Pipe Flow Calculator

Convert between flow rate, velocity and pipe size using continuity.

Please note: These are idealised textbook models using representative material data. They are for study, sizing and sanity-checking only — never for final design. Real engineering requires code-compliant analysis, verified material certificates and a qualified engineer’s sign-off.

What the Pipe Flow Calculator does

The continuity equation ties flow rate, pipe area and velocity together: Q = A v. Since area depends on the square of diameter, small changes in pipe size have an outsized effect on velocity — and therefore on noise, erosion and pressure loss.

Formula

  • Q = A × v
  • A = π D² ÷ 4
  • D = √(4Q ÷ (π v))
  • Mass flow = Q × ρ

Inputs explained

InputUnitRequiredNotes
Solve forone of 3 optionsYes
Pipe inside diameternumberIn some modesShown Solve for is Flow rate from velocity, or Solve for is Velocity from flow rate.
Pipe inside diameter unitone of 9 optionsIn some modesShown Solve for is Flow rate from velocity, or Solve for is Velocity from flow rate.
Flow velocitym/sIn some modesAccepts more than 0. Shown Solve for is Flow rate from velocity, or Solve for is Pipe diameter for a target velocity.
Flow rateL/sIn some modesAccepts more than 0. Shown Solve for is Velocity from flow rate, or Solve for is Pipe diameter for a target velocity.
Fluidone of 7 optionsOptional

How to use it

  1. Choose Solve for and Fluid.
  2. Fill in the remaining inputs the form shows for your choice.
  3. Select Calculate.

Worked example

Water at 2 m/s through a 50 mm pipe.

Diameter
50 mm
Velocity
2 m/s

A = π × 0.05² ÷ 4 = 1,963.5 mm². Q = 2 × 0.0019635 = 3.927 L/s, or 235.6 L/min.

Frequently asked questions

What velocity should I design for?

1 to 2.5 m/s suits most water services. Below 0.5 m/s sediment settles; above 3 m/s you get noise, erosion and a real risk of water hammer.

Why does a slightly smaller pipe make such a difference?

Area goes with diameter squared and pressure drop with velocity squared, so pressure loss scales roughly with the fifth power of diameter. A 10% smaller pipe loses about 60% more pressure.

Method and sources

Method. Continuity — flow rate as cross-sectional area times velocity — with the Reynolds number reported to identify the flow regime.

Assumptions

  • Incompressible fluid, full pipe, and a uniform velocity profile assumed for the average.

Limitations

  • Average velocity conceals the profile: laminar flow peaks at twice the average at the centreline, which matters for erosion and mixing.
  • The calculation assumes a full pipe. Partially full gravity flow follows different relationships entirely.
  • Compressible flow — gases at significant pressure drop — is outside this model.

Sources

  • The continuity equation and Reynolds' flow-regime criterion — Classical fluid mechanics. The flow-rate relationship and the laminar-to-turbulent transition bands.

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