What do dissolution experiments tell us about natural weathering?
- 1 March 1993
- journal article
- Published by Elsevier in Chemical Geology
- Vol. 105 (1-3), 1-15
- https://doi.org/10.1016/0009-2541(93)90115-y
Abstract
No abstract availableKeywords
This publication has 28 references indexed in Scilit:
- Control of dissolution rates of orthosilicate minerals by divalent metal–oxygen bondsNature, 1992
- On the relative dissolution rates of some oxide and orthosilicate mineralsJournal of Colloid and Interface Science, 1991
- An AEM-TEM study of weathering and diagenesis, Abert Lake, Oregon: II. Diagenetic modification of the sedimentary assemblageGeochimica et Cosmochimica Acta, 1991
- An aem-tem study of weathering and diagenesis, Abert Lake, Oregon: I. Weathering reactions in the volcanicsGeochimica et Cosmochimica Acta, 1991
- Transmission electron microscopy of subsolidus oxidation and weathering of olivineContributions to Mineralogy and Petrology, 1990
- A surface complex reaction model for the pH-dependence of corundum and kaolinite dissolution ratesGeochimica et Cosmochimica Acta, 1988
- Role of surface speciation in the low-temperature dissolution of mineralsNature, 1988
- The coordination chemistry of weathering: I. Dissolution kinetics of δ-Al2O3 and BeOGeochimica et Cosmochimica Acta, 1986
- Formation of Iddingsite Rims on Olivine: A Transmission Electron Microscope StudyClays and Clay Minerals, 1984
- Semiconducting oxides: effects of solid and solution properties on dissolution kinetics of cobaltous oxideJournal of the Chemical Society, Faraday Transactions 1: Physical Chemistry in Condensed Phases, 1981