clint; Polyak, Désirée E. USGS Numbered Series https://doi.org/10.3133/pp1802U	report	January 2017
Effects of Fe(III) Oxide Mineralogy and Phosphate on Fe(II) Secondary Mineral Formation during Microbial Iron Reduction O’Loughlin, Edward J.; Boyanov, Maxim I.; Gorski, Christopher A. Minerals, Vol. 11, Issue 2 https://doi.org/10.3390/min11020149	journal	January 2021
Electron Donor Utilization and Secondary Mineral Formation during the Bioreduction of Lepidocrocite by Shewanella putrefaciens CN32 O’Loughlin, Edward J.; Gorski, Christopher A.; Flynn, Theodore M. Minerals, Vol. 9, Issue 7 https://doi.org/10.3390/min9070434	journal	July 2019

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