Sound radiation in turbulent channel flows
Sound radiation in turbulent channel flows
Lighthill’s acoustic analogy is formulated for turbulent channel flow with pressure as the acoustic variable, and integrated over the channel width to produce a two-dimensional inhomogeneous wave equation. The equivalent sources consist of a dipole distribution related to the sum of the viscous shear stresses on the two walls, together with monopole and quadrupole distributions related to the unsteady turbulent dissipation and Reynolds stresses respectively. Using a rigid-boundary Green function, an expression is found for the power spectrum of the far-field pressure radiated per unit channel area. Direct numerical simulations (DNS) of turbulent plane Poiseuille and Couette flow have been performed in large computational domains in order to obtain good resolution of the low-wavenumber source behaviour. Analysis of the DNS databases for all sound radiation sources shows that their wavenumber–frequency spectra have non-zero limits at low wavenumber. The sound power per unit channel area radiated by the dipole distribution is proportional to Mach number squared, while the monopole and quadrupole contributions are proportional to the fourth power of Mach number. Below a particular Mach number determined by the frequency and radiation direction, the dipole radiation due to the wall shear stress dominates the far field. The quadrupole takes over at Mach numbers above about 0.1, while the monopole is always the smallest term. The resultant acoustic field at any point in the channel consists of a statistically diffuse assembly of plane waves, with spectrum limited by damping to a value that is independent of Mach number in the low-M limit.
269-302
Hu, Zhiwei
dd985844-1e6b-44ba-9e1d-fa57c6c88d65
Morfey, Christopher L.
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Sandham, Neil D.
0024d8cd-c788-4811-a470-57934fbdcf97
2003
Hu, Zhiwei
dd985844-1e6b-44ba-9e1d-fa57c6c88d65
Morfey, Christopher L.
d5f9a8d0-7d8a-4915-a522-bf49dee111f2
Sandham, Neil D.
0024d8cd-c788-4811-a470-57934fbdcf97
Hu, Zhiwei, Morfey, Christopher L. and Sandham, Neil D.
(2003)
Sound radiation in turbulent channel flows.
Journal of Fluid Mechanics, 475, .
(doi:10.1017/S002211200200277X).
Abstract
Lighthill’s acoustic analogy is formulated for turbulent channel flow with pressure as the acoustic variable, and integrated over the channel width to produce a two-dimensional inhomogeneous wave equation. The equivalent sources consist of a dipole distribution related to the sum of the viscous shear stresses on the two walls, together with monopole and quadrupole distributions related to the unsteady turbulent dissipation and Reynolds stresses respectively. Using a rigid-boundary Green function, an expression is found for the power spectrum of the far-field pressure radiated per unit channel area. Direct numerical simulations (DNS) of turbulent plane Poiseuille and Couette flow have been performed in large computational domains in order to obtain good resolution of the low-wavenumber source behaviour. Analysis of the DNS databases for all sound radiation sources shows that their wavenumber–frequency spectra have non-zero limits at low wavenumber. The sound power per unit channel area radiated by the dipole distribution is proportional to Mach number squared, while the monopole and quadrupole contributions are proportional to the fourth power of Mach number. Below a particular Mach number determined by the frequency and radiation direction, the dipole radiation due to the wall shear stress dominates the far field. The quadrupole takes over at Mach numbers above about 0.1, while the monopole is always the smallest term. The resultant acoustic field at any point in the channel consists of a statistically diffuse assembly of plane waves, with spectrum limited by damping to a value that is independent of Mach number in the low-M limit.
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Published date: 2003
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Local EPrints ID: 10376
URI: http://eprints.soton.ac.uk/id/eprint/10376
ISSN: 0022-1120
PURE UUID: d4a1f30b-7796-44e0-a079-f73da87eb5da
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Date deposited: 03 Feb 2006
Last modified: 16 Mar 2024 03:03
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Author:
Christopher L. Morfey
Author:
Neil D. Sandham
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