Biotic Fe(III) reduction of magnetite coupled to H2 oxidation: Implication for radioactive waste geological disposal
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Detrital magnetite carried in rivers 3.0- to 2.7-Ga ago would have dissolved at high pH2 via microbial reduction of Fe3+ to soluble Fe2+ using H2.
“Detrital magnetite carried in rivers 3.0- to 2.7-Ga ago would have dissolved at high pH2 via microbial reduction of Fe3+ to soluble Fe2+ using H2 (199), providing an upper limit of pH2 ≤ 10−2 bar (200).”
From The Archean atmosphere (2020) · cites this paper as [199]
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References 48 · Cited by 4
- Authors
- Schütz, M. K., Bildstein, O., Schlegel, M. L., & Libert, M.
- Affiliations
- Commissariat à l'Énergie Atomique et aux Énergies Alternatives (FR)
- Corresponding author
- Schütz, Marta K.
- Venue
- Chemical Geology
- Publisher
- Elsevier BV
- Published
- 2015-12
- Volume
- 419
- Pages
- 67-74
- ISSN
- 0009-2541 (ISSN-L)
- OpenAlex
- W2197342390
- Cited by
- 4
- References
- 48
- Citations by year
- 2020: 1 · 2019: 1 · 2018: 1 · 2017: 1
- FWCI
- 0.48
- Type
- journal article
- Language
- en
- Open access
- closed
- Locations
- Chemical Geology (publishedVersion)
- HAL (submittedVersion)
- Funders
- European Community's Seventh Framework Programme (238579)
- Topics
- Physical Sciences › Environmental Science › Environmental Engineering › Microbial Fuel Cells and Bioremediation
- Physical Sciences › Chemistry › Inorganic Chemistry › Radioactive element chemistry and processing
- Life Sciences › Biochemistry, Genetics and Molecular Biology › Molecular Biology › Geomagnetism and Paleomagnetism Studies
- Keywords
- magnetite, hydrogen oxidation, hydrogen concentration, vivianite, iron dissolution, phosphate, oxide passivation, metal corrosion, radioactive waste geological disposal, bacterial activity
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