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Size and Shape of Montmorillonite Crystallites

Published online by Cambridge University Press:  01 July 2024

Edward C. Jonas  and
Robert M. Oliver
Edward C. Jonas
Affiliation:
Department of Geology, The University of Texas
Robert M. Oliver
Affiliation:
Clayton Foundation Biochemical Institute, The University of Texas, Austin, Texas
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Abstract

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Spray drying dilute suspensions of bentonitic montmorillonite produces a powder that shows totally random orientation of the crystallites within a sample large enough to diffract X-rays. The powder is collected by an electrostatic precipitator and can be handled in the normal mounting processes without introducing preferred orientation. Electron micrographs show this powder to be composed on a small scale of thin, crumpled, and rolled films. The extremely small montmorillonite crystallites that make up the film are oriented with [001] directions perpendicular to the film surface. Orientation within the plane of the film is random as shown by selected area electron diffraction. Crumpling and rolling of the film is sufficient to make the orientation of [001] directions random in three dimensions in a large sample when X-ray diffraction is registered.

The X-ray diffraction patterns all show diffraction maxima (both hk and 00l), and their relative intensities with respect to each other can be determined. The line broadening of the 06 and the 003 peaks was studied. The average crystallite size as calculated from the line broadening varied from six to eleven unit layers thick for four bentonitic montmorillonites. The average lateral dimension of crystallites varied from 140 Å to 250 Å. Ratios of lateral dimensions to thickness varied from 2.3 to 3.4.

Type
Symposium on Electron-Optical Study of Smectites
Information
Clays and Clay Minerals , Volume 15 , February 1967 , pp. 27 - 33
Copyright
Copyright © 1967, The Clay Minerals Society

References

Greene-Kelly, R. (1964) The specific surface areas of montmorillonites: Clay Minerals Bull. 5, No. 31, 392–401.CrossRefGoogle Scholar
Hofmann, U., Weiss, A., Koch, G., Mehler, A. and Scholz, A. (1955) Intracrystalline swelling, cation exchange, and anion exchange of minerals of the montmorillonite group and of kaolinite: Clays and Clay Minerals, Proc. 4th Conf., Natl, Acad. Sci.— Natl. Res. Council Pub. 456, 273–87.Google Scholar
Jonas, E. C. and Kuykendall, J. R. (1966) Preparation of montmorillonites for random powder diffraction: Clay Minerals 6, No. 3, 232–6.CrossRefGoogle Scholar
Kahn, H. P. (1959) Studies on the size and shape of clay particles in aqueous suspension: Clays and Clay Minerals, Proc. 6th Conf., Pergamon Press, New York, 220–36.Google Scholar
Klug, E. P. and Alexander, L. E. (1957) X-ray Diffraction Procedures: John Wiley, New York, 491–538.Google Scholar
Longuet-Escard, J., Mering, J. and Brindley, Geo. (1960) Analysis of hk bands of montmorillonite: C.B. Acad. Sci., Paris 251, 106–8.Google Scholar
Mathieu-Sicaud, A., Mering, J. and Perrin-Bennet, C. (1951) Electron microscopic study of montmorillonite and he stoni to saturated with different cations: Bull. Soc. franc. Mineral74, 439–56.Google Scholar
Scherrer, P. (1918) Analysis of external and internal structure of colloidal particles by means of X-rays: Nachrichten von der Konig. Gesallsch. Wissensch, zu Güttingen-Math Phys. Kl., 98–100.Google Scholar
Warren, B. E. (1941) X-ray methods: Jour. Applied Physics 12, 375–83.CrossRefGoogle Scholar
Whitehouse, U. G., Jeffrey, L. M. and Debbrecht, J. D. (1960) Differential settling tendencies of clay minerals in saline waters: Clays and Clay Minerals, Proc. 7th Conf., Pergamon Press, New York, 1–79.Google Scholar