Study on the simulation method and mesoscopic characteristics of rock freeze-thaw damage

被引:45
作者
Feng, Qiang [1 ]
Hou, Shaojie [1 ]
Liu, Weiwei [1 ]
Zhang, Shuang [1 ]
Li, Wenshuai [1 ]
Tian, Maolin [1 ]
机构
[1] Shandong Univ Sci & Technol, Sch Civil Engn & Architecture, Shandong Key Lab Civil Engn Disaster Prevent & Mit, Qingdao 266590, Peoples R China
关键词
CT scanning test; Freeze-thaw cycle; Frost heaving coefficient; Melting coefficient; Numerical simulation method; Damage characteristics; CT;
D O I
10.1016/j.compgeo.2022.105038
中图分类号
TP39 [计算机的应用];
学科分类号
081203 ; 0835 ;
摘要
The damage to saturated rock caused by freeze-thaw cycles seriously affects the stability of projects in cold regions. To accurately obtain the mechanical characteristics of rock after freeze-thaw damage, this paper ex-tracts the microscopic pore structure parameters of freeze-thaw sandstone based on CT scanning tests. Functional relationships between the number of freeze-thaw cycles and both the frost heaving coefficient and thawing coefficient of pore particles are established, and a new method to simulate the mechanical behavior of freezing -thawing rock is proposed based on PFC3D. The CT test results show that the freeze-thaw cycle causes a certain degree of damage to the mesopore structure of sandstone. The sensitivity of each pore structure parameter to characterize the damage is pore volume > effective porosity > porosity > pore radius > fractal dimension > throat length > throat radius > coordination number. Numerical simulation results show that with the increase in the number of freeze-thaw cycles, the internal damage degree of sandstone is more obvious, and the bearing capacity declines. In addition, the rock mainly produces tensile cracks during the freeze-thaw cycle, and failure occurs first outside the rock. The research results reveal the freeze-thaw damage mechanism of rock more accurately.
引用
收藏
页数:22
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