首页> 外文期刊>Journal of porous media >TRANSIENT NATURAL CONVECTION FLOW IN A RECTANGULAR CAVITY FILLED WITH A POROUS MATERIAL WITH LOCALIZED HEATING FROM BELOW AND THERMAL STRATIFICATION
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TRANSIENT NATURAL CONVECTION FLOW IN A RECTANGULAR CAVITY FILLED WITH A POROUS MATERIAL WITH LOCALIZED HEATING FROM BELOW AND THERMAL STRATIFICATION

机译:多孔材料填充的矩形腔体中的瞬时自然对流流动,从下面开始进行局部加热并进行热分层

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摘要

The transient natural convection flow with thermal stratification in a rectangular cavity filled with fluid saturated porous medium obeying Darcy's law has been studied. Prior to the time t~* = 0, the flow in the cavity is assumed to be motionless and all four walls of the cavity are at the same constant temperature. At time t~* = 0, the temperatures of the vertical walls are suddenly increased which vary linearly with the distance y and at the same time on the bottom wall an isothermal heat source is placed centrally. This sudden change in the wall temperatures gives rise to unsteadiness in the problem. The horizontal temperature difference induces and sustains a buoyancy driven flow in the cavity which is then controlled by the vertical temperature difference. The partial differential equations governing the transient natural convection flow have been solved numerically. The local and average Nusselt numbers decrease rapidly in a small time interval after the start of the impulsive change in the wall temperatures and the steady state is reached quickly. The time required to reach the steady state depends on the Rayleigh number and the thermal stratification parameter.
机译:根据达西定律,研究了在充满流体饱和多孔介质的矩形腔体中具有热分层的瞬态自然对流。在时间t * = 0之前,假定空腔中的流动是不动的,并且空腔的所有四个壁处于相同的恒定温度。在时间t * * = 0时,垂直壁的温度突然升高,其随着距离y线性变化,并且同时在底壁的中央放置等温热源。壁温的突然变化导致问题的不稳定。水平温度差在腔中引起并维持浮力驱动的流动,然后由垂直温度差控制该流动。数值计算了控制瞬态自然对流的偏微分方程。壁温的脉冲变化开始后的短时间内,局部和平均Nusselt数迅速下降,并迅速达到稳态。达到稳态所需的时间取决于瑞利数和热分层参数。

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