Sound Transmission Through a Cascade
We consider now the scattering of an incident acoustic mode of m = —8 and n = 0 and compare that to the scattering of a vortical disturbance. We take the upwash component to be the same at the mean radius and equal to unity for both disturbances. For the vortical disturbance the upwash is constant along the radius but for the acoustic mode it changes slightly (about 10%). This upwash corresponds to an acoustic mode with a coefficient c_8,o = 1.18. In the two cases, Mo = 0.3536, Mq = 0.1, Mr = 0.1, rh/rt = 0.6667, c/rm = 0.3491
at the mean radius, Cj = 3n, and a grid of {nx x n x nr} = {161 x 21 x 21} is used. The vortical disturbance has Ur = 0.
Figure (4) compares the magnitude of the unsteady lift coefficient along the span for the two cases. The lift coefficient is much higher for the acoustic disturbance. This may be explained by the fact that the wavelength of the acoustic wave in the x-direction is much larger than that of the vortical wave. This causes phase cancellation along the blade in the case of the vortical disturbance thus reducing the lift coefficient compared to the case of upstream acoustic disturbance.
The magnitude of the upstream and downstream acoustic coefficients for the two cases are compared in Table (2). The acoustic coefficients are much higher in the case of the acoustic disturbance especially for the first acoustic mode.
Table 2. Magnitude of the upstream and downstream acoustic coefficients cmn for acoustic and vortical incident disturbances.
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This is because the incident acoustic wave is the same as the first propagating duct mode and hence has identical radial profile.
Comparing the upstream and downstream coefficients in the case of acoustic disturbance, we see that most of the acoustic energy of the incident acoustic waves has been transmitted and propagated downstream and that the part which is refected is relatively small.
2. Conclusions
Numerical results are presented to examine the effect of mean swirl on the aerodynamic and acoustic coefficients of an annular cascade. The results suggest that the swirl introduces additional nonuniformities which modify the physics of the scattering in three major ways: (i) it modifies the number of propagating acoustic modes in the duct, (ii) it changes their radial variation in the duct, and (iii) it causes significant amplitude and radial phase variation of the incident disturbances.
Acknowledgments
This research was supported by The Office of Naval Research grant No. N00014-00-1-0130 with Dr. Ki-Han Kim as program manager. H. M. Atassi would like to thank the Ohio Aerospace Institute Aeroacoustic Consortium for its support.
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