Abstract
This paper is concerned with the behaviour of buoyant plumes driven by a source of bubbles. It is shown experimentally that, when a bubble plume rises through a stratified environment, fluid can be transported vertically for some distance and then some of this fluid can leave the plume and spread out horizontally at its own density level. A simple plume model which regards the plume as a single entity is discussed in order to make a first assessment of the effects of gas expansion and bubble slip velocity in this stratified case. However, the experiments reveal a more complicated plume structure in which the bubbles remain in the centre part of the plume, and only the outer part of the plume spreads out into the environment at certain levels. On the basis of these observations a double-plume model is proposed which regards the plume as being composed of two parts: an inner circular plume (which contains all the bubbles of gas) and an outer annular plume.
Publisher
Cambridge University Press (CUP)
Subject
Mechanical Engineering,Mechanics of Materials,Condensed Matter Physics
Reference15 articles.
1. Topham, D. R. 1974 The hydrodynamic aspects of the behaviour of oil released under sea ice.Int. Rep. Dept. Electrical Engng, Univ. Alberta.
2. Ditmars, J. D. & Cederwall, K. 1974 Analysis of air-bubble plumes.Proc. 14th Conf. Coastal Engng, Copenhagen,p.2209.
3. Kobus, H. E. 1968 Analysis of the flow induced by air-bubble systems.Proc. 11th Conf. Coastal Engng, London,pp.1016–1031.
4. Morton, B. R. 1962 Coaxial turbulent jets.Int. J. Heat Mass Transfer 5,955–965.
5. Turner, J. S. 1963 The motion of buoyant elements in turbulent surroundings.J. Fluid Mech. 16,1–16.
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