Influence of cations on the strength of clayey rocks
Abstract
The strength of clay rocks is largely determined by their water content and the proportions of its various categories. At present, most authors consider water categories from the standpoint of their formation under the influence of the energy field of the clay particle. It is known that the intensity of any energy field decreases approximately exponentially, and therefore the transition of water from one category to another is gradual and smooth. When the particle field is superimposed on water, its structure is distorted as a result of changes in the character of the translational motion of water molecules.
Область исследования:
(Archived) Without section
Funding:
None
References
- Grimm R. Mineralogy of clays. Izd-vo inostr. lit-ry, 1956. (in Russian)
- Dostovalov V. N. On the Cause of Lowering of Water Freezing Temperature in Dispersed Soils from the Molecular-Kinetic Point of View. Sb. "Merzlotnye issledovaniya", MGU, iss. VII, 1967. (in Russian)
- Mikhailov I. G., Syrnikov Yu. P. About the influence of ions on the structure of water. Zh. strukturnoi khimii, vol. I, No. 1, 1960. (in Russian)
- Parkhomenko S. G. Freezing of soils and loose rocks. Mat. k osnovam ucheniya o merzlotnykh zonakh zemnoi kory. Iss. 3, 1956. (in Russian)
- Samoilov O. Ya. Structure of aqueous solutions of electrolytes and hydration of ions. AN SSSR, 1957. (in Russian)
- Fageler P. Mode of cations and water in mineral soils. Selkhozgiz, 1936. (in Russian)
- Shumsky P. A. Fundamentals of Structural Ice Science. AN SSSR, 1955. (in Russian)
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