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NATURAL-CONVECTION HEAT TRANSFER IN CHANNELS WITH ISOTHERMALLY HEATED CONVEX SURFACES

机译:等温加热的凸面通道的自然对流传热

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摘要

This article reports on a numerical investigation conducted to study laminar naturalconvection heat transfer in channels with convex surfaces that are isothermally heated. Six Grashof number (Gr) values (10 e Gr e 104) and 11 radii of curvature (1 eje 1) are considered. The results are displayed in terms of streamline and isotherm plots, centerline pressure profiles, inlet mass flow rates, and local and average Nusselt number estimates. At the lowest radius of curvature (j 1), computations reveal the formation of recirculation zones in the exit section for all values of Grashof number considered. As the radius of curvature increases, the Gr value at which recirculation occurs also increases, until it disappears at j values greater than 1.5. For all configurations studied, the average Nusselt number Nu results indicate an increase in heat transfer with increasing Grashof number values. Moreover, the value of j at which Nu peaks increases with increasing Gr. Inlet volume flow rate and average Nusselt number correlations are presented.
机译:本文报道了一项数值研究,以研究具有等温加热的凸面通道中的层流自然对流换热。考虑六个Grashof数(Gr)值(10 e Gr e 104)和11曲率半径(1 eje 1)。结果以流线图和等温线图,中心线压力曲线,入口质量流率以及局部和平均Nusselt数估算值显示。在最低曲率半径(j 1)处,计算结果表明,对于所考虑的所有Grashof值,出口段均形成了回流区。随着曲率半径的增加,发生再循环的Gr值也增加,直到在大于1.5的j值消失为止。对于所研究的所有配置,平均努塞尔数Nu的结果表明,随着Grashof数值的增加,传热也随之增加。此外,随着Gr的增加,Nu峰值处的j值也增加。给出了入口体积流量和平均努塞尔数相关性。

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