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(20%) Route the following inflow hydrograph through a linear-reservoir.
Time (hr) | 0 | 1 | 2 | 3 | 4 | 5 | 6 | 7 | 8 | 9 | 10 |
Inflow (m3/s) | 0 | 10 | 20 | 30 | 40 | 50 | 40 | 30 | 20 | 10 | 0 |
Assume baseflow is 0 m3/s, K= 3 hr, Delta t= 1 hr.
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(20%) Given the following inflow hydrograph to a certain
stream channel reach, calculate the outflow by the Muskingum method.
Time (hr) | 0 | 1 | 2 | 3 | 4 | 5 | 6 | 7 | 8 | 9 | 10 | 11 | 12 |
Inflow (m3/s) | 10 | 20 | 40 | 80 | 120 | 150 | 120 | 60 | 50 | 40 | 30 | 20 | 10 |
Assume baseflow is 10 m3/s, K= 1 hr, X= 0.2, and Delta t= 1 hr.
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(20%) Use the Clark method to derive a 3-hr unit hydrograph
for a catchment with the following time-area diagram:
Time (hr) | 0 | | 3 | | 6 | | 9 | | 12 |
Area (km2) | | 57 | | 72 | | 39 | | 15 |
Use K= 3 hr, and Delta t= 3 hr.
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(40%) Please answer each question in one clear-and-concise paragraph:
1. In reservoir routing, when the inflow and the outflow coincide, the outflow is a maximum. Why?
2. What is the theoretical value of the discharge coefficient thorough a weir, based on critical flow? In U.S. customary units?
In SI units?
3. What is McCarthy's contribution to hydrology? Explain.
4. What is Seddon's contribution to hydrology? Explain.
5. What is Hayami's contribution to hydrology? Explain.
6. What is Cunge's contribution to hydrology? Explain.
7. What is Clark's contribution to hydrology? Explain.
8. Why does the time-area method overestimate the flood peak?
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