Hydraulic Jump

A hydraulic Jump is a phenomenon in the science of Hydraulics , frequently observed in open channel flow. When liquid at high velocity discharges into a zone of lower velocity, a rather abrupt rise (a step or standing wave) occurs in the liquid surface. The rapidly flowing liquid expands (which in an open channel appears as an increase in elevation), converting some of the initial kinetic energy of flow into a lower kinetic energy, an increased potential energy and the remainder to irreversible losses (turbulence which ultimately coverts the energy to heat).

The phenomenon is dependent upon the initial fluid speed. If the initial fluid speed is below the Critical speed then no jump is possible. For relatively low initial flow speeds above the critical speed an undulating wave appears. As the flow speed increases further the transition grows more abrupt, and at high enough speeds the front will break and curl back upon itself. This rise can be accompanied by violent turbulence, eddying, air entrainment, and surface undulations.

Although different terminology has been used historically, three different manifestations of the phenomena are amenable to analysis by the same techniques; hence from the standpoint of the physics involved they are simply variations of one another seen from different frames of reference. Shown in figures in this article, the three different manifestations are:

The stationary hydraulic jump (rapidly flowing water transitions in a stationary jump to slowly moving water as shown in Figures 1 and 2)

The Tidal Bore (a wall or undulating wave of water moves upstream against water flowing downstream as shown in Figures 3 and 4 — if considered from a frame of reference which moves with the wave front, this is amenable to the same analysis as a stationary jump)

A Cascade (a wall or undulating wave of water moves downstream overtaking a shallower downstream flow of water as shown in Figure 5 — if considered from a frame of reference which moves with the wave front, this is amenable to the same analysis as a stationary jump)

These phenomena are addressed in an extensive literature from a number of technical viewpoints.
¹ ² ³ ⁴ ⁵ ⁶ ⁷ ⁸ ⁹ ¹⁰ ¹¹ ¹²

CLASSES OF HYDRAULIC JUMPS

Hydraulic jumps can be seen in both a stationary form and a dynamic or moving form. Practically they are subject to explanation using the same analytic approaches, and are simply variants of a single phenomena.

Moving hydraulic jump

A Tidal Bore (or bore) is a hydraulic jump which occurs when the incoming tide forms a wave (or waves) of water that travel up a river or narrow bay against the direction of the current. As is true for hydraulic jumps in general, bores take on various forms depending upon the difference in the waterlevel upstream and down, ranging from an undular wavefront to a Shock-wave-like wall of water. Figure 3 shows a tidal bore with the characteristics common to shallow upstream water - a large elevation difference is observed. Figure 4 shows a tidal bore with the characteristics common to deep upstream water - a small elevation difference is observed and the wavefront undulates. In both cases the tidal wave moves at the speed characteristic of waves in water of the depth found immediately behind the wave front.

Another variation of the moving hydraulic jump is the cascade. In the cascade (an example of which is found in Figure 5), a wall or undulating wave of water moves downstream overtaking a shallower downstream flow of water.

Stationary hydraulic jump

The stationary hydraulic jump, most frequently seen on rivers and on engineered features such as outfalls of dams and irrigation works, occurs when a flow of liquid at high velocity discharges into a zone of the river or engineered structure which can only sustain a lower velocity. When this occurs, the water slows in a rather abrupt rise (a step or standing wave) on the liquid surface. Comparing the characteristics before and after, one finds:

ANALYSIS OF THE HYDRAULIC JUMP ON A LIQUID SURFACE

north channel.]]
In spite of the apparent complexity of the flow transition, application of simple analytic tools to a two dimensional analysis were historically effective in providing analytic results which closely paralleled both field and laboratory results. Analyses have

Height of the jump - the relationship between the depths before and after the jump as a function of flow rate.

Energy loss in the jump

Location of the jump on a natural or an engineered structure

Character of the jump – undular or abrupt

Height of the jump

There are several methods of predicting the height of a hydraulic jump.This section outlines the approaches at an overview level only.

They all reach common conclusions that:

The ratio of the water depth before and after the jump depend solely on the velocity of the water entering the jump (or equivalently upon the speed of the wave over-running the moving water in a tidal wave or cascade).

The height of the jump can be many times the initial depth of the water.

; Applying Bernoulli's Principle
Assuming a two-dimensional situation with flow rate (q) as shown by figure 1 below, Bernoulli's Equation may be applied since:

The flow can be assumed to be essentially Inviscid over the short range of the jump − Viscosity (internal friction) = 0

The flow is Steady (i.e., the quantity into and out of the region of analysis are constant and equal)

The fluid (water) may be treated as incompressible − density ( $ho$ ) is essentially constant.

The form of Bernoulli's equation, for an incompressible flow in a uniform Gravitational Field , is:

:

{v_0^2 \over 2}+gh_0+{p_0 \over 
ho}={v^2 \over 2}+gh_1+{p \over 
ho}

: ''v'' = fluid Velocity along the streamline (

v_0

= initial velocity &

v_1

= final velocity)
: ''g'' = Acceleration Due To Gravity (essentially constant for this case)
: ''h'' = Height of the fluid (

h_0

= initial height and (

h_1

= final height)
: ''p'' = Pressure along the streamline (

p_0

= initial pressure)
: ''

ho

'' = Density of the fluid (essentially constant for this case)

Since the pressure at the surface is essentially constant, this reduces to

:

{v_0^2 \over 2}+gh_0={v_1^2 \over 2}+gh_1

:; Applying the Continuity Principle
In Fluid Dynamics , the Equation Of Continuity is effectively an equation of Conservation Of Mass . Considering any fixed closed surface within an incompressible moving fluid, the fluid flows into a given volume at some points and flows out at other points along the surface with no net change in mass within the space since the density is constant. Its differential form the equation of continuity is:

:

{\partial 
ho \over \partial t} + 
abla \cdot (
ho \mathbf{v}) = 0

where

ho

is density, t is time, and v is fluid velocity.

Since the density is constant and we are considering only a 2-dimensional case, this integrates to:

:

v_0 \ 	imes \ h_0 = v_1 \ 	imes \ h_1

: or

\ \  v_1  = v_0 	imes {h_0 \over h_1}

Substituting yields a Cubic Equation which can be solved using Cardano’s Method to determine that:

:

{h_1 \over h_0}   =rac{-1 \pm{\sqrt{1+{rac{8v_0^2}{gh_0}}}}}{2}

Negative answers do not yield meaningful physical solutions, so this reduces to:

:

{h_1 \over h_0}   =rac{-1 +{\sqrt{1+{rac{8v_0^2}{gh_0}}}}}{2}

on the Burdekin River in Queensland , Australia showing pronounced hydraulic jump induced by down-stream obstructions and a grade change. ]]
This produces three solutions:

When $rac{8v_0^2}{gh_0} = 8$ , then ${h \over h_0} = 1$ (i.e., there is no jump)

When $rac{8v_0^2}{gh_0} < 8$ , then ${h \over h_0} < 1$ (i.e., there is a negative jump - this can be shown as not conserving energy and is only physically possible if some force were to accelerate the fluid at that point)

When $rac{8v_0^2}{gh_0} > 8$ or $rac{v_0^2}{gh_0} > 1$ , then ${h \over h_0} > 1$ (i.e., there is a positive jump)

Since

rac{v_0^2}{gh_0} = Fr^2

, where

\ Fr

is the Dimensionless Froude Number , this is equivalent to the condition that

\ Fr > 1

. Since the

\ \sqrt{gh_0}

is the speed of a shallow Gravity Wave , the condition that

Fr > 1

is equivalent to stating that the initial velocity represents Supercritical Flow (Froude number > 1) while the final velocity represents Subcritical Flow (Froude number < 1).

;Jump height in terms of flow

The ratio of the flow height before the jump and after the jump can be simply expressed in terms of the Froude number of the incoming flow. The greater that the flow is Supercritical , the more pronounced the jump will be.

:

{h_1 \over h_0}   =rac} -1}}{2}

Practically this means that water accelerated by large drops can create stronger standing waves in the form of hydraulic jumps as it decelerates at the base of the drop. Such standing waves, when found downstream of a Weir or natural rock ledge, can form an extremely dangerous "keeper" with a water wall that "keeps" floating objects (e.g., logs, kayaks or kayakers) recirculating in the standing wave for extended periods.

; Alternate but equivalent approach applying the Impulse-Momentum Principle

A similar analysis, reaching exactly the same results, derives the same results starting with the impulse-momentum principle.

:

Net \ Impulse = Change \ in \ momentum

ho (gh_0 - gh_1)t= 
ho \left ( {v_1^2 \over 2} -  {v_0^2 \over 2} 
ight )t

{v_0^2 \over 2}+gh_0={v_1^2 \over 2}+gh_1

This equation yields the same overall relationship between jump height and Froude number.

Energy dissipation by a hydraulic jump

on the Mississippi River showing a pronounced hydraulic jump.]]

One of the most important engineering applications of the hydraulic jump is to dissipate energy in canals, dam spillways, and similar structures so that the excess kinetic energy does not damage these structures. The energy dissipation or Head Loss across a hydraulic jump is a function of the magnitude of the jump. The larger the jump as expressed in the fraction of final height to initial height, the greater the head loss.

Analytically (using the model developed by R.W. Fox & A.T. McDonald), the fractional energy loss (FEL) can be expressed in terms of the Froude number (

Fr_0

) for the incident flow as:

:

FEL = rac {(\sqrt{1+8Fr_0^2} - 3)^3} {8 {(\sqrt{1+8Fr_0^2} - 1)(\sqrt{Fr_0^2 + 2})}}

Since

Fr_0 = \sqrt{rac{v_0^2}{gh_0}}

this is equivalent to concluding the energy loss can be predicted by predicting or measuring the speed and depth of the entering water.

Location of hydraulic jump in a streambed or an engineered structure

In the design of a Dam the energy of the fast-flowing stream over a Spillway must be partially dissipated to prevent Erosion of the streambed downstream, which could ultimately lead to failure of the dam. This can be done by arranging for the formation of an hydraulic jump to dissipate energy. To limit damage, this hydraulic jump normally occurs on an Apron engineered to withstand hydraulic forces and to prevent local Cavitation and other phenomena which accelerate erosion.

In the design of a spillway and apron, the engineers select the point at which a hydraulic jump will occur. Obstructions (such as a lip) or slope changes are routinely designed into the apron to force a jump as a specific location — obstructions are unnecessary as the slope change alone is normally sufficient. To trigger the hydraulic jump without obstacles, an apron is designed such that the flat slope of the apron retards the rapidly flowing water from the face of the dam. If the apron slope is insufficient to maintain the original high velocity, a jump will occur.

spillway at the head of the Capilano River in North Vancouver, British Columbia , Canada .]]Two methods of designing an induced jump are common:

If the downstream flow is restricted by the down-stream channel such that water backs up onto the foot of the spillway, that downstream water level can be used to identify the location of the jump.

If the spillway continues to drop for some distance, but the slope changes such that it will no longer support supercritical flow, the depth in the lower subcritical flow region is sufficient to determine the location of the jump.

In both cases, the final depth of the water is determined by the downstream characteristics. The jump will occur if and only if the level of inflowing (supercritical) water level (

h_0

) satisfies the condition:

:

h_0 ={h_1\over 2} \left ( {-1 + \sqrt {1  + 8F_{rate}^2h_1/g}} 
ight )

: ''

F_{rate}

'' = fluid Flow Rate
: ''g'' = Acceleration Due To Gravity (essentially constant for this case)
: ''h'' = Height of the fluid (

h_0

= initial height while

h_1

= final downstream height)

Applying wave theory to the hydraulic jump

In Fluid Dynamics , gravity waves are waves generated in a Fluid which has as the restoring Force , Gravity . Gravity waves on an air-water interface are called surface gravity waves or Surface Wave s. Hydraulic jumps, Ocean Waves and Tsunamis can all be treated as examples of gravity waves.

The wave speed or celerity (speed of individual waves, as opposed to the speed of a group of waves) of Gravity Wave s in shallow water is given by:

$v = \sqrt{gh}\sqrt{rac{ anh{(kh)}}{kh}}$ which approaches $\sqrt{gh}$ for small h;

v = wave speed or celerity (m/s)

g = gravitational acceleration (9.81 m/s&²)

h = water depth (m)

$k = rac{2\pi}{\lambda}$ wave number where $\lambda$ is the Wavelength .

The constraints on the approximation for the speed of a gravity wave as

\sqrt{gh}

for shallow depths are:

For wavelengths close to or less than 1.7 cm the surface tension cannot be neglected so that this approximation is invalid.

For depths significantly greater than the wavelength, $\lambda$ , of the wave the speed of the wave is governed only by the wavelength following the equation $speed = {g \lambda \over {2\pi}}$ where g is the acceleration of gravity.

A hydraulic jump can be viewed as discontinuous waves of all frequencies (wavelengths), which are generated and propagate from a point near the jump. The waves propagate both upstream and downstream. Since a large fraction of the waves fall in a wavelength range where they are shallow water gravity waves that move at the same speed for a given depth, they move upstream at the same rate; however as the water shallows upstream, their speed drops quickly, limiting the rate at which they can propagate upstream to

\sqrt{gh}

. Shorter wavelengths, which propagate more slowly than the speed of the wave in the deeper downstream water, are swept away downstream. Still, a fairly wide range of wavelengths and frequencies are present, so Fourier Analysis would suggest that a relatively abrupt wave front can be formed; this is indeed observed.

Viewing the hydraulic jump from a wave perspective provides another insight into the phenomena. When the incoming water speed is slow enough, a number of the longer wavelength waves propagate faster than the incoming flow, and can Disperse upstream as well as downstream. The deeper the incoming water is the more pronounced the dispersion effect will be. Only a small subset of frequencies (wavelengths) will match the speed of the flow. This truncation of the Fourier spectrum results in a hydraulic jump characterized by undulating waves rather than an abrupt jump. When visible undulations are present, the wavelength of the visible undulations provide a direct indication of the speed of the water upstream of the hydraulic jump.

This characteristic behavior allows one to estimate the prejump water depth and water speed simply by observing the height of the jump, the characteristics of the jump, and correlating them as tabulated below. Such an “eyeball” estimate is routinely used by river runners while judging rapids; their conclusions are generally based on an intuitive sense rather than an analytic approach.

Tabular summary of the analytic conclusions

HYDRAULIC JUMP VARIATIONS

Although the previous discussion has focused on the straight-forward simple channel approximation, a number of variations are amenable to similar analyses as well. They also serve the important function of allowing the student to perform simple experiments with everyday objects.

Shallow fluid hydraulic jumps

;The hydraulic jump in your sink
Figure 2 above illustrates a daily example of a hydraulic jump can be seen when brushing your teeth, in the sink. Around the place where the tap water hits the sink, you will see a smooth looking flow pattern. A little further away, you will see a sudden 'jump' in the water level. This is a hydraulic jump.

The nature of this jump differs from those previously discussed in the following ways:

The water is flowing radially. As a result it continuously grows shallower and slows due to friction (the Froude number drops) up to the point where the jump occurs.

The flow depth is thin enough that the surface tension can no longer be neglected, changing the wave solution conclusions. The higher speed of the surface tension waves bleed off the high frequency component, making an undular jump the dominant form.Surface tension effects can be seen by looking closely at the region inside the hydraulic jump. There you will observe thin waves radiating radially and axially from the point of water impact.

Changes in the behavior of the jump can be observed by changing the flow rate.

Internal wave hydraulic jumps

Hydraulic jumps in abyssal fan formation

Turbidity Current s can result in internal hydraulic jumps (i.e., hydraulic jumps as Internal Wave s in fluids of different density) in Abyssal Fan formation. The internal hydraulic jumps have been associated with salinity or temperature induced Stratification as well as with density differences due to suspended materials. When the bed slope over which the turbidity current flattens, the slower rate of flow is mirrored by increased sediment deposition below the flow, producing a gradual backward slope (i.e., a slope which rises against the current). Where a hydraulic jump occurs, the signature is an abrupt backward slope, corresponding to the rapid reduction in the flow rate at the point of the jump.¹³

Atmospheric hydraulic jumps

INDUSTRIAL AND RECREATIONAL APPLICATIONS FOR HYDRAULIC JUMPS

Industrial

The hydraulic jump is the most commonly used choice of design engineers for energy dissipation below spillways and outlets. A properly designed hydraulic jump can provide for 60-70% energy dissipation of the energy in the basin itself, limiting the damage to structures and the streambed. Even with such efficient energy dissipation, stilling basins must be carefully designed to avoid serious damage due to uplift, vibration, Cavitation , and abrasion. An extensive literature has been developed for this type of engineering.

Recreational

In Kayaking and Canoeing paddlers will often stop and Playboat in standing waves and hydraulic jumps en-route while traveling rivers. The standing waves and shock fronts of hydraulic jumps make popular locations for such recreation.

Similarly, kayakers and Surfers have been known to ride bores up rivers.

SEE ALSO

Shock Wave

Tidal Bore

Turbulence

Laminar Flow

REFERENCES AND NOTES

	CATEGORIES ABOUT HYDRAULIC JUMP

	hydraulics

	fluid dynamics

	wave mechanics

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Hydraulic Jump