- Asked 2/27
- 2076 Chaitra · 8 marks
Slope-area flood discharge, 7 km reach
Short answer
Compute conveyance K1, K2, Km from Manning's n. Trial with energy equation including velocity head and eddy loss for expansion yields friction slope and discharge. Q ≈ 29.6 m³/s.
Calculate the flood discharge of a stream by the slope area method given as below:
| Upstream | Downstream |
|---|---|
| Upstream flow area = 45 m | Downstream flow area = 50 m |
| Upstream wetted perimeter = 26 m | Downstream wetted perimeter = 28 m |
| Upstream velocity head coefficient = 1.18 | Downstream velocity head coefficient = 1.23 |
Falling difference = 1.15 m, Reach length = 7 km, Manning's coefficient n = 0.03. The eddy loss coefficient of 0.3 for gradual expansion and 0.1 for gradual contraction.
Given: m, m, ; m, m, ; fall m; m; . The area increases downstream (expansion), so .
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
Here (expansion), so .
| Trial | assumed | |||||||
|---|---|---|---|---|---|---|---|---|
| 1 | 29.520 | 0.6560 | 0.5904 | 0.02588 | 0.02185 | 0.00121 | 1.15282 | 29.556 |
| 2 | 29.556 | 0.6568 | 0.5911 | 0.02595 | 0.02191 | 0.00121 | 1.15283 | 29.557 |
The trials converge to and shown in the last row.
Answer: Discharge .
✓ Answer checked by Claude Sonnet 5.5
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