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A numerical study on natural convection and entropy generation in a porous enclosure with heat sources

机译:带有热源的多孔罩中自然对流和熵产生的数值研究

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In this paper, fluid flow and thermal characteristics associated with natural convection heat transfer in a porous enclosure containing high temperature heat sources placed on top and bottom walls are studied. For this purpose, two-dimensional, time-dependent Navier-Stokes equations with Darcy-Brinkman-Forchheimer terms are solved in a Cartesian framework by using Streamline Upwind Petrov-Calerkin (SUPG) based finite element method. The effect of heat sources on flow pattern, entropy generation and temperature distribution are studied for different Darcy numbers, porosities and Rayleigh numbers. The results show that maximum entropy generation due to heat transfer irreversibility is observed in the vicinity of heat sources due to the presence of high thermal gradient. The global entropy generation due to fluid friction is found to increase in convection dominated regime. It is also observed that with increasing Darcy number, porosity and Rayleigh number the surface averaged Nusselt number for both top and bottom heat sources is increased.
机译:在本文中,研究了在具有高温热源的多孔外壳中,自然对流换热与自然对流换热相关联,该多孔外壳中的高温和高温分别位于顶壁和底壁上。为此,使用基于流线上风Petrov-Calerkin(SUPG)的有限元方法,在笛卡尔框架中求解带有Darcy-Brinkman-Forchheimer项的二维时间相关Navier-Stokes方程。研究了不同达西数,孔隙率和瑞利数对热源对流型,熵产生和温度分布的影响。结果表明,由于存在高的热梯度,在热源附近观察到由于传热不可逆而产生的最大熵。发现由于流体摩擦而产生的整体熵在对流主导状态下增加。还观察到,随着达西数,孔隙率和瑞利数的增加,顶部和底部热源的表面平均努塞尔数均增加。

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