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Non-isothermal Transport of Multi-phase Fluids in Porous Media. The Entropy Production

机译:多孔介质中多相流体的非等温传输。熵产生

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We derive the entropy production for transport of multi-phase fluids in a non-deformable, porous medium exposed to differences in pressure, temperature, and chemical potentials. Thermodynamic extensive variables on the macro-scale are obtained by integrating over a representative elementary volume (REV). Contributions come from porous media specific properties, phase volumes, surface areas and contact lines. Curvature effects are neglected. Using Euler homogeneity of the first order, we obtain the Gibbs equation for the REV. From this we define the intensive variables, the temperature, pressure and chemical potentials, and, using the balance equations, we derive the entropy production for the REV. The entropy production defines sets of independent conjugate thermodynamic fluxes and forces in the standard way. The transport of two-phase flow of immiscible components is used to give a first illustration of the equations.
机译:我们得出了在不可变形的多孔介质中暴露于压力,温度和化学势差下的多相流体传输的熵产。宏观尺度上的热力学广泛变量是通过对代表性基本体积(REV)进行积分获得的。贡献来自多孔介质的特定属性,相体积,表面积和接触线。曲率效应被忽略。使用一阶Euler均匀性,我们获得REV的Gibbs方程。据此,我们定义了强度变量,温度,压力和化学势,并使用平衡方程式,得出了REV的熵产生。熵产生以标准方式定义了独立的共轭热力学通量和力的集合。不混溶组分的两相流的输送用于给出方程式的第一说明。

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