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18-Env-A2 Hydrology and Municipal Hydraulics Engineering · December 2013

Question 1 of 7: Conceptual Runoff Models, Pipe Flow in a Concrete Sewer and Elevated Reservoirs

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

Notes on this paper

National Exams — December 2013 — 04-Env-A2 / Hydrology and Municipal Hydraulics Engineering. 3 hours duration; closed book with a candidate-prepared 8½×11 in double-sided aid sheet; Casio or Sharp approved calculator only. Any five questions constitute a complete paper (first five answers marked, 20 marks each, 100 marks total); all seven are solved below for completeness.

Reference texts. Davis & Cornwell, Introduction to Environmental Engineering (6th ed.) — hydrology, stormwater management and water-demand chapters; Metcalf & Eddy, Wastewater Engineering: Treatment and Resource Recovery (5th ed.) — sanitary sewer hydraulics, Manning/Harmon design formulas; MWH’s Water Treatment: Principles and Design (3rd ed.) — distribution systems, pipe-network analysis and pump selection; Chow, Open-Channel Hydraulics — Manning's n tables and specific-energy theory; Chow, Maidment & Mays, Applied Hydrology — flood-frequency analysis; CCME water quality guidelines — cold-water fishery thermal protection.

Problem 1: Conceptual Runoff Models, Pipe Flow in a Concrete Sewer and Elevated Reservoirs (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.

(i) Conceptual Runoff Models in Hydraulic Structure Design

A conceptual model of runoff represents a watershed as a small number of lumped, physically-motivated storage/routing elements whose parameters are calibrated to observed rainfall-runoff behaviour, rather than solving the full physics from first principles. Two common engineering-design examples: (1) the unit hydrograph method (e.g., SCS dimensionless unit hydrograph), which converts a design storm hyetograph directly into an inflow hydrograph used to size a culvert, detention pond outlet structure or spillway — the designer needs the peak flow and its timing, not a full physically distributed simulation; and (2) the SCS Curve Number (CN) method, a lumped conceptual loss model that converts rainfall depth to runoff depth from a single calibrated parameter (land use, soil group, antecedent moisture), routinely used to size storm sewers, culverts and detention basins across a whole municipality where a fully physically-based model would be impractical to calibrate site-by-site.

(ii) Concrete Sewer Pipe: Velocity, Reynolds Number and Friction Loss

Given.

Given data
QuantitySymbolValue
Pipe length$L$500 m
Pipe diameter$d$250 mm = 0.250 m
Full flow rate$Q$100 L/s = 0.100 m³/s
Material—concrete ($\varepsilon\approx0.3$ mm, smooth new concrete)
L = 500 m, d = 250 mm Q = 100 L/s
Concrete sewer pipe schematic — length $L$, diameter $d$, full-flow discharge $Q$.

Find. (a) $V$ in m/s, (b) $Re$ and flow regime, (c) head loss $H_f$.

Approach. Get $V$ from continuity ($V=Q/A$); get $Re$ from $Re=Vd/\nu$ to classify the flow; get the Darcy friction factor $f$ from the Swamee–Jain explicit correlation and apply Darcy–Weisbach for $H_f$.

Check: water temperature is not stated; a standard design value of 20°C ($\nu\approx1.0\times10^{-6}$ m²/s) is assumed. Concrete pipe roughness is not stated either; $\varepsilon=0.3$ mm (smooth, new concrete — the low end of the typical 0.3–3.0 mm range) is used, giving a conservative (lower-bound) friction loss; older/rougher concrete would give a somewhat larger $H_f$.
  1. Average velocity (continuity). $$A=\frac{\pi d^2}{4}=\frac{\pi(0.250)^2}{4}=0.04909\ \text{m}^2,\qquad V=\frac{Q}{A}=\frac{0.100}{0.04909}=\boxed{2.04\ \text{m/s}}.$$
  2. Reynolds number. $$Re=\frac{Vd}{\nu}=\frac{2.037\times0.250}{1.0\times10^{-6}}=\boxed{5.09\times10^{5}}\ \Rightarrow\ Re\gg4000,\ \textbf{turbulent flow}.$$
  3. Friction factor (Swamee–Jain). $$f=\frac{0.25}{\left[\log_{10}\!\left(\dfrac{\varepsilon}{3.7d}+\dfrac{5.74}{Re^{0.9}}\right)\right]^2}=\frac{0.25}{\left[\log_{10}(3.243\times10^{-4}+4.19\times10^{-5})\right]^2}=\boxed{0.0212}.$$
  4. Head loss (Darcy–Weisbach). $$H_f=f\frac{L}{d}\frac{V^2}{2g}=0.0212\times\frac{500}{0.250}\times\frac{(2.037)^2}{2\times9.81}=\boxed{8.96\ \text{m}}\ \text{over the 500 m run}.$$
QuantityValue
Full-flow area, $A$0.0491 m²
Average velocity, $V$2.04 m/s
Reynolds number, $Re$5.09×10&sup5; — turbulent
Friction factor, $f$0.0212
Friction head loss, $H_f$8.96 m over 500 m

(iii) Functions of Elevated Water Reservoirs

Three functions of an elevated (or standpipe/water-tower) reservoir that reduce the need for continuous pumping: (1) peak-demand shaving — the tower fills during low-demand hours (overnight) using steadily-running, efficiently-sized pumps, then gravity-discharges during the daily peak, so the pump station is sized to the average/near-average demand rather than the much larger instantaneous peak; (2) fire-flow and emergency storage — the elevated volume supplies the large, short-duration fire flow (or covers a pump/power outage) without requiring standby pumps to start and ramp up instantaneously, and without oversizing the everyday pump station just to cover a rare event; and (3) system pressure stabilization — because the water surface elevation directly sets the hydraulic grade line for the surrounding pressure zone, the tower damps out the pressure transients that would otherwise occur every time a pump starts, stops or a large demand (fire flow, water-main break) suddenly changes, reducing the number of pump starts/stops (and associated wear/energy cost) needed to hold pressure within the distribution system's target range.

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