Natural Convection Heat Transfer

E. F. Atwan, R. Sakr
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引用次数: 7

Abstract

A numerical and experimental investigation for natural convection heat transfer from a pipe embedded in a semi-infinite, liquid-saturated porous medium is carried out. The surface of the medium is assumed to be impermeable. The governing equations for Darcy flow are solved using finite element method. The finite element formulation is based on a two-dimension Galerkin approach. Extensive series of numerical solutions are conducted over a wide range of the governing parameters 2 h/R8, 10 Ra250, where h/R, and Ra are the burial depth/pipe radius ratio, and the Darcy-Rayleigh number, respectively. The effects of these parameters on both the temperature and flow fields and on the pipe surface heat transfer rate are analyzed. Experiments are conducted on an electrically heated brass pipe buried in a liquid-saturated porous medium enclosed in a vertical container to validate the present predictions. Sand grains with nominal diameter 2.7 mm saturated with water are used as the porous medium. The experimental data are compared with both the present predictions and with those available in the literature and fair agreement is noticed. Correlating equations for the average Nusselt number are obtained as functions of Darcy-Rayleigh number and the pipe burial depth ratio.
自然对流传热
对半无限饱和多孔介质中管道的自然对流换热问题进行了数值和实验研究。假定介质表面是不透水的。采用有限元法求解了达西流的控制方程。有限元公式基于二维伽辽金方法。在较宽的控制参数2h/R8,10Ra250范围内进行了广泛的数值解,其中h/R和Ra分别为埋深/管半径比和达西-瑞利数。分析了这些参数对温度场、流场和管道表面换热率的影响。在电加热的黄铜管上进行了实验,该黄铜管埋在垂直容器内的饱和液体多孔介质中,以验证目前的预测。采用标称直径2.7 mm的含水饱和砂粒作为多孔介质。实验数据与目前的预测和文献中已有的数据进行了比较,并注意到比较一致。得到了平均努塞尔数作为达西-瑞利数和管道埋深比的函数的相关方程。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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