We report an experimental study of the properties of the velocity boundary layer in turbulent Rayleigh-Bénard convection in a cylindrical cell. The measurements were made at Rayleigh numbers Ra in the range 2.8 × 10 8 < Ra < 5.6 × 10 9 and were conducted with the convection cell tilted with an angle θ relative to gravity, at θ = 0. and 3.4 o , respectively. The fluid was water with Prandtl number P r = 5.3. It is found that at small tilt angles (θ 1 o ), the measured viscous boundary layer thickness δ v scales with the Reynolds number Re with an exponent close to that for a Prandtl-Blasius laminar boundary layer, i.e. δ v ∼ Re −0.46±0.03 . For larger tilt angles, the scaling exponent of δ v with Re decreases with θ. The normalized mean horizontal velocity profiles measured at the same tilt angle but with different Ra are found to have an invariant shape. But for different tilt angles, the shape of the normalized profiles is different.It is also found that the Reynolds number Re based on the maximum mean horizontal velocity scales with Ra as Re ∼ Ra 0.43 and the Reynolds number Re σ based on the maximum rms velocity scales with Ra as Re σ ∼ Ra 0.55 , with both exponents do not seem to depend on the tilt angle θ.Several wall quantities are also measured directly and their dependency on Re are found to agree well with those predicted for a classical laminar boundary layer. These are the wall shear stress τ (∼ Re 1.46 ), the viscous sublayer δ w (∼ Re 0.75 ), the friction velocity u τ (∼ Re −0.86 ) and the skin friction coefficient c f (∼ Re −0.46 ). Again, all these near-wall quantities do not seem to depend on the tilt angle.We also examined the dynamical scaling method proposed bys Zhou and Xia [Phys. Rev. Lett. 104, 104301 (2010)] and found that in both the laboratory and the dynamical frames the mean velocity profiles show deviations from the theoretical Prandtl-Blasius profile, with the deviations increase with Ra. But profiles obtained from dynamical scaling in general have better agreement with the theoretical profile. It is also found that the effectiveness of this method appears to be independent of Ra.1. Introduction
Rayleigh-Bénard convectionRayleigh-Bénard (RB) convection, which is a fluid layer heated from below and cooled from the top, is an idealized model to study turbulent flows involving heat transport and has attracted much attention during the past few decades (Siggia 1994;Kadanoff 2001;Ahlers, Grossmann & Lohse 2009;. The system is characterized by two control parameters: the Rayleigh number Ra, Prandtl number P r, which are defined arXiv:1209.6415v1 [physics.flu-dyn]