CE530- OPEN CHANNEL HYDRAULICS
SPRING 2005
SECOND MIDTERM
MONDAY, NOVEMBER 14, 2005, 1600-1715
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 3),
and return this sheet with your work.
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(20%) What is the discharge in a rectangular channel of bottom width b = 10 m, bed slope So = 0.001, Manning's
n= 0.025, and flow depth y = 1 m?
- (20%) A 10-ft high weir is located at the downstream end of a wide rectangular channel of bottom slope
So = 0.0045 and Darcy-Weisbach friction factor fD = 0.036.
The unit-width discharge in the wide rectangular channel is 5.68 cfs/ft.
- Calculate the upstream Froude number.
- Calculate the upstream flow depth.
- What is the type of water-surface profile immediately upstream of the weir?
- Calculate the length of the water-surface profile.
- (60%) Please answer the following questions in a brief statement.
- What are rolls waves? When and where do they typically form?
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What is the minimum value of Manning's n that can be achieved in practice? What type of surface would that be?
In the absence of more information, what is the value of Manning's n generally adopted for small upstream natural streams?
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How does the composite value of Manning's n change from very low flow (Example: a river drought) to very high flow (the Probable Maximum Flood)
in a typical natural stream?
- Why is Newton's law of viscosity applicable to laminar free-surface (overland) flow?
- 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 hydraulic parameters.
What are these?
- How many types of water surface profiles (WSP) are there in gradually varied flow (GVF)?
Which GVF WSP's are completely horizontal?
- What are the five characteristic values to which the flow depth gradient Sy tends in WSP computations?
To which ones is Sy asymptotic in the upstream or downstream end?
- Which one is the most common type of WSP? When does it occur?
- Do a tabular comparison between the direct-step and standard-step methods of steady gradually varied flow computation.
State at least seven differences.
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