1. Research on Deterioration Mechanism and Dynamic Triaxial Compression Characteristics of Freeze–Thaw Sandstone.
- Author
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Meng, Fandong, Zhai, Yue, Li, Yubai, Xie, Qingyu, Gao, Huan, Li, Yan, and Dong, Qi
- Subjects
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ROCK mechanics , *FREEZE-thaw cycles , *IMPACT loads , *HOPKINSON bars (Testing) , *SANDSTONE , *DAMAGE models , *NUCLEAR magnetic resonance , *SCANNING electron microscopes - Abstract
Rock engineering in cold regions is in special environment of freeze–thaw cycle (FTC) and complex stress, and its mechanical properties would be seriously affected. To investigate the effects of FTC and complex dynamics on the engineering properties of rocks, the degradation characteristics of the physical and mechanical properties of Tongchuan sandstone after different FTC have been studied through nuclear magnetic resonance test, scanning electron microscope test and split Hopkinson pressure bar test. The study found that the micropores of the sandstone increased significantly after freeze–thaw (FT), and the variation of aperture uniformity coefficient and permeability showed that FT80 was an inflection point, and the damage degree of FT80 increased sharply. When the freezing temperature is − 20 °C, the liquid water inside the pores with a pore size of not less than 3.38 nm will freeze. Failure to fully consider the effects of unfrozen porosity and water content will underestimate the ability of FT to degrade rocks. The coupling effect of FT, confining pressure (CP) and SR shows the strengthening of rock strength, in which SR has the greatest impact on the dynamic strength of FT sandstone, followed by CP, and FT damage is the least. The triaxial dynamic damage constitutive model of FT rock considering FT damage and impact load damage is established, it is verified that the proposed model is reasonable. Highlights: The microstructure evolution characteristics of sandstone after freeze–thaw damage are discussed in detail. The degradation mechanism of freeze–thaw sandstone is deeply studied and a damage model considering water content and unfrozen pores is established. The triaxial dynamic damage constitutive model of rock considering freeze–thaw damage and impact load damage is established. [ABSTRACT FROM AUTHOR]
- Published
- 2023
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