Transition phenomena in unstably stratified turbulent flows

Abstract

We study experimentally and theoretically transition phenomena caused by the external forcing from Rayleigh-Benard convection with the large-scale circulation (LSC) to the limiting regime of unstably stratified turbulent flow without LSC whereby the temperature field behaves like a passive scalar. In the experiments we use the Rayleigh-Bénard apparatus with an additional source of turbulence produced by two oscillating grids located nearby the side walls of the chamber. When the frequency of the grid oscillations is larger than 2 Hz, the large-scale circulation (LSC) in turbulent convection is destroyed, and the destruction of the LSC is accompanied by a strong change of the mean temperature distribution. However, in all regimes of the unstably stratified turbulent flow the ratio $[({\ell }_x{\nabla }_{x}T{)}^2+({\ell }_y{\nabla }_{y}T{)}^2+({\ell }_z{\nabla }_{z}T{)}^2]/<{\theta }^2>$ varies slightly (even in the range of parameters whereby the behaviour of the temperature field is different from that of the passive scalar). Here ${\ell }_i$ are the integral scales of turbulence along x, y, z directions, T and θare the mean and fluctuating parts of the fluid temperature. At all frequencies of the grid oscillations we have detected the long-term nonlinear oscillations of the mean temperature. The theoretical predictions based on the budget equations for turbulent kinetic energy, turbulent temperature fluctuations and turbulent heat flux, are in agreement with the experimental results.

14 pages, 14 figures, REVTEX4-1, revised version

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• Sheared stably stratified turbulence and large-scale waves in a lid driven cavity
• Tracer dispersion in the turbulent convective layer
• Large-scale circulations in a shear-free convective turbulence: Mean-field simulations
• Experimental investigation of turbulence and turbulent thermal diffusion in strongly inhomogeneous and anisotropic forced convection
• Detection of standing internal gravity waves in experiments with convection over a wavy heated wall