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Free keywords:
turbulence simulation; turbulent boundary layers; turbulent convection
Abstract:
In thermal convection for very large Rayleigh numbers (Ra), the thermal and viscous boundary layers are expected to undergo a transition from a classical state to an ultimate state. In the former state, the boundary-layer thicknesses follow a laminar-like Prandtl-Blasius-Polhausen scaling, whereas in the latter, the boundary layers are turbulent with logarithmic corrections in the sense of Prandtl and von Karman. Here, we report evidence of this transition via changes in the boundary-layer structure of vertical natural convection (VC), which is a buoyancy-driven flow between differentially heated vertical walls. The numerical dataset spans Ra values from 105 to 109 and a constant Prandtl number value of 0.709. For this Ra range, the VC flow has been previously found to exhibit classical state behaviour in a global sense. Yet, with increasing Ra, we observe that near-wall higher-shear patches occupy increasingly larger fractions of the wall areas, which suggest that the boundary layers are undergoing a transition from the classical state to the ultimate shear-dominated state. The presence of streaky structures-reminiscent of the near-wall streaks in canonical wall-bounded turbulence-further supports the notion of this transition. Within the higher-shear patches, conditionally averaged statistics yield a logarithmic variation in the local mean temperature profiles, in agreement with the log law of the wall for mean temperature, and an Ra-0.37 effective power-law scaling of the local Nusselt number. The scaling of the latter is consistent with the logarithmically corrected 1/2 power-law scaling predicted for ultimate thermal convection for very large Ra. Collectively, the results from this study indicate that turbulent and laminar-like boundary layer coexist in VC at moderate to high Ra and this transition from the classical state to the ultimate state manifests as increasingly larger shear-dominated patches, consistent with the findings reported for Rayleigh-Benard convection and Taylor-Couette flows.
