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 () from to , to construct a detailed flow map in thermal convection in a range and , where is the Rayleigh number and is the Prandtl number. Depending on , , and , 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 () and high (), by the corner-roll growth at high () and low (), and by the dipole at high () and high (). Strikingly, the dimensionless flow-reversal frequency scales linearly with an increase in , and the slope varies from 1.04 at low to 0.328 at high . 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 , 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 when is varied from to .
25 More- Received 27 October 2019
- Accepted 3 September 2020
DOI:https://doi.org/10.1103/PhysRevFluids.5.103501
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