Accurate modeling of dense granular flows is critical for achieving two-phase sediment transport simulations. This study proposes an improved μ(I)-rheology model enhanced by a novel L1-regularization technique and integrates it into the Material Point Method (MPM) framework. We first identify numerical instabilities inherent to the standard μ(I)-rheology under vanishing shear rates and derive a regularization strategy to resolve ill-conditioned viscosity divergence. The reformulated model is then coupled with MPM to simulate dense granular flows problem with the large deformation characteristic, leveraging its coupled Eulerian-Lagrangian descriptions to avoid the mesh distortion. Numerical benchmarks demonstrate that the L1-regularized μ(I)-rheology achieves superior numerical conditioning while retaining fidelity to the original rheological behavior. Comparison with experimental data validate the framework’s robustness in capturing key flow dynamics.

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MPM Modelling of Dense Granular Flows with Simplified L1 Regularized Μ(I)-Rheology Model

  • Hang Feng,
  • Zhen-Yu Yin

摘要

Accurate modeling of dense granular flows is critical for achieving two-phase sediment transport simulations. This study proposes an improved μ(I)-rheology model enhanced by a novel L1-regularization technique and integrates it into the Material Point Method (MPM) framework. We first identify numerical instabilities inherent to the standard μ(I)-rheology under vanishing shear rates and derive a regularization strategy to resolve ill-conditioned viscosity divergence. The reformulated model is then coupled with MPM to simulate dense granular flows problem with the large deformation characteristic, leveraging its coupled Eulerian-Lagrangian descriptions to avoid the mesh distortion. Numerical benchmarks demonstrate that the L1-regularized μ(I)-rheology achieves superior numerical conditioning while retaining fidelity to the original rheological behavior. Comparison with experimental data validate the framework’s robustness in capturing key flow dynamics.