Concept

1. What is a hydraulic jump?

A hydraulic jump is the rapid transition from supercritical (shallow, fast) flow to subcritical (deeper, slower) flow in an open channel. It dissipates a large portion of the flow’s kinetic energy over a relatively short distance – which is why stilling basins are placed just downstream of spillways, power outlets and sluices.

For a horizontal, rectangular channel the jump is characterised by two conjugate depths: pre‑jump depth y1 and sequent depth y2, related through the momentum equation.

Formulas

2. Basic hydraulic relations used in the tool

2.1 Froude number & unit discharge

For a rectangular channel of width B:

Discharge & unit discharge
Q = B · y₁ · V₁ (if not prescribed)
q = Q / B = y₁ · V₁ (unit discharge)
Upstream Froude number
Fr₁ = V₁ / √(g · y₁)
Supercritical flow requires Fr₁ > 1.

In the tool, you can supply either Q, B and y₁ (and it computes V₁), or directly V₁ and y₁.

2.2 Conjugate (sequent) depth

The Bélanger equation for a rectangular, horizontal channel gives:

Depth ratio
y₂ / y₁ = 0.5 · [ √(1 + 8·Fr₁²) − 1 ]

Sequent depth
y₂ = (y₁ / 2) · [ √(1 + 8·Fr₁²) − 1 ]

Once y₂ is known, the post‑jump velocity is simply V₂ = q / y₂, and the downstream Froude number Fr₂ = V₂ / √(g · y₂), which should be < 1.

Energy

3. Energy loss and jump classification

3.1 Specific energy & loss

Specific energy (per unit weight) in a rectangular channel is:

Specific energy
E = y + V² / (2g)
Upstream: E₁ = y₁ + V₁² / (2g)
Downstream: E₂ = y₂ + V₂² / (2g)
Energy loss in the jump: ΔE = E₁ − E₂

For a classical hydraulic jump in a rectangular channel, ΔE can also be expressed directly in terms of the conjugate depths:

Energy loss from conjugate depths
ΔE = (y₂ − y₁)³ / (4 · y₁ · y₂)

3.2 Qualitative jump type (Fr₁‑based)

The tool labels the jump approximately as:

Design

4. Jump length correlations & stilling basin length

4.1 Jump length formulas implemented in the tool

There is no single “exact” length for a hydraulic jump – different experiments give different correlations. The tool implements two simple empirical forms and lets you choose which one to adopt:

(1) Height‑based correlation
Lⱼ ≈ kLj · (y₂ − y₁)
with kLj typically in the range 6–7 for classical jumps.
(2) Sequent‑depth‑based correlation (USBR‑style)
Lⱼ ≈ cy2 · y₂
For a plain USBR Type I basin, cy2 ≈ 6 is often used.

In the tool, you can select:

4.2 Stilling basin length

Once a jump length Lj is adopted, the “hydraulic” basin length is inflated by a factor kbasin to allow for appurtenances, uncertainties and model bias:

Basin length
Lbasin = kbasin · Lⱼ
Typical preliminary choice: kbasin ≈ 1.0–1.2.
USBR

5. USBR stilling basin types – quick guidance

The tool gives a very simplified suggestion for an appropriate USBR stilling basin type, based solely on Fr₁ and V₁. This is for guidance only; final selection must follow USBR EM‑25 and project‑specific analysis.

The suggestion in the tool is deliberately conservative and meant to trigger the right chapter of the design manual – not to replace detailed design.

Example

6. Worked example (matches the quick design tool)

Consider a spillway stilling basin with the following preliminary design values:

Discharge Q: 80 m³/s
Basin width B: 10 m
Pre‑jump depth y₁: 0.60 m
Gravity g: 9.81 m/s²
Height‑based factor kLj: 6.9
y₂‑based factor cy2: 6.0
Basin factor kbasin: 1.1
Tailwater depth ytail: (assume ≈ y₂)

Step 1 – Unit discharge and pre‑jump velocity

Unit discharge: q = Q / B = 80 / 10 = 8.0 m²/s.
Pre‑jump velocity: V₁ = q / y₁ = 8.0 / 0.60 ≈ 13.3 m/s.

Step 2 – Upstream Froude number

Fr₁ = V₁ / √(g · y₁) = 13.3 / √(9.81 · 0.60).
√(9.81 · 0.60) ≈ √5.89 ≈ 2.43, so Fr₁ ≈ 13.3 / 2.43 ≈ 5.5 strong jump.

Step 3 – Conjugate depth y₂

Use the Bélanger equation:

y₂ = (y₁ / 2) · [ √(1 + 8·Fr₁²) − 1 ]
Fr₁² ≈ 5.5² ≈ 30.251 + 8·Fr₁² ≈ 1 + 8·30.25 ≈ 1 + 242 ≈ 243
√243 ≈ 15.6[√(1 + 8·Fr₁²) − 1] ≈ 15.6 − 1 = 14.6
y₂ ≈ (0.60 / 2) · 14.6 = 0.30 · 14.6 ≈ 4.4 m

So the sequent depth is about y₂ ≈ 4.4 m.

Step 4 – Energy loss

Specific energies:

Energy loss: ΔE ≈ 9.6 − 4.6 ≈ 5.0 m (about half the specific energy is dissipated in the jump).

Step 5 – Jump length & basin length

Height‑based correlation:

Lj (height‑based) = kLj · (y₂ − y₁)
= 6.9 · (4.4 − 0.6) ≈ 6.9 · 3.8 ≈ 26 m

y₂‑based correlation:

Lj (y₂‑based) = cy2 · y₂ = 6.0 · 4.4 ≈ 26.4 m

The two estimates are very similar (≈26 m). If we choose the conservative “max” option, Lj,adopt ≈ 26.4 m. For kbasin = 1.1:

Lbasin = kbasin · Lj ≈ 1.1 · 26.4 ≈ 29 m

So a stilling basin floor length of about 29 m is indicated for this discharge and depth, before refining the layout with blocks, piers, end sill and detailed code provisions.

Step 6 – USBR type

With Fr₁ ≈ 5.5 and V₁ ≈ 13.3 m/s, the tool will typically suggest a USBR Type III basin (chute blocks + baffle blocks + end sill) as a starting point, or Type II if baffle blocks are not acceptable. A precise choice requires referring to USBR EM‑25.

The example above is intentionally slightly rounded; the tool will compute the same quantities with full precision and show you the detailed intermediate results.

Workflow

7. How to use this with the online tool

  1. Start from your spillway / outlet rating curve to estimate Q, B and y₁ at the basin entrance.
  2. Enter these into the Hydraulic Jump & Stilling Basin – Quick Design tool.
  3. Inspect Fr₁, y₂, energy loss and jump length.
  4. Adjust kLj, cy2 and kbasin to match your design philosophy (plain basin vs. heavily appurtenanced).
  5. Check the USBR type suggestion and cross‑reference with the relevant manual chapter.
  6. Once a tentative layout is chosen, move on to anti‑scour checks, floor thickness, uplift, key length and downstream river morphodynamics.

This page is intentionally “design‑office friendly”: it shows what the tool is doing, so you can quickly sanity‑check outputs against hand calculations or other software.