Statistical and geometrical properties of thermal plumes in turbulent Rayleigh-Bénard convection

Abstract

We present a systematic experimental study of geometric and statistical properties of thermal plumes in turbulent Rayleigh-Bénard convection using the thermochromic-liquid-crystal (TLC) technique. The experiments were performed in three water-filled cylindrical convection cells with aspect ratios 2, 1, and 0.5 and over the Rayleigh-number range $5\times 10^7\le Ra\le 10^{11}$. TLC thermal images of horizontal plane cuts at various depths below the top plate were acquired. Three-dimensional images of thermal plumes were then reconstructed from the two-dimensional slices of the temperature field. The results show that the often-called sheetlike plumes are really one-dimensional structures and may be called rodlike plumes. We find that the number densities for both sheetlike/rodlike and mushroomlike plumes have power-law dependence on $Ra$ with scaling exponents of $\sim 0.3$, which is close to that between the Nusselt number $Nu$ and $Ra$. This result suggests that it is the plume number that primarily d ermines the scaling exponent of the $Nu$-$Ra$ scaling relation. The evolution of the aspect ratio of sheetlike/rodlike plumes reveals that as $Ra$ increases the plume geometry changes from more-elongated to less-elongated. Our study of the plume area fraction (fraction of coverage over the surface of the plate) further reveals that the increased plume numbers with $Ra$ mainly comes from increased plume emission, rather than fragmentation of plumes. In addition, the area, perimeter, and the shape complexity of the two-dimensional horizontal cuts of sheetlike/rodlike plumes were studied and all are found to obey log-normal distributions.

22 pages, 16 figures, submitted to the New Journal of Physics

References in corpus (2)

• Large scale dynamics in turbulent Rayleigh-Benard convection
• Lagrangian studies in convective turbulence

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• A pressure-free long-time stable reduced-order model for two-dimensional Rayleigh-Bénard convection
• Off-center gravity induces large-scale flow patterns in spherical Rayleigh-Bénard