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Abstract In the previous chapters it has been assumed that the deformation of a soil is uniquely determined by the stress. This means that a time dependent response has been excluded. In reality the behavior is strongly dependent on time, however, especially for clay soils. In compression of a soil the porosity decreases, and as a result there is less space available for the pore water. This pore water can be expelled from the soil, but in clays this may take a certain time, due to the small permeability. This process is called consolidation . Its basic equations are considered in this chapter.
Abstract In the previous chapters it has been assumed that the deformation of a soil is uniquely determined by the stress. This means that a time dependent response has been excluded. In reality the behavior is strongly dependent on time, however, especially for clay soils. In compression of a soil the porosity decreases, and as a result there is less space available for the pore water. This pore water can be expelled from the soil, but in clays this may take a certain time, due to the small permeability. This process is called consolidation . Its basic equations are considered in this chapter.
Consolidation
Verruijt, Arnold (author)
2017-07-26
7 pages
Article/Chapter (Book)
Electronic Resource
English
TIBKAT | 1971
|Wiley | 2007
|VACUUM CONSOLIDATION METHOD AND VACUUM CONSOLIDATION SYSTEM
European Patent Office | 2016
|