18-Env-A2 Hydrology and Municipal Hydraulics Engineering · May 2015
Nivaar worked solution (AI-drafted; not reviewed by a licensed engineer)
National Exams — May 2015 — 04-Env-A2 / Hydrology and Municipal Hydraulics Engineering. 3 hours duration; closed book with a candidate-prepared 8.5×11 in double-sided aid sheet; Casio or Sharp approved calculator only. Any five questions constitute a complete paper (only the first five answers as they appear in the work book are marked); all seven are solved below for completeness. Each question ("Problem") is worth 20 marks, with sub-part weights shown in brackets.
Reference texts. Chow, Open-Channel Hydraulics; Linsley, Kohler & Paulhus, Hydrology for Engineers (3rd ed.); Walski et al., Advanced Water Distribution Modeling and Management; Davis & Cornwell, Introduction to Environmental Engineering (6th ed.); Metcalf & Eddy, Wastewater Engineering: Treatment and Resource Recovery (5th ed.).
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 4-node network (A, B, C, D) with 5 pipes forming two loops (A-B-C-A and B-D-C-B), inflow 1000 L/s at A, and outflows of 100 L/s at B, 300 L/s at C and 600 L/s at D:
| Pipe | Length, $L$ (m) | Diameter, $d$ (mm) |
|---|---|---|
| AB | 400 | 250 |
| BC | 600 | 200 |
| CD | 400 | 300 |
| AC | 600 | 200 |
| BD | 400 | 300 |
Find. The flow in each of the five pipes.
Approach. Start from an initial flow distribution that satisfies continuity at every node, then apply Hardy-Cross loop-balancing corrections $\Delta Q = -\dfrac{\sum KQ|Q|^{n-1}}{n\sum K|Q|^{n-1}}$ (with $n=1.852$) to Loop 1 (A→B→C→A) and Loop 2 (B→D→C→B, sharing pipe BC) until both loops' signed head-loss sums vanish.
| Pipe | Flow, $Q$ |
|---|---|
| AB | 672.3 L/s (A→B) |
| AC | 327.8 L/s (A→C) |
| BC | 117.4 L/s (B→C) |
| BD | 454.9 L/s (B→D) |
| CD | 145.1 L/s (C→D) |
Static head $H_s$ is the elevation difference alone between the supply (suction) water surface and the discharge water surface — the head a pump must overcome even at zero flow, entirely independent of pipe size, roughness or flow rate: $H_s = z_{discharge} - z_{suction}$. Friction head $H_f$ is the additional head consumed by fluid friction along the pipe as flow actually moves through it, and it grows with the square of velocity (Darcy–Weisbach $H_f = f(L/d)(V^2/2g)$, or equivalently $H_f = KQ^2$ for a fixed pipe): it is zero at zero flow and rises steeply as $Q$ increases. The total dynamic head the pump must supply at any operating flow is $H = H_s + H_f(Q) = H_s + KQ^2$, which is exactly the system curve plotted in part (iii).
(a) Pump efficiency is the ratio of useful hydraulic power delivered to the fluid to the shaft (brake) power supplied to the pump: $$\eta_{pump} = \frac{P_{hydraulic}}{P_{shaft}} \times 100\%,$$ where $P_{shaft}$ is read from the motor/driver curve (or measured by a torque-and-speed test) at the operating point. Manufacturer pump curves typically plot $\eta$ directly against $Q$ alongside the head curve, so $P_{shaft}=P_{hydraulic}/\eta$ can be read off without a separate torque measurement.
(b) Hydraulic (water) power is the rate of useful work done raising and moving the fluid against the total dynamic head at the operating point: $$P_{hydraulic} = \rho g Q H = \gamma Q H,$$ with $\rho$ the fluid density (kg/m³), $g$ gravitational acceleration, $Q$ the discharge (m³/s) and $H$ the total head (m) delivered by the pump at that $Q$ — i.e. $Q$ and $H$ are read at the operating point identified in part (iii), not at shutoff or free discharge.