- 2078 Kartik · 8 marks
Slope-area discharge, 10 km reach
Short answer
Slope-area method with Manning’s conveyance and trial correction for velocity head and expansion eddy loss (ke=0.3) gives discharge ≈ 44.2 m³/s.
The high flow water surface elevations of a stream at two sections 10 km apart are 306.920 m and 306.650 m. The cross-sectional area and wetted perimeters are as follows:
| Section | Area (m) | Wetted perimeter (m) |
|---|---|---|
| A | 73.3 | 26.80 |
| B | 93.4 | 30.23 |
Assume n = 0.02. The eddy loss coefficient is 0.30 for gradual expansion and 0.10 for gradual contraction. Estimate the discharge in the stream. Section A is upstream of B.
Given: m, m, m, m, , km, fall m. Velocity-head coefficients are taken as . The area increases downstream, so the reach is an expansion and .
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 | 43.786 | 0.5974 | 0.4688 | 0.01819 | 0.01120 | 0.00210 | 0.27489 | 44.181 |
| 2 | 44.181 | 0.6027 | 0.4730 | 0.01852 | 0.01140 | 0.00213 | 0.27498 | 44.188 |
| 3 | 44.188 | 0.6028 | 0.4731 | 0.01852 | 0.01141 | 0.00213 | 0.27498 | 44.188 |
The trials converge to and shown in the last row.
Answer: Discharge .
✓ Answer checked by Claude Sonnet 5.5
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