| A further effect that leads
to an attenuation of sound pressure is the atmospheric absorption.
As the sound waves propagate
through the air, sound energy is lost due to friction between air molecules
and because of further properties of the molecules. This loss depends on
the air temperature und humidity. High frequencies are much more affected
by atmospheric absoprtion than low frequencies. Therefore, one can hear
only the bass tones at greater distance from an open air concert. |
|
Attenuation by air absorption at 20 °C and 70 % relative humidity
(after ISO 9613-2)
| 125 Hz |
0,3 dB/km |
| 250 Hz |
1,1 dB/km |
| 500 Hz |
2,8 dB/km |
| 1000 Hz |
5,0 dB/km |
| 2000 Hz |
9,0 dB/km |
| 8000 Hz |
76,6 dB/km |
|