Modeling multiscale evolution of numerous voids in shocked brittle material
Yin Yu1, Wenqiang Wang2, Hongliang He2
1National Key Laboratory of Shock Wave and Detonation Physics, Institute of Fluid Physics, CAEP, 621900, Mianyang, People's Republic of China and Department of Physics and Key Laboratory for Radiation Physics and Technology of Ministry of Education, Sichuan University, 610064, Chengdu, People's Republic of China.
This study models shock-wave compression in brittle materials, revealing how void evolution drives plasticity and deformation. Findings enable systematic design of porous materials for specific shock applications.
Area of Science:
- Materials Science
- Computational Mechanics
- Physics
Background:
- Understanding the multiscale influence of void evolution on material properties is computationally challenging.
- Shock-wave compression in brittle materials involves complex microscopic and macroscopic phenomena.
Purpose of the Study:
- To develop a computational model for simulating shock-wave compression in brittle materials.
- To investigate the mechanisms of shock plasticity and deformation driven by void evolution.
- To establish relationships between material porosity, shock parameters, and macroscopic properties.
Main Methods:
- Developed a discrete element method (lattice model) for shock-wave compression simulation.
- Employed a model interaction-parameter-mapping procedure for validation against experimental data.
- Analyzed shock-wave splitting, void collapse, media slippage, and vortex patterns.
Main Results:
- The model accurately reproduced experimental shock-wave profiles, showing wave splitting into elastic and deformation components.
- Void collapse in the deformation wave causes volume shrinkage and deformation.
- Media slippage and rotation, visualized as vortex patterns, significantly contribute to shock plasticity, increasing with pressure.
Conclusions:
- Shock plasticity in porous brittle materials is driven by both void collapse and media slippage/rotation.
- Material porosity dictates elastic wave amplitude; porosity and shock stress jointly control deformation wave propagation and final equilibrium states.
- The study provides a framework for designing porous brittle materials with tailored shock behaviors for specific applications.
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