Jointed rock mass in cold regions is often subjected to the sequential cyclic loading–unloading followed by freeze–thaw cycles. Studying the inductive correlation mechanism between the cyclic loading–unloading damage of jointed rock mass and subsequent freeze–thaw cycles is of great significance for the scientific evaluation of the long-term stability of related rock engineering projects. Sequential cyclic loading–unloading, freeze–thaw tests, and subsequent uniaxial loading were conducted on jointed rock masses, integrated with NMR, AE, and DIC monitoring, to examine how prior cyclic damage influences subsequent freeze–thaw damage and governs the macro- to meso-scale damage evolution under uniaxial loading. The results indicate that the impacts of the sequential effects of cyclic loading–unloading followed by freeze–thaw cycles on the evolution of rock mass pore structure exhibit significant scale differences. Cyclic loading–unloading primarily promote the emergence of micro- and small pores, while freeze–thaw cycles accelerate the expansion and connectivity of mesopores and macropores. Although cyclic loading–unloading have a limited impact on the overall porosity of the rock mass, the number of microscopic pores significantly increases. During the freeze‑thaw phase, frost‑heave pressure drives the interconnection and coalescence of micro‑pores, forming meso‑ and macro‑pores with increased susceptibility to frost‑heave damage, which in turn exacerbates the overall freeze‑thaw deterioration. During the stage of stable damage of the rock mass, energy and ringdown counts decrease with decreasing freezing temperature. At high levels of loading–unloading stress, the damage mechanism transitions from crack propagation to crack sliding, promoting more sudden failure. The freeze–thaw cycle dominates the process of deterioration of rock mass initiation strength and fracture toughness, and compressive strength also decreases accordingly with decreasing freezing temperature. Higher levels of macroscopic joint damage significantly reduce the peak strength of the rock mass and induce more pronounced mesoscale damage evolution under loading.
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