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Immobilization of radionuclides and heavy metals through anaerobic bio-oxidation of Fe(II).

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TLDR
The potential of a bioremediative strategy for HMR stabilization in reducing environments based on the recently described anaerobic nitrate-dependent Fe(II) oxidation by Dechlorosoma species is demonstrated.
Abstract
Adsorption of heavy metals and radionuclides (HMR) onto iron and manganese oxides has long been recognized as an important reaction for the immobilization of these compounds. However, in environments containing elevated concentrations of these HMR the adsorptive capacity of the iron and manganese oxides may well be exceeded, and the HMR can migrate as soluble compounds in aqueous systems. Here we demonstrate the potential of a bioremediative strategy for HMR stabilization in reducing environments based on the recently described anaerobic nitrate-dependent Fe(II) oxidation by Dechlorosoma species. Bio-oxidation of 10 mM Fe(II) and precipitation of Fe(III) oxides by these organisms resulted in rapid adsorption and removal of 55 microM uranium and 81 microM cobalt from solution. The adsorptive capacity of the biogenic Fe(III) oxides was lower than that of abiotically produced Fe(III) oxides (100 microM for both metals), which may have been a result of steric hindrance by the microbial cells on the iron oxide surfaces. The binding capacity of the biogenic oxides for different heavy metals was indirectly correlated to the atomic radius of the bound element. X-ray absorption spectroscopy indicated that the uranium was bound to the biogenically produced Fe(III) oxides as U(VI) and that the U(VI) formed bidentate and tridentate inner-sphere complexes with the Fe(III) oxide surfaces. Dechlorosoma suillum oxidation was specific for Fe(II), and the organism did not enzymatically oxidize U(IV) or Co(II). Small amounts (less than 2.5 microM) of Cr(III) were reoxidized by D. suillum; however, this appeared to be inversely dependent on the initial concentration of the Cr(III). The results of this study demonstrate the potential of this novel approach for stabilization and immobilization of HMR in the environment.

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Citations
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Microorganisms pumping iron: anaerobic microbial iron oxidation and reduction

TL;DR: Biological iron apportionment has been described as one of the most ancient forms of microbial metabolism on Earth, and as a conceivable extraterrestrial metabolism on other iron-mineral-rich planets such as Mars.
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Microbial perchlorate reduction: rocket-fuelled metabolism

TL;DR: The recent completion of the whole-genome sequence of the perchlorate-reducing microorganism Dechloromonas aromatica offers further insight into the evolution and regulation of this unique metabolic pathway.
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Anaerobic redox cycling of iron by freshwater sediment microorganisms.

TL;DR: The results indicate that the wetland sediments contained organisms such as Geobacter sp.
Journal ArticleDOI

Atom Exchange between Aqueous Fe(II) and Goethite: An Fe Isotope Tracer Study

TL;DR: It is proposed that sorption and dissolution sites are linked via conduction through the bulk crystal, as was recently demonstrated for hematite, for extensive mixing between aqueous Fe(II) and goethite, which has significant implications for heavy metal sequestration and release and reduction of soil and groundwater contaminants.
Journal ArticleDOI

Insight into the evolution of the iron oxidation pathways.

TL;DR: The iron paleochemistry, the phylogeny, the physiology of the iron oxidizers, and the nature of the cofactors of the redox proteins involved in these pathways suggest a possible scenario for the timescale in which each type of Fe(II) oxidation pathways evolved.
References
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Book

Bergey's Manual of Systematic Bacteriology

TL;DR: BCL3 and Sheehy cite Bergey's manual of determinative bacteriology of which systematic bacteriology, first edition, is an expansion.
Book

Organic geochemistry of natural waters

E. M. Thurman
TL;DR: The first part of the book as mentioned in this paper is a general overview of the amount and general nature of dissolved organic carbon in natural waters, and the second part is a summary of the data that has accumulated from many disciplines over the last decade.
Book

Surface Complexation Modeling: Hydrous Ferric Oxide

TL;DR: In this article, the generalized two-layer model is used to analyze the Coulombic effect of Hydrous Ferric Oxide, and anion and cation sorsption on HFOs are investigated.
Book

The geochemistry of natural waters

TL;DR: The Hydrologic Cycle and Chemical Background of Natural Waters as mentioned in this paper, the Carbonate System and pH Control 5 Clay Minerals and Ion Exchange 6 Stability Relationships and Silicate Equilibria 7 Kinetics 8 Weathering and Water Chemistry, I: Principles 9 Water Chemistry Chemistry, II: Examples 10 Acid Deposition and Surface Water Chemistry 11 Evaporation and Saline Waters 12 The Oceans 13 Redox Eilibria 14 Redox Conditions in Natural Waters 15 Trace Elements 16 Mathematical and Numerical Models 17 Isotopes Appendices
Journal ArticleDOI

Multiple-scattering calculations of x-ray-absorption spectra

TL;DR: A high-order multiple-scattering approach to the calculation of polarized x-ray-absorption spectra, which includes both x- Ray- absorption fine structure and x-Ray- absorption near-edge structure, is presented.
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