Experimental study of convection in the compressible regime

Abstract

An experiment of thermal convection with significant compressible effects is presented. The high-gravity environment of a centrifuge and the choice of xenon gas enable us to observe an average adiabatic temperature gradient up to 3.5 K cm${}^{-1}$ over a 4 cm high cavity. At the highest rotation rate investigated, 9990 rpm, the superadiabatic temperature difference applied to the gas layer is less than the adiabatic temperature difference. The convective regime is characterized by a large Rayleigh number, about 10${}^{12}$, and dominant Coriolis forces (Ekman number of order 10${}^{-6}$). The analysis of temperature and pressure fluctuations in our experiments shows that the dynamics of the flow is in a quasi-geostrophic regime. Still, a classical power law (exponent 0.3 $\pm$ 0.04) is observed between the Nusselt number (dimensionless heat flux) and the superadiabatic Rayleigh number (dimensionless superadiabatic temperature difference). However, a potential hysteresis is seen between this classical high flux regime and a lower heat flux regime. It is unclear whether this is due to compressible or Coriolis effects. In the transient regime of convection from an isothermal state, we observe a local decrease of temperature which can only be explained by adiabatic decompression.

References in corpus (5)

• High Rayleigh number turbulent convection in a gas near the gas-liquid critical point
• Subcritical convection of liquid metals in a rotating sphere using a quasi-geostrophic model
• Anelastic Versus Fully Compressible Turbulent Rayleigh-Bénard Convection
• Rayleigh-Benard stability and the validity of quasi-Boussinesq or quasi-anelastic liquid approximations
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Cited by in corpus (4)

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• Acoustic modes of rapidly rotating ellipsoids subject to centrifugal gravity
• Geophysical flows over topography, a playground for laboratory experiments