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首页> 外文期刊>Advances in Mechanical Engineering >Hydromagnetic Natural Convection Flow in a Fluid-Saturated Porous Medium with Nonuniform Heat Generation
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Hydromagnetic Natural Convection Flow in a Fluid-Saturated Porous Medium with Nonuniform Heat Generation

机译:流体饱和多孔介质中的氢细自然对流流动,具有不均匀的发热

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摘要

Convective flows can develop naturally within the porous materials if they are subject to external heating with/without internal heat source. In this work, the heat is assumed to be generated internally within the porous enclosure at a rate proportional to a power of the temperature difference. This relation is an approximation of the state of some exothermic chemical reaction. An inclined magnetic field is imposed to the porous enclosure. Darcy, model is used to formulate the porous layer and finite difference method is applied to solve the governing equations. The obtained results indicate that strong internal heating can generate significant maximum fluid temperatures above the heated wall temperature, and location of the maximum fluid temperature moves towards the center of the top wall by strengthening the magnetic field. Local heating exponent does not have a major effect on the flow and temperature distributions as well as the heat transfer performance within the porous medium. The large magnetic fields, regardless of direction, are effective to suppress the convective flows and reduce the rate of heat transfer.
机译:如果它们通过/不含内部热源的外部加热,则对流流动可以在多孔材料内自然地发展。在这项工作中,假设热量以与温度差的功率成比例的速率在多孔外壳内部产生。该关系是一些放热化学反应的状态的近似。倾斜磁场施加到多孔外壳。达西,模型用于制定多孔层,应用有限差分方法来解决控制方程。所得结果表明,强的内部加热可以产生高于加热壁温度的最大的最大流体温度,并且通过强化磁场,最大流体温度的位置朝向顶壁的中心移动。本地加热指数对流动和温度分布的主要影响以及多孔介质内的传热性能产生重大影响。无论方向如何,大磁场都有效地抑制对流流程并降低传热速率。

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