Thermally driven vertical convection (VC) - the flow in a box heated on one side and cooled on the other side, is investigated using direct numerical simulations with Rayleigh numbers over the wide range of 10(7) <= Ra <= 10(14) and a fixed Prandtl number Pr = 10 in a two-dimensional convection cell with unit aspect ratio. It is found that the dependence of the mean vertical centre temperature gradient S on Ra shows three different regimes: in regime I (Ra less than or similar to 5 x 10(10)), S is almost independent of Ra; in the newly identified regime II (5 x 10(10) less than or similar to Ra less than or similar to 10(13)), S first increases with increasing Ra (regime IIa), reaches its maximum and then decreases again (regime IIb); and in regime III (Ra greater than or similar to 10(13)), S again becomes only weakly dependent on Ra, being slightly smaller than in regime I. The transition from regime I to regime II is related to the onset of unsteady flows arising from the ejection of plumes from the sidewall boundary layers. The maximum of S occurs when these plumes are ejected over approximately half of the area (downstream) of the sidewalls. The onset of regime III is characterized by the appearance of layered structures near the top and bottom horizontal walls. The flow in regime III is characterized by a well-mixed bulk region owing to continuous ejection of plumes over large fractions of the sidewalls, and, as a result of the efficient mixing, the mean temperature gradient in the centre S is smaller than that of regime I. In the three different regimes, significantly different flow organizations are identified: in regime I and regime IIa, the location of the maximal horizontal velocity is close to the top and bottom walls; however, in regime IIb and regime III, banded zonal flow structures develop and the maximal horizontal velocity now is in the bulk region. The different flow organizations in the three regimes are also reflected in the scaling exponents in the effective power law scalings Nu similar to Ra-beta and Re similar to Ra-gamma. Here, Nu is the Nusselt number and Re is the Reynolds number based on maximal vertical velocity (averaged over vertical direction). In regime I, the fitted scaling exponents (beta approximate to 0.26 and gamma approximate to 0.51) are in excellent agreement with the theoretical predictions of beta = 1/4 and gamma = 1/2 for laminar VC (Shishkina, Phys. Rev. E., vol. 93, 2016, 051102). However, in regimes II and III, beta increases to a value close to 1/3 and gamma decreases to a value close to 4/9. The stronger Ra dependence of Nu is related to the ejection of plumes and the larger local heat flux at the walls. The mean kinetic dissipation rate also shows different scaling relations with Ra in the different regimes.

Wang, Q., Liu, H., Verzicco, R., Shishkina, O., Lohse, D. (2021). Regime transitions in thermally driven high-Rayleigh number vertical convection. JOURNAL OF FLUID MECHANICS, 917 [10.1017/jfm.2021.262].

Regime transitions in thermally driven high-Rayleigh number vertical convection

Roberto Verzicco;
2021-01-01

Abstract

Thermally driven vertical convection (VC) - the flow in a box heated on one side and cooled on the other side, is investigated using direct numerical simulations with Rayleigh numbers over the wide range of 10(7) <= Ra <= 10(14) and a fixed Prandtl number Pr = 10 in a two-dimensional convection cell with unit aspect ratio. It is found that the dependence of the mean vertical centre temperature gradient S on Ra shows three different regimes: in regime I (Ra less than or similar to 5 x 10(10)), S is almost independent of Ra; in the newly identified regime II (5 x 10(10) less than or similar to Ra less than or similar to 10(13)), S first increases with increasing Ra (regime IIa), reaches its maximum and then decreases again (regime IIb); and in regime III (Ra greater than or similar to 10(13)), S again becomes only weakly dependent on Ra, being slightly smaller than in regime I. The transition from regime I to regime II is related to the onset of unsteady flows arising from the ejection of plumes from the sidewall boundary layers. The maximum of S occurs when these plumes are ejected over approximately half of the area (downstream) of the sidewalls. The onset of regime III is characterized by the appearance of layered structures near the top and bottom horizontal walls. The flow in regime III is characterized by a well-mixed bulk region owing to continuous ejection of plumes over large fractions of the sidewalls, and, as a result of the efficient mixing, the mean temperature gradient in the centre S is smaller than that of regime I. In the three different regimes, significantly different flow organizations are identified: in regime I and regime IIa, the location of the maximal horizontal velocity is close to the top and bottom walls; however, in regime IIb and regime III, banded zonal flow structures develop and the maximal horizontal velocity now is in the bulk region. The different flow organizations in the three regimes are also reflected in the scaling exponents in the effective power law scalings Nu similar to Ra-beta and Re similar to Ra-gamma. Here, Nu is the Nusselt number and Re is the Reynolds number based on maximal vertical velocity (averaged over vertical direction). In regime I, the fitted scaling exponents (beta approximate to 0.26 and gamma approximate to 0.51) are in excellent agreement with the theoretical predictions of beta = 1/4 and gamma = 1/2 for laminar VC (Shishkina, Phys. Rev. E., vol. 93, 2016, 051102). However, in regimes II and III, beta increases to a value close to 1/3 and gamma decreases to a value close to 4/9. The stronger Ra dependence of Nu is related to the ejection of plumes and the larger local heat flux at the walls. The mean kinetic dissipation rate also shows different scaling relations with Ra in the different regimes.
2021
Pubblicato
Rilevanza internazionale
Articolo
Esperti anonimi
Settore ING-IND/06 - FLUIDODINAMICA
English
convection in cavities
Wang, Q., Liu, H., Verzicco, R., Shishkina, O., Lohse, D. (2021). Regime transitions in thermally driven high-Rayleigh number vertical convection. JOURNAL OF FLUID MECHANICS, 917 [10.1017/jfm.2021.262].
Wang, Q; Liu, H; Verzicco, R; Shishkina, O; Lohse, D
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Utilizza questo identificativo per citare o creare un link a questo documento: https://hdl.handle.net/2108/315692
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