Abstract
To date, a comprehensive understanding of the influence of the Prandtl number (
$Pr$
) on flow topology in turbulent Rayleigh–Bénard convection (RBC) remains elusive. In this study, we present an experimental investigation into the evolution of flow topology in quasi-two-dimensional turbulent RBC with
$7.0 \leq Pr \leq 244.2$
and
$2.03\times 10^{8} \leq Ra \leq 2.81\times 10^{9}$
. Particle image velocimetry (PIV) measurements reveal the flow transitions from multiple-roll state to single-roll state with increasing
$Ra$
, and the transition is hindered with increasing
$Pr$
, i.e. the transitional Rayleigh number
$Ra_t$
increases with
$Pr$
. We mapped out a phase diagram on the flow topology change on
$Ra$
and
$Pr$
, and identified the scaling of
$Ra_t$
on
$Pr$
:
$Ra_t \sim Pr^{0.93}$
in the low
$Pr$
range, and
$Ra_t \sim Pr^{3.3}$
in the high
$Pr$
range. The scaling in the low
$Pr$
range is consistent with the model of balance of energy dissipation time and plume travel time that we proposed in our previous study, while the scaling in the high
$Pr$
range implies a new governing mechanism. For the first time, the scaling of
$Re$
on
$Ra$
and
$Pr$
is acquired through full-field PIV velocity measurement,
$Re \sim Ra^{0.63}\,Pr^{-0.87}$
. We also propose that increasing horizontal velocity promotes the formation of the large-scale circulation (LSC), especially for the high
$Pr$
case. Our proposal was verified by achieving LSC through introducing horizontal driving force
$Ra_H$
by tilting the convection cell with a small angle.
Funder
National Natural Science Foundation of China
China Postdoctoral Science Foundation
Higher Education Discipline Innovation Project
Publisher
Cambridge University Press (CUP)