INGENIA

HYD-05

Bélanger hydraulic jump

Sequent depth y2/y1 = ½ (−1 + √(1+8 Fr₁²)).

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Rapidly varied flowBélanger 1828USBR

Governing equation

y2y1=12(−1+1+8Fr12), Fr1=V1gy1\dfrac{y_2}{y_1}=\dfrac12\left(-1+\sqrt{1+8\mathrm{Fr}_1^2}\right),\ \mathrm{Fr}_1=\dfrac{V_1}{\sqrt{gy_1}}

V1∈[0.5,15]V_1 \in \left[0.5, 15\right]

where

y_1
Upstream depth (m)
V_1
Upstream velocity (m/s)
\mathrm{Fr}_1
Upstream Froude (—)
y_2
Sequent depth (m)

The figure, part by part

Each numbered marker wears the color of its card. Hover a card to light the marker. Tap a marker to jump to that card. The slider walks a red point along the curve; Animate drawing traces it like a pen.

HYD-05 · pipe
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①

Governing law — red

y2y1=12(−1+1+8Fr12), Fr1=V1gy1\dfrac{y_2}{y_1}=\dfrac12\left(-1+\sqrt{1+8\mathrm{Fr}_1^2}\right),\ \mathrm{Fr}_1=\dfrac{V_1}{\sqrt{gy_1}}

V1∈[0.5,15]V_1 \in \left[0.5, 15\right]

V1=0.5V_1 = 0.5Fr1=0.046\mathrm{Fr}_1 = 0.046

②

Domain of the variable — blue

V_1_{\min} = 0.5,\quad V_1_{\max} = 15

V1∈[0.5,15]V_1 \in \left[0.5, 15\right]

V1=0.5V_1 = 0.5V1=0.5V_1 = 0.5

③

Response curve — green

y2y1=12(−1+1+8Fr12), Fr1=V1gy1\dfrac{y_2}{y_1}=\dfrac12\left(-1+\sqrt{1+8\mathrm{Fr}_1^2}\right),\ \mathrm{Fr}_1=\dfrac{V_1}{\sqrt{gy_1}}

V1∈[0.5,15]V_1 \in \left[0.5, 15\right]

V1=0.5V_1 = 0.5Fr1=0.046\mathrm{Fr}_1 = 0.046

④

Rate of change — amber

dFr1dV1\frac{\mathrm{d}\mathrm{Fr}_1}{\mathrm{d}V_1}

V1∈[0.5,15]V_1 \in \left[0.5, 15\right]

V1=0.591V_1 = 0.591Fr1′=0.184\mathrm{Fr}_1^{\prime} = 0.184

Lecture brief

Historical brief

Open-channel and pipe flow were written by Chezy, Manning, Darcy and Weisbach in the nineteenth century, then Bakhmeteff and Bélanger on the hydraulic jump. The sheets compute conveyance, head loss and gradually varied profiles. This sheet (HYD-05 — Bélanger hydraulic jump) is the form associated with Bélanger 1828 · USBR. Working symbols: y1y_1, V1V_1 →\rightarrow Fr1\mathrm{Fr}_1, y2y_2. Momentum and continuity across a free jump on a horizontal floor close on Bélanger's sequent-depth relation.

Purpose

Purpose: compute Fr1\mathrm{Fr}_1, y2y_2 from y1y_1, V1V_1 in Hydraulics via y2y1=12(−1+1+8Fr12), Fr1=V1gy1\dfrac{y_2}{y_1}=\dfrac12\left(-1+\sqrt{1+8\mathrm{Fr}_1^2}\right),\ \mathrm{Fr}_1=\dfrac{V_1}{\sqrt{gy_1}} Sequent depth y2/y1 = ½ (−1 + √(1+8 Fr₁²)). Use it when a real hydraulics question must be answered in SI before a code check.

Live realistic example

In symbols

Live case. Given y1=0.400 my_1 = 0.400\,\mathrm{m}, V1=6.000 m/sV_1 = 6.000\,\mathrm{m/s}, the governing relation y2y1=12(−1+1+8Fr12), Fr1=V1gy1\dfrac{y_2}{y_1}=\dfrac12\left(-1+\sqrt{1+8\mathrm{Fr}_1^2}\right),\ \mathrm{Fr}_1=\dfrac{V_1}{\sqrt{gy_1}} yields Fr1=3.029 —\mathrm{Fr}_1 = 3.029\,\mathrm{—}, y2=1.525 my_2 = 1.525\,\mathrm{m}. Rectangular frictionless floor, no slope, aerated jump. Move a slider: the numbers are this situation, not a canned story.

Calculator

Inputs

Outputs

  • Upstream Froude \mathrm{Fr}_13.029 —
  • Sequent depth y_21.525 m
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HYD-05 · pipe
00:0 / 00:08

Narration of this film

Rectangular frictionless floor, no slope, aerated jump.

Momentum and continuity across a free jump on a horizontal floor close on Bélanger's sequent-depth relation.

Reading speed

Watch on YouTube