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LES of a bi-periodic turbulent flow with effusion 19<br />

SUCTION WALL<br />

y<br />

z<br />

x<br />

Figure 12. Time-averaged solution from Run C over a cutting plane located in the suction si<strong>de</strong><br />

at 0.5 d below the plate. The thick black/white ellipses correspond to the projection of the aperture<br />

inl<strong>et</strong>. (a): Contours and isolines of time-averaged streamwise velocity. (b): Contours and<br />

isolines of time-averaged normal velocity. (c): Contours and isolines of time-averaged spanwise<br />

velocity. (d): Contours of Q criterion. Isolines of time-averaged streamwise velocity as in (a). A<br />

schematic in the centre of the figure shows the direction of rotation of the vortices; the dotted<br />

line shows the location of the cutting plane y = −2.5 d displayed in this figure.<br />

This criterion, based on the second invariant of the velocity gradient tensor, is used to<br />

locate vortical structures: when the Q criterion is positive, the rotation rate is superior<br />

to the strain rate. In figure 12(d), positive values of the Q criterion are observed downstream<br />

of the hole. Two counter-rotating streamwise vortices are created at the lateral<br />

edges of the hole: their distance to the suction wall is approximately 0.5 d. A schematic<br />

in the middle of figure 12 shows the direction of rotation of the vortices. Downstream<br />

of the perforation, the spanwise spacing b<strong>et</strong>ween the vortices increases and they slightly<br />

move away from the suction wall. This vortical structure has already been reported both<br />

experimentally and numerically in MacManus & Eaton (2000), where their formation<br />

process is d<strong>et</strong>ailed. Figures 12(a,d) also show that the streamwise vortices <strong>de</strong>limitate the<br />

low streamwise velocity zones (shown by isolines).<br />

The flow near the perforated plate on the suction si<strong>de</strong> proves to be highly threedimensional,<br />

with streamwise vortices appearing downstream of the perforation. This<br />

organisation is then very different from an i<strong>de</strong>alised concept of a uniform suction.

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