Rock damage constitutive model based on residual intensity characteristics under freeze-thaw and load

被引:0
|
作者
Zhang H. [1 ]
Meng X. [2 ]
Peng C. [3 ]
Yang G. [2 ]
Ye W. [2 ]
Shen Y. [2 ]
Liu H. [2 ]
机构
[1] School of Science, Xi'an University of Science and Technology, Xi'an
[2] College of Architecture and Civil Engineering, Xi'an University of Science and Technology, Xi'an
[3] Infrastructure Branch of China Construction Eighth Bureau Third Construction Co., Ltd., Nanjing
来源
关键词
Constitutive model; Damage; Freeze-thaw cycle; Model parameter; Residual strength;
D O I
10.13225/j.cnki.jccs.2018.1681
中图分类号
学科分类号
摘要
The deformation and failure characteristics of rock are the fundamental mechanics problems directly faced in a geotechnical engineering construction project in cold region. To simulate the whole process of rock deformation and failure under freeze-thaw and load, the rock micro-elements in the axial direction are abstracted into four parts: the undamaged part, the freeze-thaw damaged part, the loading damaged part and the coupling damaged part of freeze-thaw and load, and the axial stress is supported by the four parts together, with the three damaged parts can share the residual stress. Using the Weibull distribution to describe the heterogeneity of rock materials, the coupling effect of the freeze-thaw and load on the total damage is expressed quantitatively based on the D-P failure criterion, and the damage constitutive model based on the characteristics of the residual strength is established for freeze-thaw and loaded rock. In terms of rock deformation and failure characteristics, the theoretical expression of the model parameters is derived. To verify the rationality of the model, the freeze-thaw cycle and triaxial compression tests of the red sandstone is conducted, the law of rock deformation and failure is analyzed, the effects of freeze-thaw cycles and confining pressure on their mechanical properties are revealed. It is shown that the damage model reflects the whole process of deformation and failure of freeze-thaw and loaded rock, at the same time, the effects of freeze-thaw cycles and confining pressure on the deformation properties of rock can be characterized. The evolution path of total damage reflects the consistency of the micro-mechanical response and macroscopic characteristics of the deformation and failure of rock, and the nonlinear influence characteristics of freeze-thaw and load on total damage expansion is portrayed, the macroscopic mechanical effects induced by mesoscopic damage evolution are explored which can provide a theoretical basis for revealing the mechanism of rock freeze-thaw damage. © 2019, Editorial Office of Journal of China Coal Society. All right reserved.
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页码:3404 / 3411
页数:7
相关论文
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