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18-Env-B2 Water Resources · December 2018

Question 2 of 6: Trapezoidal Channel — Normal and Critical Depth

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 2: Trapezoidal Channel — Normal and Critical Depth (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 source exam gives the discharge, bottom width, and side slope but does not state the channel’s longitudinal slope S; no slope value appears anywhere on it. Normal depth cannot be found from Manning’s equation without one. Per the exam’s own Note 1 (“if doubt exists…submit a clear statement of any assumptions made”), this solution assumes S = 0.001 (the same mild municipal grade explicitly given for the sewer in Question 4) and n = 0.013 for the stated concrete lining (troweled-finish concrete, Chow Table 5-6). The critical-depth answer in part (b) does not depend on either assumption.

Given. A trapezoidal, concrete-lined channel carrying a steady discharge, with the bottom width and side slope shown below (slope and roughness as assumed above).

Given data
QuantitySymbolValue
DischargeQ15 m³/s
Bottom widthb4.5 m
Side slope (H:V)m1.5
Manning roughness (assumed, concrete)n0.013
Longitudinal slope (assumed)S0.001

Find. (a) the normal depth yn; (b) the critical depth yc.

b (bottom width = 4.5 m) y 1 m 1.5:1 (H:V) water surface
Trapezoidal channel cross-section: bottom width b, depth y, side slope m (horizontal run per unit vertical rise).

Approach. Solve Manning’s equation iteratively for the uniform (normal) flow depth using the assumed slope and roughness, then locate the critical depth independently from the Froude-number-unity condition, which needs neither.

  1. Set up the trapezoidal geometry and Manning’s equation. For depth y: area, wetted perimeter, and hydraulic radius are $$A(y) = (b + m\,y)\,y, \qquad P(y) = b + 2y\sqrt{1+m^{2}}, \qquad R(y) = A(y)/P(y)$$ and uniform flow satisfies $Q = \dfrac{1}{n}A\,R^{2/3}S^{1/2}$.
  2. Solve for normal depth by iteration. Substituting b = 4.5 m, m = 1.5, n = 0.013, S = 0.001 and searching for the y that gives Q = 15 m³/s converges to $$A_n = 7.04\ \text{m}^2, \quad P_n = 8.59\ \text{m}, \quad R_n = 0.819\ \text{m}, \quad V_n = Q/A_n = 2.13\ \text{m/s}$$ $$y_n = \boxed{1.14\ \text{m}}$$
  3. Locate the critical depth from Fr = 1. Critical flow in a non-rectangular section occurs where $Q^{2}T/(gA^{3}) = 1$, with top width $T(y) = b + 2m\,y$. Solving this (independent of n and S) for the same Q, b, m gives $$A_c = 5.51\ \text{m}^2, \quad T_c = 7.30\ \text{m}, \quad V_c = Q/A_c = 2.72\ \text{m/s}$$ $$y_c = \boxed{0.934\ \text{m}}$$ Substituting back confirms $V_c/\sqrt{gA_c/T_c} = 1.00$.
  4. Compare the two depths. Since yn (1.14 m) exceeds yc (0.934 m), the assumed mild slope produces subcritical normal flow, which is the expected regime for a gently-graded, concrete-lined municipal channel.
Final Results
QuantityValue
Normal depth, yn (assumed S, n)1.14 m
Velocity at normal depth, Vn2.13 m/s
Critical depth, yc0.934 m
Velocity at critical depth, Vc2.72 m/s
Flow regime at normal depthSubcritical (yn > yc)