Calculatorism

Velocity Head Calculator

Enter flow velocity to compute velocity head h_v=v²/(2g), the kinetic-energy term of Bernoulli's equation. v=3 m/s → h_v≈0.459 m; double the speed → 4× the head.

Input Data

Section average velocity (m/s).
m/s

Results

Velocity head h_v (m of water).
0.4587m

At a glance:Velocity head (symbol h_v) is the hydraulic quantity that converts the kinetic energy of a flow into an equivalent water-column height. Bernoulli's equation expresses the total energy per unit weight of fluid as the sum of three heads: pressure head (p/γ), elevation head (z) and velocity head (v²/2g), all with unit metres (m) so they add directly into 'total head'. The velocity head formula is h_v=v²/(2g), where v is the velocity (m/s) and g the gravitational acceleration (9.81 m/s²). Its physical meaning: if a stream at speed v converts all its kinetic energy losslessly into height (e.g. shoots straight up to rest), the height it reaches is exactly h_v; conversely, water falling freely from height h_v reaches final speed v — the inverse of Torricelli's law v=√(2gh). Term by term: the numerator v² shows kinetic energy scales with the square of speed, so doubling the speed makes the velocity head four times larger; the denominator 2g normalises kinetic energy into a height unit. Example: v=3 m/s → h_v=3²/(2×9.81)=9/19.62≈0.459 m, meaning this flow's kinetic energy equals the potential of a ~0.459 m water column. Applications: (1) pipe energy analysis — when computing head loss along a line, the velocity head must be included in each section's energy; (2) Pitot-tube speed measurement — the difference between the 'stagnation head' and the 'static head' is exactly the velocity head, from which v=√(2g·h_v); (3) pump and pipe-system design — head and energy balance must contain the kinetic term; (4) open-channel specific energy — the v²/2g in E=y+v²/2g is the velocity head. Notes: (1) v is usually the section average; strictly the kinetic head needs a 'kinetic-energy correction factor' α (laminar α=2, turbulent α≈1.03–1.1, engineering often uses 1) to correct for non-uniform velocity profile; (2) at higher speeds the velocity head dominates the total head, while it is often negligible in low-speed pipe flow; (3) use consistent units (v in m/s) to get head in m.

Formula

Velocity head: h_v = v²/(2g), g=9.81 m/s²

v velocity (m/s); h_v equivalent water-column height (m)

Inverse of Torricelli: v = √(2g·h_v)

$$h_v = \frac{v^2}{2g}$$

How to Use

  1. Enter the (average) section velocity v (m/s).
  2. The tool computes h_v=v²/(2g).
  3. For total head, also add pressure head p/γ and elevation head z.

Case Studies

Kinetic term in pipe flow

Average pipe velocity v=3 m/s.

h_v=3²/(2×9.81)≈0.459 m.

This flow's kinetic energy equals a ~0.459 m water column and must be counted in the section total head.

Pitot tube: head difference back-computes velocity

Pitot tube measures stagnation head minus static head (i.e. velocity head) h_v=0.459 m.

Back-compute v=√(2×9.81×0.459)≈3.00 m/s.

Velocity head and velocity convert both ways — the principle of Pitot-tube speed measurement.

Content review: Calculatorism Science Team. Results are for reference only; please refer to the relevant authorities for the official figures.

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