Hostname: page-component-cd9895bd7-dk4vv Total loading time: 0 Render date: 2024-12-23T11:14:07.300Z Has data issue: false hasContentIssue false
  • English
  • Français

Appearance of Long-Spacing Reflection Larger Than 24 Å for Glycolated Interstratified Kaolinite/Smectite

Published online by Cambridge University Press:  28 February 2024

Katsutoshi Tomita ,
Hidewo Takahashi  and
Motoharu Kawano
Katsutoshi Tomita
Affiliation:
Institute of Earth Sciences, Faculty of Science, Kagoshima University, 1-21-35 Korimoto, Kagoshima 890, Japan
Hidewo Takahashi
Affiliation:
Department of Geology, Faculty of Education, Kagoshima University, 1-20-6 Korimoto, Kagoshima 890, Japan
Motoharu Kawano
Affiliation:
Department of Environmental Sciences and Technology, Faculty of Agriculture, Kagoshima University, 1-21-24, Korimoto, Kagoshima 890, Japan
Rights & Permissions [Opens in a new window]

Abstract

An abstract is not available for this content so a preview has been provided. As you have access to this content, a full PDF is available via the ‘Save PDF’ action button.
Image of the first page of this content. For PDF version, please use the ‘Save PDF’ preceeding this image.'

Keywords

Interstratifled kaolinite/smectiteLong-spacing
Type
Notes
Information
Clays and Clay Minerals , Volume 43 , Issue 5 , October 1995 , pp. 643 - 645
Copyright
Copyright © 1995, The Clay Minerals Society

References

Hendricks, S. B., and Teller, E. A. 1942. X-ray interference in partially ordered layer lattices. J. Chem. Phys. 10: 146–167.Google Scholar
Kakinoki, J., and Komura, Y. 1952. Intensity of X-ray diffraction by a one-dimensionally disordered crystal. I. General derivation in cases of the “Reichweite” S = 0 and 1. J. Phys. Soc. Japan 7: 30–35.CrossRefGoogle Scholar
Kakinoki, J., and Komura, Y. 1954a. Intensity of X-ray diffraction by a one-dimensionally disordered crystal. II. General derivation in the case of the correlation range S ≥ 2. J. Phys. Soc. Japan 9: 169–176.Google Scholar
Kakinoki, J., and Komura, Y. 1954b. Intensity of X-ray diffraction by a one-dimensionally disordered crystal. III. The close-packed structure. J. Phys. Soc. Japan 9: 177–183.Google Scholar
Kakinoki, J., and Komura, Y. 1965. Diffraction by a one-dimensionally disordered crystal. I. The intensity equation. Acta Crystallogr. 17: 579–586.Google Scholar
Reynolds, R. C., 1980. Interstratified clay minerals. In Crystal Structures of Clay Minerals and Their X-Ray Identification. Brindley, G. W., and Brown, G., eds. London: Min-eralogical Society, 249–303.Google Scholar
Reynolds, R. C., 1983. Calculation of absolute diffraction intensities for mixed-layered clays. Clays & Clay Miner. 31: 233–234.Google Scholar
Tomita, K., and Takahashi, H. 1986. Quantification curves for the X-ray powder diffraction analysis of mixed-layer kaolinite/smectite. Clays & Clay Miner. 34: 323–329.Google Scholar