16-Civ-A5 Hydraulic Engineering · December 2017
Nivaar worked solution (AI-drafted; not reviewed by a licensed engineer)
National Exams — 16-Civ-A5 Hydraulic Engineering — December 2017. 3 hours, closed book (one 8.5×11 aid sheet permitted). Six questions of equal value; candidates answer any five. All six are solved here as a study resource. Unless stated, local losses and velocity head are neglected; water ρ = 1000 kg/m³, ν = 1.31×10−6 m²/s.
Reference texts: D. A. Chin, Water-Resources Engineering (3rd ed.), Ch. 2 (flow in closed conduits) & Ch. 7 (water-distribution systems); A. Osman Akan, Open Channel Hydraulics; M. Hanif Chaudhry, Open-Channel Flow (2nd ed.), Ch. 3 (hydraulic jump); Chadwick, Morfett & Borthwick, Hydraulics in Civil and Environmental Engineering.
Question text not reproduced: the examination questions are © Engineers and Geoscientists BC. Open the official past paper (linked at the top of this page) to read the question, then follow the worked solution below.
Given. A rectangular channel carrying a fixed discharge with a known shallow supercritical approach depth.
| Channel width B | 6.5 m |
| Discharge Q / unit discharge q | 20 m³/s / 3.077 m²/s |
| Upstream (supercritical) depth $z_1$ | 0.2 m |
Find. (a) the momentum (specific-force) equation of the jump; (b) the conjugate downstream depth $z_2$; (c) why momentum, not energy, governs.
(a) Momentum equation. Apply the momentum principle to the control volume spanning the jump in a horizontal, rectangular channel, neglecting boundary friction over the short length. The net hydrostatic pressure force equals the change in momentum flux. Per unit width (with $q=Q/B$): $$\underbrace{\tfrac{1}{2}\gamma z_1^2 + \dfrac{\gamma q^2}{g\,z_1}}_{\text{section 1}} = \underbrace{\tfrac{1}{2}\gamma z_2^2 + \dfrac{\gamma q^2}{g\,z_2}}_{\text{section 2}},\qquad\text{i.e. the specific force } M = \dfrac{q^2}{g\,z}+\dfrac{z^2}{2}\ \text{is conserved.}$$ Dividing through and rearranging yields the Bélanger conjugate-depth relation $$\dfrac{z_2}{z_1} = \tfrac{1}{2}\left(\sqrt{1+8\,\mathrm{Fr}_1^{\,2}}-1\right).$$
(b) Downstream depth. A short calculation gives the approach Froude number and then $z_2$:
(c) Why momentum, not energy. A hydraulic jump is a highly turbulent, roller-dominated transition that dissipates a large but a priori unknown amount of mechanical energy (here 9.2 m of head, converted to turbulence and heat). The energy equation cannot be applied across the jump because the loss term is exactly the unknown we lack. The momentum equation, by contrast, involves only the external forces on the control volume — the hydrostatic pressure forces and (negligible) boundary friction — and the momentum flux, none of which require knowledge of the internal dissipation. It therefore closes with the given depths and discharge alone, which is why the conjugate-depth relation is derived from momentum.
| Quantity | Value |
|---|---|
| Unit discharge q | 3.077 m²/s |
| $V_1$ / $\mathrm{Fr}_1$ | 15.38 m/s / 10.98 (supercritical) |
| Downstream depth $z_2$ | 3.01 m |
| $V_2$ / $\mathrm{Fr}_2$ | 1.02 m/s / 0.19 (subcritical) |
| Energy dissipated $\Delta E$ | 9.20 m |