Forsteritic olivine: effect of crystallographic direction on dissolution kinetics
- 31 May 2000
- journal article
- Published by Elsevier in Geochimica et Cosmochimica Acta
- Vol. 64 (10) , 1765-1772
- https://doi.org/10.1016/s0016-7037(99)00442-1
Abstract
No abstract availableKeywords
This publication has 14 references indexed in Scilit:
- What do dissolution experiments tell us about natural weathering?Published by Elsevier ,2003
- Directional dissolution kinetics of willemiteGeochimica et Cosmochimica Acta, 1993
- Olivine dissolution kinetics at near-surface conditionsChemical Geology, 1992
- Control of dissolution rates of orthosilicate minerals by divalent metal–oxygen bondsNature, 1992
- Olivine dissolution at 25°C: Effects of pH, CO2, and organic acidsGeochimica et Cosmochimica Acta, 1991
- Neutralization of industrial waste acids with olivine — The dissolution of forsteritic olivine at 40–70°CChemical Geology, 1989
- Weathering, the carbon cycle, and the differentiation of the continental crust and mantleJournal of Geophysical Research, 1988
- Role of surface speciation in the low-temperature dissolution of mineralsNature, 1988
- Changes in surface area and morphology and the mechanism of forsterite dissolutionGeochimica et Cosmochimica Acta, 1978
- Dislocation substructure of mantle-derived olivine as revealed by selective chemical etching and transmission electron microscopyPhysics and Chemistry of Minerals, 1978