Flow structure and momentum transport for buoyancy driven mixing flows in long tubes at different tilt angles
Buoyancy driven mixing of fluids of different densities ( ρ 1 and ρ 2 ) in a long circular tube is studied experimentally at the local scale as a function of the tilt angle from vertical ( 15 ° ≤ θ ≤ 60 ° ) and of the Atwood number [ 10 − 3 ≤ At = ( ρ 2 − ρ 1 ) / ( ρ 2 + ρ 1 ) ≤ 10 − 2 ] . Particle...
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Veröffentlicht in: | Physics of fluids (1994) 2011-03, Vol.23 (3), p.035105-035105-14 |
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Sprache: | eng |
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Zusammenfassung: | Buoyancy driven mixing of fluids of different densities (
ρ
1
and
ρ
2
) in a long circular tube is studied experimentally at the local scale as a function of the tilt angle from vertical
(
15
°
≤
θ
≤
60
°
)
and of the Atwood number
[
10
−
3
≤
At
=
(
ρ
2
−
ρ
1
)
/
(
ρ
2
+
ρ
1
)
≤
10
−
2
]
. Particle Image Velocimetry (PIV) and Laser Induced Fluorescence (LIF) measurements in a vertical diametral plane provide the velocity and the relative concentration (and, hence, density) fields. A map of the different flow regimes observed as a function of At and
θ
has been determined: as At increases and
θ
is reduced, the regime varies from laminar to intermittent destabilizations and, finally, to developed turbulence. In the laminar regime, three parallel stable layers of different densities are observed; the velocity profile is linear and well predicted from the density profile. The thickness of the intermediate layer can be estimated from the values of At and
θ
. In the turbulent regime, the density varies slowly with
z
in the core of the flow: there, transverse turbulent momentum transfer is dominant. As At decreases and
θ
increases, the density gradient
β
in the core (and, hence, the buoyancy forces) becomes larger, resulting in higher extremal velocities and indicating a less efficient mixing. While the mean concentration varies with time in the turbulent regime, the mean velocity remains constant. In the strong turbulent regime (highest At and lowest
θ
values), the transverse gradient of the mean concentration and the fluctuations of concentration and velocity remain stationary, whereas they gradually decay with time when turbulence is weaker. |
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ISSN: | 1070-6631 1089-7666 |
DOI: | 10.1063/1.3560005 |