Control of dissolution rates of orthosilicate minerals by divalent metal–oxygen bonds
- 1 January 1992
- journal article
- letter
- Published by Springer Nature in Nature
- Vol. 355 (6356) , 157-159
- https://doi.org/10.1038/355157a0
Abstract
No abstract availableKeywords
This publication has 8 references indexed in Scilit:
- Olivine dissolution at 25°C: Effects of pH, CO2, and organic acidsGeochimica et Cosmochimica Acta, 1991
- Mechanisms of silica dissolution as inferred from the kinetic isotope effectGeochimica et Cosmochimica Acta, 1990
- Coordination chemistry of weathering: Kinetics of the surface‐controlled dissolution of oxide mineralsReviews of Geophysics, 1990
- Controls on silicate dissolution rates in neutral and basic pH solutions at 25°CGeochimica et Cosmochimica Acta, 1989
- Role of surface speciation in the low-temperature dissolution of mineralsNature, 1988
- Acid dissolution of willemite (Zn, Mn)2 SiO4) and hemimorphite (Zn4Si2O7(OH)2 H2O)Metallurgical Transactions B, 1983
- Mechanism of pyroxene and amphibole weathering—I. Experimental studies of iron-free mineralsGeochimica et Cosmochimica Acta, 1981
- The mechanism of octahedral complex formation by labile metal ionsCoordination Chemistry Reviews, 1970