2005Rock and Soil MechanicsRequires access

Triaxial strength and deformation properties of frozen silty clay under low confining pressure

Jianhua Hu

Open publisher page 11 citations

Abstract

High and low confining pressures have different effects on the deformational properties and mechanical index of frozen soil. Triaxial compression tests were carried out for frozen silty clay under three different temperatures and four confining pressures at different strain rates. The test results indicate that the stress-strain curves behave in the same form under different confining pressures and different strain rates at the same temperature of frozen soil; the triaxial shear strength has a linear relationship with confining pressure and temperature, and an exponential relationship with strain rate; the deformation modulus, independent of confining pressure, has a linear relationship with temperature, and an exponential relationship with strain rates. And then the deformational property is explained from the viewpoint of structural changes of frozen soil.

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What this paper is about

High and low confining pressures have different effects on the deformational properties and mechanical index of frozen soil. Triaxial compression tests were carried out for frozen silty clay under three different temperatures and four confining pressures at different strain rates. The test results indicate that the stress-strain curves behave in the same form under different confining pressures and different strain rates at the same temperature of frozen soil; the triaxial shear strength has a linear relationship with confining pressure and temperature, and an exponential relationship with strain rate; the deformation modulus, independent of confining pressure, has a linear relationship with temperature, and an exponential relationship with strain rates. And then the deformational property is explained from the viewpoint of structural changes of frozen soil.

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Available abstract

High and low confining pressures have different effects on the deformational properties and mechanical index of frozen soil. Triaxial compression tests were carried out for frozen silty clay under three different temperatures and four confining pressures at different strain rates. The test results indicate that the stress-strain curves behave in the same form under different confining pressures and different strain rates at the same temperature of frozen soil; the triaxial shear strength has a linear relationship with confining pressure and temperature, and an exponential relationship with strain rate; the deformation modulus, independent of confining pressure, has a linear relationship with temperature, and an exponential relationship with strain rates. And then the deformational property is explained from the viewpoint of structural changes of frozen soil.

Key concepts: Overburden pressure, Geotechnical engineering, Triaxial shear test, Deformation (meteorology), Materials science, Strain rate, Geology, Shear (geology)

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