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Oscillations, Waves, and Interactions - GWDG

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84 D. Ronneberger et al.<br />

(flow velocity) / (speed of sound)<br />

0.3<br />

0.2<br />

0.1<br />

0.3<br />

0.2<br />

0.1<br />

0.3<br />

0.2<br />

a<br />

b<br />

c<br />

C<br />

A 1<br />

0.1<br />

0 1 2 3 4 5<br />

frequency [kHz]<br />

A 2<br />

Figure 10. Power spectral density <strong>and</strong> coherence of the pressure in the backmost cavity<br />

of the unmodified resonator section plotted as a function of the frequency <strong>and</strong> of the flow<br />

velocity. (a) power spectral density (normalized to the background spectrum); (b) coherence<br />

between two locations the azimuthal coordinates of which differ by ∆ϕ = 180 o ; (c) like (b)<br />

with ∆ϕ = 120 o .<br />

2.2 Higher-order modes<br />

Regarding the possible technical application of the sound-induced static pressure<br />

drop, the excitation <strong>and</strong> the effect of higher-order modes have been studied. It is anticipated<br />

that some of these propagate in the resonator section, but are evanescent in<br />

the rigid ducts so that the mostly unwelcome propagation of the amplified controlling<br />

sound is suppressed. We are particularly interested in circumferential modes which<br />

are easier to h<strong>and</strong>le than radial modes. Then the amplitudes of the flow velocity <strong>and</strong><br />

the pressure depend on the azimuthal coordinate ϕ according to (û, ˆv, ˆp) ∼ exp(imϕ)<br />

wherein m is the azimuthal wavenumber <strong>and</strong> |m| is the azimuthal order of the mode.<br />

Because of the evanescence of the considered modes we have to ab<strong>and</strong>on the radiated<br />

pressure fluctuations <strong>and</strong> the acoustic transmission coefficient as sources of<br />

information in this study; instead we analyze the pressure in the backmost cavity.<br />

The spectum of the pressure is more complex, <strong>and</strong> it contains more peaks than the<br />

radiated pressure spectra shown in Fig. 2; in addition the ‘background spectrum’ on<br />

top of which the peaks are observed exhibits a stronger dependency on the frequency<br />

than the radiated pressure. The background spectrum was therefore approximated<br />

A 3<br />

A 4<br />

dB<br />

110<br />

00<br />

−10 −1<br />

1.0<br />

0.5<br />

0<br />

−0.5<br />

−1.0

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