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6<br />
The dispersal, decay and instability of multiple trailing-line<br />
vortices<br />
Peter W. Duck ∗<br />
The importance of the dispersal, decay and breakdown of trailing-line vortices is<br />
now a key aerodynamic issue. The classical flow that has spawned much research<br />
activity over many years has been the (viscous) solution of Batchelor 1 , describing<br />
the downstream evolution of a solitary vortex generated behind one side of a wing.<br />
Various aspects of the stability of this flow have been presented over the years (see<br />
for example 2 3 4 ). The dominant mode of instability is generally of short wavelength<br />
(and is therefore inviscid), and as a consequence growth rates are quite large (which<br />
can lead to breakdown, which is advantageous from a practical point of view).<br />
In this paper the approach adopted involves (i) the determination of the downstream<br />
evolution of a multiple vortex system and (ii) an investigation of the shortwavelength<br />
(inviscid) stability of this developing flow. The theory is mathematically<br />
rational, being based on the assumption of large Reynolds numbers.<br />
Consider first the downstream developing baseflow; assuming a uniform flow far<br />
outside the trailing vortex system, it is then possible to reduce the Navier-Stokes<br />
equations to the following nondimensional form:<br />
UX + vy + wz =0, UUX + vUy + wUz = Uyy + Uzz,<br />
UvX + vvy + wvz = vyy + vzz − py, UwX + vwy + wwz = wyy + wzz − pz.<br />
Here (U, v, w) are the velocity components in the (X, y, z) directions respectively,<br />
and p is pressure; the scaling in the downstream direction X is long, and includes a<br />
Reynolds number factor (implying a slow downstream flow evolution, compared to the<br />
vertical y and crossflow z directions). Correspondingly the velocity components in the<br />
y and z directions are an order smaller in Reynolds number than the X component.<br />
The system is parabolic in nature (the streamwise diffusion terms have been eliminated),<br />
and can therefore be solved in a ‘marching’ fashion, downstream from some<br />
prescribed initial conditions. A variety of such conditions have been implemented,<br />
including two counter-rotating vortices and various systems involving four vortices.<br />
When considering the stability of the base states (as described above), it is possible<br />
to perform a 2D (inviscid) stability analysis, which reduces the (in)stability problem to<br />
the following partial eigenvalue problem (in which either the streamwise wavenumber<br />
α is specified and the wavespeed c is treated as an eigenvalue, or vice versa):<br />
∂2 ˜p<br />
∂y2 + ∂2 ˜p 2 ∂U ∂ ˜p 2 ∂U ∂ ˜p<br />
− −<br />
∂z2 U − c ∂y ∂y U − c ∂z ∂z − α2 ˜p =0,<br />
where ˜p is the pressure eigenfunction. Using this type of approach, it is feasible to<br />
rapidly and efficiently investigate different vortex configurations, in order to optimise<br />
trailing-vortex characteristics with regard to dispersal, decay and breakdown.<br />
∗ School of Mathematics, University of Manchester, England<br />
1 Batchelor, J. Fluid Mech. 20, 645 (1964).<br />
2 Lessen et al. J. Fluid Mech. 63, 743 (1974)<br />
3 Lessen &Paillet J. Fluid Mech. 65, 769 (1974)<br />
4 Duck &Foster, ZAMP 31, 524 (1980)