Capillary water retention curve and shear strength of unsaturated soils

Author:

Zhou Annan12,Huang Ruiqiu3,Sheng Daichao4

Affiliation:

1. School of Transportation Science and Engineering, Beihang University, Beijing 100191, China.

2. School of Civil, Environmental and Chemical Engineering, Royal Melbourne Institute of Technology (RMIT), Melbourne VIC 3001, Australia.

3. State Key Laboratory of Geohazards Prevention and Geoenvironment Protection, Chengdu University of Technology, Chengdu, Sichuan 610059, China.

4. National Engineering Laboratory for High-Speed Railway Construction, Central South University, Changsha, Hunan 410075, China.

Abstract

This paper proposes a new water retention model for unsaturated soils, which takes into account capillary condensation of adsorbed water. In this model, the degree of saturation of a soil is separated into that based on capillary water and that based on adsorbed water. Through analysis of a partially saturated two-cylinder system, a new shear strength criterion for unsaturated soils is proposed, in which only the degree of saturation based on capillary water contributes to the variation of shear strength with suction. The proposed shear strength criterion is justified against thermodynamic principles and is compared against existing criteria in the literature, which shows that it provides a much improved prediction of the experimental data for a wide range of suction values.

Publisher

Canadian Science Publishing

Subject

Civil and Structural Engineering,Geotechnical Engineering and Engineering Geology

Reference54 articles.

1. A constitutive model for partially saturated soils

2. A microstructurally based effective stress for unsaturated soils

3. Unsaturated soil mechanics

4. Campbell, G.S., and Shiozawa, S. 1992. Prediction of hydraulic properties of soils using particle-size distribution and bulk density data. In Indirect methods for estimating the hydraulic properties of unsaturated soils. Edited by M.T. van Genuchten, F.J. Leij, and L.J. Lund. University of California, Riverside, Calif. pp. 317–328.

5. Capillary Condensation due to van der Waals Attraction in Wet Slits

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