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This study examines the effects of wet-dry cycles on the hydraulic properties and microstructure of granite residual soil (GRS), revealing that unsaturated permeability increases with moisture content and wet-dry cycles. Key findings include a bimodal pore size distribution, with significant reductions in intra- and inter-aggregate pore volumes after six cycles, indicating changes in pore network structure. The research provides insights into the hydraulic behavior of GRS, which is crucial for slope stabili
- Author
- San Dar
- Language
- EN