2008
DOI: 10.1016/j.coldregions.2007.11.001
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Strength distributions of warm frozen clay and its stochastic damage constitutive model

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Cited by 93 publications
(48 citation statements)
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“…From the volumetric strain-axial strain curves, it is indicated that the volume of specimen is compressed at first and then dilated under low confining pressures, while it is merely compressed under high confining pressures. e determination method of peak values of stress-strain curves can be obtained as follows: (a) when the stress-strain curves present strain softening, the maximum value of σ 1 − σ 3 is taken as the strength of frozen soil in this paper and (b) when the stress-strain curves present strain hardening, the value of σ 1 − σ 3 at axial strain ε a � 20% is taken as the strength of frozen soil [33]. e relationship between deviatoric stress q and mean stress p is depicted in Figure 2, which indicates that the strength increases first and then decreases with increasing mean stress p.…”
Section: Test Results Analysismentioning
confidence: 99%
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“…From the volumetric strain-axial strain curves, it is indicated that the volume of specimen is compressed at first and then dilated under low confining pressures, while it is merely compressed under high confining pressures. e determination method of peak values of stress-strain curves can be obtained as follows: (a) when the stress-strain curves present strain softening, the maximum value of σ 1 − σ 3 is taken as the strength of frozen soil in this paper and (b) when the stress-strain curves present strain hardening, the value of σ 1 − σ 3 at axial strain ε a � 20% is taken as the strength of frozen soil [33]. e relationship between deviatoric stress q and mean stress p is depicted in Figure 2, which indicates that the strength increases first and then decreases with increasing mean stress p.…”
Section: Test Results Analysismentioning
confidence: 99%
“…Based on phenomenological method, basic assumptions by Lai et al [33,39] are carried out for frozen soils. At first, on a macroscale, the soil specimen, regarded as a representative volume element (abbreviated as RVE), is isotropic and contains the basic information of damage, while it is a microheterogeneous material in the mesolevel.…”
Section: Formulation Of the Damage Statistical Constitutivementioning
confidence: 99%
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“…Ohkubo et al [6] investigated the pore distribution of compacted clay by NMR. Lai et al [7] reported that the compressive strength of frozen clay linearly increased as temperature decreased and exponentially increased as the strain rate increased by studying the uniaxial compressive strength of saturated frozen clay at different strain rates and freezing temperatures. Li et al [8][9][10] made significant contributions to studies of frozen soil.…”
Section: Introductionmentioning
confidence: 99%
“…4,5 Research on creep constitutive model of frozen soil has been conducted since the 1960s. Li et al 6 established a statistical constitutive model by using the continuum damage theory and introducing the Drucker-Prager criterion as its parameter of macroscopic element strength. Based on the results that have been obtained in earlier studies, the non-linear Newtonian element can be substituted for the linear one to improve the Nishihara model.…”
Section: Introductionmentioning
confidence: 99%