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Oriented-aggregate specimens of clay for X-ray analysis made by pressure

Published online by Cambridge University Press:  14 March 2018

W. A. Mitchell
W. A. Mitchell*
Affiliation:
Macaulay Institute for Soil Research, Aberdeen
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Extract

The use of preferentially oriented aggregate specimens of clay for X-ray diffraction has been widely adopted since its origination by Bradley, Grim and Clark (1937). It is an extremely useful technique giving greatly enhanced intensity of diffraction from the basal planes of platey minerals relative to that from the general planes; the amount of one particular clay mineral which can be identified in a mixture is very much less than by the normal powder method.

Type
Research Article
Information
Clay Minerals Bulletin , Volume 2 , Issue 10 , December 1953 , pp. 76 - 78
Copyright
Copyright © The Mineralogical Society of Great Britain and Ireland 1953

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References

Bradley, W. F., Grim, R. E. and Clark, G. L., 1937. Zeit. f. Krist. 97, 216–222.Google Scholar
Brown, G. 1953. J. Soil Sci. 4, 229.CrossRefGoogle Scholar
Dion, H. G., 1944. Soil Sci. 58, 411.CrossRefGoogle Scholar
Mitchell, B. D. and Mackenzie, R. C., 1953. In preparation.Google Scholar
Tamm, O. 1922. Meddel. Statens Skogsförsöksanst. 19, 385. Ibid., 26, 167.Google Scholar