- Asked 2/27
- 2074 Asoj · 12 marks
Slope-area discharge, 1300 m reach
Short answer
With fall 0.4 m over 1300 m, geometric mean conveyance K_m=342,113, initial estimate 6001 m³/s. Iterative correction for velocity heads (no eddy loss) yields discharge 5754.8 m³/s.
Calculate the flood discharge of a stream by the slope area method given the following data:
Upstream flow area = 3500 m Upstream wetted perimeter = 650 m Upstream velocity head coefficient = 1.17 Downstream flow area = 3250 m Downstream wetted perimeter = 621 m Downstream velocity head coefficient = 1.21 Falling difference = 0.4 m Reach length = 1300 m Manning's coefficient n = 0.03
Given: m, m, ; m, m, ; fall m, m, . No eddy-loss coefficient is given, so is assumed.
Method: Manning's equation gives conveyance and . The friction slope is found from the energy equation between the two sections, so the discharge is found by trial.
Step 1: Conveyance
Step 2: First trial (no velocity head)
Step 3: Correct for velocity head and eddy loss
With : .
| Trial | assumed | |||||||
|---|---|---|---|---|---|---|---|---|
| 1 | 6001.064 | 1.7146 | 1.8465 | 0.17531 | 0.21027 | 0.00000 | 0.36504 | 5732.829 |
| 2 | 5732.829 | 1.6380 | 1.7639 | 0.15999 | 0.19189 | 0.00000 | 0.36810 | 5756.770 |
| 7 | 5754.850 | 1.6442 | 1.7707 | 0.16122 | 0.19337 | 0.00000 | 0.36785 | 5754.850 |
The trials converge to and shown in the last row.
Answer: Discharge .
(If a contraction loss of were included, would be about 5732 m/s, a change of 0.4 %.)
✓ Answer checked by Claude Sonnet 5.5
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