Hostname: page-component-586b7cd67f-2brh9 Total loading time: 0 Render date: 2024-11-25T09:39:20.980Z Has data issue: false hasContentIssue false
  • English
  • Français

Hydration properties of vermiculite

Published online by Cambridge University Press:  14 March 2018

J. Keay  and
A. Wild
J. Keay
Affiliation:
The University, Reading
A. Wild
Affiliation:
The University, Reading
Get access

Abstract

Dehydration curves have been obtained for vermiculite saturated with Mg2+, Ca2+, Sr2+, Ba2+ and Na2+. Three of the hydration phases of Mg-vermiculite give energies of hydration of −3·8±0·1, −5·5±0·1, and −18±3 K cal per mole of water. The heat of hydration of vermiculite has been found to vary with the saturating cation, and to decrease with decreasing energy of hydration of the cation. Values for the heats of hydration of vermiculite saturated with Mg2+, Ca2+, Sr2+, Ba2+ and Na+ are reported.

Type
Research Article
Information
Clay Minerals Bulletin , Volume 4 , Issue 25 , July 1961 , pp. 221 - 228
Copyright
Copyright © The Mineralogical Society of Great Britain and Ireland 1961

Access options

Get access to the full version of this content by using one of the access options below. (Log in options will check for institutional or personal access. Content may require purchase if you do not have access.)

References

Keay, J., 1960. Ph.D. Thesis, University of Reading.Google Scholar
Matsuura, T., 1954. Bull. chem. Soc., Japan, 27, 281.Google Scholar
Walker, G. F., and Milne, A., 1950. Trans. Fourth Int. Congr. Soil Sci., 2, 62.Google Scholar
Walker, G. F., 1956. Clays and Clay Minerals (A. Swineford, editor). Nat.Acad. Sci.-Nat. Res. Counc., Washington, Publ. 456, p. 101.Google Scholar
Walker, G. F., and Cole, W. F., 1957. The Differential Thermal Investigationof Clays (R. C. Mackenzie, editor). Mineralogical Society, London. Chapter 7, p. 191.Google Scholar