Hydraulic Jumps - Colorado State University Walterpierre/ce_old/classes/CIVE 401/projects... · A...

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Hydraulic Jumps CIVE 401 Project Nicolette Lind - Jessica McCallum - Maiwand M-Yaqoob

Transcript of Hydraulic Jumps - Colorado State University Walterpierre/ce_old/classes/CIVE 401/projects... · A...

Page 1: Hydraulic Jumps - Colorado State University Walterpierre/ce_old/classes/CIVE 401/projects... · A hydraulic jump will not occur when a flow goes from ... which causes a “jump”

Hydraulic Jumps

CIVE 401 Project

Nicolette Lind - Jessica McCallum - Maiwand M-Yaqoob

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What is a hydraulic jump?● A hydraulic jump is defined as a rise in the level of water in an open channel

● Can be calculated, designed and controlled by engineers

● Often designed to occur over dam spillways

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When/why do they occur?● A hydraulic jump occurs when a liquid at a high velocity discharges into a zone

that has a lower velocity

● The slowing of the liquid leads to an increase in height that changes the kinetic

energy of the liquid into potential energy

● Some of the energy is dissipated in the form of heat due to turbulence

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Theory● Raleigh (1914) calculated the change in fluid depth associated with the shock

wave from a hydraulic jump and introduced the principles of continuity and

conservation of momentum

● The continuity states that the flow rate (Q) must be equal before and after the

hydraulic jump

● The conservation of momentum helps determine the energy dissipated within the

hydraulic jump

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DiagramsExample diagrams of hydraulic jumps are shown below.

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Applicable Equations Froude Number: Fr = V/√(gL)

Where: Fr = Froude number

V = Velocity

g = gravity

L = depth of flow

Critical Flow Depth: yc = (y₁/2)(√(1+8Fr₁²)-1)

Where: yc = critical flow depth

y₁ = upstream measured depth

Fr = Froude number

Upstream Energy Level: E₁ = y₁ + (V₁²/2g)

Where: E₁ = upstream energy level

V₁ = Velocity upstream

y₁ = upstream measured depth

g = gravity

Head Loss: hL = (y₂-y₁)⁸/(4y₁y₂)

Where: hL = head loss in the hydraulic jump

y₁ = upstream measured depth

y₂ = downstream measured depth

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Importance of Froude Number● Defines subcritical flow or supercritical flow

● A froude number greater than 1 is a supercritical flow whereas a froude number

less than 1 is a subcritical flow

● In order to have a hydraulic jump the froude number needs to be greater than or

equal to 1

● A hydraulic jump occurs when the flow goes from supercritical flow (Fr > 1) to

subcritical flow (Fr < 1) or from an unstable flow to a stable flow

● A hydraulic jump will not occur when a flow goes from subcritical flow (Fr < 1) to

a supercritical flow (Fr > 1)

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Types of Jumps● Weak (Undular) Jump

○ Low energy dissipation rate

○ Smooth downstream water surface

● Oscillating Jump

○ Irregular fluctuations of flow

○ Causes turbulence downstream

● Steady Jump

○ Jump forms steadily at same location and is well balanced

○ Turbulence is confined within the jump

● Strong Jump

○ Large change in depth of the water surface

○ High energy dissipation rate

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Hydraulic Jump Classification

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Advantages ✔● Dissipates the energy of water over a spillway

● Prevents scouring on the downstream side of the dam structure

● Traps air in the water

○ Useful for removing wastes and pollution in the water

● Reverses the flow of water

○ Can be used to mix chemicals for water purification

● Maintains a high water level on the downstream side

○ Useful for irrigation purposes

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Disadvantages ✖● Downstream turbulence can cause damage and degradation of

channel banks

● May cause erosion on hydraulic surfaces

● Undesirable condition for fish passage

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Energy Dissipation● Hydraulic jumps are one of the most effective options in dissipating energy over

water structures

● Energy is dissipated in the form of heat

● Turbulent flow and secondary waves cause most of the energy dissipation

● Applying the conservation of momentum equation, the energy loss can be

calculated by:

ΔE = (y₂ - y₁)³ / (4y₁y₂)

Where:

y₁ = Flow depth at supercritical flow

y₂ = Flow depth at subcritical flow

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The diagram above illustrates a hydraulic jump and the energy loss from E1 to E2. The supercritical depth (y1) jumps to a larger depth, subcritical depth (y2), as the velocity decreases from V1 to V2.

Energy Loss Diagram

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Applications● Industrial

○ Hydraulic jumps are commonly designed by engineers to dissipate energy below dam spillways,

weirs and outlets.

● Recreational

○ Hydraulic jumps in rivers are often used for fun/sport by kayakers, canoers, and rafters.

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Well-Known Hydraulic Jumps● Hoover Dam

● Crystal Rapid in Grand Canyon

● Cache la Poudre River Spillways

● Your sink!

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Crystal RapidCrystal Rapid is one of the most feared rapids in the Colorado River. It has several

large holes with a garden of rocks beneath. The rapids were formed in 1966 when a

flash flood washed debris into the river. The large holes are great examples of

hydraulic jumps and make Crystal Rapid one of the most complex environments for

water sports enthusiasts.

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Important People● Leonardo Da Vinci first described hydraulic jumps in the 16th Century

● Giorgio Bidone published the first experimental investigations

● Henry Darcy calculated flow measurements in open channels

● Henry Bazin, a colleague of Henry Darcy, continued Darcy’s work of flow

measurements and flow over weirs

● Adhemar Barre de Saint Venant developed shallow water equations which still

hold even during hydraulic jumps

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Interesting Facts● BYU conducted research relating the number of fatalities due to submerged

hydraulic jumps in the United States

● The number of deaths recorded was 458 and the number of fatal sites was 244

● The majority of these deaths occurred in dams

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Conclusion● A hydraulic jump is defined as a rise in the level of water

● Hydraulic jumps occur when a supercritical flow (Fr > 1) encounters a submerged

object such as a dam or weir throwing the water upward and changing the flow

from a supercritical flow to a subcritical flow (Fr < 1), which causes a “jump”

● An advantage of hydraulic jumps is the ability to dissipate energy in dams,

channels, and similar structures

● A disadvantage of hydraulic jumps is the downstream turbulence which can cause

erosion and degradation of channels

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Questions?

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Referenceshttp://udel.edu/~inamdar/EGTE215/Jump_weirs.pdf

http://89.31.100.18/~iahrpapers/82799.pdf

https://www.rdb.ethz.ch/projects/project.php?proj_id=9798&z_detailed=1&z_popular=1&z_keywords=1

http://www.aboutcivil.org/hydraulic-jump-calculations-effects-applications.html

http://optimist4u.blogspot.com/2011/04/hydraulic-jump-and-its-practical.html (photo)

http://www.engineeringexceltemplates.com/blog.aspx?categoryid=5 (photo)

http://onlinecalc.sdsu.edu/onlinechannel12.php

http://www.fsl.orst.edu/geowater/FX3/help/4_Calculations/_Hydraulic_Jumps.htm

http://krcproject.groups.et.byu.net/

http://www.aboutcivil.org/hydraulic-jump-calculations-effects-applications.html

https://barr.com/projects/2331107900 (photo)

http://krcproject.groups.et.byu.net/ (photo)

http://large.stanford.edu/courses/2007/ph210/bechtol1/

http://www.usbr.gov/lc/hooverdam/history/articlesmain.html

http://grandcanyonhistory.clas.asu.edu/sites_coloradorivercorridor_crystalrapids.html