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Convective heat transfer along ratchet surfaces in vertical natural convection

Published online by Cambridge University Press:  28 June 2019

Hechuan Jiang
Affiliation:
Center for Combustion Energy, Key Laboratory for Thermal Science and Power Engineering of Ministry of Education, Department of Energy and Power Engineering, Tsinghua University, 100084 Beijing, China
Xiaojue Zhu
Affiliation:
Center of Mathematical Sciences and Applications, and School of Engineering and Applied Sciences, Harvard University, Cambridge, MA 02138, USA
Varghese Mathai
Affiliation:
School of Engineering, Brown University, Providence, RI 02912, USA
Xianjun Yang
Affiliation:
Center for Combustion Energy, Key Laboratory for Thermal Science and Power Engineering of Ministry of Education, Department of Energy and Power Engineering, Tsinghua University, 100084 Beijing, China
Roberto Verzicco
Affiliation:
Dipartimento di Ingegneria Industriale, University of Rome ‘Tor Vergata’, Via del Politecnico 1, 00133 Roma, ItalyPhysics of Fluids Group and Max Planck Center Twente, University of Twente, PO Box 217, 7500AE Enschede, The Netherlands
Detlef Lohse
Affiliation:
Physics of Fluids Group and Max Planck Center Twente, University of Twente, PO Box 217, 7500AE Enschede, The NetherlandsMax Planck Institute for Dynamics and Self-Organization, 37077 Göttingen, Germany
Chao Sun*
Affiliation:
Center for Combustion Energy, Key Laboratory for Thermal Science and Power Engineering of Ministry of Education, Department of Energy and Power Engineering, Tsinghua University, 100084 Beijing, ChinaPhysics of Fluids Group and Max Planck Center Twente, University of Twente, PO Box 217, 7500AE Enschede, The Netherlands
*
†Email address for correspondence: chaosun@tsinghua.edu.cn

Abstract

We report on a combined experimental and numerical study of convective heat transfer along ratchet surfaces in vertical natural convection (VC). Due to the asymmetry of the convection system caused by the asymmetric ratchet-like wall roughness, two distinct states exist, with markedly different orientations of the large-scale circulation roll (LSCR) and different heat transport efficiencies. Statistical analysis shows that the heat transport efficiency depends on the strength of the LSCR. When a large-scale wind flows along the ratchets in the direction of their smaller slopes, the convection roll is stronger and the heat transport is larger than the case in which the large-scale wind is directed towards the steeper slope side of the ratchets. Further analysis of the time-averaged temperature profiles indicates that the stronger LSCR in the former case triggers the formation of a secondary vortex inside the roughness cavity, which promotes fluid mixing and results in a higher heat transport efficiency. Remarkably, this result differs from classical Rayleigh–Bénard convection (RBC) with asymmetric ratchets (Jiang et al., Phys. Rev. Lett., vol. 120, 2018, 044501), wherein the heat transfer is stronger when the large-scale wind faces the steeper side of the ratchets. We reveal that the reason for the reversed trend for VC as compared to RBC is that the flow is less turbulent in VC at the same $Ra$. Thus, in VC the heat transport is driven primarily by the coherent LSCR, while in RBC the ejected thermal plumes aided by gravity are the essential carrier of heat. The present work provides opportunities for control of heat transport in engineering and geophysical flows.

Information

Type
JFM Papers
Copyright
© 2019 Cambridge University Press 
Figure 0

Figure 1.(a) A sketch of a convection cell with asymmetric ratchets on vertical side plates. (b) Schematic showing the flow configuration where the LSCR moves along the smaller slope side of the ratchets, referred to subsequently as VC-case-A. (c) Schematic of the flow configuration where the LSCR travels towards the steeper slope of the ratchets, subsequently referred to as VC-case-B.

Figure 1

Table 1.Properties of working fluid for water at 40 $^{\circ }$C and Novec 7200 at 25 $^{\circ }$C.

Figure 2

Figure 2.(a) Nusselt number $Nu$ as a function of Rayleigh number $Ra$ in the smooth and rough cells. (b) The $Nu$ enhancement as a function of $Ra$ for the two cases. The open symbols correspond to experimental data and the filled symbols correspond to numerical data.

Figure 3

Table 2.Grid convergence studies for VC-case-B at $Ra=5.7\times 10^{9}$.

Figure 4

Figure 3.Reynolds number $Re$ as a function of the Rayleigh number $Ra$. The $Re$ is defined as $Re=V_{LSC}H/\unicode[STIX]{x1D708}$, where $V_{LSC}=(\langle u_{x}\rangle _{S})_{max}$ is the maximum mean vertical velocity of LSCR.

Figure 5

Figure 4.(a,d) Shadowgraph visualization at $Ra=5.7\times 10^{9}$ and $Pr=4.3$ for (a) VC-case-A and (d) VC-case-B. The directions of LSCR are clockwise in both cases. The corresponding movies (supplementary movie 1 for VC-case-A and movie 2 for VC-case-B) are available at https://doi.org/10.1017/jfm.2019.446. (b,e) Instantaneous temperature field from direct numerical simulations at $Ra=5.7\times 10^{9}$ and $Pr=4.3$ for (b) VC-case-A and (e) VC-case-B. The left-hand insets show an enlarged portion of the representative plot for the selected windows. (c,f) Instantaneous vertical velocity field from direct numerical simulations at $Ra=5.7\times 10^{9}$ and $Pr=4.3$ for (c) VC-case-A and (f) VC-case-B. In both cases the flow is quite calm and not turbulent.

Figure 6

Figure 5.(a) The dimensionless mean vertical velocity as a function of position $z/H$ for VC-case-A (solid line) and VC-case-B (dashed line) at $Ra=5.7\times 10^{9}$ and $Pr=4.3$. The inset shows an enlarged portion of the plot near the roughness elements. The black line indicates where the tips of roughness elements are. (b) Time-averaged vertical velocity fields for VC-case-A, superposed by the velocity vectors. The selected window is located at the middle of the hot plate. (c) Time-averaged vertical velocity fields for VC-case-B, superposed by the velocity vector. The selected window is located at the same place as for VC-case-A.

Figure 7

Figure 6.(a,c) Profiles of the time-averaged temperature $\langle \unicode[STIX]{x1D703}\rangle$ from direct numerical simulations at $Ra=5.7\times 10^{9}$ for (a) VC-case-A and (c) VC-case-B. The selected portions are located at the middle of the hot plate. The solid lines show the data for the position above the valley of the ratchet element, the dashed lines denote the profile at the middle of the ratchet roughness and the dashed-dot lines denote the profile near the peak of the ratchet element. (b,d) The thermal boundary layer (BL) thickness (red circles) and secondary vortex zone (SV) thickness (blue diamonds) averaged in time as functions of $x/L$ for (b) VC-case-A and (d) VC-case-B.

Figure 8

Figure 7.Local $Nu_{r}$ at hot plate as a function of $x/L$ for VC-case-A (filled circles) and VC-case-B (filled diamonds), where $x/L$ denotes the position of each ratchet centre. The local $Nu_{r}$ is defined as $Nu_{r}=J_{r}/(\unicode[STIX]{x1D712}~\unicode[STIX]{x1D6E5}/H)$ and $J_{r}=1/(W\unicode[STIX]{x1D706})~\unicode[STIX]{x1D712}\int (\unicode[STIX]{x2202}\langle \unicode[STIX]{x1D703}\rangle /\unicode[STIX]{x2202}\hat{n})\,\text{d}S$, where $\hat{n}$ is the unit vector perpendicular to the surface of the ratchet element and the integration $\int (\cdot )\,\text{d}S$ is along the surface of roughness element.

Figure 9

Figure 8.(a) Sketch of flow structures in RBC with ratchet-like roughness on the horizontal walls, which shows the process of plume emission. (b) The compensated plots of $Nu$ with $Ra$ for RBC and VC with ratchet-like roughness on hot and cold plates. The data for RBC are from Jiang et al. (2018). (c) Sketch of flow structures in VC with the ratchet-like roughness on the vertical walls, which shows the process of blocking the flow.

Jiang et al. supplementary movie 1

Shadowgraph visualization for VC-case A

Download Jiang et al. supplementary movie 1(Video)
Video 2.8 MB

Jiang et al. supplementary movie 2

Shadowgraph visualization for VC-case B

Download Jiang et al. supplementary movie 2(Video)
Video 3 MB