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Effects of Bound Phosphate on the Bioreduction of Lepidocrocite (γ-FeOOH) and Maghemite (γ-Fe 2 O 3 ) and Formation of Secondary Minerals
Abstract
Natural Fe(III) oxides typically contain a range of trace elements including P. Although solution phase and adsorbed P (as phosphate) have been shown to impact the bioreduction of Fe(III) oxides and the formation of "biogenic" secondary minerals, little is known about the potential effects of occluded/incorporated phosphate. We have examined the bioreduction of Fe(III) oxides (lepidocrocite (γ-FeOOH) and maghemite (γ-Fe2O3)) containing 0-3 mass% P as "bound" (a term we use to include both adsorbed and occluded/incorporated) phosphate. Kinetic dissolution studies showed congruent release of Fe and P, suggesting that the phosphate in these materials was incorporated within the particles; however, 53% or 86% of the total phosphate associated with the lepidocrocites containing 0.7 or 3 mass% P, respectively, was extracted with 0.1 M NaOH and can be considered to be adsorbed, both to exterior surfaces and within micropores. In the absence of phosphate, lepidocrocite was rapidly reduced to magnetite by Shewanella putrefaciens CN32, and over time the magnetite was partially transformed to ferrous hydroxy carbonate (FHC). The presence of 0.2-0.7 mass% P significantly inhibited the initial reduction of lepidocrocite but ultimately resulted in greater Fe(II) production and the formation of carbonate green rust. The bioreduction of maghemite with and without bound phosphate resulted in solid-state conversion to magnetite, with subsequent formation of FHC. We also examined the potential…
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Vivianite was not observed in any experimental systems (P:Fe = 0.005), and vivianite formation requires substantial phosphate (not observed at P:Fe lower than 0.08).
“Vivianite formation requires the presence of substantial phosphate (e.g., vivianite was not observed at P:Fe rations lower than 0.08 [33,43,48,63]), and vivianite was not observed in any of our experimental systems (P:Fe = 0.005 [63]).”
From Electron Donor Utilization and Secondary Mineral Formation during the Bioreduction of Lepidocrocite by Shewanella putrefaciens CN32 (2019) · cites this paper as [63]
Formate is utilized as an electron donor for dissimilatory iron reduction by S. putrefaciens CN32.
“Formate essentially served as a positive control given that we have previously shown that formate is utilized as an electron donor for DIR by S. putrefaciens CN32 [16,28,44,55,63].”
From Electron Donor Utilization and Secondary Mineral Formation during the Bioreduction of Lepidocrocite by Shewanella putrefaciens CN32 (2019) · cites this paper as [63]
Magnetite was not observed as a secondary mineral in any experimental systems, likely due to trace levels of phosphate present in the lepidocrocite used, as low phosphate suppresses magnetite formation during DIR of Fe(III) oxides.
“However, magnetite was not observed as a secondary mineral in any of our experimental systems, likely due to trace levels of phosphate present in the lepidocrocite used in our experiments [63], as low levels of phosphate are known to suppress magnetite formation during DIR of Fe(III) oxides [28,33,44,47,63].”
From Electron Donor Utilization and Secondary Mineral Formation during the Bioreduction of Lepidocrocite by Shewanella putrefaciens CN32 (2019) · cites this paper as [63]
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Hansel, C. M., Benner, S. G., & Fendorf, S. (2005) · Environmental Science & Technology · doi:10.1021/es050666z · Cited by 619
Green rust formation controls nutrient availability in a ferruginous water column
Zegeye, A., Bonneville, S., Benning, L. G., Sturm, A., Fowle, D. A., Jones, C., Canfield, D. E., Ruby, C., MacLean, L. C., Nomosatryo, S., et al. (2012) · Geology · doi:10.1130/g32959.1 · Cited by 214
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Amirbahman, A., Sigg, L., & Gunten, U. V. (1997) · Journal of Colloid and Interface Science · doi:10.1006/jcis.1997.5116 · Cited by 96
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Cited by
Sorted by citations
Etique, M., Jorand, F. P. A., & Ruby, C. (2016) · Geobiology · doi:10.1111/gbi.12170 · Cited by 37
O’Loughlin, E. J., Gorski, C. A., Flynn, T. M., & Scherer, M. M. (2019) · Minerals · doi:10.3390/min9070434 · Cited by 28
Self-citation
Metadata
- Authors
- O’Loughlin, E. J., Boyanov, M. I., Flynn, T. M., Gorski, C. A., Hofmann, S. M., McCormick, M. L., Scherer, M. M., & Kemner, K. M.
- Affiliations
- Biosciences Division, Argonne National Laboratory, Argonne, Illinois 60439-4843, United States
- Department of Civil and Environmental Engineering, University of Iowa, Iowa City, Iowa 52242-1527, United States
- Department of Biology, Hamilton College, Clinton, New York 13323, United States
- Venue
- Environmental Science & Technology
- Publisher
- American Chemical Society (ACS)
- Published
- 2013-08-02
- Volume
- 47
- Issue
- 16
- Pages
- 9157-9166
- ISSN
- 0013-936X
- 1520-5851
- Cited by
- 90
- References
- 4
- Language
- en
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