18-Env-A2 Hydrology and Municipal Hydraulics Engineering · May 2016
Nivaar worked solution (AI-drafted; not reviewed by a licensed engineer)
National Exams — May 2016 — 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 and water-distribution chapters; Metcalf & Eddy, Wastewater Engineering: Treatment and Resource Recovery (5th ed.) — sanitary sewer collection systems; MWH’s Water Treatment: Principles and Design (3rd ed.) — pipe-network analysis and pump selection; Chow, Open-Channel Hydraulics — Manning's n tables, specific-energy and sediment-transport theory; Linsley, Hydrology for Engineers — hydrologic cycle, hydrograph analysis and IDF curves; Walski, Advanced Water Distribution Modeling and Management — Hardy-Cross network solutions and pump affinity laws.
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.
Three important abstractions subtract from gross rainfall to leave the "rainfall excess" that actually becomes direct runoff and shapes the hydrograph: interception — rainfall caught on vegetation canopy that evaporates without ever reaching the ground; depression storage — water ponding in small surface depressions that must fill before overland flow can begin; and infiltration — water entering the soil profile, governed by soil type, antecedent moisture and land cover, typically the largest of the three abstractions in most storm events. Because these abstractions are satisfied first, a hydrograph's rising limb only begins once their combined capacity is exceeded, which is why a dry, permeable watershed produces a delayed, low peak while a saturated or impervious one produces an almost immediate, high peak for the same storm.
| Factor | Description | Effect on peak flow | Effect on time to peak |
|---|---|---|---|
| Watershed shape & drainage-area size | An elongated watershed spreads tributary flow paths over a wide range of travel times; a compact, fan-shaped watershed concentrates them. | Fan-shaped → higher, sharper peak (flows arrive together); elongated → lower, more attenuated peak. | Fan-shaped → shorter time to peak; elongated → longer time to peak. |
| Slope & imperviousness (land cover) | Steeper slopes and greater impervious cover increase overland-flow velocity and reduce infiltration losses. | Steeper/more impervious → higher peak flow (more rainfall excess, faster delivery). | Steeper/more impervious → shorter time to peak (faster travel time). |
Given.
| Quantity | Symbol | Value |
|---|---|---|
| Original impeller diameter | $D_1$ | 100 mm |
| New impeller diameter | $D_2$ | 140 mm |
| Speed | $N$ | constant (same casing/motor) |
Find. The new BEP capacity $Q_2$, head $H_2$, brake power $P_2$, expected efficiency $\eta_2$, and the % capacity improvement.
Approach. At constant speed, geometrically similar impeller trims within the same casing obey the pump affinity laws: $Q\propto D$, $H\propto D^2$, $P\propto D^3$, with efficiency approximately unchanged for a modest trim ratio.
| Quantity | Value |
|---|---|
| New optimum capacity, $Q_2$ | 0.01512 m³/s (15.1 L/s) |
| New head, $H_2$ | 24.5 m |
| New brake power, $P_2$ | 5.51 kW |
| Expected efficiency, $\eta_2$ | ≈66% (unchanged from $D_1$) |
| % capacity improvement | 40.0% |