Soil arching is a common load transfer mechanism in geotechnical engineering, which is significantly influenced by soil particle size distribution (PSD). Existing studies have not fully understood the PSD effect, specifically the mean particle size (d50) and coefficient of uniformity (Cu), on the arching evolution and critical height. To this end, this study tries to investigate the PSD effect on the evolution of soil arching using the discrete element method. A series of two-dimensional trapdoor tests were simulated on eight specimens with varying d50 and Cu. The macroscopic responses and microscopic mechanisms were systematically analyzed. Simulations reveal that an increase in d50 or Cu leads to a reduction in the critical arching height. This indicates that coarser and better-graded granular soils promote a more rapid development of soil arching effect, thereby enhancing the initial load-transfer efficiency. At the microscopic level, specimens with larger d50 develop stronger yet sparser force chains and exhibit greater normal contact force anisotropy, while specimens with higher Cu form denser contact networks with larger coordination numbers, resulting in more stable force transmission. The findings of this study strongly suggest that PSD significantly controls the soil arching development process through its governing role in fabric formation and force chain structure. Besides, the implications of this study offer direct relevance for optimizing backfill material design in geotechnical practices, notably in pile-supported embankments and underground excavation projects.
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