Mineral Surface Reactions at the Nanoscale

Reactions at mineral surfaces are central to all geochemical processes. As minerals comprise the rocks of the Earth, the processes occurring at the mineral–aqueous fluid interface control the evolution of the rocks and hence the structure of the crust of the Earth during processes such as metamorphi...

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Detalles Bibliográficos
Autor Principal:	Putnis, Christine V.
Formato:	Online
Idioma:	inglés
Publicado:	MDPI - Multidisciplinary Digital Publishing Institute 2021
Subjects:	QE1-996.5 Q1-390 metadynamics minerals n/a microstructure dissolution-reprecipitation stabilization albite mineral–water interface simulation krennerite mineralogy mineral replacement calcite pyrite dissolution-precipitation goethite recrystallization gold–(silver) tellurides isotopes non-classical nucleation calaverite interfacial precipitation toxic metals metasomatism adsorption amorphous pre-nucleation clusters surface dissolution hematite cyanide MOFs leaching Raman spectroscopy sodalite carbonation rate spectra retreat velocity additives liquid precursors bioaragonite brucite kinetics re-adsorption brushite polymorphs dissolution–precipitation hydrothermal experiments apatite ferrihydrite mesocrystals catalysts carbonic anhydrase XPS replacement reaction mineral growth carbon capture and storage interfaces citrate classical nucleation theory REEs phosphate wollastonite polarization microscopy natural porous gold sylvanite analcime calcium phosphate Fe atom exchange nepheline biomineralisation interface-coupled dissolution–reprecipitation hydrothermal method thema EDItEUR::R Earth Sciences, Geography, Environment, Planning
Acceso en liña:	33649
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Mineral Surface Reactions at the Nanoscale

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