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  • Articles: DFG German National Licenses  (33)
  • Electronic Resource  (33)
  • 1
    Electronic Resource
    Electronic Resource
    s.l. : American Chemical Society
    Environmental science & technology 26 (1992), S. 925-929 
    ISSN: 1520-5851
    Source: ACS Legacy Archives
    Topics: Chemistry and Pharmacology , Energy, Environment Protection, Nuclear Power Engineering
    Type of Medium: Electronic Resource
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  • 2
    Electronic Resource
    Electronic Resource
    s.l. : American Chemical Society
    Environmental science & technology 26 (1992), S. 205-207 
    ISSN: 1520-5851
    Source: ACS Legacy Archives
    Topics: Chemistry and Pharmacology , Energy, Environment Protection, Nuclear Power Engineering
    Type of Medium: Electronic Resource
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  • 3
    Electronic Resource
    Electronic Resource
    s.l. : American Chemical Society
    Environmental science & technology 26 (1992), S. 2228-2234 
    ISSN: 1520-5851
    Source: ACS Legacy Archives
    Topics: Chemistry and Pharmacology , Energy, Environment Protection, Nuclear Power Engineering
    Type of Medium: Electronic Resource
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  • 4
    Electronic Resource
    Electronic Resource
    s.l. : American Chemical Society
    Environmental science & technology 25 (1991), S. 1062-1067 
    ISSN: 1520-5851
    Source: ACS Legacy Archives
    Topics: Chemistry and Pharmacology , Energy, Environment Protection, Nuclear Power Engineering
    Type of Medium: Electronic Resource
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  • 5
    Electronic Resource
    Electronic Resource
    s.l. : American Chemical Society
    Environmental science & technology 28 (1994), S. 1205-1210 
    ISSN: 1520-5851
    Source: ACS Legacy Archives
    Topics: Chemistry and Pharmacology , Energy, Environment Protection, Nuclear Power Engineering
    Type of Medium: Electronic Resource
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  • 6
    ISSN: 1476-4687
    Source: Nature Archives 1869 - 2009
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
    Notes: [Auszug] At the onset of anaerobic conditions, Fe(m) is the most abundant potential electron acceptor for organic-matter oxidation in most fresh-water sedimentary environments13'14. The accumulation of Fe(n) during the anaerobic oxidation of organic matter in numerous pristine and contaminated aquifers ...
    Type of Medium: Electronic Resource
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  • 7
    Electronic Resource
    Electronic Resource
    Oxford, UK : Blackwell Publishing Ltd
    FEMS microbiology letters 195 (2001), S. 0 
    ISSN: 1574-6968
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Biology
    Notes: The discovery that all hyperthermophiles that have been evaluated have the capacity to reduce Fe(III) has raised the question of whether mechanisms for dissimilatory Fe(III) reduction have been conserved throughout microbial evolution. Many studies have suggested that c-type cytochromes are integral components in electron transport to Fe(III) in mesophilic dissimilatory Fe(III)-reducing microorganisms. However, Pyrobaculum islandicum, the hyperthermophile in which Fe(III) reduction has been most intensively studied, did not contain c-type cytochromes. NADPH was a better electron donor for the Fe(III) reductase activity in P. islandicum than NADH. This is the opposite of what has been observed with mesophiles. Thus, if previous models for dissimilatory Fe(III) reduction by mesophilic bacteria are correct, then it is unlikely that a single strategy for electron transport to Fe(III) is present in all dissimilatory Fe(III)-reducing microorganisms.
    Type of Medium: Electronic Resource
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  • 8
    Electronic Resource
    Electronic Resource
    Oxford, UK : Blackwell Publishing Ltd
    FEMS microbiology reviews 20 (1997), S. 0 
    ISSN: 1574-6976
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Biology
    Notes: Until recently, nonenzymatic processes were generally considered to account for much of the Fe(III) reduction in subsurface environments. However, it is now clear that enzymatic Fe(III) reduction catalyzed by microorganisms which conserve energy to support growth by completely oxidizing organic compounds to carbon dioxide accounts for most of the Fe(III) reduction. Microbial Fe(III) reduction in deep pristine aquifers releases dissolved inorganic carbon into groundwater which may increase aquifer porosity. The Fe(II) released into the groundwater is an important groundwater quality problem in many aquifers. Microbial oxidation of organic contaminants coupled to Fe(III) reduction removes significant amounts of pollutants from many contaminated aquifers. Fe(III) reduction and hence contaminant removal can be accelerated in aquifer sediments with the addition of Fe(III) chelators or humic substances. Both of these amendments alleviate the need for Fe(III) reducers to come into direct physical contact with Fe(III) oxides in order to reduce them. Some Fe(III)-reducing microorganisms can reduce contaminant metals and metalloids such as uranium, technetium, cobalt, chromium and selenium. This metabolism may be useful for remediation of metal-contaminated subsurface environments. Fe(III) reducers and some of the insoluble Fe(II) products of Fe(III) reduction can reducively dechlorinate chlorinated contaminants. Magnetite that is similar to that produced by known Fe(III)-reducing microorganisms has been recovered at depths as great as 6.7 km on Earth and has been observed in a Martian meteorite. Thus, microbial oxidation of organic matter coupled to the reduction of Fe(III) to Fe(II) appears to be a important process in a variety of subsurface environments.
    Type of Medium: Electronic Resource
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  • 9
    ISSN: 1574-6968
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Biology
    Notes: Geobacter sulfurreducens produces a single, membrane-associated Fe3+ reductase activity when grown on fumarate or Fe3+. The activity was initially isolated by solubilization of membranes with the non-ionic detergent dodecyl-β-D-maltoside, and partially purified by a combination of ion exchange chromatography and preparative non-denaturing gel electrophoresis. Molecular mass of the reductase, as determined by gel filtration chromatography, was approximately 300 kDa. Cofactor analysis of the purified reductase demonstrates that it contains a hemoprotein and flavin adenine dinucleotide. Kinetic and inhibitor studies show that the reductase is specific for NADH as electron donor, and confirm that the reductase enzymatically reduces Fe3+. The cytochrome associated with the complex undergoes a reoxidation upon addition of Fe3+ compounds, indicating an ability to pass reducing equivalents to Fe3+. This is the first description of a purified NADH-dependent Fe3+ reductase from a microorganism capable of coupling Fe3+ reduction to growth.
    Type of Medium: Electronic Resource
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  • 10
    ISSN: 1745-6584
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Energy, Environment Protection, Nuclear Power Engineering , Geosciences
    Notes: Rates of biodegradation were measured in a petroleum hydrocarbon-contaminated aquifer using a combination of field and laboratory methods. These methods are based on tracking concentration changes of substrates (both electron donors and acceptors) or final products of microbial metabolism over time. Ground water at the study site (Hanahan, South Carolina) is anoxic, and sulfate reduction is the predominant terminal electron accepting process. Laboratory studies conducted with sediment cored from the site showed that 14C-toluene was mineralized to 14CO2 with a first-order degradation rate constant (ktol) of -0.01 d−1 under sulfate-reducing conditions. Under nitrate-amended, Fe(III)-amended, or nonamended (methanogenic) conditions, toluene was not significantly mineralized. 14C-Benzene was degraded at low but measurable rates (kben= -0.003 d−1) under sulfate-reducing conditions whereas degradation under methanogenic conditions was negligible. These results illustrate the extreme sensitivity of laboratory-measured biodegradation rates to terminal electron-accepting conditions, and show the necessity of carefully matching experimental conditions to in situ conditions. Concentration decreases of toluene along aquifer flowpaths, when the uncertainty of ground-water flow velocities was considered, indicated ktol values ranging from -0.0075 to -0.03 d−1. Concentration decreases of sulfate and concentration increases of dissolved inorganic carbon (DIC), when normalized for assumed stoichiometric oxidation of toluene coupled to sulfate reduction, yielded a kso4 range of -0.005 to -0.02 d−1, and a kDIC value range of +0.00075 to +0.003 d−1. Because both laboratory and field methods have numerous sources of uncertainty, a combination of these methods is the most appropriate procedure for evaluating biodegradation rate constants in contaminated ground-water systems.
    Type of Medium: Electronic Resource
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