Direct numerical simulations of turbulent Taylor-Couette flow are performed up to inner cylinder Reynolds numbers of Rei = 105 for a radius ratio of η = ri/ro = 0.714 between the inner and outer cylinders. With increasing Rei, the flow under- goes transitions between three different regimes: (i) a flow dominated by large coher- ent structures, (ii) an intermediate transitional regime, and (iii) a flow with developed turbulence. In the first regime the large-scale rolls completely drive the meridional flow, while in the second one the coherent structures recover only on average. The presence of a mean flow allows for the coexistence of laminar and turbulent boundary layer dynamics. In the third regime, the mean flow effects fade away and the flow becomes dominated by plumes. The effect of the local driving on the azimuthal and angular velocity profiles is quantified, in particular, we show when and where those profiles develop.
Ostilla Mónico, R., van der Poel, E., Verzicco, R., Grossmann, S., Lohse, D. (2014). Boundary layer dynamics at the transition between the classical and the ultimate regime of Taylor-Couette flow. PHYSICS OF FLUIDS, 26(1), 015114 [10.1063/1.4863312].
Boundary layer dynamics at the transition between the classical and the ultimate regime of Taylor-Couette flow
VERZICCO, ROBERTO;
2014-01-01
Abstract
Direct numerical simulations of turbulent Taylor-Couette flow are performed up to inner cylinder Reynolds numbers of Rei = 105 for a radius ratio of η = ri/ro = 0.714 between the inner and outer cylinders. With increasing Rei, the flow under- goes transitions between three different regimes: (i) a flow dominated by large coher- ent structures, (ii) an intermediate transitional regime, and (iii) a flow with developed turbulence. In the first regime the large-scale rolls completely drive the meridional flow, while in the second one the coherent structures recover only on average. The presence of a mean flow allows for the coexistence of laminar and turbulent boundary layer dynamics. In the third regime, the mean flow effects fade away and the flow becomes dominated by plumes. The effect of the local driving on the azimuthal and angular velocity profiles is quantified, in particular, we show when and where those profiles develop.File | Dimensione | Formato | |
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