- 2067 Mangsir (old course) · 8 marks
Slope-area discharge, 10 km reach, 104.77 m
Short answer
Conveyances K₁=7163.5, K₂=9902.5, Kₘ=8424.4; starting with fall 0.27 m over 10 km, then iterating with velocity head and expansion loss (ke=0.3) gives discharge Q ≈ 44.2 m³/s.
Calculate the discharge of a stream having high water surface elevations noted at two sections A and B, 10 km apart. These elevations and other salient hydraulic properties are given below.
| Section | Water surface elevation (m) | Area of x-section (m) | Hydraulic radius (m) |
|---|---|---|---|
| A | 104.77 | 73.293 | 2.733 |
| B | 104.500 | 93.375 | 3.089 |
The eddy loss coefficient is 0.3 for gradual expansion, 0.1 for gradual contraction and Manning's roughness is 0.02.
Given: m, m, m, m, , km, fall m. Velocity-head coefficients are taken as 1. Section B has the larger area, so the reach expands and . The wetted perimeter is found from ( m, m).
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 | 43.764 | 0.5971 | 0.4687 | 0.01817 | 0.01120 | 0.00209 | 0.27488 | 44.158 |
| 2 | 44.158 | 0.6025 | 0.4729 | 0.01850 | 0.01140 | 0.00213 | 0.27497 | 44.165 |
| 3 | 44.165 | 0.6026 | 0.4730 | 0.01851 | 0.01140 | 0.00213 | 0.27497 | 44.165 |
The trials converge to and shown in the last row.
Answer: Discharge .
✓ Answer checked by Claude Sonnet 5.5
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