Relationship between Shear Strength and Soil Water Characteristic Curve of the dispersive soil of Rioverde city, S.L.P., México
PCT-13-6_en
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Keywords

unsaturated soils
effective stress
soil-water retention curve
matric suction
triaxial test CD

How to Cite

[1]
C. A. García Ezquivel, E. Rojas González, G. Gallegos Fonseca, M. de la L. Pérez Rea, and G. Hernández Padrón, “Relationship between Shear Strength and Soil Water Characteristic Curve of the dispersive soil of Rioverde city, S.L.P., México”, PCT, vol. 7, no. 13, pp. 103–117, Jul. 2024, doi: 10.61820/pct.v7i13.1485.

Abstract

Classical soil mechanics is developed with the study of saturated soils. With it, constitutive models are established that can explain the mechanical and volumetric behavior of these two-phase systems based on Terzaghi's effective stress principle. However, in a large part of the earth's surface there are soils in an unsaturated state that present unusual behaviors. The shear strenght parameters that define the failure envelope of unsaturated soils are: effective cohesion (c´), effective friction angle (φ´) and change in shear resistance generated by change in matric suction. (φb). These parameters are important for slope stability analysis and foundation design. This article presents a series of Consolidated-Drained triaxial tests at different degrees of saturation, which were carried out in a wetting trajectory in a soil with dispersive characteristics in the city of Rioverde, S.L.P., México. The water-soil retention curve is determined for both drying and wetting trajectories with the filter paper technique. The results are presented in diagrams of effective stress vs. deviator stress (p´- q´), deviator stress vs. suction (q´-S), degree of saturation vs. effective friction angle (Sw – φ´) and degree of saturation vs. effective cohesion (Sw – c´). It is observed that the soil under study reaches a maximum resistance for a suction of 2000 kpa and is reduced by 60% for higher suction values.

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References

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