A damage-softening and dilatancy prediction model of coarse-grained materials considering freeze-thaw effects

被引:19
|
作者
Ling, Xianzhang [1 ,2 ]
Tian, Shuang [1 ,2 ]
Tang, Liang [1 ,2 ]
Li, Shanzhen [1 ,2 ]
机构
[1] Harbin Inst Technol, Sch Civil Engn, Harbin 150090, Heilongjiang, Peoples R China
[2] Chinese Acad Sci, State Key Lab Frozen Soil Engn, Northwest Inst Ecoenvironm & Resources, Lanzhou 730000, Gansu, Peoples R China
基金
中国国家自然科学基金;
关键词
Prediction model; Strain-softening; Dilatancy; Coarse-grained material; Freeze-thaw cycle; CONSTITUTIVE MODEL; SHEAR-STRENGTH; MECHANICAL-PROPERTIES; STATE PARAMETER; SALINE SOILS; BEHAVIOR; CONSTRUCTION; MODULUS; BALLAST; CYCLES;
D O I
10.1016/j.trgeo.2019.100307
中图分类号
TU [建筑科学];
学科分类号
0813 ;
摘要
The variations in mechanical properties of coarse-grained materials (CGM) caused by freeze-thaw cycles must be considered when designing subgrades in seasonally frozen regions. In this study, consolidated-drained triaxial tests are performed to investigate the properties of CGM under different numbers of freeze-thaw cycles and effective confining pressures. Typical test results are presented and discussed. Strain softening and dilatancy are observed during shearing. Motivated by experimental observations, a stress-strain prediction model that can reflect the residual strength is proposed, using the framework of continuum damage mechanics. A dilatancy prediction equation is then developed by taking the deviatoric stress as the rate of energy consumption. The effect of freeze-thaw cycles on the mechanical behaviour of CGM is fully incorporated in the degradation of the elastic modulus, peak, and residual strengths in the current model. A comparison of the predicted and test results highlights the suitability of the proposed model for capturing the effect of freeze-thaw cycles on the mechanical properties of CGM. Overall, the investigation demonstrates the potential for using strain-softening and dilatancy models to predict geotechnical degradation characteristics of CGM in seasonally cold regions.
引用
收藏
页数:13
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