We propose a diagnostic technique to detect instability waves in a subsonic round jet using a phased microphone array. The detection algorithm is analogous to the beamforming technique, which is typically used with a far-field microphone array to localize noise sources. By replacing the reference solutions used in the conventional beamforming with eigenfunctions from linear stability analysis, the amplitudes of instability waves in the axisymmetric and first two azimuthal modes are inferred. Experimental measurements with particle image velocimetry and a database from direct numerical simulation are incorporated to design a conical array that is placed just outside the mixing layer near the nozzle exit. The proposed diagnostic technique is tested in experiments by checking for consistency of the radial decay, streamwise evolution and phase correlation of hydrodynamic pressure. The results demonstrate that in a statistical sense, the pressure field is consistent with instability waves evolving in the turbulent mean flow from the nozzle exit to the end of the potential core, particularly near the most amplified frequency of each azimuthal mode. We apply this technique to study the effects of jet Mach number and temperature ratio on the azimuthal mode balance and evolution of instability waves. We also compare the results from the beam-forming algorithm with the proper orthogonal decomposition and discuss some implications for jet noise.
IntroductionLarge-scale structures in turbulent jets are often qualitatively associated with Kelvin-Helmholtz instabilities of the inflectional mean-velocity profile (Crighton & Gaster 1976;Mankbadi & Liu 1981). In acoustically excited jets, pressure and velocity fluctuations have been successfully predicted using eigenfunctions obtained from linear stability analysis (Zaman & Hussain 1980;Mankbadi 1985;Tam & Morris 1985;Tanna & Ahuja 1985). While large-scale coherent structures reminiscent of instability waves have also been observed in natural jets (Brown & Roshko 1974;Michalke & Fuchs 1975;Maestrello & Fung 1979;Morris, Giridharan & Lilley 1990;Arndt, Long & Glauser 1997;Jordan et al. 2004;Hall, Pinier & Glauser 2006), it is difficult to assert whether they can be quantitatively identified with instability waves. One difficulty stems from a lack of time-resolved three-dimensional flow measurements, which are necessary for such an identification. A second and more fundamental difficulty is that turbulence in the jet consists of eddies with a range of length scales and lifetimes; thereby, it is unclear whether there is an appropriate scale-separation