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Introduction to Acoustics

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128 Part A Propagation of Sound<br />

Part A 4.6<br />

Normalized impedance<br />

800<br />

5.7° 400<br />

0.057°<br />

600<br />

400<br />

200<br />

200<br />

0<br />

0<br />

–200<br />

1 10<br />

–200<br />

100 1 10 100<br />

400<br />

200<br />

0<br />

–200<br />

1<br />

Real<br />

–Imaginary<br />

Normalized impedance<br />

0.029° 400<br />

0.018°<br />

200<br />

–200<br />

10 100 1<br />

Frequency (Hz)<br />

0<br />

10 100<br />

Frequency (Hz)<br />

Fig. 4.10 Normalized surface impedance predicted for the<br />

four-layer structure, speed of sound in air = 329 m/s (corresponding<br />

<strong>to</strong> an air temperature of −4 ◦ C) for grazing angles<br />

between 0.018 ◦ and 5.7 ◦<br />

code known as the fast field program for air–ground<br />

systems (FFLAGS) that models sound propagation in<br />

a system of fluid layers and porous elastic layers [4.79].<br />

This numerical theory (FFLAGS) may be used also<br />

<strong>to</strong> predict the ground impedance at low frequencies.<br />

In Fig. 4.9, the predictions for the surface impedance<br />

at a grazing angle of 0.018 ◦ are shown as a function of<br />

frequency for the layered porous and elastic system described<br />

by Table 4.1 and compared with those for a rigid<br />

porous ground with the same surface flow resistivity and<br />

porosity.<br />

The influence of ground elasticity is <strong>to</strong> reduce the<br />

magnitude of the impedance considerably below 50 Hz.<br />

Potentially this is very significant for predictions of lowfrequency<br />

noise, e.g., blast noise, at long range.<br />

Figure 4.10 shows that the surface impedance of this<br />

four-layer poro-elastic system varies between grazing<br />

angles of 5.7 ◦ and 0.57 ◦ but remains more or less constant<br />

for smaller grazing angles. The predictions show<br />

two resonances. The lowest-frequency resonance is the<br />

most angle dependent. The peak in the real part changes<br />

from 2 Hz at 5.7 ◦ <strong>to</strong> 8 Hz at 0.057 ◦ . On the other hand<br />

the higher-frequency resonance peak near 25 Hz remains<br />

relatively unchanged with range.<br />

The peak at the lower frequency may be associated<br />

with the predicted coincidence between the Rayleigh<br />

wave speed in the ground and the speed of sound in<br />

air (Fig. 4.11). Compared with the near pressure dou-<br />

Propagation velocity (m/s)<br />

360<br />

320<br />

280<br />

240<br />

200<br />

160<br />

120<br />

0.3 0.5 0.7 1 2 4 6 8 10 20<br />

Frequency (Hz)<br />

Fig. 4.11 Rayleigh-wave dispersion curve predicted for the<br />

system described by Table 4.1<br />

Sound level (dB re free field)<br />

8<br />

6<br />

4<br />

2<br />

FFLAGS<br />

prediction<br />

Prediction<br />

using Zeff<br />

0<br />

1 10 100<br />

Frequency (Hz)<br />

Fig. 4.12 Excess attenuation spectra predicted for source<br />

height 2 m, receiver height 0.1 m and horizontal range of<br />

6.3 km by FFLAGS (assumed speed of sound in air of<br />

329 m/s) and by classical theory using impedance calculated<br />

for 0.018 ◦ grazing angle<br />

bling predicted by classical ground impedance models,<br />

the predicted reduction of ground impedance at low frequencies<br />

above layered elastic ground can be interpreted

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