Buoyancy effects in steeply inclined air-water
bubbly shear flow in a rectangular channel
K. Sanaullah1, M. Arshad2, A. Khan1, and I.R. Chughtai2
1Faculty of Engineering, UNIMAS, Kota Samarahan, Malaysia
2Department of Chemical Engineering, Nilore, Islamabad, Pakistan
E-mail: skhairuddin@feng.unimas.my
Keywords: gas-liquid bubbly flow, void fraction, mean shear velocity
Pages: 463–473
Abstract
We report measurements of two-dimensional (B/D = 5) fully turbulent and developed duct flows (overall length/depth, L/D = 60; D-based Reynolds number Re > 104) for inclinations to 30° from vertical at low voidages (< 5 % sectional average) representative of disperse regime using tap water bubbles (4-6 mm) and smaller bubbles (2 mm) stabilised in ionic solution. Pitot and static probe instrumentation, primitive but validated, provided adequate (10 % local value) discrimination of main aspects of the mean velocity and voidage profiles at representative streamwise station i.e L/D
= 40. Our results can be divided into three categories of behaviour. For
vertical flow (0°) the evidence is inconclusive as to whether bubbles are
preferentially trapped within the wall-layer as found in some, may be most earlier experimental works. Thus, the
4-mm bubbles showed indication of voidage retention but the 2-mm bubbles
did not. For nearly vertical flow (5°) there was pronounced profiling of voidage especially with 4-mm bubbles
but the transverse transport was not suppressed sufficiently to induce any
obvious layering. In this context, we also refer to similarities with previous
work on one-phase vertical and nearly vertical mixed convection flows
displaying buoyancy inhibited mean shear turbulence. However, with inclined
flow (10+ degrees) a distinctively layered pattern was invariably manifested in
which voidage confinement increased with increasing inclination. In this paper
we address flow behavior at near vertical conditions. Eulerian, mixed and VOF
models were used to compute voidage and mean velocity profiles.
DOI: http://dx.doi.org/10.1134/S0869864315040071
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