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Flood waves, dispersion

The shock wave acts as a liquid atomizer up to the point at which the momentum of the shock wave is able to disperse the liquid stream. By analogy with two-phase flow in packed columns, such hydrodynamic conditions can be construed as flooding. Hence, the region of stable atomization is mapped in terms of a flooding coefficient, defined as the mass flow ratio of undispersed liquid to the total liquid subject to the shock-wave field... [Pg.136]

See other pages where Flood waves, dispersion is mentioned: [Pg.137]    [Pg.144]    [Pg.428]    [Pg.16]    [Pg.13]    [Pg.26]    [Pg.255]    [Pg.289]    [Pg.1020]    [Pg.799]    [Pg.154]    [Pg.807]    [Pg.37]    [Pg.270]    [Pg.133]   
See also in sourсe #XX -- [ Pg.7 ]



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