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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Bibliographic Details
Main Author: Putnis, Christine V. (auth)
Format: Electronic Book Chapter
Language:English
Published: MDPI - Multidisciplinary Digital Publishing Institute 2019
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520 |a 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 metamorphism, metasomatism, and weathering. In recent years focus has been concentrated on mineral surface reactions made possible through the development of advanced analytical methods such as atomic force microscopy (AFM), advanced electron microscopies (SEM and TEM), phase shift interferometry, confocal Raman spectroscopy, and advanced synchrotron-based applications, to enable mineral surfaces to be imaged and analyzed at the nanoscale. Experiments are increasingly complemented by molecular simulations to confirm or predict the results of these studies. This has enabled new and exciting possibilities to elucidate the mechanisms that govern mineral-fluid reactions. In this Special Issue, "Mineral Surface Reactions at the Nanoscale", we present 12 contributions that highlight the role and importance of mineral surfaces in varying fields of research. 
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653 |a metadynamics 
653 |a minerals 
653 |a n/a 
653 |a microstructure 
653 |a dissolution-reprecipitation 
653 |a stabilization 
653 |a albite 
653 |a mineral-water interface 
653 |a simulation 
653 |a krennerite 
653 |a mineralogy 
653 |a mineral replacement 
653 |a calcite 
653 |a pyrite 
653 |a dissolution-precipitation 
653 |a goethite 
653 |a recrystallization 
653 |a gold-(silver) tellurides 
653 |a isotopes 
653 |a non-classical nucleation 
653 |a calaverite 
653 |a interfacial precipitation 
653 |a toxic metals 
653 |a metasomatism 
653 |a adsorption 
653 |a amorphous 
653 |a pre-nucleation clusters 
653 |a surface 
653 |a dissolution 
653 |a hematite 
653 |a cyanide 
653 |a MOFs 
653 |a leaching 
653 |a Raman spectroscopy 
653 |a sodalite 
653 |a carbonation 
653 |a rate spectra 
653 |a retreat velocity 
653 |a additives 
653 |a liquid precursors 
653 |a bioaragonite 
653 |a brucite 
653 |a kinetics 
653 |a re-adsorption 
653 |a brushite 
653 |a polymorphs 
653 |a dissolution-precipitation 
653 |a hydrothermal experiments 
653 |a apatite 
653 |a ferrihydrite 
653 |a mesocrystals 
653 |a catalysts 
653 |a carbonic anhydrase 
653 |a XPS 
653 |a replacement reaction 
653 |a mineral growth 
653 |a carbon capture and storage 
653 |a interfaces 
653 |a citrate 
653 |a classical nucleation theory 
653 |a REEs 
653 |a phosphate 
653 |a wollastonite 
653 |a polarization microscopy 
653 |a natural porous gold 
653 |a sylvanite 
653 |a analcime 
653 |a calcium phosphate 
653 |a Fe atom exchange 
653 |a nepheline 
653 |a biomineralisation 
653 |a interface-coupled dissolution-reprecipitation 
653 |a hydrothermal method 
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