Skip to main content
Log in

Quantitative Fabric of Wet Kaolinite

  • General
  • Published:
Clays and Clay Minerals

Abstract

A method is described for quantitatively expressing orientation of kaolinite particles in a wet clay mass. Wet clay is impregnated with a polyalcohol which permits grinding of a very flat surface (without disrupting the original fabric) for quantitative X-ray measurement. In the specific procedure discussed, a Norelco diffractometer equipped with a pole figure device and a Geiger detector was employed to measure by reflection the diffracted intensity of the 002 and 020 kaolinite reflections. The amplitude of the 002 peak to the amplitude of the 020 peak is called the peak ratio, PK, which quantitatively expresses particle orientation at any chosen angle to the specimen surface. Limits of orientation are random and maximum orientation. For the kaolinite tested, truly random orientation was achieved which gave a PR = 2.0. Maximum orientation found experimentally was PR = 200 for thoroughly dispersed slurry slowly dried on a glass slide. Vertical and lateral variations can be measured either continuously or in steps of any chosen size.

This is a preview of subscription content, log in via an institution to check access.

Access this article

Price excludes VAT (USA)
Tax calculation will be finalised during checkout.

Instant access to the full article PDF.

Similar content being viewed by others

References

  • Brindley, G. W. (1953) An X-ray method for studying orientation of micaceous minerals in shales, clays, and similar materials: Min. Mag. 30, 71–78.

    Google Scholar 

  • Brindley, G. W., and Kurtossy, S. S. (1961) Quantitative determination of kaolinite by X-ray diffraction: Amer. Min. 46, 1205–15.

    Google Scholar 

  • Hayes, J. B. (1963) Kaolinite from Warsaw geodes, Keokuk region, Iowa: Iowa Acad. Sci. 70, 261–72.

    Google Scholar 

  • Mitchell, J. K. (1956) The fabric of natural clays and its relation to engineering properties: Proc. High. Res. Bd. 35, 693–713.

    Google Scholar 

  • Raitburd, C. M. (1958) The use of X-ray structural analysis in the study of the crystal-lographic orientation of clay minerals: Conf. on Research Use Clays, May–June 1957, 779–94; Translation by Alice A. Parcel, U.S.G.S., Menlo Park, California.

    Google Scholar 

  • Raitburd, C. M. (1960) Study of microstructure of clay by the X-ray method: Akad. Nauk. CCCR, Kom no Izucheniyer Glin Otdel. Geol.-Geograf. Nauk., 108–17; Translation by Alice A. Parcel U.S.G.S., Menlo Park, California.

    Google Scholar 

Download references

Author information

Authors and Affiliations

Authors

Rights and permissions

Reprints and permissions

About this article

Cite this article

Martin, R.T. Quantitative Fabric of Wet Kaolinite. Clays Clay Miner. 14, 271–287 (1966). https://doi.org/10.1346/CCMN.1966.0140124

Download citation

  • Published:

  • Issue Date:

  • DOI: https://doi.org/10.1346/CCMN.1966.0140124

Navigation