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nor the outer layer solely responsible for turbulent energy<br />

production: but rather ascribing this process to their<br />

interaction.<br />

Grass (1971) reported on extensive experiments using smooth and<br />

rough walls (u*k/u=0.0, 20.7, 84.7; k is the roughness height)<br />

and found that ejections and inrushes remained unchanged. Offen<br />

& Kline (1974) proposed a kinematic description <strong>of</strong> the link<br />

between the inner and outer flow, hypothesising that pairing <strong>of</strong><br />

vortices associated with two to four bursts led to bulges in the<br />

superlayer. Kovasznay et al (1970) were the first to notice the<br />

saddle point on the upstream facing (rear) side <strong>of</strong> the outer flow<br />

bulges at a height <strong>of</strong> y/6 = 0.8 when seen in a reference frame<br />

convected with the flow.<br />

Antonia & Bisset (1990), used a spanwise array <strong>of</strong> hot wires to<br />

detect bursts and sweeps, and found that the streamwise length<br />

<strong>of</strong> a sweep was about twice that <strong>of</strong> a burst, with a value <strong>of</strong> about<br />

960 wall units at y*=15. The spanwise extent <strong>of</strong> a sweep was<br />

about 2<strong>5%</strong> larger than that <strong>of</strong> a burst.<br />

Both the length and width <strong>of</strong> sweeps and bursts were found to<br />

increase with distance from the wall and contours <strong>of</strong> with<br />

9/3x and d/dz showing the presence <strong>of</strong> a three dimensional<br />

shear layer associated with the end <strong>of</strong> the burst phase and<br />

marking the probable interface between a burst and a sweep. They<br />

also found that the largest values <strong>of</strong> instantaneous du/dz were<br />

comparable with those <strong>of</strong> the mean velocity gradient at the wall.<br />

Al-4

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