首页> 外文会议>Geotechnical frontiers >Microstructure-Based Random Finite Element Simulation of Thermal and Hydraulic Conduction Processes in Unsaturated Frozen Soils
【24h】

Microstructure-Based Random Finite Element Simulation of Thermal and Hydraulic Conduction Processes in Unsaturated Frozen Soils

机译:基于微结构的非饱和冻土热力和水力传导过程的随机有限元模拟

获取原文

摘要

The freeze-thaw cycles in unsaturated frozen soils can cause serious damage to civil infrastructure. In this paper, a microstructure-based four-phase clay model is generated in Matlab. The model is then converted into a finite element software Comsol. The thermal, hydraulic and mechanical properties of each phase (soil particle, ice, water and air) of the clay are applied randomly to each pixel of the image model based on the volumetric content of each phase. The simulation results show that: (1) The thermal and hydraulic flow are observed during the freeze-thaw cycle. (2) The temperature, matric suction and potential head are obtained during the thawing process of the clay model. (3) The internal stress distribution versus time are calculated during the freezing process. The simulation results agree well with the engineering experience, which provides a simulation model to microstructurally analyze the thermal, hydraulic and mechanical properties of unsaturated frozen soils.
机译:非饱和冻土中的冻融循环会严重破坏民用基础设施。本文在Matlab中生成了基于微观结构的四相粘土模型。然后将模型转换为有限元软件Comsol。基于每个相的体积含量,将粘土的每个相(土壤颗粒,冰,水和空气)的热,水力和机械特性随机应用于图像模型的每个像素。仿真结果表明:(1)在冻融过程中观察到了热流和水力流。 (2)在粘土模型的解冻过程中获得了温度,基质吸力和势能扬程。 (3)在冻结过程中计算内部应力分布与时间的关系。仿真结果与工程经验非常吻合,后者提供了一个仿真模型,以微观结构分析非饱和冻土的热,水力和力学性能。

著录项

相似文献

  • 外文文献
  • 中文文献
  • 专利
获取原文

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号