International audienceThis work focuses on the study of the transition from steady to chaotic behavior in mixed convection flow over a backward-facing step. Direct numerical simulations are performed in a two-dimensional horizontal channel of expansion ratio ER = 2 at step level. The effects of the temperature difference between the heated bottom wall and the inflow temperature are investigated by keeping constant the Richardson number at 1. The covered range of Grashof and Reynolds numbers is respectively 3.31 × 104 ⩽ Gr ⩽ 2.72 × 105 and 182.03 ⩽ Re ⩽ 521.34. The thermal and dynamical instabilities which cause the onset of unsteady flow are described in detail. A spectral and phase portrait analysis of the temperature time series allows us...
International audienceThe thermal effect on axisymmetry breaking and transition to turbulence in the...
The transition process from steady to turbulent convection via subharmonic bifurcation in thermocapi...
International audienceNatural convection of air between two infinite vertical differentially heated ...
International audienceThis work focuses on the study of the transition from steady to chaotic behavi...
Effect of the backward-facing step heights on turbulent mixed convection flow along a vertical flat ...
The effects of backward-facing and forward-facing steps on a turbulent buoyancy-dominated mixed-conv...
Measurements of turbulent mixed convection flow over a two-dimensional, vertical backward-facing ste...
The development of secondary instabilities in a boundary layer over a backward-facing step is invest...
The transition process from steady convection to chaos is experimentally studied in thermocapillary ...
Transition to turbulence of natural convection flows ensuing in a fluid layer between two differenti...
The transition mechanisms of natural convection flows ensuing in a fluid layer between two different...
The aim of the present study is the analysis of the transition to turbulence of natural convection f...
This paper presents a numerical solution to a two-dimensional laminar mixed convection flow in a ver...
Mixed convective flow and heat transfer characteristics for two-dimensional laminar flow in a channe...
Mixed convective heat transfer results for laminar, buoyancy-assisting, two-dimensional flow in a ve...
International audienceThe thermal effect on axisymmetry breaking and transition to turbulence in the...
The transition process from steady to turbulent convection via subharmonic bifurcation in thermocapi...
International audienceNatural convection of air between two infinite vertical differentially heated ...
International audienceThis work focuses on the study of the transition from steady to chaotic behavi...
Effect of the backward-facing step heights on turbulent mixed convection flow along a vertical flat ...
The effects of backward-facing and forward-facing steps on a turbulent buoyancy-dominated mixed-conv...
Measurements of turbulent mixed convection flow over a two-dimensional, vertical backward-facing ste...
The development of secondary instabilities in a boundary layer over a backward-facing step is invest...
The transition process from steady convection to chaos is experimentally studied in thermocapillary ...
Transition to turbulence of natural convection flows ensuing in a fluid layer between two differenti...
The transition mechanisms of natural convection flows ensuing in a fluid layer between two different...
The aim of the present study is the analysis of the transition to turbulence of natural convection f...
This paper presents a numerical solution to a two-dimensional laminar mixed convection flow in a ver...
Mixed convective flow and heat transfer characteristics for two-dimensional laminar flow in a channe...
Mixed convective heat transfer results for laminar, buoyancy-assisting, two-dimensional flow in a ve...
International audienceThe thermal effect on axisymmetry breaking and transition to turbulence in the...
The transition process from steady to turbulent convection via subharmonic bifurcation in thermocapi...
International audienceNatural convection of air between two infinite vertical differentially heated ...