Structure and reactivity of the hydrated hematite (0001) surface
By T. Trainor, A. Chaka, P. Eng, Matthew Newville, G. Waychunas, J. Catalano, G. Brown. 2004
294 citations recorded by the source corpus.
Subfields: Inorganic Chemistry, Renewable Energy, Sustainability and the Environment, Water Science and Technology
View Paper: https://www.semanticscholar.org/paper/f04a2efb3f338cded655873dec1c6541e303cd2a
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In Inorganic Chemistry
In Renewable Energy, Sustainability and the Environment
Citations in the corpus
- Nanoparticulate Iron Oxide Minerals in Soils and Sediments: Unique Properties and Contaminant Scavenging Mechanisms (2005, background): “Work on single crystal surfaces shows that the stoichiometry of hematite must change as a function of crystallite size due to the removal of Fe(III) ions and addition of H+ at the surfaces (Trainor et al., 2004).”