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Encyclopedia > Acoustic velocity

Particle velocity or sound particle velocity is the velocity v of air particles in m/s. It is not to be confused with the speed of sound c, also measured in m/s. Usually in acoustics the particle velocity is measured as the particle velocity level Lv in decibels.


The particle velocity v in m/s is:

Sound pressure p in N/m2 = Pa
Acoustic impedance, sound impedance, or Characteristic impedance Z in N·s/m³
Sound intensity J in W/m2


The sound velocity is connected to particle displacement or particle amplitude ξ in m by:

acoustic impedance Z in N·s/m3
sound particle velocity v in m/s
frequency f in Hz
sound pressure p in N/m2 = Pa
angular frequency ω = 2 · π · f


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  Results from FactBites:
 
Acoustic impedance - Wikipedia, the free encyclopedia (301 words)
The acoustic impedance Z (or sound impedance) is the ratio of sound pressure p to particle velocity v in a medium or acoustic component.
Z can be either measured in its consituient units (pressure per velocity) or in rayls.
The acoustic impedance Z of an acoustic component (in Pa·s/m) is the ratio of sound pressure p to particle velocity v at a transition with a previous component:
Borehole Geophysics and Petrophysics - Acoustic logging (1336 words)
In acoustic logging, a transmitter located in the borehole emits a pulse of mechanical energy which is recorded by one or more receivers located in the borehole some distance away from the transmitter.
The compressional wave amplitude is used to determine the presence of cement grout behind steel casing and to assess the degree of bonding to the casing and the formation, in 'the cement bond log'.
In addition to the head waves, other modes of acoustic energy are present in the full waveform that arise because acoustic energy that is incident on the borehole wall at angles greater than the critical angle is completely reflected back into the borehole (ie, the borehole acts as a waveguide).
  More results at FactBites »


 
 

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