浸入式流体流经多孔基质垂直通道的传热和传质效应研究

Mangala Kandagal, Ramesh Kempepatil
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引用次数: 0

摘要

在本文中,我们研究了在对称的双垂直区域中,不相溶流体流动的传热和传质问题。文章讨论了热量产生和吸收的特性。由两个垂直区域组成的通道中充满了多孔基质和粘性流体。在这两种情况下,我们都考虑了发生牛顿式发热和吸热的流体。假定多孔基质的通道壁是热稳定和不导电的。采用分析方法求解控制方程。布林克曼数(Br)、比奥特数(Bi)、格拉肖夫数(Gr)、粘度比(m)、发热量和热导率的变化以图表形式表示。我们还研究了格拉肖夫数的增加对两个区域流体流动的影响。同样,多孔介质中热量和动量传输的变化在很大程度上受到粘度、通道宽度、源和汇的影响。此外,当格拉肖夫数增大时,浮力也会增大,从而导致产生和吸收热量的流体流量增加。
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An investigation of the heat and mass transfer effects in vertical channels with immersible fluid flow through a porous matrix
In this article, we investigated the heat and mass transfer of immiscible fluid flow in symmetric two‐vertical regions with a porous matrix in region‐II. The properties of heat generation and absorption are discussed. The channel, consisting of two vertical regions, is filled with a porous matrix with viscous fluids. In both cases, we considered the fluids that undergo Newtonian heat generation and absorption. It was assumed that the porous matrix's channel wall was thermally stable and electrically non‐conducting. The analytical method is used to solve governing equations. Variations in Brinkman Number (Br), Biot Number (Bi), Grashof (Gr) number, viscosity ratio (m), heat generation, and thermal conductivity are illustrated graphically. And we examined the increase in Grashof number, which has effects on fluid flows in both regions. Similarly, the change of heat and momentum transmission in porous media is greatly affected by the viscosity, channel width, source, and sink. Also, when the Grashof number increases, buoyancy increases, leading to an increase in the fluid flow for heat generation and absorption.
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