- Article
Experimental Study on Crack Propagation and Changes in Micropores of Clay Under Dry–Wet Cycles
- Fan Zhang,
- Zengguang Xu and
- Junyu Zhao
- + 4 authors
Clay cracking is a widespread phenomenon in natural environments, and the presence of cracks significantly influences the physical–mechanical properties and hydraulic permeability of soils. To investigate the evolution of clay cracks and the associated changes in internal pore structure, laboratory wetting–drying cycle experiments combined with nuclear magnetic resonance (NMR) analyses were conducted. The results indicate that differences in clay dry density exert a strong influence on the initiation of major cracks. After three or four wetting–drying cycles, major cracks open abruptly rather than through a gradual process. Subsequently, all cracks continue to develop, accompanied by an increase in crack area. During the drying process, the area of major cracks increases with decreasing water content, and the crack growth rate exhibits a slow–fast–slow trend. The pores of the tested clay are predominantly micropores, and pore water mainly exists in the form of bound water. The opening of major cracks has a pronounced effect on pore water content, and significant changes in pore size distribution occur during subsequent wetting–drying cycles after major crack initiation.
8 February 2026





