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The collapse mechanism in partly saturated soil
Abstract A study has been made of the metastable structure of partly saturated soilt that collapse when wetted under load. This has been done using the scanning electron microscope on air-dried specimens of collapsing soil representative of various types. These include aeolian sand from South Africa, loess from Europe, clay from America and a range of compacted soils. The nature of the intergranular contacts has been studied at magnifications up to 20,000. It is shown that a common basic collapse mechanism applies to the different types of soil ranging from sand to clay.
The collapse mechanism in partly saturated soil
Abstract A study has been made of the metastable structure of partly saturated soilt that collapse when wetted under load. This has been done using the scanning electron microscope on air-dried specimens of collapsing soil representative of various types. These include aeolian sand from South Africa, loess from Europe, clay from America and a range of compacted soils. The nature of the intergranular contacts has been studied at magnifications up to 20,000. It is shown that a common basic collapse mechanism applies to the different types of soil ranging from sand to clay.
The collapse mechanism in partly saturated soil
Barden, L. (author) / McGown, A. (author) / Collins, K. (author)
Engineering Geology ; 7 ; 49-60
1973-02-02
12 pages
Article (Journal)
Electronic Resource
English
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