基于LTNE的二维饱和多孔介质平板热流固完全耦合数值分析

针对目前多孔介质热流固耦合数学模型多为不完全耦合模型，且物理模型多为一维或一维轴对称模型的现状，对二维饱和多孔介质平板热流固完全耦合问题进行数学建模和数值分析. 采用强耦合方式实现热流固3个物理场的完全耦合. 在平板左侧施加30 ℃流体和固体温度边界条件及固定位移边界条件，平板其他边界温度场和位移场假设为自然边界条件，平板四周加载0 Pa的孔隙压力边界条件. 利用COMSOL Multiphysics有限元分析软件的偏微分方程（PDEs）模式实现上述完全耦合模型的求解，得到渗流场、应变场以及双温度场的数值解. 数值结果表明，随时间增加，流体和固体温度、应变及孔隙压力沿x轴方向传递，同时发现x轴方向应变远大于y轴方向应变. 此外，随时间增加，y轴方向应变和孔隙压力最大值逐渐减小. 研究建立的数学模型和数值解有助于深入认识二维饱和多孔介质热流固完全耦合力学行为.

Numerical analysis of fully coupled thermoporoelastic behavior of two-dimensional saturated porous media flat plate under LTNE condition

Most of current thermoporoelastic models of porous media are incomplete coupled ones, and the physical models mostly adopt one-dimensional or one-dimensional axisymmetric models. In view of this point, a fully coupled model of a two-dimensional saturated porous media flat plate was presented and the corresponding numerical simulation was carried out. The fully coupled of three physical fields (heat, fluid flow, and solid stress/deformation) were realized by means of strong coupling. The boundary conditiorns were assumed as follows: As for the temperature field and the displacement field, 30 ℃ fluid and solid temperature boundary conditions and fixed displacement boundary conditions were exerted on the left side of the plate, and naturual boundary conditions were prescribed on the other sides of the plate. Meanwhile, 0 Pa pore pressure boundary conditions were loaded around the plate. The numerical solutions of flow field, strain field and two temperature fields were obtained by the PDEs pattern of COMSOL Multiphysics FEA software. Numerical results showed that fluid and solid temperature, strain and pore pressure transfer along the x-axis direction with increasing time, and the strain in the x-direction is much larger than that in the y-direction. In addition, it was found that the maximum values of y-direction strain and pore pressure gradually decrease with time. The presented mathematical model and numerical solutions are of benefit to provide deep insights into the fully thermoporoelastic coupled behavior of two-dimensional saturated porous media.