CIV E 445 - APPLIED HYDROLOGY SPRING 2003 SOLUTIONS TO HOMEWORK 12 , CHAPTER 10
Problem 12-1
The total rainfall depth is: P = 16 cm. With CN = 81, and R = 2.54 cm/in., the effective rainfall depth (i.e., runoff) (Eq. 5-9) is: Q = 8.988 cm. Assuming φ between 1 and 2 cm/h: [(2 - φ) • 1 + (5 - φ) • 1 + (4 - φ) • 1 + (3 - φ) • 1] = 8.988.
The accumulated effective rainfall depth is: 9.00 cm. The total runoff volume is: 85 km2 • 9 cm = 765 km2-cm = 7.65 hm3. The calculations are shown in the following table:
The sum of outflow hydrograph ordinates is 765 km2-cm/h. 765 km2-cm/h • 1 h = 765 km2-cm = 7.65 hm3, which is the same as the total runoff volume. ANSWER. Problem 12-2
Since Δt = 1 h, and K = 3 h: Δt /K = 1/3, and from the Table 8-1, the linear reservoir-routing coefficients are the following: (20+40+60+40+24+16) km2 • 1 cm = 200 km2-cm = 2 hm3. Since the duration of the SI unit hydrograph (1 cm of runoff) is 2 h, the rainfall intensity is 0.50 cm/h.
Problem 12-3
THANK YOU FOR RUNNING EH1000A.
THANK YOU FOR RUNNING EH1000A. PLEASE CALL AGAIN. ANSWER.
THANK YOU FOR RUNNING EH1000A.
THANK YOU FOR RUNNING EH1000A. PLEASE CALL AGAIN. ANSWER.
Problem 12-4 Using program EH 1000A, the peak outlow is 134.642 m3/s and the time-to-peak is 36 h. The computer run for this problem is provided in the following:
THANK YOU FOR RUNNING EH1000A.
THANK YOU FOR RUNNING EH1000A. PLEASE CALL AGAIN. ANSWER. |