Experiments have been conducted in a water flume to simulate finite-length line sources of heat that issue horizontally at ground level into a coflowing turbulent shear flow. The downstream development of each buoyant jet is documented by detailed mean temperature measurements, which are analyzed to determine the jet trajectory, spread rates, and distance to the point of liftoff from the surface. In addition, a three-dimensional, parabolic, numerical model based on the fundamental conservation equations is developed. Model predictions of several buoyant jets compare reasonably with the experimental data and suggest that the strength of the streamwise vorticity plays an important role in governing liftoff of a buoyant wall jet from the surface.
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Three-Dimensional Buoyant Wall Jets Released Into a Coflowing Turbulent Boundary Layer
J. R. Sinclair,
J. R. Sinclair
Department of Mechanical Engineering, University of Waterloo, Waterloo, Ontario, Canada N2L 3G1
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P. R. Slawson,
P. R. Slawson
Department of Mechanical Engineering, University of Waterloo, Waterloo, Ontario, Canada N2L 3G1
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G. A. Davidson
G. A. Davidson
Department of Mechanical Engineering, University of Waterloo, Waterloo, Ontario, Canada N2L 3G1
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J. R. Sinclair
Department of Mechanical Engineering, University of Waterloo, Waterloo, Ontario, Canada N2L 3G1
P. R. Slawson
Department of Mechanical Engineering, University of Waterloo, Waterloo, Ontario, Canada N2L 3G1
G. A. Davidson
Department of Mechanical Engineering, University of Waterloo, Waterloo, Ontario, Canada N2L 3G1
J. Heat Transfer. May 1990, 112(2): 356-362 (7 pages)
Published Online: May 1, 1990
Article history
Received:
October 31, 1988
Revised:
June 7, 1989
Online:
May 23, 2008
Citation
Sinclair, J. R., Slawson, P. R., and Davidson, G. A. (May 1, 1990). "Three-Dimensional Buoyant Wall Jets Released Into a Coflowing Turbulent Boundary Layer." ASME. J. Heat Transfer. May 1990; 112(2): 356–362. https://doi.org/10.1115/1.2910385
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