18-Env-A2 Hydrology and Municipal Hydraulics Engineering · December 2017
Question 4 of 7
Nivaar worked solution (AI-drafted; not reviewed by a licensed engineer)
Notes on this paper
National Exams — December 2017 — 04-Env-A2 Hydrology and Municipal Hydraulics Engineering (3 hours, closed book with an 8½×11 candidate aid-sheet). Instructions state any five (5) of the seven problems constitute a complete paper (100 marks); all seven are solved in full below for completeness.
Reference texts: Linsley, Kohler & Paulhus, Hydrology for Engineers; Chow, Open-Channel Hydraulics; Walski et al., Advanced Water Distribution Modeling and Management; Davis & Cornwell, Introduction to Environmental Engineering.
Check: the exam gives no friction factor, Manning's n or roughness for the corrugated steel pipe. A standard absolute roughness for corrugated steel pipe, $\varepsilon\approx45\ \text{mm}$ (from standard hydraulics roughness tables), is assumed here to obtain the Darcy–Weisbach friction factor.
Find. (a) $Q$ in m³/min; (b) $Re$ and flow regime; (c) head loss $H_f$.
Approach. Continuity for $Q$; $Re=VD/\nu$ for the regime; Colebrook–White (fully rough, high-$Re$ regime) for the friction factor, then Darcy–Weisbach for $H_f$.
Reynolds number and regime.
$$Re = \frac{VD}{\nu} = \frac{3\times0.6}{1.00\times10^{-6}} = \boxed{1.8\times10^{6}}$$
$Re\gg4000$, so the flow is unambiguously turbulent; at this Reynolds number and relative roughness the flow is in the fully-rough regime (friction factor essentially independent of $Re$).
Friction factor and head loss. Relative roughness $\varepsilon/D=45/600=0.075$. Solving Colebrook–White,
$$\frac{1}{\sqrt f}=-2\log_{10}\!\left(\frac{\varepsilon/D}{3.7}+\frac{2.51}{Re\sqrt f}\right)$$
at $Re=1.8\times10^6$ gives $f\approx0.087$ (fully-rough asymptote). Applying Darcy–Weisbach,
$$H_f = f\,\frac{L}{D}\,\frac{V^2}{2g} = 0.087\times\frac{1200}{0.6}\times\frac{3^2}{2(9.81)} = \boxed{80\ \text{m}}$$
Quantity
Value
$Q$
50.9 m³/min
$Re$
$1.8\times10^6$ (turbulent, fully rough)
$f$ (Colebrook–White)
0.087
$H_f$
≈ 80 m
(ii) Grass-lined trapezoidal channel — discharge and Reynolds number (7 marks)
Given.
Quantity
Value
Normal depth, $y$
4 m
Base width, $b$
5 m
Side slope
$z=3$ (3 horizontal : 1 vertical)
Manning's $n$ (grass-lined, assumed)
0.030
Bed slope, $S_0$
3%
Check: the exam labels the side slope "H:V of 1:3", which read literally (H=1:V=3) is an unworkably steep, near-vertical batter for an earthen grass channel. The conventional grass-channel batter this phrasing is taken to mean is 3 horizontal : 1 vertical ($z=3$, i.e. "1 (vertical) in 3 (horizontal)"), the standard mowable slope range (3:1–4:1 H:V) for grass linings — used below. Manning's $n=0.030$ (typical "grass, average stand" value) is assumed since the exam does not supply one.
Find. (a) Discharge $Q$; (b) Reynolds number and flow regime.
Approach. Trapezoidal geometry for $A$, $P$, $R$; Manning's equation for uniform-flow velocity and discharge; hydraulic-radius-based Reynolds number, $Re=4VR/\nu$, for the regime check.
Reynolds number.
$$Re = \frac{4VR}{\nu} = \frac{4\times9.90\times2.24}{1.00\times10^{-6}} = \boxed{8.9\times10^{7}}$$
$Re\gg2000$, so the flow is unambiguously turbulent.
Check: the resulting velocity (9.9 m/s) is a direct consequence of the printed 3% bed slope combined with a 4 m flow depth in Manning's equation, but it is far beyond the accepted non-erosive velocity range for a grass lining (typically ≤ 1.5–2 m/s); a real channel with this slope and discharge would need a rigid or riprap lining, not grass. The calculation is carried through with the data exactly as given.
Quantity
Value
$A$
68 m²
$R$
2.24 m
$V$
9.90 m/s
$Q$
673 m³/s
$Re$
$8.9\times10^7$ (turbulent)
(iii) Specific energy over a bed rise (7 marks)
Given. Same trapezoidal channel ($b=5$ m, $z=3$); $Q=15\ \text{m}^3/\text{s}$; upstream normal depth $Y_1=3$ m; bed rise $\Delta z=0.6$ m; negligible friction loss between the two sections.
Fig. 3 — Specific-energy profile over the bed rise: the same trapezoidal section carries the flow both upstream and over the crest.
Find. Depth of flow $Y_2$ over the crest of the bed rise.
Approach. Specific energy is conserved (no friction loss, no change in total head other than the bed-elevation rise): $E_1=E_2+\Delta z$. Before solving for $Y_2$, verify the crossing is not choked by checking the available energy above the upstream value against the minimum specific energy (critical depth) for this discharge.
Check for choking — critical depth and minimum specific energy. Solving $\dfrac{Q^2T}{gA^3}=1$ for the trapezoidal section ($T=b+2zY$) gives $Y_c=0.82\ \text{m}$, $E_{min}=1.13\ \text{m}$. The maximum bed rise the flow can climb without choking is
$$\Delta z_{max} = E_1-E_{min} = 3.007-1.126 = 1.88\ \text{m}$$
Since $\Delta z = 0.6\ \text{m} < \Delta z_{max}=1.88\ \text{m}$, the crossing is not choked and a subcritical $Y_2$ exists.