What determines size distributions of heavy drops in a synthetic turbulent flow?
Nonlinear Processes in Geophysics, Volume 16, Issue 6, 2009, pp.677-690
We present results from an individual particle based model for the
collision, coagulation and fragmentation of heavy drops moving in a
turbulent flow. Such a model framework can help to bridge the gap
between the full hydrodynamic simulation of two phase flows, which can
usually only study few particles and mean field based approaches for
coagulation and fragmentation relying heavily on parameterization and
are for example unable to fully capture particle inertia. We study the
steady state that results from a balance between coagulation and
fragmentation and the impact of particle properties and flow properties
on this steady state. We compare two different fragmentation mechanisms,
size-limiting fragmentation where particles fragment when exceeding a
maximum size and shear fragmentation, where particles break up when
local shear forces in the flow exceed the binding force of the particle.
For size-limiting fragmentation the steady state is mainly influenced by
the maximum stable particle size, while particle and flow properties
only influence the approach to the steady state. For shear fragmentation
both the approach to the steady state and the steady state itself depend
on the particle and flow parameters. There we find scaling relationships
between the steady state and the particle and flow parameters that are
determined by the stability condition for fragmentation.