This study develops a three-dimensional fluid-particle coupling numerical model based on the discrete element method (DEM), incorporating point cloud volume sampling technology to achieve high-precision dynamic calculation of particle porosity. The model comprehensively considers the coupling effects of pore structure evolution on pore water pressure fields, establishing governing equations that couple porosity-change-induced (PI) and diffusion-induced (DI) pressurization/depressurization mechanisms. The accuracy of the proposed method is validated through three classical benchmark problems: Terzaghi’s one-dimensional consolidation, undrained triaxial tests, and the Mandel-Cryer effect. Using this approach, the complete process from liquefaction instability to reconsolidation densification in saturated loose sand is successfully simulated, accurately reproducing key liquefaction phenomena including excess pore water pressure accumulation and dissipation as well as microscopic pore structure reorganization. The study achieves quantitative separation of the relative contributions of PI and DI mechanisms during liquefaction, revealing that they synergistically constitute the fundamental control system of the entire process: the liquefaction triggering stage is primarily dominated by the PI mechanism, the development stage shows gradually increasing influence of the DI mechanism, and the reconsolidation stage is entirely controlled by the DI mechanism. This numerical framework provides a powerful tool for in-depth understanding of the fundamental physical mechanisms of soil liquefaction, offering significant theoretical and practical value for prediction and risk assessment of seismic liquefaction hazards.
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