Reynolds Number Calculator

Calculate the Reynolds number to determine if fluid flow is laminar or turbulent based on velocity, diameter, and viscosity.

Reynolds Number

Reynolds number (Re) is a dimensionless quantity used in fluid mechanics to predict whether fluid flow will be laminar (smooth and orderly) or turbulent (chaotic and mixing). It is one of the most important parameters in engineering design of pipes, aircraft, ships, pumps, and heat exchangers.

Reynolds number formula: Re = (ρ × v × L) ÷ μ

Or equivalently using kinematic viscosity: Re = (v × L) ÷ ν

Where:

  • ρ (rho) = fluid density (kg/m³)
  • v = flow velocity (m/s)
  • L = characteristic length (m), pipe diameter for internal flow; chord length for airfoils
  • μ (mu) = dynamic viscosity (Pa·s = kg/(m·s))
  • ν (nu) = kinematic viscosity = μ ÷ ρ (m²/s)

Flow regime interpretation:

  • Re < 2,300: Laminar flow, fluid moves in smooth parallel layers, low mixing, predictable
  • 2,300 < Re < 4,000: Transition zone, unstable, can be either
  • Re > 4,000: Turbulent flow, chaotic mixing, higher heat transfer, higher friction losses

Common fluid properties at 20°C:

  • Water: ρ = 998 kg/m³, μ = 1.002×10⁻³ Pa·s, ν = 1.004×10⁻⁶ m²/s
  • Air: ρ = 1.204 kg/m³, μ = 1.825×10⁻⁵ Pa·s, ν = 1.516×10⁻⁵ m²/s
  • Honey: ρ ≈ 1,400 kg/m³, μ ≈ 10 Pa·s (very high viscosity)

Worked example: Water flowing through a 50 mm (0.05 m) diameter pipe at 2 m/s. At 20°C: ν = 1.004×10⁻⁶ m²/s.

Re = (v × D) ÷ ν = (2 × 0.05) ÷ 1.004×10⁻⁶ = 0.10 ÷ 0.000001004 = 99,602

Re » 4,000 → turbulent flow. The engineer must account for higher pressure drop (using the Darcy-Weisbach equation) and select a pump accordingly.

A note on the name. Osborne Reynolds was an Irish-born engineer at the University of Manchester who in 1883 ran the classic dye experiment that defined the field. He injected a thin stream of colored dye into a pipe carrying water and slowly increased the flow rate. At low rates the dye stream stayed straight and steady. At a critical speed it suddenly broke apart into swirling eddies. The dimensionless ratio that predicted this transition is now named for him. His experimental apparatus is still on display in Manchester.

Why the ratio matters. Re is the ratio of inertial forces (ρvL) to viscous forces (μ) in the fluid. When viscosity dominates, the fluid moves in smooth parallel layers and damps out any disturbances. When inertia dominates, small disturbances amplify into turbulent eddies. That is the deep reason behind the 2,300/4,000 thresholds: they mark where one force regime hands off to the other.


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