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Computational Mechanics Research and Support for Aerodynamics ...

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conditions from Example 1 defined in the new HEC-18 update was adopted here with the following<br />

given parameters:<br />

Upstream channel width <strong>and</strong> bridge opening width (W)= 40 ft (12.2 m)<br />

Total discharge (Q) = 2800 ft 3 /s (79.3 m 3 /s)<br />

Upstream channel discharge (Q 1 ) = 2000 ft 3 /s (56.6 m 3 /s)<br />

Upstream floodplain discharge = 800 ft 3 /s (22.7 m 3 /s)<br />

Upstream channel flow depth (h u )= 10.0 ft (3.0 m)<br />

Bridge opening height (h b ) = 8.0 ft (2.4 m)<br />

Deck thickness (T) = 3 ft (0.91 m)<br />

Bed material D 50 = 15 mm (V c = 6.0 ft/s, 1.8 m/s, V c is the critical velocity <strong>for</strong> the sediment size)<br />

Upstream channel velocity (V=Q 1 /(W hu )) = 2000/(40 x 10) = 5.0 ft/s (1.5 m/s)<br />

Figure 2.4 presents Equations 2.2 <strong>and</strong> 2.3 <strong>for</strong> several different upstream velocities <strong>and</strong> other quantities<br />

defined as above. It was noted that the initial fit allows <strong>for</strong> separation zone thickness significantly<br />

greater than zero <strong>for</strong> the cases where the water level was just slightly above the bottom line of the<br />

bridge superstructure (<br />

. Although Equations 2.2 <strong>and</strong> 2.3 fit to the experimental scour<br />

data well, creation of a significant separation zone when the water is at a level that just touches the<br />

superstructure is counterintuitive. Also there was a discontinuity introduced between the two regions<br />

described by the curves – be<strong>for</strong>e overtopping <strong>and</strong> after overtopping.<br />

Figure 2.4 Initial fit based on Equations 2.2 <strong>and</strong> 2.3<br />

TRACC/TFHRC Y2Q2 Page 14

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