Jet Velocity Calculator

Pick a method and enter known values. Get velocity, discharge, and thrust in seconds accurately. Compare scenarios with the built‑in example data table below.

Choose method *
Tip: If you measured flow, use the flow method.
Required for pressure method.
Required for head method.
Required for flow method.
Water is about 1000 kg/m³ near room temperature.
Use 1.0 for ideal conditions, lower for losses.
Velocity will also be shown in m/s.
Nozzle size (used for discharge, thrust, Reynolds)
Optional, but recommended for discharge and thrust.
If you know area directly, enter it here.
Water is about 1 cP near room temperature.
Default is standard gravity in m/s².
Results will appear above this form after submission.

Formulas used

Pressure method
v = C √(2 ΔP / ρ)
ΔP in pascals, ρ in kg/m³, v in m/s.
Head method
v = C √(2 g H)
g in m/s², H in meters.
Flow method
v = C (Q / A)
Q in m³/s, A in m².

Extra relationships
  • A = π d² / 4 and Q ≈ A v
  • q = ½ ρ v² (dynamic pressure)
  • F = ρ Q v (jet thrust / momentum flux)
  • Re = ρ v d / μ (Reynolds number)

How to use this calculator

  1. Select a method: pressure, head, or flow rate.
  2. Enter density and the required method input values.
  3. Enter nozzle diameter, or switch to area entry.
  4. Adjust the coefficient if you expect losses.
  5. Choose your output unit and press calculate.
  6. Use CSV or PDF buttons to save the results.

Example data table

These scenarios show typical ranges for water-like fluids and common nozzle sizes.

# Method Input ρ (kg/m³) Nozzle Velocity (m/s) Discharge (L/s)
1 Pressure ΔP = 200 kPa, C = 0.98 1000 d = 10 mm ≈ 19.60 ≈ 1.54
2 Pressure ΔP = 3 bar, C = 1.00 1000 d = 6 mm ≈ 24.49 ≈ 0.69
3 Head H = 15 m, C = 0.97 998 d = 12 mm ≈ 16.68 ≈ 1.89
4 Head H = 3 ft, C = 1.00 1000 d = 8 mm ≈ 4.24 ≈ 0.21
5 Flow Q = 8 L/s, C = 1.00 1000 d = 25 mm ≈ 16.30 8.00

Jet velocity basics for real systems

A jet velocity estimate connects pressure, elevation, and nozzle geometry to a measurable exit speed. This calculator supports three common inputs: pressure difference, head height, and volumetric flow. Each method reports velocity, estimated discharge, dynamic pressure, thrust, and an optional Reynolds number check for flow regime insight.

1) What “jet velocity” means

Jet velocity is the average exit speed at the nozzle. For an ideal nozzle, almost all available energy becomes kinetic energy. In practice, friction and contraction reduce speed, so the coefficient C (often 0.90–1.00) adjusts the ideal result to better match measurements.

2) Pressure method: typical ranges

For water near ρ ≈ 1000 kg/m³, ΔP = 100 kPa gives v ≈ √(2ΔP/ρ) ≈ 14.14 m/s (C = 1). ΔP = 200 kPa yields about 20.0 m/s. A 3 bar drop (300 kPa) gives about 24.5 m/s, consistent with many wash and spray systems.

3) Head method: converting height to speed

Head is gravitational potential per unit weight. With standard gravity g = 9.80665 m/s², a 10 m head gives v ≈ √(2gH) ≈ 14.0 m/s (C = 1). A useful rule: 1 m of water head is about 9.81 kPa of pressure head equivalence.

4) Flow method: Q and nozzle sizing

When flow is measured, velocity is v = Q/A. Area for a circular nozzle is A = πd²/4. For d = 10 mm, A ≈ 7.85×10⁻⁵ m². If Q = 1.5 L/s (0.0015 m³/s), then v ≈ 19.1 m/s before applying C.

5) Discharge and thrust outputs

Once v is known, discharge is Q ≈ A·v (if area is provided). Thrust follows momentum flux: F = ρQv. Example: water, Q = 0.0015 m³/s, v = 19 m/s gives F ≈ 28.5 N. This helps compare nozzle options or estimate reaction loads.

6) Dynamic pressure and impact intuition

Dynamic pressure q = ½ρv² is a compact “impact” metric. With water and v = 20 m/s, q ≈ 200 kPa. Higher q often means stronger cleaning, cutting, or erosion potential, but surface distance, spray breakup, and target angle still matter.

7) Reynolds number and viscosity check

Re = ρvd/μ indicates whether the jet is laminar, transitional, or turbulent near the nozzle. With water μ ≈ 1 cP (0.001 Pa·s), d = 10 mm, v = 20 m/s gives Re ≈ 200,000, typically turbulent. Higher viscosity lowers Re significantly.

8) Practical validation tips

Use consistent units, and prefer measured density and viscosity when accuracy matters. If your nozzle has known losses, set C below 1. Compare results to measured flow at the nozzle, and ensure the selected method matches what you actually measured in the field.

Frequently asked questions

1) Which method should I choose?

Use pressure if you know the drop across the nozzle. Use head if you know elevation or tank level. Use flow if you measured Q and know the nozzle diameter or area.

2) What coefficient C should I use?

Start with C = 1.00 for ideal estimates. For real nozzles, 0.90–0.99 is common depending on losses, contraction, and roughness. If you have test data, tune C to match measured velocity or flow.

3) Why is density required?

Density links pressure energy to kinetic energy in the pressure method. Lower density fluids produce higher velocity for the same pressure drop. Density also affects thrust, dynamic pressure, and Reynolds number outputs.

4) Can I calculate velocity without nozzle size?

Yes, for pressure and head methods you can compute velocity without diameter. However, discharge, thrust, and Reynolds number depend on nozzle size, so provide diameter or area for those extra outputs.

5) How accurate is the thrust value?

Thrust uses F = ρQv and assumes the jet exits cleanly and uniformly. Real jets can diverge or break up, reducing effective momentum at distance. Use it as a near‑nozzle estimate or comparative metric.

6) What viscosity should I enter for water?

Near room temperature, water is about 1 cP. Warmer water is slightly lower, and colder water is higher. If you need better precision, use a temperature‑based viscosity value from a reliable table.

7) Why do results differ between methods?

Each method reflects different measurements and assumptions. Pressure and head assume energy conversion, while flow is purely geometric. Losses, measurement location, and nozzle behavior can cause differences. The coefficient helps reconcile ideal estimates with reality.

Built for clear inputs, fast results, and simple exporting.

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