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Air Absorption
This section provides some further details regarding acoustic air
absorption [326]. For a plane wave, the decline of
acoustic intensity as a function of propagation distance
is given
by
where
Tables F.1 and F.2 (adapted from
[322]) give some typical values for air.
Table:
Attenuation constant
(in inverse
meters) at 20tex2html_wrap_inline^&cir#circ; C and standard atmospheric pressure
| Relative |
Frequency in Hz |
| Humidity |
1000 |
2000 |
3000 |
4000 |
| 40 |
0.0013 |
0.0037 |
0.0069 |
0.0242 |
| 50 |
0.0013 |
0.0027 |
0.0060 |
0.0207 |
| 60 |
0.0013 |
0.0027 |
0.0055 |
0.0169 |
| 70 |
0.0013 |
0.0027 |
0.0050 |
0.0145 |
|
Table:
Attenuation in dB per kilometer at
20tex2html_wrap_inline^&cir#circ;C and standard atmospheric pressure.
| Relative |
Frequency in Hz |
| Humidity |
1000 |
2000 |
3000 |
4000 |
| 40 |
5.6 |
16 |
30 |
105 |
| 50 |
5.6 |
12 |
26 |
90 |
| 60 |
5.6 |
12 |
24 |
73 |
| 70 |
5.6 |
12 |
22 |
63 |
|
Previous:
Speed of Sound in AirNext:
Problems
written by Julius Orion Smith III
Julius Smith's background is in electrical engineering (BS Rice 1975, PhD Stanford 1983). He is presently Professor of Music and Associate Professor (by courtesy) of Electrical Engineering at
Stanford's Center for Computer Research in Music and Acoustics (CCRMA), teaching courses and pursuing research related to signal processing applied to music and audio systems. See
http://ccrma.stanford.edu/~jos/ for details.