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陈飞熊, 李宁, 程国栋. 饱和正冻土多孔多相介质的理论构架[J]. 岩土工程学报, 2002, 24(2): 213-217.
引用本文: 陈飞熊, 李宁, 程国栋. 饱和正冻土多孔多相介质的理论构架[J]. 岩土工程学报, 2002, 24(2): 213-217.
CHEN Feixiong, LI Ning, CHENG Guodong. The theoretical frame of multi-phase porous medium for the freezing soil[J]. Chinese Journal of Geotechnical Engineering, 2002, 24(2): 213-217.
Citation: CHEN Feixiong, LI Ning, CHENG Guodong. The theoretical frame of multi-phase porous medium for the freezing soil[J]. Chinese Journal of Geotechnical Engineering, 2002, 24(2): 213-217.

饱和正冻土多孔多相介质的理论构架

The theoretical frame of multi-phase porous medium for the freezing soil

  • 摘要: 通过对冻土多孔多相微元体的平衡方程、各相成分之间的变形协调方程 ,推导出冻土体 (考虑土骨架与冰颗粒之间相互作用力———冻胀力 )的有效应力原理、正冻土单元的连续性方程及各相成分的能量转换与传递方程 ;在此基础上提出了正冻土的控制微分方程的理论框架 ,从而建立了在多孔固液介质的质量守恒方程与多孔多相介质的热、能守恒方程的基础上的全面考虑冻土中骨架、冰、水三相介质水、热、力与变形真正的耦合作用的数理方程 ,比当前国际流行的正冻土流体动力学模型、刚冰模型和热力学模型更全面地描述了正冻土的水、热、力与变形的实际状态

     

    Abstract: Based on the equilibrium, continuity and energy principles of the multi phase porous medium, the heat moisture deformation (HMD) coupled theoretical frame is established for the freezing soil in this paper, with the consideration of the force interaction between the soil skeleton and ice particle, and the energy jump behaviors during the phase changing between ice and water. The proposed model is more advanced than the commonly used Hydrodynamic models,Rigid ice models and Thermomechanical models.

     

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