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Recent work on clays and clay minerals of the Wagingen group

Published online by Cambridge University Press:  14 March 2018

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Extract

Clay mineral research was started at Wagingen in 1935 by Dr F. A. van Baren. Later Dr J. Ch. L. Favejee continued his work. Some papers were published on X-ray work, based on Dutch clays. The clay fractions of Dutch clays are mixtures of quartz, illite, kaolinite and montmorillonite in varying proportions. Favejee and Hardon analysed also a number of characteristic soil colloids from Java. The lateritic soils contain kaolinite; the very heavy black clays are montmorillonite, the terra-rossa soils on limestones contain (meta) halloysite; the same mineral was found in the (podzolic) mountain soils. In the true residual soils no mixtures of clay minerals were observed.

Type
Research Article
Copyright
Copyright © The Mineralogical Society of Great Britain and Ireland 1947

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References

Publications

Edelman, C. H., 1935. Relations between the crystal structure of minerals and their base-exchange capacity. Trans. 3rd Intern. Congr. Soil Science 3, 9799.Google Scholar
Edelman, C. H., van Baren, F. A. and Favejee, J. C. L., 1939. Mineralogische onderzoekingen aan klcien en kleimineralen. 1. General discussion of the mineralogical composition of clays and qualitative X-ray analyses of some Dutch clays. Mededeelingen, Landbouwhooge school 43, 5, 4152.Google Scholar
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