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CE-311 Open Channel Flow Laboratory · Experiment 1

🌊 Formation of a Hydraulic Jump

A virtual re-creation of the flume experiment. Set the discharge and sluice-gate opening to launch a fast supercritical stream, then raise the tailgate until the tailwater matches the sequent depth and a stable jump stands still in the test section. Measure it, record six observations, and compute the jump characteristics.

Aim

To study the formation of a hydraulic jump in a rectangular channel and to determine the characteristics of the jump — sequent depths, Froude number, height, length and energy loss.

Theory

A hydraulic jump forms when a supercritical stream (Fr > 1) meets a subcritical tailwater of sufficient depth. The stream abruptly rises from its initial depth y₁ to its sequent depth y₂ through a turbulent roller, dissipating energy. For a horizontal rectangular channel the momentum equation gives the Belanger sequent-depth relation:

Fr₁ = V₁/√(g·y₁)  •  y₂/y₁ = ½(√(1 + 8·Fr₁²) − 1)  •  ΔE = (y₂ − y₁)³ / (4·y₁·y₂)  •  L ≈ 6.9(y₂ − y₁)

Classification by Fr₁: 1–1.7 undular · 1.7–2.5 weak · 2.5–4.5 oscillating · 4.5–9 steady · >9 strong jump.

Apparatus

Re-circulating rectangular tilting flume (10 m × 0.30 m × 0.60 m), upstream and downstream sluice gates, pump with delivery valve, pointer gauge, collecting tank & stopwatch, steel ruler.

Procedure — perform it here

Match the tailwater to the sequent depth y₂ to hold the jump still.
Unit discharge q
V₁ (supercritical)
Froude number Fr₁
Sequent depth y₂
Jump type

Observations & Computations

Width of flume B = 0.30 m. Record at least 6 observations at different discharges / gate settings (only a stable jump can be recorded).

No.Q (L/s)y₁ (cm)y₂ (cm)Fr₁y₂/y₁ hj=y₂−y₁ (cm)L (cm)ΔE (m)Type
No observations yet — form a stable jump and press “Record reading”.

Results

Average height of jump hj (cm)
Average length of jump L (cm)
Average energy loss ΔE (m)

Questions & Precautions

What is the purpose of a hydraulic jump and its applications?

It dissipates surplus kinetic energy of supercritical flow, preventing scour downstream of spillways, sluice gates and chutes. It is also used to mix chemicals, aerate water, and raise the downstream water level for irrigation off-takes.

Why can't the energy equation be applied directly across the jump?

The jump is highly turbulent with an unknown, large energy loss in the roller, so energy is not conserved across it. The momentum equation is applied instead, giving the Belanger sequent-depth relation; the energy loss is then found as the difference E₁ − E₂ = (y₂−y₁)³/(4y₁y₂).

Jump types (undular, weak, oscillating, strong)

Undular (Fr₁ 1–1.7): surface undulations, little loss. Weak (1.7–2.5): smooth roller, ~5–18% loss. Oscillating (2.5–4.5): an unstable jet causes surface waves travelling downstream. Steady/strong (>4.5): a well-defined, stable jump dissipating 45–85% of the energy.

Precautions: ensure the sluice gate is seated properly; form the jump near the gate within the test section; vary the flow and adjust the tailgate accordingly; take readings only after the jump is steady.