Jump to content

Acoustic radiation pressure

From Wikipedia, the free encyclopedia

This is an old revision of this page, as edited by InternetArchiveBot (talk | contribs) at 03:56, 26 June 2017 (Rescuing 1 sources and tagging 1 as dead. #IABot (v1.4beta4)). The present address (URL) is a permanent link to this revision, which may differ significantly from the current revision.

Acoustic radiation pressure is the apparent pressure difference between the average pressure at a surface moving with the displacement of the wave propagation (the Lagrangian pressure) and the pressure that would have existed in the fluid of the same mean density when at rest. Numerous authors make a distinction between the phenomena of Rayleigh radiation pressure and Langevin radiation pressure.

See also

References

  • RT Beyer (1978). "Radiation pressure—the history of a mislabeled tensor" (PDF). The Journal of the Acoustical Society of America. Bibcode:1978ASAJ...63.1025B. doi:10.1121/1.381833.[permanent dead link]
  • Boa‐Teh Chu, Apfel RE (December 1982). "Acoustic radiation pressure produced by a beam of sound". J. Acoust. Soc. Am. 72 (6): 1673–1687. Bibcode:1982ASAJ...72.1673C. doi:10.1121/1.388660.
  • Hasegawa T, Kido T, Iizuka T, Matsuoka C (2000). "A general theory of Rayleigh and Langevin radiation pressures". J Acoust Soc Jpn E. 21 (3): 145–152. doi:10.1250/ast.21.145. ISSN 0388-2861. Archived from the original on 2012-02-29. {{cite journal}}: Unknown parameter |deadurl= ignored (|url-status= suggested) (help)