1964
DOI: 10.2514/3.2604
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Pressure gradient effects on nonequilibrium far wakes

Abstract: To summarize, the following conclusions are noteworthy: 1) The azimuthal component of velocity is nonzero in contrast to nonrotating case in which v$> = 0.2) The rotating effect generates vorticity in that, for large distances, the flow pattern is irrotational in the nonrotating case. In the rotating case, the azimuthal component of velocity is responsible for vorticity for large R.3) The wave-like terms f n (hR) (corresponding to a boundary layer) appearing in the solution, effective in a small distance from … Show more

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