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Roshko (1974), observed that a turbulent mixing layer also<br />

contains large-scale spanwise vortex motions which persist in the<br />

presence <strong>of</strong> smaller scale turbulence. Winant & Browand (1974)<br />

went further in reporting that vortex pairing was the main<br />

mechanism behind shear layer growth at low Reynolds numbers.<br />

Brown and Roshko found the same process to be equally important<br />

at high Reynolds number. Dimotakis & Brown (1976) found this<br />

behaviour to be a dominant feature even at Reynolds numbers <strong>of</strong><br />

10 7 . As detailed above, Hernan & Jiminez (1982) found that fluid<br />

is engulfed during pairing and is entrained by the vortices<br />

between pairing, typically with most <strong>of</strong> the growth occurring by<br />

entrainment rather than engulfment. A comprehensive study <strong>of</strong> the<br />

entrainment phenomenon by Panides & Chevray (1990), identified<br />

key elements <strong>of</strong> the mechanisms from simultaneous flow<br />

visualisation and one point two-component laser doppler<br />

anemometry. Ho & Huerre (1984) indicated that not only pairing<br />

interactions may occur, but also three-fold interactions or<br />

higher order events, especially for locations close to the<br />

initial instability.<br />

b) Spreading angle and three dimensional instability- Muller<br />

& Gyr (1986) used an analysis by Jiminez (1980) to calculate the<br />

spreading angle <strong>of</strong> the shear layer. Jiminez found (figure 9 ;<br />

from Muller & Gyr, 1986) that the ratio <strong>of</strong> the area P^ <strong>of</strong><br />

vortices <strong>of</strong> neighbouring generations was about 4 giving a ratio<br />

<strong>of</strong> 2 for the linear scale since<br />

=2 x 1.75 x 1.17 = 4.1<br />

pairing entrainment engulfment<br />

1-9

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