The Discrete Element Method (DEM) with microscopic numerical model of fluid flow is applied for simulating fluidized debris flow to examine the effect of excessive pore water pressure. The model uses a two-way coupling scheme, that is, the model solves fluid pressure in void spaces surrounded by particle elements used in the DEM to consider compressibility of fluid by particle movement and fluid flow across the void space by pressure difference, on the other hand, the calculated fluid pressure is applied for particles involved in the void space as a body force in proportional to occupied area in the void space. Also, the scheme uses a grid-generation method with advancing-front technique to update boundary fluid-grids automatically during calculation. Numerical simulations are conducted to mimic a simple fluidized debris flow, which was done by lab-scale test. The results are compared with experimental data of lab-scale test, also simulation result of dry condition and different permiability. As a result, it is clarified that the microscopic fluid flow model represents localized pore water pressure under dynamics of particles, and is a useful tool to analyze fluidized landslide and debris flow.
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