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NARROW
GeoRef Subject
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all geography including DSDP/ODP Sites and Legs
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Australasia
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Primary terms
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Australasia
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igneous rocks
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anorthosite (1)
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ultramafics
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isotopes
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radioactive isotopes (1)
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Mesozoic
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Carrara Marble (1)
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metals
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alkali metals
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cesium (1)
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alkaline earth metals
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magnesium (1)
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metamorphic rocks
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metamorphism (2)
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United States
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Montana
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Acceptance of the 2020 Roebling Medal of the Mineralogical Society of America
Stress orientation–dependent reactions during metamorphism
The replacement of a carbonate rock by fluorite: Kinetics and microstructure
Control of silicate weathering by interface-coupled dissolution-precipitation processes at the mineral-solution interface
Transient Porosity Resulting from Fluid–Mineral Interaction and its Consequences
The effect of a copolymer inhibitor on baryte precipitation
Replacement and ion exchange reactions of scolecite in a high pH aqueous solution
Surface-specific measurements of olivine dissolution by phase-shift interferometry
Influence of temperature and Cl on the hydrothermal replacement of calcite by apatite and the development of porous microstructures
Hydrothermal replacement of Aragonite by Calcite: interplay between replacement, fracturing and growth
Mechanism of leached layer formation during chemical weathering of silicate minerals
Experimental investigations into the silicification of olivine: Implications for the reaction mechanism and acid neutralization
Effects of kinetics and mechanisms of crystal growth on ion-partitioning in solid solution–aqueous solution (SS–AS) systems
Abstract Ion-partitioning between aqueous solutions and growing crystals is controlled by both the equilibrium thermodynamics of the solid solution-aqueous solution system and departures from equilibrium. In this chapter the various factors which influence ion-distribution coefficients are reviewed with specific emphasis on the role of supersatura-tion on crystal-growth mechanisms and growth rate, the role of the surface chemistry and structure of the crystal in controlling ion incorporation and finally on the role of organic molecules and background electrolytes in modifying the dynamics of water exchange around the ions which are potentially incorporated into a growing crystal. Examples to illustrate the general principles involved are taken from room-temperature experimental studies of crystal growth in solid solution-aqueous solution systems.