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Effects of aqueous complexation on reductive precipitation of uranium by Shewanella putrefaciens

We have examined the effects of aqueous complexation on rates of dissimilatory reductive precipitation of uranium by Shewanella putrefaciens. Uranium(VI) was supplied as sole terminal electron acceptor to Shewanella putrefaciens (strain 200R) in defined laboratory media under strictly anaerobic cond...

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Autores principales: Haas, Johnson R, Northup, Abraham
Formato: Texto
Lenguaje:English
Publicado: BioMed Central 2004
Materias:
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC1475784/
https://www.ncbi.nlm.nih.gov/pubmed/35412771
http://dx.doi.org/10.1186/1467-4866-5-41
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author Haas, Johnson R
Northup, Abraham
author_facet Haas, Johnson R
Northup, Abraham
author_sort Haas, Johnson R
collection PubMed
description We have examined the effects of aqueous complexation on rates of dissimilatory reductive precipitation of uranium by Shewanella putrefaciens. Uranium(VI) was supplied as sole terminal electron acceptor to Shewanella putrefaciens (strain 200R) in defined laboratory media under strictly anaerobic conditions. Media were amended with different multidentate organic acids, and experiments were performed at different U(VI) and ligand concentrations. Organic acids used as complexing agents were oxalic, malonic, succinic, glutaric, adipic, pimelic, maleic, citric, and nitrilotriacetic acids, tiron, EDTA, and Aldrich humic acid. Reductive precipitation of U(VI), resulting in removal of insoluble amorphous UO(2 )from solution, was measured as a function of time by determination of total dissolved U. Reductive precipitation was measured, rather than net U(VI) reduction to U(IV), to assess overall U removal rates from solution, which may be used to gauge the influence of chelation on microbial U mineralization. Initial linear rates of U reductive precipitation were found to correlate with stability constants of 1:1 aqueous U(VI):ligand and U(IV):ligand complexes. In the presence of strongly complexing ligands (e.g., NTA, Tiron, EDTA), UO(2 )precipitation did not occur. Our results are consistent with ligand-retarded precipitation of UO(2), which is analogous to ligand-assisted solid phase dissolution but in reverse: ligand exchange with the U(4+ )aquo cation acts as a rate-limiting reaction moderating coordination of water molecules with U(4+), which is a necessary step in UO(2 )precipitation. Ligand exchange kinetics governing dissociation rates of ligands from U(VI)-organic complexes may also influence overall UO(2 )production rates, although the magnitude of this effect is unclear relative to the effects of U(IV)-organic complexation. Our results indicate that natural microbial-aqueous systems containing abundant organic matter can inhibit the formation of biogenic amorphous UO(2).
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spelling pubmed-14757842006-06-10 Effects of aqueous complexation on reductive precipitation of uranium by Shewanella putrefaciens Haas, Johnson R Northup, Abraham Geochem Trans Research Article We have examined the effects of aqueous complexation on rates of dissimilatory reductive precipitation of uranium by Shewanella putrefaciens. Uranium(VI) was supplied as sole terminal electron acceptor to Shewanella putrefaciens (strain 200R) in defined laboratory media under strictly anaerobic conditions. Media were amended with different multidentate organic acids, and experiments were performed at different U(VI) and ligand concentrations. Organic acids used as complexing agents were oxalic, malonic, succinic, glutaric, adipic, pimelic, maleic, citric, and nitrilotriacetic acids, tiron, EDTA, and Aldrich humic acid. Reductive precipitation of U(VI), resulting in removal of insoluble amorphous UO(2 )from solution, was measured as a function of time by determination of total dissolved U. Reductive precipitation was measured, rather than net U(VI) reduction to U(IV), to assess overall U removal rates from solution, which may be used to gauge the influence of chelation on microbial U mineralization. Initial linear rates of U reductive precipitation were found to correlate with stability constants of 1:1 aqueous U(VI):ligand and U(IV):ligand complexes. In the presence of strongly complexing ligands (e.g., NTA, Tiron, EDTA), UO(2 )precipitation did not occur. Our results are consistent with ligand-retarded precipitation of UO(2), which is analogous to ligand-assisted solid phase dissolution but in reverse: ligand exchange with the U(4+ )aquo cation acts as a rate-limiting reaction moderating coordination of water molecules with U(4+), which is a necessary step in UO(2 )precipitation. Ligand exchange kinetics governing dissociation rates of ligands from U(VI)-organic complexes may also influence overall UO(2 )production rates, although the magnitude of this effect is unclear relative to the effects of U(IV)-organic complexation. Our results indicate that natural microbial-aqueous systems containing abundant organic matter can inhibit the formation of biogenic amorphous UO(2). BioMed Central 2004-10-01 /pmc/articles/PMC1475784/ /pubmed/35412771 http://dx.doi.org/10.1186/1467-4866-5-41 Text en Copyright © 2004 American Institute of Physics
spellingShingle Research Article
Haas, Johnson R
Northup, Abraham
Effects of aqueous complexation on reductive precipitation of uranium by Shewanella putrefaciens
title Effects of aqueous complexation on reductive precipitation of uranium by Shewanella putrefaciens
title_full Effects of aqueous complexation on reductive precipitation of uranium by Shewanella putrefaciens
title_fullStr Effects of aqueous complexation on reductive precipitation of uranium by Shewanella putrefaciens
title_full_unstemmed Effects of aqueous complexation on reductive precipitation of uranium by Shewanella putrefaciens
title_short Effects of aqueous complexation on reductive precipitation of uranium by Shewanella putrefaciens
title_sort effects of aqueous complexation on reductive precipitation of uranium by shewanella putrefaciens
topic Research Article
url https://www.ncbi.nlm.nih.gov/pmc/articles/PMC1475784/
https://www.ncbi.nlm.nih.gov/pubmed/35412771
http://dx.doi.org/10.1186/1467-4866-5-41
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