Bacterial Reduction of Ferric Iron in a Stratified Eutrophic Lake
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Summary
Of the iron sources tested with cultures of anaerobic iron-reducing bacteria, FeCl3 was the most readily reduced and goethite the least, while biomass yield was greater in the presence of Fe(III), and the organism was able to use H2 as a source of reducing power.
- Type
- article
- Published
- 1983-01-01
- Cited by
- 120
- References
- 25
- OpenAlex
- https://openalex.org/W2085710491
- Semantic Scholar
- https://api.semanticscholar.org/CorpusID:59194259
Keywords
Anoxic waters, Chemistry, Goethite, Bacteria, Facultative
References
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- Factors Affecting Methanogenesis and Associated Anaerobic Processes in the Sediments of a Stratified Eutrophic Lake
- A note on the isolation and enumeration of bacteria which deposit and reduce ferric iron
- Increased sensitivity in the measurement of ATP in freshwater samples with a comment on the adverse effect of membrane filtration
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- Iron and manganese in Lake Vechten (The Netherlands) - dynamics and role in the cycle of reducing power
- Uptake of Fe (II) by a Diatom in Oxic Culture Medium
- Chapter I The Disintegration of Micro-organisms
Cited by
- Novel Mode of Microbial Energy Metabolism: Organic Carbon Oxidation Coupled to Dissimilatory Reduction of Iron or Manganese
- Etude de la prolifération des algues vertes dans le bassin d'Arcachon
- Humic acids enhance the microbially mediated release of sedimentary ferrous iron
- The Chemistry of Phosphate and Nitrogen Compounds in Sediments
- Effects of electron acceptors on soluble reactive phosphorus in the overlying water during algal decomposition
- Competitive Mechanisms for Inhibition of Sulfate Reduction and Methane Production in the Zone of Ferric Iron Reduction in Sediments
- Interrelated contributions to freshwater science over 78 years: A guide to published work from the Freshwater Biological Association, Institute of Freshwater Ecology and Centre for Ecology and Hydrology, 1929-2006
- Microbial Iron Reduction by Enrichment Cultures Isolated from Estuarine Sediments
- Biogeochemical Conditions Favoring Magnetite Formation during Anaerobic Iron Reduction
- Eutrophication trend of lakes in the Tampa Bay watershed and the role of submerged aquatic vegetation in buffering lake water phosphorus concentration
- Regulation of Dissimilatory Fe(III) Reduction Activity in Shewanella putrefaciens
- Availability of Ferric Iron for Microbial Reduction in Bottom Sediments of the Freshwater Tidal Potomac River
- Organic Matter Mineralization with Reduction of Ferric Iron in Anaerobic Sediments
- Anaerobic Microbial Dissolution of Transition and Heavy Metal Oxides
- Hydrogen and Formate Oxidation Coupled to Dissimilatory Reduction of Iron or Manganese by Alteromonas putrefaciens
- Kinetics of microbial Fe(III) oxyhydroxide reduction : The role of mineral properties
- Rust dissolution and removal by iron-reducing bacteria: A potential rehabilitation of rusted equipment
- Bacterial cycling of minerals that affect plant growth in waterlogged soils: a review
- Microbial reduction of manganese oxides - Interactions with iron and sulfur
- Nitrate reduction in marine sediment: Pathways and interactions with iron and sulfur cycling
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