A non-linear viscoelastic material model with progressive damage based on microstructural evolution and phase transition in polycrystalline ice for design against ice impact

•A viscoelastic material model with progressive damage for ice under impact loading.•Iterative algorithm for pressure- and rate-dependent progressive damage.•The model is implemented with Lagrangian FEM, coupled FEM-SPH, and ALE-FEM.•Validation against physical creep and ice crushing tests with vari...

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Bibliographic Details
Published inInternational journal of impact engineering Vol. 176; p. 104563
Main Authors Mokhtari, Mojtaba, Kim, Ekaterina, Amdahl, Jørgen
Format Journal Article
LanguageEnglish
Published Elsevier Ltd 01.04.2023
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Summary:•A viscoelastic material model with progressive damage for ice under impact loading.•Iterative algorithm for pressure- and rate-dependent progressive damage.•The model is implemented with Lagrangian FEM, coupled FEM-SPH, and ALE-FEM.•Validation against physical creep and ice crushing tests with various speeds.•Modelling cyclic transition from solid-like intact to fluid-like viscous crushed ice. This study presents a nonlinear viscoelastic material model incorporating a progressive damage framework with an iterative algorithm for glacial/freshwater polycrystalline ice subject to compressive impact load induced by ice-structure interaction. The damage model accounts for microcracking, dynamic recrystallisation, pressure melting, and high-shear elastic failure with a pressure- and rate-dependent convex failure locus. The constitutive laws are written in Fortran and implemented as a vectorised user material (VUMAT) in Abaqus with three different numerical methods, Lagrangian FEM, coupled FEM-SPH, and ALE-FEM. The constitutive model together with the implemented numerical methods are validated against two different types of laboratory-scale physical tests, indentation of cone-shaped ice and triaxial creep. The proposed model implemented with the coupled FEM-SPH method enables simulation of the cyclic transition from solid-like intact ice to the fluid-like pulverised/granular substance, progressively extruded with viscous rheology.
ISSN:0734-743X
1879-3509
DOI:10.1016/j.ijimpeng.2023.104563