Heat transfer in rotating Rayleigh-Benard convection with rough plates

被引:12
作者
Joshi, Pranav [1 ,2 ,3 ]
Rajaei, Hadi [1 ,2 ]
Kunnen, Rudie P. J. [1 ,2 ]
Clercx, Herman J. H. [1 ,2 ]
机构
[1] Eindhoven Univ Technol, Fluid Dynam Lab, Dept Appl Phys, POB 513, NL-5600 MB Eindhoven, Netherlands
[2] Eindhoven Univ Technol, JM Burgers Ctr Fluid Dynam, POB 513, NL-5600 MB Eindhoven, Netherlands
[3] Natl Aerosp Labs, Expt Aerodynam Div, Bangalore 560017, Karnataka, India
关键词
Benard convection; geophysical and geological flows; rotating turbulence; TURBULENT THERMAL-CONVECTION; LARGE-SCALE CIRCULATION; PLANETARY CORES; UNIFYING THEORY; EKMAN LAYERS; TRANSPORT; BOUNDARY; SURFACES; FLOWS;
D O I
10.1017/jfm.2017.660
中图分类号
O3 [力学];
学科分类号
08 ; 0801 ;
摘要
This experimental study focuses on the effect of horizontal boundaries with pyramid-shaped roughness elements on the heat transfer in rotating Rayleigh-Benard convection. It is shown that the Ekman pumping mechanism, which is responsible for the heat transfer enhancement under rotation in the case of smooth top and bottom surfaces, is unaffected by the roughness as long as the Ekman layer thickness delta(E) is significantly larger than the roughness height k. As the rotation rate increases, and thus delta(E) decreases, the roughness elements penetrate the radially inward flow in the interior of the Ekman boundary layer that feeds the columnar Ekman vortices. This perturbation generates additional thermal disturbances which are found to increase the heat transfer efficiency even further. However, when delta(E) approximate to k, the Ekman boundary layer is strongly perturbed by the roughness elements and the Ekman pumping mechanism is suppressed. The results suggest that the Ekman pumping is re-established for delta(E) << k as the faces of the pyramidal roughness elements then act locally as a sloping boundary on which an Ekman layer can be formed.
引用
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页数:12
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