Thermal convection in octagonal-shaped enclosures

Prabir Kumar Kar, Yada Nandu Kumar, P. K. Das, and Rajaram Lakkaraju
Phys. Rev. Fluids 5, 103501 – Published 7 October 2020
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Abstract

Flow-reversal phenomena in a classical two-dimensional (2D) Rayleigh-Bénard convection, in a square enclosure, are usually explained through growth and merging of diagonally opposite counterrotating corner rolls. To probe further the corner-roll growth dynamics, we have altered the square enclosure edges by additional slanted conduction walls, so that the enclosure resembles an octagonal shape. We have performed a series of 2D numerical simulations by varying the slanted wall inclination angle (α) from 0 to 45, to construct a detailed flow map in thermal convection in a range 5×105Ra108 and 0.8Pr2.0, where Ra is the Rayleigh number and Pr is the Prandtl number. Depending on Ra, Pr, and α, flow features in the octagonal enclosure can exist in the form of a uniform circulation, a two-roll, a mixed, a periodic, a quasiperiodic, or multiple flow states superimposed on each other. The flow reversals in the octagonal enclosure take place in several ways, for example, by the ejection of mushroom-shaped plumes alternatively from the opposite slanted walls at low Ra (105) and high Pr (2), by the corner-roll growth at high Ra (108) and low Pr (1.2), and by the dipole at high Ra (108) and high Pr (2). Strikingly, the dimensionless flow-reversal frequency scales linearly with an increase in α, and the slope varies from 1.04 at low Ra=5×105 to 0.328 at high Ra=108. We have shown the flow reversals are a consequence of competition between the dipole (a two-roll state where a cold roll sits above a hot roll) and the quadrupole (the four corner rolls) modes with the monopole mode. A uniform circulation with flow-reversal results if the quadrupole mode wins, and a two-roll state with a reversal results, if the dipole wins. At high Ra(108), the dipole strengthens, and the core bulk region shows hydrodynamic instabilities in the form of turbulent-like engulfments. We have uncovered the mechanism responsible for the observed engulfments due to the increase in turbulence production in the core bulk region by the buoyancy. As a result, we have observed that total heat transport also increases up to 14% when α is varied from 0 to 45.

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  • Received 27 October 2019
  • Accepted 3 September 2020

DOI:https://doi.org/10.1103/PhysRevFluids.5.103501

©2020 American Physical Society

Physics Subject Headings (PhySH)

Fluid Dynamics

Authors & Affiliations

Prabir Kumar Kar1, Yada Nandu Kumar2, P. K. Das3, and Rajaram Lakkaraju4,*

  • 1School of Energy Science & Engineering, Indian Institute of Technology Kharagpur, Bengal-721302, India
  • 2Centre for Theoretical Studies, Indian Institute of Technology Kharagpur, Bengal-721302, India
  • 3Department of Mechanical Engineering, Indian Institute of Technology Kharagpur, Bengal-721302, India
  • 4Computational Mechanics Group, Department of Mechanical Engineering, Indian Institute of Technology Kharagpur, Bengal-721302, India

  • *Corresponding author: rajaram.lv@gmail.com

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Issue

Vol. 5, Iss. 10 — October 2020

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