(25%) A weir is located at the downstream end of a wide rectangular channel of bottom slope
So = 0.0035 and dimensionless Chezy friction factor f = 0.0035.
The unit-width discharge in the wide rectangular channel is q = 0.4 m3/s/m.
Immediately upstream of the weir, the flow is subcritical, with depth 1.5 m.
- Calculate the Froude number of the normal flow in the upstream channel.
- Calculate the normal flow depth in the upstream channel.
- Calculate the normal flow velocity in the upstream channel.
- Calculate the length of the C1 water-surface profile.
(25%) A hydraulically wide
supercritical flow channel with So = 0.025 flows into a critical flow channel
of So = 0.004. The dimensionless Chezy friction factor f is the same is both channels.
The unit-width discharge is 2.2 m2/s.
Find the length of the C3 water surface profile in the critical flow channel.
(25%) Please answer the following questions in a brief statement.
- What is the difference between the brute force method and Newton's iteration to solve the normal depth equation? Be specific.
- In gradually varied flow in a hydraulically wide channel,
the flow depth gradient Sy is a function of three
parameters. What are these?
- What is the typical range of variation of the angle of friction φ in granular materials (sand and gravel)?
- When the water is clear of sediment, does it tend to erode the boundary more, or less? Why? Be specific.
- What, in your opinion, should be done to manage the Oroville reservoir
safely, in view of the failure of the spillways?
(25%) State eight (8) differences between the direct step and standard step methods of steady gradually varied flow computation.
Formulas you may need:
So = f F2
F2 = v2/ (gy)
q = vy
yc = (q2/g)1/3
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