Resumen
To investigate the effects of long-term freeze?thaw cycles on the physical and mechanical properties as well as the attenuation trend of rocks, this study conducted saturated freeze?thaw tests on coarse sandstone and fine sandstone samples collected from the slopes of Muli Coal Mine in Qinghai Province. The samples underwent different numbers of freeze?thaw cycles, and their porosity, longitudinal wave velocity, and uniaxial compression strength were studied. The variations in the physical and mechanical properties of the two types of sandstone with respect to the number of freeze?thaw cycles were analyzed. Take uniaxial compressive strength (UCS) as the integrity index, and decay laws of rock integrity were analyzed based on the decay equation suggested in previous studies. We found that the decay index ?, which is commonly assumed to be constant, varies with the number of freeze?thaw cycles. Furthermore, the ? values varied between different rock types. For fine sandstone, the ? decreases with an increase in the number of freeze?thaw cycles, ranging from 0.00385 to 0.005. However, for coarse sandstone, the ? initially decreases and then increases with an increase in the number of freeze?thaw cycles. The range of ? for coarse sandstone is between 0.00376 and 0.00481. Finally, we established a relationship between the decay index, porosity, and longitudinal wave velocity in the fine sandstones. This relationship provides a more straightforward way to evaluate the integrity of fine sandstones subjected to different numbers of freeze?thaw cycles.