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首页> 外文期刊>Current Forestry Reports >Entropy Generation Analysis for a Radiative Micropolar Fluid Flow Through a Vertical Channel Saturated with Non-Darcian Porous Medium
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Entropy Generation Analysis for a Radiative Micropolar Fluid Flow Through a Vertical Channel Saturated with Non-Darcian Porous Medium

机译:通过垂直沟道饱和与非Darcian多孔介质饱和的熵生成分析

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AbstractIn this study, an analytical investigation of convective heat transfer and entropy generation analysis of flow of micropolar fluid is presented. The infinite channel is assumed to be saturated with porous material and the walls are maintained at different constant temperatures. The Eringen thermo-micro-polar material model is used to simulate the rheological flow in the channel. The fluid is assumed to be gray, absorbing, emitting but non-scattering medium, and the Rosseland’s approximation is utilized to simulate the radiative heat flux component of heat transfer in energy transport equation. The resulting governing equations are then solved under physically viable boundary conditions at the channel walls using the Adomian decomposition method. The influences of emerging thermophysical parameters are addressed through graphs. The computations show that the increase in the Grashof number and radiation parameter causes to increase the entropy generation. Further, the effect of viscous dissipation was taken into account since it significantly affects heat transfer and entropy generation characteristics and cannot be ignored.
机译:<标题>抽象 在本研究中,提出了对流传热和熵生成分析的分析研究。假设无限通道用多孔材料饱和,并且壁保持在不同的恒定温度下。 eringen热微极性材料模型用于模拟通道中的流变流动。假设流体是灰色的,吸收,发射但非散射介质,并且利用Rosseland的近似来模拟能量传输方程中传热的辐射热通量分量。然后使用ADOMian分解方法在通道壁的物理上可行的边界条件下解决所得到的控制方程。通过图表解决了新兴热物理参数的影响。计算表明,格雷什数量和辐射参数的增加导致增加熵生成。此外,考虑了粘性耗散的效果,因为它显着影响传热和熵生成特征,并且不能被忽略。

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