When a sound wave strikes a surface,
it is reflected. However, some of the wave may be absorbed. The
absorption coefficient may be read from the Table knowing the dB
reduction that occurred on reflection.
For most materials, the average absorption of a surface is reasonably
well defined by an angle of incidence of 45°.
| dB
Change |
Absorption Coefficient
|
dB Change
|
Absorption Coefficient |
|
-1
|
0.21
|
-8
|
0.84
|
|
-2
|
0.37
|
-9
|
0.87
|
|
-3
|
0.50
|
-10
|
0.90
|
|
-4
|
0.60
|
-11
|
0.92
|
|
-5
|
0.68
|
-12
|
0.94
|
|
-6
|
0.75
|
-14
|
0.95
|
|
-7
|
0.80
|
-15
|
0.96
|
The term "ground interference effect"
is used to describe the broad absorption effect of ground such as sand,
earth and fields. Hard surfaces such as roads and parking
lots show an interference effect too, as shown by a blue line below,
but are not included in the term "ground interference effect".
The ground interference effect provides
natural sound attenuation as the wave grazes across open land. In most
cases of sound propagation outdoors, the ground surface does not supply
much sound absorption in comparison with the perfect absorption
provided by the sky. However, the impedance of the ground is
important in providing sound attenuation through the so-called ground
interference effect.

The figure above shows the basis for this
effect -- when the ground is soft, the wave that reflects can he out of
phase with the direct wave from source to receiver. This leads to
destructive interference over a broad frequency band. The upper limit
of this frequency band is determined only by geometry, and
automatically scales if the full scale geometry is reproduced in the
model.

The lower limit of this band, and the magnitude of the interference
effect are determined by geometry and impedance of the
ground. The data in the two figures show the simulation of
ground effect by two different research groups.

In both cases, the field data is that of
Parkin and Scholes.