Heat transport by turbulent Rayleigh-B\'enard convection for \ 0.8 and 4× 1011 \ 2×1014: Ultimate-state transition for aspect ratio = 1.00
Abstract
We report experimental results for heat-transport measurements by turbulent Rayleigh-B\'enard convection in a cylindrical sample of aspect ratio D/L = 1.00 (D = 1.12 m is the diameter and L = 1.12 m the height). They are for the Rayleigh-number range 4×1011 2×1014 and for Prandtl numbers \ between 0.79 and 0.86. For < *1 2× 1013 we find = N0 γeff with γeff = 0.321 0.002 and N0 = 0.0776, consistent with classical turbulent Rayleigh-B\'enard convection in a system with laminar boundary layers below the top and above the bottom plate and with the prediction of Grossmann and Lohse. For > 1* the data rise above the classical-state power-law and show greater scatter. In analogy to similar behavior observed for = 0.50, we interpret this observation as the onset of the transition to the ultimate state. Within our resolution this onset occurs at nearly the same value of 1* as it does for = 0.50. This differs from an earlier estimate by Roche et al. which yielded a transition at U 1.3× 1011 -2.5 0.5. A -independent *1 would suggest that the boundary-layer shear transition is induced by fluctuations on a scale less than the sample dimensions rather than by a global -dependent flow mode. Within the resolution of the measurements the heat transport above 1* is equal for the two values, suggesting a universal aspect of the ultimate-state transition and properties. The enhanced scatter of \ in the transition region, which exceeds the experimental resolution, indicates an intrinsic irreproducibility of the state of the system.
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