4.7 Article

Mean velocity and temperature profiles in turbulent Rayleigh-Benard convection at low Prandtl numbers

Journal

JOURNAL OF FLUID MECHANICS
Volume 918, Issue -, Pages -

Publisher

CAMBRIDGE UNIV PRESS
DOI: 10.1017/jfm.2021.255

Keywords

Benard convection; buoyant boundary layers; turbulent convection

Funding

  1. Hong Kong Research Grants Council [16301719, N_HKUST604/19, 16305819]
  2. National Natural Science Foundation of China [11772111, 91952101, 11702128, 11961160719, 91752201]
  3. Deutsche Forschungsgemeinschaft [DFG-SPP 1881]

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This study investigates the mean velocity and temperature profiles in turbulent Rayleigh-Benard convection at low Prandtl numbers through direct numerical simulation, revealing changes in flow patterns and proposing balance equations to describe the distribution characteristics of velocity and temperature.
We report a direct numerical simulation (DNS) study of the mean velocity and temperature profiles in turbulent Rayleigh-Benard convection (RBC) at low Prandtl numbers (Pr). The numerical study is conducted in a vertical thin disk with Pr varied in the range 0.17 <= Pr <= 4.4 and the Rayleigh number (Ra) varied in the range 5 x 10(8) <= Ra <= 1 x 10(10). By varying Pr from 4.4 to 0.17, we find a sharp change of flow patterns for the large-scale circulation (LSC) from a rigid-body rotation to a near-wall turbulent jet. We numerically examine the mean velocity equation in the bulk region and find that the mean horizontal velocity profile u(z) can be determined by a balance equation between the mean convection and turbulent diffusion with a constant turbulent viscosity.t. This balance equation admits a self-similarity jet solution, which fits the DNS data well. In the boundary-layer region, we find that both the mean temperature profile T(z) and u(z) can be determined by a balance equation between the molecular diffusion and turbulent diffusion. Within the viscous boundary layer, both u(z) and T(z) can be solved analytically and the analytical results agree well with the DNS data. Our careful characterisation of the mean velocity and temperature profiles in low-Pr RBC provides a further understanding of the intricate interplay between the LSC, plume emission and boundary-layer dynamics, and pinpoints the physical mechanism for the emergence of a pronounced LSC in low-Pr RBC.

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