Lab 04:  The Hydraulic Jump


[RDA] Good morning

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[RDA] Today we are going to demonstrate the hydraulic jump.

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[RDA] The hydraulic jump is an open-channel flow phenomenon by which the flow passes suddenly from supercritical upstream of the jump, to subcritical downstream.

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[RDA] The hydraulic jump is formed in a horizontal channel when the headwater condition is sufficiently low and the tailwater condition is sufficiently high.

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[RDA] The hydraulic jump always occurs with a loss of energy.

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[RDA] The formula for the energy loss is:

ΔE = (y2 - y1)3 / (4 y1 y2)

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[RDA] We turn on the pump.

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[RDA] We set the bed slope equal to zero and check the level [Point to the level].

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[RDA] The hydraulic jump is established. [Wait to the jump to form]

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[RDA] [Point to the gage] Note that the point gage is at zero.

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[RDA] Now we are going to measure the height ot the bottom of the flume.

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[RDA] The height is X mm.

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[RDA] Now we are going to measure the height to the upstream water surface.

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[RDA] The height is Y mm.

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[RDA] The upstream depth is:  y1 = X - Y

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[RDA] Now we are going to measure the height to the downstream water surface.

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[RDA] The height is Z mm.

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[RDA] The downstream depth is:  y2 = X - Z


[RDA] The energy loss due to the jump is:

ΔE = (y2 - y1)3 / (4 y1 y2)

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[RDA] Thank you.