Bull Creek Watershed has a reservoir with storage relationship
S = AH,
where A is the area (300 ac) and H is the depth or head of the reservoir in feet.
For simplicity, the area is assumed to be constant with depth. The outflow is governed by the equation
Q = 56.25H3/2,
where Q is in cfs. Route the storm hydrograph represented in the following table through the reservoir, using the fourth-order Runge-Kutta method.
The governing equation is
The fourth-order R-K equation will be used as shown in Equations 1 and 2. The assumption is made that H0 = 0 ft and Qout(H0) = 0 cfs. Values of Qin are interpolated as necessary, and values of Qout are found from the equation Q = 56.25H3/2.
Time (hr) | Inflow (cfs) |
12 | 40 |
24 | 35 |
36 | 37 |
48 | 125 |
60 | 340 |
72 | 575 |
84 | 722 |
96 | 740 |
108 | 673 |
120 | 456 |
132 | 250 |
144 | 140 |
156 | 10 |
Equation 1
Equation 2
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