For a long time,
SPH used an empirical term to describe viscosity and shear
effects. However, as demonstrated by numerous researchers (e.g.
Morris
et al. 1997), this is
inadequate for describing viscous flow effects properly.
At present, we are researching how to capture coherent turbulent
structures within complex free-surface flow fields by enhancing the
description of viscous effects. To this end, we have implemented
the particle equivalent of a Sub-Grid Scale (SGS) description
in a type of Large-Eddy
Simulation (LES) simulation. Similar work has been for
Incompressible SPH
(I-SPH) for free-surface flows by Lo & Shao (2002), etc., but
to date, not for (slightly) compressible SPH.
The animations on this page represent our first attempts to implement a
combined SPH and sub-particle scale (SPS) scheme. As our model is
still slightly compressible, we have used Favre-averaging with a
standard Smagorinsky viscosity model. For the solid walls, we
have used Monaghan's repulsive force boundary condition (Monaghan
& Kos 1999).
For
my ICCE2004 presentation complete with animations, click here (62MB) -
please be patient!
2-D Weakly
Plunging
Breaking Wave on a Beach
This 2-D breaking wave (surf similarity number 0.4) demonstrates the
one of the key advantages of using SPH to model free-surface
hydrodynamics. The overturning wavefront is nicely captured, and
this is then followed by the highly turbulent flow field predicted by
the SPS-LES scheme as the turbulent bore propagates up the beach
generating turbulent flow structures that persist beyond the passage of
the original wave (avi: 5.5MB).
3-D Weakly
Plunging
Breaking Wave on a Beach
This 3-D breaking wave is essentially the same case as for the 2-D case
above, only in 3-D. The simulation is too coarse, but is a taster
of things to come. As part of the effort towards capturing
coherent turbulent structures (focussing on their formation mechanisms,
role and importance), the same SPH-SPS scheme has been implemented and
looks to be capturing some eddies even at this coarse resolution (avi:
14MB).
The following animation is the same case, but looking at the vertical
vorticity in a horizontal plane at an intermediate water depth (avi:
17MB):
Solitary Wave
with periodic Open Boundaries
Clearly, this is not a turbulent flow
field! However, this case demonstrates that SPH-SPS does not
produce any spurious flow phenomena (i.e. is not doing anything it
shouldn't), and also shows that a solitary wave can be propagated
without loss of form which is difficult to do with empirical viscosity.