Low frequency vibration induced streaming in a Hele-Shaw cell
Abstract
When an acoustic wave propagates in a fluid, it can generate a second order flow
whose characteristic time is much longer than the period of thewave.Within a range of
frequency between ten and several hundred Hz, a relatively simple and versatile way
to generate streaming flow is to put a vibrating object in the fluid. The flow develops
vortices in the viscous boundary layer located in the vicinity of the source of vibrations,
leading in turn to an outer irrotational streaming called Rayleigh streaming. Because
the flow originates from non-linear time-irreversible terms of the Navier-Stokes equation,
this phenomenon can be used to generate efficient mixing at low Reynolds number,
for instance in confined geometries. Here, we report on an experimental study of
such streaming flow induced by a vibrating beam in a Hele-Shaw cell of 2 mm span
using long exposure flowvisualization and particle-image velocimetry measurements.
Our study focuses especially on the effects of forcing frequency and amplitude on
flow dynamics. It is shown that some features of this flow can be predicted by simple
scaling arguments and that this vibration-induced streaming facilitates the generation
of vortices.
Domains
Physics [physics] Mechanics [physics] Fluid mechanics [physics.class-ph] Physics [physics] Physics [physics] Fluid Dynamics [physics.flu-dyn] Nonlinear Sciences [physics] Pattern Formation and Solitons [nlin.PS] Physics [physics] Condensed Matter [cond-mat] Soft Condensed Matter [cond-mat.soft]
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