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Abstract Feda, J., 1988. Collapse of loess upon wetting. Eng. Geol., 25: 263–269. The results of a series of tests conducted on loess samples from one locality, tested under the condition of confined and hydrostatic compression are presented and analyzed. The samples are of different water content and saturation and display different degrees of collapse upon wetting. Based on the experimental results, a collapse surface is depicted and the phenomenon hypothetically generalized for other types of collapse. The structural collapse causes the mechanical behaviour of samples to be more uniform. The effect of the hydrostatic stress conditions is reflected in the tendency of samples to deform isotropically, although, originally, they are anisotropic. The phenomenon of collapse cannot be explained by the principle of effective stresses.
Abstract Feda, J., 1988. Collapse of loess upon wetting. Eng. Geol., 25: 263–269. The results of a series of tests conducted on loess samples from one locality, tested under the condition of confined and hydrostatic compression are presented and analyzed. The samples are of different water content and saturation and display different degrees of collapse upon wetting. Based on the experimental results, a collapse surface is depicted and the phenomenon hypothetically generalized for other types of collapse. The structural collapse causes the mechanical behaviour of samples to be more uniform. The effect of the hydrostatic stress conditions is reflected in the tendency of samples to deform isotropically, although, originally, they are anisotropic. The phenomenon of collapse cannot be explained by the principle of effective stresses.
Collapse of loess upon wetting
Feda, Jaroslav (Autor:in)
Engineering Geology ; 25 ; 263-269
03.09.1986
7 pages
Aufsatz (Zeitschrift)
Elektronische Ressource
Englisch
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