Talk
Abstract:
Fluctuations and Structures in Dilute Sedimentation
Peter
J. Mucha
Department of Mathematics
Massachusetts Institute of Technology
mucha@math.mit.edu
This work was done in collaboration with Michael
P. Brenner, Dept. of Mathematics, MIT; and Boris
I. Shraiman, Bell Labs, Lucent Technologies.
Particulate suspension flows arise in a number of industrial,
environmental, and biological contexts. In the creeping flow
(Re=0) limit, the particles in these dynamically-evolving heterogeneous
flows interact via a long-range advection, decaying as small
inverse powers of particle separation. We consider the dilute,
creeping flow limit of a noncolloidal suspension of monodisperse
rigid spheres sedimenting under gravity in an otherwise Newtonian
incompressible liquid. Nonintegrability of the microstructural
Green's functions makes macroscopic averaging difficult, and
leads to the troublesome possibility that velocity fluctuations
diverge with increasing system size as proposed by Caflisch
and Luke. Simulations indicate the presence of coherent "blobs,"
which control the velocity fluctuations and particle diffusivity.
Non-trivial scaling of density correlation times is explained
in terms of particle displacements, and conditional density
correlations demonstrate that the blobs are long-lived structures.
Results are compared with recent experiments.
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