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Hydraulics, open channels and fluid power

Gradually varied flow depth gradient

Rate of change of depth along a prismatic channel with the bed slope S₀, friction slope Sf and local Froude number Fr, with x increasing downstream and hydrostatic pressure.

Ref
HYD-30
Rev
v1
Field
Hydraulics, open channels and fluid power
Result
dy/dx

Where the depth changes slowly along a prismatic channel, the energy equation gives dy/dx = (S₀ − Sf)/(1 − Fr²), with x downstream, S₀ the bed fall, Sf the friction slope and Fr the local Froude number. The sign tells whether the surface rises or falls, and the denominator changes sign at critical flow. At Fr = 1 the formula is not defined and the flow must be treated as a control.

Rate of change of depth along a prismatic channel with the bed slope S₀, friction slope Sf and local Froude number Fr, with x increasing downstream and hydrostatic pressure. It is not defined at critical flow.

Calculator

Solve for
1e-50.1
1e-50.1
0.053
  • Numerator, S₀ − Sf4×10−4
  • Denominator, 1 − Fr²0.75
  • Change in depth over 100 m at this gradient0.05333 m

What drives the result

Each variable is moved across its typical range while the others stay at the values above. The longest bar is the key driver.

Depth gradient () current value 5.333e-4
S0Bed slopeKey driver
−7.87e-40.133
SfFriction slope
−0.1320.00132
FrLocal Froude number
−0.00590.00318
  • The depth rises by 0.05333 m per 100 m along the channel, since the bed fall exceeds the friction slope.
  • Close to Fr = 1 the denominator goes to zero, so the gradient becomes very steep and the profile is no longer gradually varied.
Chart data as tables

Ranked variables

VariableTypical rangeLowest resultHighest resultSwing ()Local stepChange in result
S0 Bed slope1e-5 to 0.1 −7.867e-40.13250.1333+10%+25 %
Sf Friction slope1e-5 to 0.1 −0.1320.001320.1333+10%−15 %
Fr Local Froude number0.05 to 3 −0.0059020.003180.009082+10%+7.53 %

Sweep of Local Froude number

Local Froude numberDepth gradient
0.054.01e-4
0.41884.851e-4
0.78750.001053
1.156−0.001187
1.525−3.017e-4
1.894−1.547e-4
2.263−9.711e-5
2.631−6.753e-5
3−5e-5

Sweep one variable

Depth gradient ()Hover, touch, or use the arrow keys on the chart
−0.025−0.02−0.015−0.01−0.0052e−180.005 0.511.522.53 Local Froude number now 5.333e-4

Variables and how each one contributes

dy/dx

Depth gradient

Result ·

What the equation gives you. Everything else feeds it.

S0

Bed slope

· typical 1e-5 to 0.1

The bed slope, positive for a fall downstream. A steeper bed raises the gradient in direct proportion to the numerator. Raising it by 10 % (to 0.0011) moves the result by +25 %, from 5.333×10−4 to 6.667×10−4.

Sf

Friction slope

· typical 1e-5 to 0.1

The friction slope, a plain ratio. More friction lowers the numerator, so the gradient falls. Raising it by 10 % (to 6.6×10−4) moves the result by −15 %, from 5.333×10−4 to 4.533×10−4.

Fr

Local Froude number

· typical 0.05 to 3

The local Froude number (not equal to 1). A Froude number nearer 1 makes the denominator smaller, so the gradient grows rapidly. Raising it by 10 % (to 0.55) moves the result by +7.53 %, from 5.333×10−4 to 5.735×10−4.

Worked example with the values above

  1. Slope difference: S₀ − Sf = 0.001 − 6×10−4 = 4×10−4.
  2. Denominator: 1 − Fr² = 1 − 0.25 = 0.75.
  3. dy/dx = 5.3333×10−4 (metres per metre).

Assumptions and limits

  • A prismatic rectangular channel with hydrostatic pressure and a uniform velocity profile.
  • For jumps: a horizontal channel, negligible friction across the jump and momentum coefficient 1.

Common mistakes

  • Using total discharge where discharge per unit width is needed.
  • Applying the jump relation when Fr₁ is below 1, where no jump forms.
  • Measuring the energy from the wrong datum.

Statistics and uncertainty

Depths near the critical depth are very sensitive: a small change in energy gives a large change in depth. Jump relations are also sensitive to the upstream Froude number, so errors in the measured depth and discharge matter.

Where it is used

  • Locating control sections and finding whether flow is subcritical or supercritical.
  • Sizing stilling basins and tracing backwater and drawdown curves.

Maths you need

  • Froude number: Fr = V/√(g D), the ratio of flow speed to wave speed
  • Specific energy: energy per unit weight measured from the bed
  • Momentum conservation: force balance across the jump

Related formulas

Practise this formula