Abstract
Matric suction can be used as one of the principal stress state variable to define the constitutive behavior of collapsing soils. The collapse behavior of a compacted soil was studied in the laboratory using a modified conventional oedometer and a tensiometer for the measurement of matric suction. The results show that collapse is a transient, continuous process. The results were used to model the volume change of a collapsible soil during wetting. The theoretical formulations derived for the model were based on unsaturated soil mechanics principles. Results obtained from the numerical model compared well with the laboratory measurements.
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© 1995 Springer Science+Business Media Dordrecht
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Fredlund, D.G., Gan, J.KM. (1995). The Collapse Mechanism of a Soil Subjected to One-Dimensional Loading and Wetting. In: Derbyshire, E., Dijkstra, T., Smalley, I.J. (eds) Genesis and Properties of Collapsible Soils. NATO ASI Series, vol 468. Springer, Dordrecht. https://doi.org/10.1007/978-94-011-0097-7_9
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DOI: https://doi.org/10.1007/978-94-011-0097-7_9
Publisher Name: Springer, Dordrecht
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