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Introduction to Acoustics

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Although the simple result of (3.319) predicts that<br />

the fraction of incident power transmitted is unity at<br />

a frequency of fc/ sin 2 θI, the presence of damping processes<br />

in the plate causes the fraction of incident power<br />

transmitted always <strong>to</strong> be less than unity. A simple way of<br />

taking this in<strong>to</strong> account makes use of a loss fac<strong>to</strong>r η (assumed<br />

<strong>to</strong> be much less than unity) for the plate, which<br />

corresponds <strong>to</strong> the fraction of s<strong>to</strong>red elastic energy that<br />

is dissipated through damping processes during one radian<br />

(a cycle period divided by 2π). Because twice the<br />

loss fac<strong>to</strong>r times the natural frequency is the time coefficient<br />

for exponential time decay of the amplitude when<br />

the system is vibrating in any natural mode, the former<br />

can be regarded as the negative of the imaginary<br />

part of a complex frequency. Then, because the natural<br />

frequency squared is always proportional <strong>to</strong> the elastic<br />

modulus, and because the loss fac<strong>to</strong>r is invariably small,<br />

the loss fac<strong>to</strong>r can be formally introduced in<strong>to</strong> the math-<br />

3.11 Spherical Waves<br />

In many circumstances of interest, applicable idealizations<br />

are waves that locally resemble waves spreading<br />

out radially from sources or from scatterers. The mathematical<br />

description of such waves has some similarities<br />

<strong>to</strong> plane waves, but important distinctions arise. The<br />

present section is concerned with a number of important<br />

situations where the appropriate coordinates are<br />

spherical coordinates.<br />

3.11.1 Spherically Symmetric Outgoing<br />

Waves<br />

For a spherically symmetric wave spreading out radially<br />

from a source in an unbounded medium, the symmetry<br />

implies that the acoustic field variables are a function of<br />

only the radial coordinate r and of time t. The Laplacian<br />

reduces then <strong>to</strong><br />

∇ 2 p = ∂2 p 2 ∂p 1 ∂<br />

+ =<br />

∂r2 r ∂r r<br />

2 (rp)<br />

∂r2 , (3.323)<br />

so the wave equation of (3.74) takes the form<br />

∂2 (rp) 1<br />

−<br />

∂r2 c2 ∂2 (rp)<br />

= 0 . (3.324)<br />

∂t2 The solution of this is<br />

f (r − ct)<br />

p(r, t) = +<br />

r<br />

g(r + ct)<br />

. (3.325)<br />

r<br />

Causality considerations (no sound before the source<br />

is turned on) lead <strong>to</strong> the conclusion that the second term<br />

Basic Linear <strong>Acoustics</strong> 3.11 Spherical Waves 65<br />

ematical model by the replacement of the real elastic<br />

modulus by the complex number (1 − iη)E. When this<br />

is done, one finds<br />

�<br />

f<br />

Zsl = ωηmpl<br />

fc<br />

� � �2 f<br />

× 1 − sin 4 �<br />

θI<br />

fc<br />

� 2<br />

sin 4 θI − iωmsl<br />

(3.321)<br />

for the slab impedance that is <strong>to</strong> be inserted in<strong>to</strong> (3.314).<br />

The extra term ordinarily has very little effect on the fraction<br />

of incident power that is transmitted except when<br />

the (normally dominant) imaginary term is close <strong>to</strong> zero.<br />

When the frequency f is fc/ sin2 θI, one finds the value<br />

of τ <strong>to</strong> be<br />

�<br />

τ = 1 + 1<br />

�−2 ωηmpl<br />

cos θI , (3.322)<br />

2 ρc<br />

rather than identically unity.<br />

x<br />

Source<br />

yL<br />

�<br />

z<br />

θ<br />

r<br />

zL<br />

v<br />

Listener<br />

Fig. 3.22 Spherical coordinates. The common situation is<br />

when the source is at the origin and the listener (sound<br />

receiver) has coordinates (r, θ, φ)<br />

on the right side of (3.325) is not an appropriate solution<br />

of the wave equation when the source is concentrated<br />

near the origin. The expression<br />

p(r, t) =<br />

f (r − ct)<br />

r<br />

xL<br />

, (3.326)<br />

y<br />

Part A 3.11

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