The Thermal Characteristics of Soil Minerals and the Use of These Characteristics in the Qualitative and Quantitative Determination of Clay Minerals in Soils-Reference-Cited by-同舟云学术

The Thermal Characteristics of Soil Minerals and the Use of These Characteristics in the Qualitative and Quantitative Determination of Clay Minerals in Soils

Published:1975 Issue: Volume: Page:529-571
ISSN:
Container-title:Soil Components
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Author:

Mackenzie R. C.,Caillère S.

Publisher

Springer Berlin Heidelberg

Link

http://link.springer.com/content/pdf/10.1007/978-3-642-65917-1_16.pdf

Reference117 articles.

1. Agafonoff, V., 1935. Etude mineralogique du sol. Trans. 3rd Int. Cong. Soil Sci. 3:74.

2. Allaway, W. H., 1949. Differential thermal analysis of clays treated with organic cations as an aid in the study of soil colloids. Proc. Soil Sci. Soc. Am. 13:183.

3. Bain, D. C., 1972. Oxidation of chlorites in soil clays and effect on DTA curves. Nature Phys. Sci. 238:142.

4. Barshad, I., 1948. Vermiculite and its relation to biotite as revealed by base exchange reactions, X-ray analysis, differential thermal curves and water content. Am. Mineral. 33:655.

5. Bradley, W. F., and R. E. Grim., 1951. High-temperature thermal effects of clay and related minerals. Am. Mineral. 36:182.

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