JJ should note that the information provided by Pearce and Sengpiel is for
the atmospheric absorption of the sound which is in addition to the the
normal 6 dB per doubling of distance or inverse square law attenuation.
Also, within the the first several hundred feet or meters from the source,
if the source and listener are near the ground and the ground is soft, you
will get additional attenuation from the ground interaction.
At longer distances, depending on wind direction and whether the temperature
is increasing or decreasing with altitude, the sound could be decreasing
much more rapidly.
>> Thanks!
>
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> and sound studio techniques
> http://www.sengpielaudio.com
The Ghost - 30 Jun 2005 01:32 GMT
> JJ should note that the information provided by Pearce and Sengpiel is
> for the atmospheric absorption of the sound which is in addition to
> the the normal 6 dB per doubling of distance or inverse square law
> attenuation.
JJ should also note that the 6dB decrease in sound pressure level per
doubling of distance applies only in the far field and only if the source
is a point source (one having dimensions that are small compared to a
wavelength). For a line source (eg a long straight-line stretch of
freeway), the decrease in the far field is 3dB per doubling of distance.
Noral Stewart - 30 Jun 2005 12:21 GMT
True and these are basics that should have been the starting point.
>> JJ should note that the information provided by Pearce and Sengpiel is
>> for the atmospheric absorption of the sound which is in addition to
[quoted text clipped - 6 lines]
> wavelength). For a line source (eg a long straight-line stretch of
> freeway), the decrease in the far field is 3dB per doubling of distance.