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
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- 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.
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