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COMPUTATION OF TURBULENT FREE CONVECTION IN OBLIQUE POROUS ENCLOSURES USING A MACROSCOPIC TWO-EQUATION MODEL

机译:宏观两方程模型对倾斜多孔壳中湍流自由对流的计算

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摘要

Computations for turbulent natural convection within an inclined cavity totally filled with a fluid saturated porous medium are presented. The finite volume method in a generalized coordinate system is applied. The inclined walls are maintained at constant but different temperatures, while the horizontal walls are kept insulated. Governing equations are written in terms of primitive variables and are recast into a general form,. Flow and heat transfer characteristics, (streamlines, isotherms and average Nusselt number), are investigated for a wide range of values of Rayleigh number and inclined angle. The turbulent model used is the standard k-ε model with a wall function. In this work, the turbulence model is first switched off and the laminar branch of the solution is found. Subsequently, the turbulence model is included so that the solution merges to the laminar branch for a reducing Ra_m. This convergence of results as Ra_m decreases can be seen as an estimate of the so-called relaminarization phenomenon. Present solutions are compared with published results and the influence of the inclination angle on Ra_(cr) is analyzed. For Ra_m greater than around 10~4, both laminar and turbulent flow solutions deviate, indicating that such critical value for Ra_m was reached.
机译:提出了在完全充满流体饱和多孔介质的倾斜空腔内进行湍流自然对流的计算。应用了广义坐标系中的有限体积法。倾斜的壁保持恒定但不同的温度,而水平的壁保持绝缘。控制方程式是根据原始变量编写的,并被重铸为一般形式。对于瑞利数和倾斜角的宽范围值,研究了流动和传热特性(流线,等温线和平均努塞尔数)。使用的湍流模型是具有壁函数的标准k-ε模型。在这项工作中,首先关闭湍流模型,然后找到解的层流分支。随后,包括湍流模型,以便解决方案合并到层流分支,以减小Ra_m。随着Ra_m减小,结果的这种收敛可以看作是对所谓的再分层现象的估计。将现有解决方案与已发表的结果进行比较,并分析了倾斜角度对Ra_(cr)的影响。当Ra_m大于10〜4时,层流和湍流解均会偏离,表明Ra_m的临界值已达到。

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