- (20%) A hydraulically wide channel is operating at Froude number F = 0.3. The unit-width discharge is q = 2.0 m2s-1.
What are two Langrange absolute celerities?
- (20%) You are observing the rising flood stage of a major river.
At your observation point, at a certain time the discharge is
495 m3 s-1, and the stage is rising at the rate of 5 mm hr-1.
At a point located 18 km upstream of your observation point, the stage is rising at the rate of 7 mm hr-1.
The surface width of the river in the study reach is 125 m. What is your estimate of the present discharge
at the upstream end of the reach?
- (40%) Please answer each question in one clear and concise paragraph:
- Compare in tabular form the kinematic, diffusion, dynamic, and inertia-pressure waves in terms of their celerity and attenuation
properties.
- What is the difference between the Muskingum and Muskingum-Cunge methods of flood routing?
- What are three ways in which the Seddon formula can be expressed? Which one did Seddon present in the year 1900?
- What flood waves are more likely to be dynamic? Why?
- What is the difference between sediment production and sediment yield? Why is is there a difference? What is this difference a function of?
- What is the difference between sediment transport and sediment routing?
- Which is the only sediment transport method that considers all modes of sediment transport, by size fractions, measured and unmeasured?
- What point or aspect of this class most caught your attention and interest?
- (20%) Write a 200-word essay on HEC-RAS. Separate explicitly into four paragraphs (5 points each):
(1) history, (2) objectives, (3) equations and solution, and (4) data requirements.
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