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The identification of minerals in soil colloids

Published online by Cambridge University Press:  27 March 2009

G. Nagelschmidt
G. Nagelschmidt
Affiliation:
Chemistry Department, Rothamsted Experimental Station, Harpenden
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Extract

X-ray, optical, dehydration and chemical methods in use for the identification of minerals in soil colloids are discussed with special regard to their limitations. These are mainly due to uncertainties about the variation of physical properties of standard minerals with decreasing grain size and the possible existence and importance of amorphous material. The aggregate method in X-ray analysis, which is specially important for soil colloids, is described. Various techniques for dehydration and optical analysis are discussed, and it is concluded that they are useful only when used in combination with X-ray data. The advantages of combining various chemical methods with X-ray analysis are pointed out.

Standard data are given for a number of minerals, and the evidence for their occurrence in soil colloids is reviewed. These minerals are quartz, cristobalite, oxides and hydroxides of iron and aluminium, minerals of the kaolinite, montmorillonite and mica groups.

Type
Research Article
Information
The Journal of Agricultural Science , Volume 29 , Issue 4 , October 1939 , pp. 477 - 501
Copyright
Copyright © Cambridge University Press 1939

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