Influence of cations on the strength of clayey rocks
Abstract
The strength of clay rocks is largely determined by their water content and the ratio of its various categories. At present, most authors consider the types of water categories in terms of their formation under the influence of the energy field of the clay particle. It is known that the strength of any energy field decreases according to the law close to exponential, so the transition of water from one category to another is gradual and smooth. When imposing a particle field on water, its structure is distorted due to changes in the nature of tRASslational motion of water molecules.
Область исследования:
(Archived) Without section
References
- Grimm R. Mineralogy of clays. PH of Foreign Literature, 1956.
- Dostovalov V. N. On the Cause of Lowering of Water Freezing Temperature in Dispersed Soils from the Molecular-Kinetic Point of View. In the collection: Permafrost Research, MSU, iss. VII, 1967.
- Mikhailov I. G., Syrnikov Yu. P. About the influence of ions on the structure of water. Journal of Structural Chemistry, vol. I, No. 1, 1960.
- Parkhomenko S. G. Freezing of soils and loose rocks. Mat. to the bases of the doctrine of permafrost zones of the Earth's crust. Iss. 3, 1956.
- Samoilov O. Ya. Structure of aqueous solutions of electrolytes and hydration of ions. AS USSR, 1957.
- Fageler P. Mode of cations and water in mineral soils. Selkhozgiz, 1936.
- Shumsky P. A. Fundamentals of Structural Ice Science. AS USSR, 1955.
Similar articles
Approximate calculation of circular groundwater intakes by gallery method
1971 V. M. Maximov, V. P. Ilyin
Pollution of mine water at open-pit mines in the Tikhvin mining district
1971 V. N. Novozhilov, M. S. Kotova, V. N. Krylov
Determination of filtration losses from the Kronotsky HPP reservoir
1971 V. I. Davidovich, S. Ya. Zhukovsky, N. P. Krasilnikova