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首页> 外文期刊>Latin American Applied Research >Transient natural convection in a horizontal fluid layer, with a blackbody bottom; heated from above by radiation
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Transient natural convection in a horizontal fluid layer, with a blackbody bottom; heated from above by radiation

机译:水平流体层中的瞬时自然对流,底部为黑体;辐射从上方加热

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摘要

Transient natural convection in a horizontal fluid layer, with a blackbody bottom, heated from above by radiation was studied experimentally and numerically. The heat flux which reaches to the bottom is absorbed by the black surface and reheats the fluid layer from thebottom, creating an adverse t4mperature gradient at the bottom of the fluid layer similar to the one observed in the classical Rayleigh-Benard problem. A mathematical model was developed and governing differential equations were numerically solved. The predictions of the model were found to be in an acceptable agreement with the experimental temperature distributions obtained in a laboratory scale pool by holographic interferometer techniques. Experimentally and numerically calculated heat convection coefficients were correlated in terms of Nusselt and Rayleigh numbers and compared with a literature correlation. It is concluded that this problem is very similar to the classical Rayleigh-Benard problem of a horizontal fluid layer heated from below.
机译:实验和数值研究了从上方加热的黑体底部水平流体层的瞬态自然对流。到达底部的热通量被黑色表面吸收,并从底部重新加热流体层,从而在流体层的底部产生不利的t4温度梯度,这与经典的Rayleigh-Benard问题中观察到的相似。建立了数学模型,并对数值方程求解了微分方程。发现该模型的预测与通过全息干涉仪技术在实验室规模水池中获得的实验温度分布在可接受的一致性内。实验和数值计算的热对流系数根据Nusselt和Rayleigh数进行关联,并与文献相关性进行比较。结论是,该问题与从下方加热的水平流体层的经典瑞利-贝纳德问题非常相似。

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