2016
DOI: 10.3390/ma9110841
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A Coupled Thermal–Hydrological–Mechanical Damage Model and Its Numerical Simulations of Damage Evolution in APSE

Abstract: This paper proposes a coupled thermal–hydrological–mechanical damage (THMD) model for the failure process of rock, in which coupling effects such as thermally induced rock deformation, water flow-induced thermal convection, and rock deformation-induced water flow are considered. The damage is considered to be the key factor that controls the THM coupling process and the heterogeneity of rock is characterized by the Weibull distribution. Next, numerical simulations on excavation-induced damage zones in Äspö pil… Show more

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Cited by 25 publications
(15 citation statements)
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“…With the increase of the displacement load, the specimen is rst in the linear elastic stage (AB); when the cracks are rst found at the stage and the number of cracks is increasing slowly, then the specimen is in the plastic deformation stage (BC); when the number of cracks is increasing dramatically and the peak stress appears at point C, next the specimen comes to the strain-softening stage (CE), and it should be noted that the most active AE events is found in this postpeak stage at point D, which also could be observed in the uniaxial compressive laboratory experiments; and nally, the specimen comes to the residual stage (EF), and the AE activities are maintained at a lower level in this stage. e whole process of the uniaxial compression is in good agreement with the observation of laboratory experiments [42,43] and numerical simulations [24,44]. e damage evolution of the specimen is shown in Figure 4.…”
Section: Validation Of the Numerical Modelsupporting
confidence: 85%
“…With the increase of the displacement load, the specimen is rst in the linear elastic stage (AB); when the cracks are rst found at the stage and the number of cracks is increasing slowly, then the specimen is in the plastic deformation stage (BC); when the number of cracks is increasing dramatically and the peak stress appears at point C, next the specimen comes to the strain-softening stage (CE), and it should be noted that the most active AE events is found in this postpeak stage at point D, which also could be observed in the uniaxial compressive laboratory experiments; and nally, the specimen comes to the residual stage (EF), and the AE activities are maintained at a lower level in this stage. e whole process of the uniaxial compression is in good agreement with the observation of laboratory experiments [42,43] and numerical simulations [24,44]. e damage evolution of the specimen is shown in Figure 4.…”
Section: Validation Of the Numerical Modelsupporting
confidence: 85%
“…As illustrated in Figure 1, the elastic damage-based constitutive law is used to evaluate the mesomechanical damage of elements with the maximum tensile stress criterion for tensile damage and the Mohr-Coulomb criterion for shear damage. The criteria can be expressed as [30][31][32][33][34][35]…”
Section: Damage Evolution Equationmentioning
confidence: 99%
“…The ice-water phase change occurring in the unit body is regarded as the heat source, and then the heat transport of transient flow in a variably saturated porous medium is described as follows [34,35]:…”
Section: Heat Transport Equationmentioning
confidence: 99%