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D. Lovley (1997)
Potential for anaerobic bioremediation of BTEX in petroleum-contaminated aquifersJournal of Industrial Microbiology and Biotechnology, 18
D. Lovley, E. Roden, E. Phillips, J. Woodward (1993)
Enzymatic iron and uranium reduction by sulfate-reducing bacteriaMarine Geology, 113
D. Lovley, J. Coates, E. Blunt-Harris, E. Phillips, J. Woodward (1996)
Humic substances as electron acceptors for microbial respirationNature, 382
F. Dunnivant, R. Schwarzenbach, D. Macalady (1992)
Reduction of substituted nitrobenzenes in aqueous solutions containing natural organic matterEnvironmental Science & Technology, 26
J. Alberts, J. Schindler, Richard Miller, D. Nutter (1974)
Elemental Mercury Evolution Mediated by Humic AcidScience, 184
D. Lovley, J. Woodward, F. Chapelle (1996)
Rapid Anaerobic Benzene Oxidation with a Variety of Chelated Fe(III) FormsApplied and Environmental Microbiology, 62
D. Lovley, E. Phillips (1988)
Novel Mode of Microbial Energy Metabolism: Organic Carbon Oxidation Coupled to Dissimilatory Reduction of Iron or ManganeseApplied and Environmental Microbiology, 54
D. Lovley, F. Chapelle (1995)
Deep subsurface microbial processesReviews of Geophysics, 33
Paul Tratnyek, D. Macalady (1989)
Abiotic reduction of nitro aromatic pesticides in anaerobic laboratory systemsJournal of Agricultural and Food Chemistry, 37
D. Lovley, Joan Woodward, F. Chapelle (1994)
Stimulated anoxic biodegradation of aromatic hydrocarbons using Fe(III) ligandsNature, 370
J. Stucki, P. Komadel, H. Wilkinson (1987)
Microbial Reduction of Structural Iron(III) in SmectitesSoil Science Society of America Journal, 51
G. Curtis, M. Reinhard (1994)
Reductive dehalogenation of hexachloroethane, carbon tetrachloride, and bromoform by anthrahydroquinone disulfonate and humic Acid.Environmental science & technology, 28 13
D. Lovley (1995)
Microbial Reduction of Iron, Manganese, and other MetalsAdvances in Agronomy, 54
D. Lovley, E. Phillips (1986)
Organic Matter Mineralization with Reduction of Ferric Iron in Anaerobic SedimentsApplied and Environmental Microbiology, 51
D. Lovley, E. Phillips (1986)
Availability of Ferric Iron for Microbial Reduction in Bottom Sediments of the Freshwater Tidal Potomac RiverApplied and Environmental Microbiology, 52
D. Lovley, M. Baedecker, D. Lonergan, I. Cozzarelli, E. Phillips, D. Siegel (1989)
Oxidation of aromatic contaminants coupled to microbial iron reductionNature, 339
F. Ponnamperuma (1972)
The Chemistry of Submerged SoilsAdvances in Agronomy, 24
J. Kostka, J. Stucki, K. Nealson, Jun Wu (1996)
Reduction of Structural Fe(III) in Smectite by a Pure Culture of Shewanella Putrefaciens Strain MR-1Clays and Clay Minerals, 44
E. Phillips, D. Lovley, E. Roden (1993)
Composition of Non-Microbially Reducible Fe(III) in Aquatic SedimentsApplied and Environmental Microbiology, 59
W. Reeburgh (1983)
Rates of biogeochemical processes in anoxic sediments.Annual Review of Earth and Planetary Sciences, 11
(1998)
Recovery of humics-reducing bacteria from a diversity of sedimentary environments
The potential for humic substances to serve as a terminal electron acceptor in microbial respiration and to function as an electron shuttle between Fe(III)‐reducing microorganisms and insoluble Fe(III) oxides was investigated. The Fe(III)‐reducing microorganism Geobacter metallireducens conserved energy to support growth from electron transport to humics as evidenced by continued oxidation of acetate to carbon dioxide after as many as nine transfers in a medium with acetate as the electron donor and soil humic acids as the electron acceptor. Growth of G. metallireducens with poorly crystalline Fe(III) oxide as the electron acceptor was greatly stimulated by the addition of as little as 100 μM of the humics analog, anthraquinone‐2,6‐disulfonate. Other quinones investigated, including lawsone, menadione, and anthraquinone‐2‐sulfonate, also stimulated Fe(III) oxide reduction. A wide phylogenetic diversity of microorganisms capable of Fe(III) reduction were also able to transfer electrons to humics. Microorganisms which can not reduce Fe(III) could not reduce humics. Humics stimulated the reduction of structural Fe(III) in clay and the crystalline Fe(III) forms, goethite and hematite. These results demonstrate that electron shuttling between Fe(III)‐reducing microorganisms and Fe(III) via humics not only accelerates the microbial reduction of poorly crystalline Fe(III) oxide, but also can facilitate the reduction of Fe(III) forms that are not typically reduced by microorganisms in the absence of humics. Addition of humic substances to enhance electron shuttling between Fe(III)‐reducing microorganisms and Fe(III) oxides may be a useful strategy to stimulate the remediation of soils and sediments contaminated with organic or metal pollutants.
Acta hydrochimica et hydrobiologica – Wiley
Published: May 1, 1998
Keywords: ; ; ; ; ; ; ; ; ;
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