Hostname: page-component-7479d7b7d-qs9v7 Total loading time: 0 Render date: 2024-07-08T12:18:57.389Z Has data issue: false hasContentIssue false
  • English
  • Français

Reply to comments of Thomas, Bohor and Frost on Aylmore, L. A. G., Sills, I. D. and Quirk, J. P. (1970) The surface area of homoionic illite and montmorillonite clay minerals as measured by the sorption of nitrogen and carbon dioxide, Clays and Clay Minerals 18, 91.

Published online by Cambridge University Press:  01 July 2024

L. A. G. Aylmore ,
I. D. Sills  and
J. P. Quirk
L. A. G. Aylmore
Affiliation:
Department of Soil Science and Plant Nutrition, University of Western Australia, Nedlands, W.A. 6009, Australia
I. D. Sills
Affiliation:
Department of Soil Science and Plant Nutrition, University of Western Australia, Nedlands, W.A. 6009, Australia
J. P. Quirk
Affiliation:
Department of Soil Science and Plant Nutrition, University of Western Australia, Nedlands, W.A. 6009, Australia
Get access Rights & Permissions [Opens in a new window]

Abstract

An abstract is not available for this content so a preview has been provided. Please use the Get access link above for information on how to access this content.
Image of the first page of this content. For PDF version, please use the ‘Save PDF’ preceeding this image.'
Type
Letter to the Editor
Information
Clays and Clay Minerals , Volume 18 , Issue 6 , December 1970 , pp. 407 - 409
Copyright
Copyright © 1970 The Clay Minerals Society

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

Aylmore, L. A. G. and Quirk, J. P. (1960). Domain or turbostratic structure of clays: Nature 187, 1046–1048.CrossRefGoogle Scholar
Aylmore, L. A. G. and Quirk, J. P. (1967) The micropore size distribution of clay mineral systems: J. Soil Sci. 18, 1–17.CrossRefGoogle Scholar
Barrer, R. M. and McLeod, D. M. (1954) Intercalation and sorption by montmorillonite: Trans. Faraday Soc. 51, 1290–1300.CrossRefGoogle Scholar
Brooks, C. S. (1955) Nitrogen adsorption experiments on several clay minerals: Soil Sci. 79, 331–347.CrossRefGoogle Scholar
Brunauer, S. (1943): The adsorption of gases and vapours. Princeton University Press, Princeton, N.J. p. 297.Google Scholar
Cahen, Raymond M. and Marechal, Joseph (1963): Anal. Chem. 35, 259–260.CrossRefGoogle Scholar
Edwards, D. G., Posner, A. M. and Quirk, J. P. (1965) The repulsion of chloride ions by negatively charged clay surfaces. Parts II and III: Trans. Faraday Soc. 61, 2816–2823.CrossRefGoogle Scholar
Greene-Kelly, R. (1964) The specific surface areas of montmorillonite: Clay Minerals Bull. 5, 392–400.CrossRefGoogle Scholar
Quirk, J. P. (1968) Particle interaction and soil swelling: Israel J. Chem. 6, 213–234.CrossRefGoogle Scholar
Thomas, Josephus Jr. and Bohor, B. F. (1968) Surface area of montmorillonite from the dynamic sorption of nitrogen and carbon dioxide: Clays and Clay Minerals 16, 83–91.CrossRefGoogle Scholar
Thomas, Josephus Jr. and Bohor, Bruce F. (1969) Surface area of vermiculite with nitrogen and carbon dioxide as adsorbates: Clays and Clay Minerals 17, 205–209.CrossRefGoogle Scholar
Thomas, Josephus Jr., Bohor, Bruce F. and Frost, Robert R. (1970) Comments on The Surface Area of Homoionic Illite and Montmorillonite Clay Minerals as Measured by the Sorption of Nitrogen and Carbon Dioxide: Clays and Clay Minerals 18, 91.Google Scholar