Water Sorption Properties of Homoionic Montmorillonite
- 1 February 1954
- journal article
- Published by Cambridge University Press (CUP) in Clays and clay minerals (National Conference on Clays and Clay Minerals)
- Vol. 3 (1) , 186-204
- https://doi.org/10.1346/ccmn.1954.0030116
Abstract
Homoionic samples of four montmorillonite clays, selected on the basis of the prop- erties which control their economic uses, were prepared by treating with two normal neutral solutions of ammonium acetate, lithium, sodium, potassium, calcium, and mag- nesium chloride. Atterberg plastic and liquid limits, slopes of the liquid limit curves, and water sorption curves were determined. Among the results suggested, the follow- ing are particularly considered: 1. The plastic state is reached when enough water is put into the system to fill all the pore space and to supply all the montmorillonite layers with water adequate for rigid layers plus a slight additional amount. 2. The type of cation is not the only factor which controls the properties of montmo- rillonite. 3. The structure of the lattice also appears to determine the properties of montmo- rillonite.Keywords
This publication has 6 references indexed in Scilit:
- The Faraday Effect of Some Molecules Chelated or Associated by Hydrogen BondingJournal of the American Chemical Society, 1954
- Crystalline Swelling of Montmorillonite: Manner of Swelling of MontmorilloniteNature, 1954
- Irreversible Dehydration in MontmorilloniteClay Minerals, 1953
- SOME CLAY‐WATER PROPERTIES OF CERTAIN CLAY MINERALS*Journal of the American Ceramic Society, 1945
- Hydration Mechanism of the Clay Mineral Montmorillonite Saturated with Various Cations1Journal of the American Chemical Society, 1940
- PLASTIC FLOW IN A NEARLY DRY CLAY BODY*Journal of the American Ceramic Society, 1936