CE530- OPEN CHANNEL HYDRAULICS
SPRING 2007
SECOND MIDTERM
MONDAY, APRIL 9, 2007, 0730-0845
Name: _________________________________ Red ID No. _________________________ Grade: ____________
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Instructions: Closed book, closed notes. Use engineering paper.
When you are finished, staple your work in sequence (1 to 4),
and return this sheet with your work.
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(20%) What is the discharge in a rectangular channel of bottom width b = 5 m, bed slope So = 0.0025, Manning's
n= 0.015, and flow depth y = 0.8 m?
- (30%) A long channel of rectangular cross section has a bed slope So = 0.0045 and (dimensionless Chezy) friction factor f = 0.0045.
The unit-width discharge in the channel is 1 m3/s/m.
A weir (located at the downstream end of the channel) produces a water-surface profile immediately upstream of it.
Immediately upstream of the weir, the flow depth is 2.4 m.
- Calculate the normal-depth Froude number in the upstream channel.
- Calculate the normal flow depth in the upstream channel.
- Calculate the normal flow velocity in the upstream channel.
- What type of water-surface profile prevails immediately usptream of the weir?
- What is the length of the water-surface profile, measured from the weir to the location where the channel is at normal depth?.
- (30%) Please answer the following questions in a brief statement.
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What is the minimum value of Manning's n? Where does it apply?
What is the maximum value of Manning's n? Where does it apply?
- Why is the permissible tractive force method preferred over the permissible velocity method in the design of open channels over erodible materials?
- What is the typical range of the angle of repose of noncohesive materials?
- Why does a canal with clear water have a lower permissible unit tractive force than a canal with high content of fine sediment?
- In gradually varied flow in a hydraulically wide channel, the flow depth gradient Sy is a function of three (geometric and physical)
parameters.
What are these?
- What are the five characteristic (preestablished) values to which the flow depth gradient Sy tends in WSP computations?
To which ones is Sy asymptotic in the upstream or downstream end?
- (20%) Do a tabular comparison between the direct-step and standard-step methods of steady gradually varied flow computation.
State at least eight differences.
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