L. Kaiktsis et al., UNSTEADINESS AND CONVECTIVE INSTABILITIES IN 2-DIMENSIONAL FLOW OVER A BACKWARD-FACING STEP, Journal of Fluid Mechanics, 321, 1996, pp. 157-187
A systematic study of the stability of the two-dimensional flow over a
backward-facing step with a nominal expansion ratio of 2 is presented
up to Reynolds number Re = 2500 using direct numerical simulation as
well as local and global stability analysis. Three different spectral
element computer codes are used for the simulations. The stability ana
lysis is performed both locally (at a number of streamwise locations)
and globally (on the entire field) by computing the leading eigenvalue
s of a base flow state. The distinction is made between convectively a
nd absolutely unstable mean flow. In two dimensions, it is shown that
all the asymptotic flow states up to Re = 2500 are time-independent in
the absence of any external excitation, whereas the flow is convectiv
ely unstable, in a large portion of the flow domain, for Reynolds numb
ers in the range 700 less than or equal to Re less than or equal to 25
00. Consequently, upstream generated small disturbances propagate down
stream at exponentially amplified amplitude with a space-dependent spe
ed. For small excitation disturbances, the amplitude of the resulting
waveform is proportional to the disturbance amplitude. However, select
ive sustained external excitation (even at small amplitudes) can alter
the behaviour of the system and lead to time-dependent flow. Two diff
erent types of excitation are imposed at the inflow: (i) monochromatic
waves with frequency chosen to be either close to or very far from th
e shear layer frequency; and (ii) random noise. It is found that for s
mall-amplitude monochromatic excitation the flow acquires a time-perio
dic behaviour if perturbed close to the shear layer frequency, whereas
the flow remains unaffected for high values of the excitation frequen
cy. On the other hand, for the random noise as input, an unsteady beha
viour is obtained with a fundamental frequency close to the shear laye
r frequency.