Comment on “The dissolution of quartz as a function of pH and time at 70 °C” by K.G. Knauss and T.J. Wolery
- 1 June 1989
- journal article
- editorial
- Published by Elsevier in Geochimica et Cosmochimica Acta
- Vol. 53 (6) , 1469-1470
- https://doi.org/10.1016/0016-7037(89)90079-3
Abstract
No abstract availableThis publication has 10 references indexed in Scilit:
- The dissolution kinetics of quartz as a function of pH and time at 70°CPublished by Elsevier ,2003
- Spectroscopic evidence for organic diacid complexation with dissolved silica in aqueous systems—I. Oxalic acidOrganic Geochemistry, 1989
- The dissolution of quartz in dilute aqueous solutions of organic acids at 25°CGeochimica et Cosmochimica Acta, 1988
- Dissolution of quartz into dilute alkaline solutions at 90°C: A kinetic studyGeochimica et Cosmochimica Acta, 1987
- Interaction of Actinide Cations with Synthetic PolyelectrolytesRadiochimica Acta, 1987
- Increased solubility of quartz in water due to complexing by organic compoundsNature, 1987
- Dependence of albite dissolution kinetics on ph and time at 25°c and 70°cGeochimica et Cosmochimica Acta, 1986
- Quartz Dissolution as Influenced by pH and the Presence of a Disturbed Surface LayerIsrael Journal of Chemistry, 1970
- The Polymerization of Monosilicic AcidJournal of the American Chemical Society, 1954
- The Reaction of Low Molecular Weight Silicic Acids with Molybdic AcidJournal of the American Chemical Society, 1953