Interactions of ferrous iron with clay mineral surfaces during sorption and subsequent oxidation

This article is licensed under aCreative Commons Attribution 3.0 Unported Licence.Natacha Van Groeningen, Laurel K. ThomasArrigo, James M. Byrne, Andreas Kappler, Iso Christl, Ruben Kretzschmar Under anoxic conditions, clay minerals sorb dissolved Fe(II) predominantly by forming surface precipitates, which transform into Fe(III)-phases upon aeration. To cite this article before page numbers are assigned, use the DOI form of citation above. The content of this RSS Feed (c) The Royal Society of Chemistry
Source: RSC - J. Environ. Monit. latest articles - Category: Environmental Health Authors: Source Type: research