Mathematical Model of Fluids Motion in Poroelastic Snow-ice Cover

M. Tokareva, A. Papin
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引用次数: 3

Abstract

The dynamics of a snow-ice cover is considered within the theory of poroelasticity. The snow-ice cover is modeled by a three-phase medium consisting of water, air and ice. The governing equations are the equations of mass conservation for each phase with phase transitions, the equations of conservation of phase momentum in the form of Darcy’s law, the equation of conservation of momentum of the whole system, the rheological equation for porosity and the equation of heat balance of snow. In the full formulation the liquid and air pressures are functions of the temperature and the corresponding densities, and the viscosity and compressibility coefficients of ice are functions of the temperature. The problem of two-dimensional nonstationary filtration of water in a thin poroelastic ice plate is considered in the model case. The solution is obtained in quadratures
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孔隙弹性冰雪覆盖层流体运动的数学模型
冰雪覆盖的动力学是在孔隙弹性理论中考虑的。冰雪覆盖是由水、空气和冰组成的三相介质来模拟的。控制方程为各相变相的质量守恒方程、达西定律形式的相动量守恒方程、整个系统的动量守恒方程、孔隙率的流变方程和雪的热平衡方程。在完整的公式中,液体和空气压力是温度和相应密度的函数,冰的粘度和压缩系数是温度的函数。在模型情况下,考虑了水在多孔弹性薄冰板中的二维非平稳过滤问题。解是在正交中得到的
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