Natural convection flows in air filled, differentially heated cavities with adiabatic horizontal walls
Résumé
Two-dimensional natural convection in air-filled differentially heated cavities with adiabatic
horizontal walls has been revisited by using stability analysis algorithms such as Newtons
iteration (steady-state solving), Arnoldis method, and the continuation method. We are
particularly interested in computing Hopf bifurcation points characterizing the onset of
time-dependent flows in these cavities.
Aspect ratios of 17 have been investigated, and accurate critical points of several unstable
modes which were not fully available in the literature have been provided for each cavity.
The critical values agree well with the results available and confirm previous observations:
for A=13 the onset of time-dependent flows is due to the detached flow structure near the
exiting corners of vertical boundary layers; for A=48 the onset of time-dependent flows
results from traveling waves in vertical boundary layers. Investigating mesh dependence
showed that the critical values obtained possess four significants figures for A=13 and
six for A=48.
Steady-state solution by Newtons iteration allowed us to discover multiple steady-state
solutions at A about 3, which have never been reported before. The first branch, B1, of
steady-state solutions exists up to a turning point where is born the second branch, B2. It
ends at another turning point at lower Rayleigh number, and one observes the third branch,
B3, for increasing Rayleigh number. Solutions on B1 do not exhibit any detached flow structure,
but those on B2 and B3 do. The detached flow structure is more pronounced on B3 than
on B2. For A=3, B3 becomes unstable because of the detached flow structure. With increasing
A, branch B1 becomes unstable to traveling waves of vertical boundary layers and the
stable part of B3 decreases and disappears completely. Due to different instability mechanisms
observed on branches B1 and B3, there exist multiple time-dependent flows of quite different
frequencies (for A=3.4 at Ra =1.15 10(8), for example), which is also a novel
phenomenon. Multiple steady-state solutions disappear between A=2.8 and 2.9 and are
believed to be closely linked to the behavior of the detached flow and the limiting effect
of increasing A.