The hydrodynamics of an oscillating porous sphere
Phys. Fluids 16, 62 (2004); doi:10.1063/1.1630051
Published 3 December 2003
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We determine the hydrodynamics of a rigid, weakly permeable sphere undergoing translational oscillations in an incompressible Newtonian fluid. We check using homogenization and scaling arguments that the flow inside the sphere may be modeled by Darcy's law and that the BeaversJosephSaffman (BJS) boundary condition still applies for oscillatory flows, provided the frequency of oscillation is not too high. The BJS boundary condition introduces a slip velocity and to leading order in
=
/a, where k is the particle permeability and a is the radius, the particle may be regarded as impermeable with a slip length independent of frequency. Under these circumstances we solve for the flow field, pressure distribution and drag explicitly and show their behavior for 0

0.05 and frequencies relevant to electroacoustics (110 MHz). From the drag we find the leading order corrections due to particle permeability of the pseudo-steady drag, Basset force and added mass. ©2004 American Institute of Physics.
= 

0.05 and frequencies relevant to electroacoustics (110 MHz). From the drag we find the leading order corrections due to particle permeability of the pseudo-steady drag, Basset force and added mass. ©2004 American Institute of Physics.
| History: | Received 19 June 2003; accepted 6 October 2003; published 3 December 2003 |
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http://link.aip.org/link/?PHFLE6/16/62/1 |
EDITORIALLY RELATED
- Comment on "The hydrodynamics of an oscillating porous sphere" [Phys. Fluids 16, 62 (2004)]
Efstathios E. Michaelides et al.
Phys. Fluids 16, 4758 (2004) - Response to "Comment on `The hydrodynamics of an oscillating porous sphere' " [Phys. Fluids 16, 4758 (2004)]
Jason R. Looker et al.
Phys. Fluids 16, 4760 (2004)
KEYWORDS and PACS
RELATED DATABASES
PUBLICATION DATA
1070-6631 (print)
1089-7666 (online)
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