Reynolds Number Calculator
Compute Re for a pipe or open-channel flow and read the regime: laminar, transitional, or turbulent.
Defaults are water at 60°F (ν = 1.21 × 10⁻⁵ ft²/s) in a 6-inch pipe at 5 ft/s.
Regime thresholds — by geometry
| Geometry | Laminar | Transitional | Turbulent |
|---|---|---|---|
| Round pipe (internal flow) | < 2,300 | 2,300–4,000 | > 4,000 |
| Non-circular duct (use Dh) | < 2,300 | 2,300–4,000 | > 4,000 |
| Open channel (use Rh) | < 500 | 500–2,000 | > 2,000 |
| Flat plate boundary layer | < 5×10⁵ | 5×10⁵ | > 5×10⁵ |
| Sphere drag (transition to wake) | < 1 | 1–10⁵ | > 10⁵ |
| Cylinder cross-flow (vortex shed.) | < 40 | 40–10⁵ | > 3×10⁵ |
The open-channel limits look lower only because they are written with L = Rh. For a full pipe Rh = D/4, so 500 and 2,000 on an Rh basis correspond to 2,000 and 8,000 on a diameter basis. Engineering practice usually treats pipe flow above Re = 2,300 as effectively turbulent and uses rough-pipe friction formulas conservatively in the transitional band.
Kinematic viscosity ν of common fluids
| Fluid / temperature | ν (US ft²/s) | ν (SI m²/s) |
|---|---|---|
| Water, 32°F (0°C) | 1.92×10⁻⁵ | 1.79×10⁻⁶ |
| Water, 40°F (4°C) | 1.66×10⁻⁵ | 1.55×10⁻⁶ |
| Water, 50°F (10°C) | 1.41×10⁻⁵ | 1.31×10⁻⁶ |
| Water, 60°F (16°C) | 1.21×10⁻⁵ | 1.13×10⁻⁶ |
| Water, 70°F (21°C) | 1.06×10⁻⁵ | 9.84×10⁻⁷ |
| Water, 80°F (27°C) | 9.30×10⁻⁶ | 8.64×10⁻⁷ |
| Water, 100°F (38°C) | 7.39×10⁻⁶ | 6.87×10⁻⁷ |
| Air, 60°F | 1.58×10⁻⁴ | 1.47×10⁻⁵ |
| SAE 10W oil, 60°F | 1.0×10⁻³ | 9.3×10⁻⁵ |
| SAE 30 oil, 60°F | 4.1×10⁻³ | 3.8×10⁻⁴ |
| Glycerin, 70°F | 6.5×10⁻³ | 6.0×10⁻⁴ |
| Mercury, 60°F | 1.21×10⁻⁶ | 1.13×10⁻⁷ |
Worked examples
Example 1 — 6-inch water main at 5 ft/s
Example 2 — Hydraulic-oil cooler line, small diameter
Reference: White, F.M. (2011). Fluid Mechanics (7th ed.). McGraw-Hill. Original concept: Reynolds, O. (1883). "An experimental investigation of the circumstances which determine whether the motion of water shall be direct or sinuous." Phil. Trans. Royal Soc. London, 174, 935–982.
Common mistakes
- Mixing length conventions. Pipe thresholds (2,300 / 4,000) assume L = D. Open-channel thresholds (500 / 2,000) assume L = Rh. If a source uses 4Rh for channels, its thresholds are about four times larger. Match the threshold to the length you entered.
- Using dynamic viscosity μ in VL/ν. This calculator takes kinematic viscosity. In US units μ/ν for water is the density, about 1.94 slug/ft³, so the wrong one is off by roughly a factor of two.
- Assuming 60°F water in winter or in process piping. Viscosity of water nearly halves between 40°F and 100°F. Use the table above.
- Reading “turbulent” as “supercritical”. Reynolds number separates laminar from turbulent. The Froude number separates subcritical from supercritical, and the two are independent.
When this calculator doesn’t apply
The thresholds are for steady, fully developed flow of a Newtonian fluid. Flow just downstream of an entrance or fitting, pulsating flow and heated pipes transition at different values. Sludges, slurries and polymer solutions are non-Newtonian and need a generalized Reynolds number. Flow through soil or filter media uses a particle-based Reynolds number, and Darcy’s law is valid only at low values of it.