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18-Env-B2 Water Resources · December 2018

Question 3 of 6: Sluice Gate and Hydraulic Jump

Nivaar worked solution (AI-drafted; not reviewed by a licensed engineer)

Notes on this paper

National Exams — December 2018 — 18-Env-B2 / Water Resources. 3 hours duration; open-book exam (any non-communicating calculator permitted). Six questions are printed; the first five as they appear in the answer book constitute a complete paper and are marked, each worth 20 marks. All six are solved below for completeness.

Reference texts. Chow, Open-Channel Hydraulics; Metcalf & Eddy, Wastewater Engineering: Treatment and Resource Recovery (5th ed.); Linsley, Kohler & Paulhus, Hydrology for Engineers; Davis & Cornwell, Introduction to Environmental Engineering (6th ed.); Freeze & Cherry, Groundwater; Fisheries Act, Canadian Environmental Protection Act, 1999; Ontario Water Resources Act and Clean Water Act, 2006 (used here as a representative province); CCME, Canada-Wide Strategy for the Management of Municipal Wastewater Effluent.

Question 3: Sluice Gate and Hydraulic Jump (20 marks)

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.

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The channel width is not given anywhere in the source. The solution below is therefore carried per unit width of channel, using the unit discharge q (m²/s); the part (b) energy-loss rate is reported as power per metre of channel width (W/m), which is the quantity that is actually determined by the given data.

Given. Reservoir (headwater) depth upstream of the gate y0 = 0.90 m (negligible approach velocity); tailwater depth downstream of the jump y2 = 0.388 m; rectangular channel; no head loss through the gate; the jump forms immediately after the vena contracta, so its depth y1 equals the gate-opening depth.

Find. (a) the vena-contracta depth y1; (b) the rate of energy dissipation through the jump, per unit channel width.

headgate y0 y1 hydraulic jump y2
Reservoir (y0) → headgate → vena contracta (y1, supercritical) → hydraulic jump → tailwater (y2).

Approach. Conserve specific energy across the gate (reservoir to vena contracta, no losses) and conserve momentum across the jump (vena contracta to tailwater); the two relations share the unknowns y1 and the unit discharge q and are solved simultaneously.

  1. Energy equation, reservoir to vena contracta. With negligible approach velocity in the reservoir and no head loss through the gate, $$y_0 = y_1 + \dfrac{q^{2}}{2g\,y_1^{2}}$$
  2. Momentum (sequent-depth) equation across the jump. For a rectangular channel, $$y_2 = \dfrac{y_1}{2}\left(\sqrt{1+8\,\mathrm{Fr}_1^{2}}-1\right), \qquad \mathrm{Fr}_1 = \dfrac{q}{\sqrt{g}\,y_1^{1.5}}$$
  3. Solve the two equations simultaneously. Substituting y0 = 0.90 m and y2 = 0.388 m and solving numerically for the physical (shallow, supercritical) root gives $$q = 0.204\ \text{m}^2/\text{s}, \qquad V_1 = q/y_1 = 4.08\ \text{m/s}, \qquad \mathrm{Fr}_1 = 5.83$$ $$y_1 = \boxed{0.0500\ \text{m}\ (50\ \text{mm})}$$ Fr1 ≫ 1 confirms the approach flow really is supercritical, as required for a jump to form downstream.
  4. Specific energy before and after the jump. With V2 = q/y2 = 0.526 m/s, $$E_1 = y_1 + \dfrac{V_1^{2}}{2g} = 0.900\ \text{m}, \qquad E_2 = y_2 + \dfrac{V_2^{2}}{2g} = 0.402\ \text{m}$$ (E1 reproduces y0 exactly, confirming energy conservation through the gate). The head lost in the jump is $\Delta E = E_1-E_2 = 0.498\ \text{m}$.
  5. Rate of energy dissipation. Power dissipated per unit width is $P' = \gamma\,q\,\Delta E$, with $\gamma = 9.81\ \text{kN/m}^3$: $$P' = \boxed{997\ \text{W/m}\ (\approx 1.00\ \text{kW per metre of channel width})}$$
Final Results
QuantityValue
Vena-contracta depth, y10.0500 m
Unit discharge, q0.204 m²/s
Approach Froude number, Fr15.83
Specific energy loss, ΔE0.498 m
Power dissipated per unit width997 W/m (≈ 1.00 kW/m)