Experiments on the Decomposition of Silicates and Discussion of Chemical Weathering
- 1 February 1961
- journal article
- Published by Cambridge University Press (CUP) in Clays and clay minerals (National Conference on Clays and Clay Minerals)
- Vol. 10 (1) , 443-459
- https://doi.org/10.1346/ccmn.1961.0100139
Abstract
Experimental investigations of chemical weathering in which powders of potassium feldspar, albite, leucite, muscovite, tremolite, olivine, and volcanic glass are treated with pure water and with dilute solutions of sulfuric, carbonic, and hydrochloric acid have been performed in an apparatus in which the mineral powder is exposed to a circulating water flow. The experiments have been continued recently by treating kaolinite and montmorillonite. The course of decomposition of these minerals depends on water flow rate, grain size, temperature, and pH of the solutions. These experiments in open systems are compared with investigations reported in the literature and with the conditions of natural weathering.Keywords
This publication has 5 references indexed in Scilit:
- Aluminium Ions in Aluminium Hydroxide, Phosphate and Soil–Water SystemsNature, 1960
- Some mineralogical equilibria in the system K 2 O-Al 2 O 3 -SiO 2 -H 2 OAmerican Journal of Science, 1959
- Some Experiments on the Interaction between Feldspars and Salt SolutionsGeologiska Föreningen i Stockholm Förhandlingar, 1956
- Die chemische Verwitterung der SilikateThe Science of Nature, 1940
- THE INFLUENCE OF ELECTROLYTES UPON THE ELECTROPHORETIC MIGRATION OF BACTERIA AND OF YEAST CELLSThe Journal of general physiology, 1926