CE530- OPEN CHANNEL HYDRAULICS
FALL 2019
SECOND MIDTERM
NOVEMBER 13, 2019, 1600-1650

Name: ______________________________ Red ID No. _______________________ Grade: ________


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.

  1. (30%) 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 = 0.5 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 (See w.s. profile below).

  2. (30%) A hydraulically wide supercritical flow channel with So = 0.03 flows into a critical flow channel of So = 0.003. The dimensionless Chezy friction factor f is the same is both channels (f = 0.003). The unit-width discharge is q = 2.5 m2/s. Find the length of the C3 water surface profile in the critical flow channel (See w.s. profile below). [Hint: Calculate the upstream Froude number and the upstream flow depth, then calculate the downstream flow depth; then calculate the length of the profile by geometry.]


  3. (20%) Please answer the following questions in a brief statement.

    • Why is it necessary to design a channel to operate with a minimum Froude number?

    • In gradually varied flow in a hydraulically wide channel, the flow depth gradient Sy is a function of three parameters. What are these?

    • What are the five asymptotic values to which the water surface tend to in gradually varied flow?

    • How many types of water surface profiles are they? Which ones are horizontal?

  4. (20%) 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

So = Sc F2

F2 = v2/ (gy)

q = vy

yc = (q2/g)1/3