Abstract
Results from direct numerical simulations of an unsteady
turbulent shear layer with
a free surface are presented. The emphasis is on the interaction
dynamics of the
free surface with the coherent vortices in the underlying turbulent
shear flow as well
as the resulting free-surface signatures. Instantaneous vortex lines
and isosurfaces
of enstrophy indicate that coherent horseshoe vortical structures
emerge from the
random initial vorticity field. These horseshoe vortices impinge,
break and reconnect
onto the free surface, and then appear as two vortex connections
with opposite signs
on the surface. The two identified vortical structures correspond to
‘splatting’ and
‘swirling’ events, which have been observed in other
experiments and simulations of
free-surface/turbulence flows. Though free-surface depressions
form near the vertical-vorticity centres in the connection processes,
only a low correlation (≈50% to 60%)
is found between the free-surface roughness (vertical deformation) and
the connected
normal vorticity. On the other hand, the free-surface curvatures and
the tangential
free-surface vorticities are better correlated (≈80% to 90%). The
balance of enstrophy
and the vorticity transport show that stretching and viscous dissipation
along the
direction of the vorticity vector dominate the vortex dynamics near
the free surface.
These two transport mechanisms are found to be responsible for the
cancellation
of the spanwise vorticity of the horseshoe-vortex heads and the
annihilation of the surface-connected normal vorticities.
Publisher
Cambridge University Press (CUP)
Subject
Mechanical Engineering,Mechanics of Materials,Condensed Matter Physics
Cited by
58 articles.
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