Multiscale modeling of coupled thermo-hydro-mechanical behavior in ice-bonded granular media subject to freeze-thaw cycles

被引:5
|
作者
Yu, Jidu [1 ]
Zhao, Jidong [1 ,2 ]
Liang, Weijian [3 ]
Zhao, Shiwei [1 ]
机构
[1] Hong Kong Univ Sci & Technol, Dept Civil & Environm Engn, Kowloon, Hong Kong, Peoples R China
[2] HKUST Shenzhen Hong Kong Collaborat Innovat Res In, Shenzhen 518045, Peoples R China
[3] Hong Kong Polytech Univ, Dept Civil & Environm Engn, Kowloon, Hong Kong, Peoples R China
基金
中国国家自然科学基金;
关键词
Frozen soil; Climate warming; Freeze-thaw cycles; Phase transition; Ice bonding effect; THM coupling; Multiscale modeling; Multiphysics modeling; Material point method; Discrete element method; PORE-WATER PRESSURES; POROUS-MEDIA; FROZEN SOILS; VOLUME; CONSOLIDATION; DEFORMATION; FORMULATION; STRENGTH; EQUATION; INSIGHTS;
D O I
10.1016/j.compgeo.2024.106349
中图分类号
TP39 [计算机的应用];
学科分类号
081203 ; 0835 ;
摘要
We present a novel multiscale framework that integrates the single -point multiphase material point method (MPM) and the discrete element method (DEM) to model the complex freeze -thaw behavior of ice -bonded granular media. The proposed numerical framework is featured by (a) employing the continuum -based MPM to solve the macroscopic governing equations for granular systems involving thermo-hydro-mechanical (THM) coupling and phase transitions, and (b) using the grain -scale discontinuum-based DEM to capture the thermodynamically sensitive mechanical behaviors of ice -bonded granular media. The multiscale framework is constructed by attaching a DEM-based representative volume element (RVE) at each material point in MPM. This RVE serves as a live sample of each material point to track the state -dependent effective stress with respect to the local deformation and thermodynamic conditions like ice saturation, bridging the macroscopic phenomena and the underlying microstructural evolution. In particular, we implement a semiimplicit staggered integration scheme for the macroscale THM-coupled MPM to boost computational efficiency and enhance numerical stability. We also propose an innovative ice saturation -dependent bond contact to effectively reproduce the thermodynamically sensitive mechanical behaviors. The new multiscale framework is first benchmarked against analytical solutions for 1D non -isothermal consolidation problems. We then demonstrate its exceptional capability in simulating intricate freeze -thaw behavior of granular media through a boundary value problem involving cyclic freeze -thaw actions. Further cross -scale analyses reveal its potential in capturing key loading- and state -dependent THM responses with explainable microstructural mechanisms during complex freezing and thawing loading conditions.
引用
收藏
页数:21
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