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Enhanced heat transport in partitioned thermal convection
Published online by Cambridge University Press: 06 November 2015
Abstract
Enhancement of heat transport across a fluid layer is of fundamental interest as well as great technological importance. For decades, Rayleigh–Bénard convection has been a paradigm for the study of convective heat transport, and how to improve its overall heat-transfer efficiency is still an open question. Here, we report an experimental and numerical study that reveals a novel mechanism that leads to much enhanced heat transport. When vertical partitions are inserted into a convection cell with thin gaps left open between the partition walls and the cooling/heating plates, it is found that the convective flow becomes self-organized and more coherent, leading to an unprecedented heat-transport enhancement. In particular, our experiments show that with six partition walls inserted, the heat flux can be increased by approximately 30 %. Numerical simulations show a remarkable heat-flux enhancement of up to 2.3 times (with 28 partition walls) that without any partitions.
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- © 2015 Cambridge University Press
References
Bao et al. supplementary movie
The movie about the onset of flow structures in the convection cell with 20 partition walls at d=2 mm and Ra=1e8 from numerical results. Left panel: The temperature (color) and velocity (arrows) fields. Here, the red and blue colors correspond to the high and low temperature regions, respectively. Right panel: The pressure field (color), where the red and blue colors respectively correspond to the high and low pressure regions.
Bao et al. supplementary movie
The movie about the onset of flow structures in the convection cell with 20 partition walls at d=2 mm and Ra=1e8 from numerical results. Left panel: The temperature (color) and velocity (arrows) fields. Here, the red and blue colors correspond to the high and low temperature regions, respectively. Right panel: The pressure field (color), where the red and blue colors respectively correspond to the high and low pressure regions.
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