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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