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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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Guardat en:
Autor principal: Putnis, Christine V.
Format: Online
Idioma:anglès
Publicat: MDPI - Multidisciplinary Digital Publishing Institute 2021
Matèries:
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
Accés en línia:33649
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