Fe(III) Oxide Reactivity Toward Biological versus Chemical Reduction
By E. Roden. 2003
298 citations recorded by the source corpus.
Subfields: Environmental Chemistry, Environmental Engineering, Renewable Energy, Sustainability and the Environment
View Paper: https://www.semanticscholar.org/paper/fcc829755255bedd10c1996591e6c4097a6d06b4
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In Environmental Chemistry
In Environmental Engineering
In Renewable Energy, Sustainability and the Environment
Citations in the corpus
- IRON IN MICROBIAL METABOLISMS (2011, background): “…such wide variations in reactivity towards microbial reduction, it is not surprising that ferric iron can represent a long-term electron acceptor for organic matter oxidation, even at depths where other anaerobic respiratory processes are thermodynamically predicted to dominate (e.g. Roden 2003).”
- Geomicrobiological cycling of iron (2005, background): “Surface area and reactivity of ferne iron oxides The rates of chemical and microbial transformations of iron minerals depend on the number of available reactive surface sites, e.g., on the number of reactive surface-OH functional groups in caseof ferric hydroxides (Roden 2003).”