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.; Scherer, Michelle M.

doi:10.3390/min9070434

Electron Donor Utilization and Secondary Mineral Formation during the Bioreduction of Lepidocrocite by Shewanella putrefaciens CN32

Journal Article · Sun Jul 14 00:00:00 EDT 2019 · Minerals

DOI:https://doi.org/10.3390/min9070434· OSTI ID:1560537

O’Loughlin, Edward J. ^[1]; ^[2]; ^[3]; Scherer, Michelle M. ^[4]

Argonne National Lab. (ANL), Argonne, IL (United States). Biosciences Div.
Univ. of Iowa, Iowa City, IA (United States). Dept. of Civil and Environmental Engineering; Pennsylvania State Univ., University Park, PA (United States). Dept. of Civil and Environmental Engineering
Argonne National Lab. (ANL), Argonne, IL (United States). Biosciences Div.; California Dept. of Water Resources, Sacramento, CA (United States)
Univ. of Iowa, Iowa City, IA (United States). Dept. of Civil and Environmental Engineering

The bioreduction of Fe(III) oxides by dissimilatory iron reducing bacteria (DIRB) may result in the production of a suite of Fe(II)-bearing secondary minerals, including magnetite, siderite, vivianite, green rusts, and chukanovite; the formation of specific phases controlled by the interaction of various physiological and geochemical factors. In an effort to better understand the effects of individual electron donors on the formation of specific Fe(II)-bearing secondary minerals, we examined the effects of a series of potential electron donors on the bioreduction of lepidocrocite ($$γ$$-FeOOH) by Shewanella putrefaciens CN32. Biomineralization products were identified by X-ray diffraction, Mössbauer spectroscopy, and scanning electron microscopy. Acetate, citrate, ethanol, glucose, glutamate, glycerol, malate, and succinate were not effectively utilized for the bioreduction of lepidocrocite by S. putrefaciens CN32; however, substantial Fe(II) production was observed when formate, lactate, H₂, pyruvate, serine, or N acetylglucosamine (NAG) was provided as an electron donor. Carbonate or sulfate green rust was the dominant Fe(II)-bearing secondary mineral when formate, H₂, lactate, or NAG was provided, however, siderite formed with pyruvate or serine. Geochemical modeling indicated that pH and carbonate concentration are the key factors determining the prevalence of carbonate green rust verses siderite.

View Accepted Manuscript (DOE)

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

Sponsoring Organization:: USDOE Office of Science - Office of Biological and Environmental Research - Subsurface Biogeochemical Research

Grant/Contract Number:: AC02-06CH11357

OSTI ID:: 1560537

Journal Information:: Minerals, Journal Name: Minerals Journal Issue: 7 Vol. 9; ISSN MBSIBI; ISSN 2075-163X

Publisher:: MDPICopyright Statement

Country of Publication:: United States

Language:: English

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