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Hydraulics, open channels and fluid power

Ideal broad-crested rectangular weir discharge

Discharge over a broad horizontal crest of width b with critical flow on the crest, from the upstream total head He above the crest including the approach velocity head.

Ref
HYD-20
Rev
v1
Field
Hydraulics, open channels and fluid power
Result
Q [m³/s]

A broad horizontal crest forces critical flow on the crest, where the depth is two thirds of the upstream total head He. The discharge is then Q = b √g (2He/3)^(3/2), with no losses assumed and free discharge. The total head includes the approach velocity head. A calibrated coefficient is needed for real installations, as friction and the crest shape reduce the flow below this ideal value.

Discharge over a broad horizontal crest of width b with critical flow on the crest, from the upstream total head He above the crest including the approach velocity head. It assumes free flow and no losses.

Calculator

Solve for
m³/s
m
0.1100
m/s²
130
m
0.025
  • Critical depth on the crest, 2He/30.4 m
  • Critical speed on the crest, √(g yc)1.981 m/s
  • Discharge per unit width, Q/b0.7924 m²/s

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.

Discharge (m³/s) current value 1.585 m³/s
bCrest widthKey driver
0.079279.2
HeUpstream total head above the crest
0.0096438.1
gGravitational acceleration
0.5062.77
  • A total head of 0.6 m over a 2 m crest gives 1.585 m³/s, with critical flow of 0.4 m depth on the crest.
  • Multiply by a calibrated coefficient, typically 0.85 to 0.95, to account for friction and crest shape in a real structure.
Chart data as tables

Ranked variables

VariableTypical rangeLowest resultHighest resultSwing (m³/s)Local stepChange in result
b Crest width0.1 to 100 m0.0792479.2479.16+10%+10 %
He Upstream total head above the crest0.02 to 5 m0.00964438.1238.11+10%+15.4 %
g Gravitational acceleration1 to 30 m/s²0.5062.7712.265+10%+4.88 %

Sweep of Upstream total head above the crest

Upstream total head above the crest (m)Discharge (m³/s)
0.020.009644
0.64251.756
1.2654.851
1.8888.842
2.5113.56
3.13318.9
3.75524.81
4.37731.23
538.12

Sweep one variable

Discharge (m³/s)Hover, touch, or use the arrow keys on the chart
010203040 12345 Upstream total head above the crest (m) now 1.585

Variables and how each one contributes

Q

Discharge

Result · m³/s

What the equation gives you. Everything else feeds it.

b

Crest width

m · typical 0.1 to 100

The crest width, in m. Raises the flow in direct proportion. Raising it by 10 % (to 2.2) moves the result by +10 %, from 1.585 to 1.743 m³/s.

g

Gravitational acceleration

m/s² · typical 1 to 30

The gravitational acceleration, in m/s². Raises the flow with the square root of g. Raising it by 10 % (to 10.79) moves the result by +4.88 %, from 1.585 to 1.662 m³/s.

He

Upstream total head above the crest

m · typical 0.02 to 5

The upstream total head above the crest, in m. Raises the flow with the power 3/2. Raising it by 10 % (to 0.66) moves the result by +15.4 %, from 1.585 to 1.828 m³/s.

Worked example with the values above

  1. Critical depth: 2He/3 = 2 × 0.6 / 3 = 0.4 m.
  2. Power 3/2: 0.25298; √g = 3.1321.
  3. Q = 2 × 3.1321 × 0.25298 = 1.5847 m³/s.

Assumptions and limits

  • Steady flow with the discharge coefficient suited to the installation and the Reynolds number.
  • For weirs: free discharge with an aerated nappe, a thin or broad crest as stated and negligible approach velocity.

Common mistakes

  • Measuring the head at the crest of the weir instead of upstream, beyond the drawdown.
  • Using a coefficient from a different weir type or scale.
  • Using the total head where the static head over the crest is needed, or the reverse.

Statistics and uncertainty

Discharge coefficients are calibrated values, normally good to 1 % to 5 %, and the head enters with a power of 1.5 to 2.5, so a 1 % error in head gives an error in flow of 1.5 % to 2.5 %.

Where it is used

  • Measuring flow in pipes, canals, rivers and flumes.
  • Setting weir crest levels and sizing overflows.

Maths you need

  • Discharge coefficient: the ratio of actual to ideal flow
  • Bernoulli equation: energy conservation along a streamline
  • Critical flow: flow at its minimum specific energy, with Froude number 1

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