In situ monitoring of lepidocrocite bio-reduction and magnetite formation by reflexion Mössbauer spectroscopy

Abstract : The miniaturized Mössbauer spectrometer (MIMOS II) was used to monitor in situ the mineralogical transformation of lepidocrocite (δ-FeOOH) in a Shewanella putrefaciens culture under anaerobic conditions using methanoate as the electron source. Magnetite was the only biogenic mineral formed during the course of the incubation. The analysis of the biogenic mineral by transmission electron microscopy (TEM) revealed cubic-shaped crystals with a relatively homogeneous grain size of about 50 nm. After one day of incubation, the departure from stoichiometry, δ, of the biogenerated magnetite was very low (δ∼0.025) and rapidly reached values close to zero. Such low values of δwere not obtained for magnetite synthesized inorganically when Fe3+ in the form of δ-FeOOH was reacted with stoichiometric quantities of soluble Fe2+ and OH-. The experimental setup used in this study could be replicated in field experiments when assessing the formation of magnetite in modern geological settings as its formation is suspected to be caused by a strong bacterial activity.
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Submitted on : Friday, July 27, 2012 - 5:18:08 PM
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Asfaw Zegeye, Mustapha Abdelmoula, Muhammad Usman, Khalil Hanna, Christian Ruby. In situ monitoring of lepidocrocite bio-reduction and magnetite formation by reflexion Mössbauer spectroscopy. American Mineralogist, Mineralogical Society of America, 2011, 96, pp.1410-1413. ⟨10.2138/am.2011.3794⟩. ⟨hal-00721546⟩

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