Abstract
The upward flow of a buoyant plume emanating from a horizontal fissure into a two-layered fluid region is considered. Solutions are computed numerically for a range of fissure widths and water depths. It is shown that for a given fluid depth and fissure size there is a minimum flow rate beneath which no steady solutions exist. At this limiting flow, the fluid detaches from the wall of the fissure via a stagnation point. Solutions exist for all values of flow rate above this minimum. Exact solutions are presented for very large flow rates.
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Hocking, G.C., Forbes, L.K. Steady flow of a buoyant plume into a constant-density layer. J Eng Math 67, 341–350 (2010). https://doi.org/10.1007/s10665-009-9324-9
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DOI: https://doi.org/10.1007/s10665-009-9324-9