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22-Agric-A4 Fluid Flow · December 2017

Question 3 of 4: Hydraulic Jump and Bump in a Wide Channel

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

Notes on this paper

04-Agric-A4, Fluid Flow — National Exams, December 2017. Open-book, 3-hour exam; four questions of equal value, all requiring calculation.

Reference texts. White, Fluid Mechanics (pipe friction/Colebrook, cavitation, open-channel hydraulic jumps and bumps, pumps & the energy equation) — the standard undergraduate text for this subject.

Problem 3: Hydraulic Jump and Bump in a Wide Channel (25 points)

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 wide (per-unit-width) horizontal channel carries supercritical flow (1) that undergoes a hydraulic jump to subcritical flow (2), then rises over a smooth 10-cm bump, passing through the critical depth exactly at the crest (3), before the bed drops back to its original level downstream (4). No losses occur except at the jump.

QuantityValue
Bump height, $h$0.10 m
Depth at crest, $y_3$ (critical)0.30 m

Find. (a) $V_4$; (b) $y_4$; (c) $V_1$; (d) $y_1$.

1 Jump 2 3 4 Bump: h = 10 cm
Figure 3 — Supercritical flow (1) jumps to subcritical (2), rises over the bump becoming critical at the crest (3), then accelerates to supercritical (4) as the bed returns to its original level.

Approach. Critical flow at the crest fixes the unit discharge $q$ and specific energy $E_3=1.5y_3$. Since sections 2 and 4 sit at the same (original) bed elevation, energy conservation over the loss-free bump gives $E_2=E_4=E_3+h$; this cubic in $y$ has one subcritical root ($y_2$) and one supercritical root ($y_4$). The hydraulic jump relation then links $y_1$ (supercritical, same $q$) to $y_2$.

  1. Unit discharge and specific energy at the crest. Critical flow means $V_3=\sqrt{gy_3}$, so $$q = V_3 y_3 = \sqrt{(9.81)(0.30)}\,(0.30) = \boxed{q\approx0.5147\ \text{m}^2/\text{s}},\qquad E_3=1.5y_3=\boxed{E_3=0.450\ \text{m}}.$$
  2. Specific energy at 2 and 4 (bed level 0, crest at $+h$). With no losses between 2, 3 and 4, the total head is constant, so $E_2=E_4=E_3+h=0.450+0.10=\boxed{0.550\ \text{m}}$.
  3. (a)–(b) Solve $y+q^2/(2gy^2)=0.550$ for its two positive roots. This cubic ($y^3-0.550y^2+0.01350=0$) has a subcritical root $y_2\approx0.4949$ m and a supercritical root $$\boxed{y_4\approx0.1950\ \text{m}} \;\Rightarrow\; V_4=\frac{q}{y_4}=\frac{0.5147}{0.1950}=\boxed{V_4\approx2.639\ \text{m/s}}.$$ (the flow chokes at the critical crest and continues accelerating on the downhill side, exactly as flow accelerates past a sonic throat.)
  4. Subcritical depth just upstream of the bump. The other root, $y_2\approx0.4949$ m, gives $V_2=q/y_2=1.040\ \text{m/s}$ ($Fr_2=0.47<1$, confirming subcritical, consistent with sitting downstream of the jump).
  5. (c)–(d) Hydraulic jump from 1 to 2. The jump relation $y_2/y_1=\tfrac12\!\left(-1+\sqrt{1+8Fr_1^2}\right)$ with $Fr_1^2=q^2/(gy_1^3)$ and the known $y_2=0.4949$ m solves (bisection) to $$\boxed{y_1\approx0.1653\ \text{m}} \;\Rightarrow\; V_1=\frac{q}{y_1}=\frac{0.5147}{0.1653}=\boxed{V_1\approx3.114\ \text{m/s}}\ \ (Fr_1\approx2.45).$$ The upstream flow is indeed supercritical, consistent with a hydraulic jump occurring there.
QuantityResult
Unit discharge, $q$0.515 m²/s
(a) $V_4$2.64 m/s
(b) $y_4$0.195 m
(c) $V_1$3.11 m/s
(d) $y_1$0.165 m
(intermediate) $y_2$, $V_2$0.495 m, 1.04 m/s