A novel unified elastoplasticity-μ(I) phase transition model for granular flows from solid-like to fluid-like states and its application

Accurate continuum modelling of granular flows is essential for predicting geohazards such as flow-like landslides and debris flows. Achieving such precision necessitates both a robust constitutive model for granular media and a numerical solver capable of handling large deformations. In this work, a novel unified phase transition constitutive model for granular media is proposed that follows a generalized Maxwell framework. The stress is divided into an elastoplastic part and a viscous part. The former utilizes a critical-state-based elastoplasticity model, while the latter employs a strain acceleration-based μ ( I ) rheology model. Key characteristics such as nonlinear elasticity, nonlinear plastic hardening, stress dilatancy, and critical state concept are incorporated into the elastoplasticity model, and the non-Newtonian μ ( I ) rheology model considers strain rate and strain acceleration (i.e., a higher-order derivative of strain) to capture changes in accelerated and decelerated flow conditions. A series of element tests is simulated using the proposed unified phase transition model, demonstrating that the novel theory effectively describes the transition of granular media from solid-like to fluid-like states in a unified manner. The proposed unified model is then implemented within the material point method (MPM) framework to simulate 2D and 3D granular flows. The results show remarkable consistency with results from experiments and other numerical methods, demonstrating the model's accuracy in capturing solid-like behaviour during inception and deposition, as well as liquid-like behaviour during propagation. • A novel unified elastoplasticity- μ ( I ) phase transition model for granular media is proposed. • Nonlinear elasticity, dilatancy, and critical state are captured in elastoplasticity. • Dependence on strain rate and strain acceleration are considered in μ ( I ) rheology. • The proposed constitutive model is well-verified against laboratory element tests. • Proposed phase transition model is implemented in MPM and validated against experiment results.

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Publication Details

Journal
Engineering Geology
Published
2025-04-06
DOI
https://doi.org/10.1016/j.enggeo.2025.108054
Citations
6
Primary Topic
Granular flow and fluidized beds
Type
article
Field-Weighted Citation Impact
8.01

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article

A novel unified elastoplasticity-μ(I) phase transition model for granular flows from solid-like to fluid-like states and its application

Weijian Liang, Zhen‐Yu Yin, Hang Feng
6 citations
Engineering Geology
Granular flow and fluidized beds
8.01
article

A novel unified elastoplasticity-μ(I) phase transition model for granular flows from solid-like to fluid-like states and its application

Weijian Liang, Zhen‐Yu Yin, Hang Feng
article en
6 citations

Abstract

Accurate continuum modelling of granular flows is essential for predicting geohazards such as flow-like landslides and debris flows. Achieving such precision necessitates both a robust constitutive model for granular media and a numerical solver capable of handling large deformations. In this work, a novel unified phase transition constitutive model for granular media is proposed that follows a generalized Maxwell framework. The stress is divided into an elastoplastic part and a viscous part. The former utilizes a critical-state-based elastoplasticity model, while the latter employs a strain acceleration-based μ ( I ) rheology model. Key characteristics such as nonlinear elasticity, nonlinear plastic hardening, stress dilatancy, and critical state concept are incorporated into the elastoplasticity model, and the non-Newtonian μ ( I ) rheology model considers strain rate and strain acceleration (i.e., a higher-order derivative of strain) to capture changes in accelerated and decelerated flow conditions. A series of element tests is simulated using the proposed unified phase transition model, demonstrating that the novel theory effectively describes the transition of granular media from solid-like to fluid-like states in a unified manner. The proposed unified model is then implemented within the material point method (MPM) framework to simulate 2D and 3D granular flows. The results show remarkable consistency with results from experiments and other numerical methods, demonstrating the model's accuracy in capturing solid-like behaviour during inception and deposition, as well as liquid-like behaviour during propagation. • A novel unified elastoplasticity- μ ( I ) phase transition model for granular media is proposed. • Nonlinear elasticity, dilatancy, and critical state are captured in elastoplasticity. • Dependence on strain rate and strain acceleration are considered in μ ( I ) rheology. • The proposed constitutive model is well-verified against laboratory element tests. • Proposed phase transition model is implemented in MPM and validated against experiment results.

Engineering GeologyVol. 352
Hong Kong Polytechnic University (HK)
Research Grants Council, University Grants Committee
Openalex Percentile: Top 2%
Granular flow and fluidized beds
8.01
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