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S TEADY S TREAMING
Abstract
▪ Abstract The time-average of a fluctuating flow often results in a nonzero mean. Such steady streaming may result directly from the action of an oscillatory nonconservative body force or, if such a force is conservative, indirectly through the action of Reynolds stresses in the main body of the fluid or in thin boundary layers at no-slip boundaries. A theory for such streaming flows is developed for homogeneous fluids. For flows with a free surface it is demonstrated that a mechanism for steady streaming exists even in an inviscid fluid. Diverse areas in which steady streaming flows may be important are discussed.
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Cited by
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Friend, J., & Yeo, L. Y. (2011) · Reviews of Modern Physics · doi:10.1103/revmodphys.83.647 · Cited by 964
Acoustofluidics 14: Applications of acoustic streaming in microfluidic devices
Wiklund, M., Green, R., & Ohlin, M. (2012) · Lab on a Chip · doi:10.1039/c2lc40203c · Cited by 521
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Karimi, A., Yazdi, S., & Ardekani, A. M. (2013) · Biomicrofluidics · doi:10.1063/1.4799787 · Cited by 384
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Faghih, M. M., & Sharp, M. K. (2018) · Fluids and Barriers of the CNS · doi:10.1186/s12987-018-0103-8 · Cited by 101
Metadata
- Authors
- Riley, N.
- Venue
- Annual Review of Fluid Mechanics
- Publisher
- Annual Reviews
- Published
- 2001-01
- Volume
- 33
- Issue
- 1
- Pages
- 43-65
- ISSN
- 0066-4189 (ISSN-L)
- 1545-4479
- OpenAlex
- W4254847624
- Cited by
- 453
- References
- 0
- FWCI
- 1.65
- Type
- journal article
- Language
- en
- Open access
- closed
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