This study investigates the accelerated deterioration of Damaidi rock art after summer rainfall, revealing the dry-wet degradation mechanisms of metamorphic sandstone. Based on conservation laws of mass, energy, and momentum, as well as unsaturated porous media theory, the Van Genuchten model is applied to describe water infiltration in unsaturated rock. The model accounts for solid matrix and pore fluid compressibility, thermal effects on fluid flow, and water vapor phase changes impacting rock deformation, establishing a coupled thermal-hydro-mechanical (THM) mathematical framework. Using COMSOL Multiphysics, numerical simulations of the dry-wet degradation process were conducted and validated against experimental data, including temperature, volumetric water content, and stress-strain curves. Key findings include: 1) Spatial heterogeneity in temperature and moisture fields, with boundary effects decaying with depth and a linear increase in temperature response lag; 2) Increased secondary porosity leading to a 17.8% rise in water diffusion coefficient by the 5th cycle; 3) Differential strain up to 0.12% from THM coupling, forming microcrack networks. The simulation results match experimental data with an average relative error below 8.2%, verifying the model’s accuracy in representing THM coupling behavior in unsaturated rock. These insights provide a theoretical foundation for understanding the weathering mechanisms of rock art substrates.
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