Skip to content
Allin

What Is the Reynolds Number? The Formula, the Units That Cancel, and Why 2 300 Is Only for Pipes

Published 6/22/2026 · 9 min read · Everyday calculators

Lena Hoffmann

Lena HoffmannScience & education writer at Allin

Mathematics · Physics

Checked against 2 sources

View profile
In short

The Reynolds number is Re = ρvL/μ, or equivalently vL/ν, where ρ is the fluid density, v a characteristic speed, L a characteristic length, μ the dynamic viscosity and ν = μ/ρ the kinematic viscosity. It compares inertial effects with viscous ones, and it is dimensionless: ρvL has units of kg·m⁻³ × m·s⁻¹ × m = kg·m⁻¹·s⁻¹, and μ in pascal-seconds is also kg·m⁻¹·s⁻¹, so the ratio is a pure number. Water at 20 °C moving 1.0 m/s through a 15 mm pipe gives 998.2 × 1.0 × 0.015 / 0.001002 = 14 900, firmly turbulent. The familiar thresholds — laminar below about 2 300, turbulent above about 4 000 — apply to flow inside a pipe, with L taken as the internal diameter, and to nothing else. A flat plate transitions near Re = 5 × 10⁵ measured from its leading edge, so quoting 2 300 for a wing, a swimmer or a sphere is a category error.

Re = ρvL/μ compares inertia with viscosity, and the units really do cancel. See the number worked out for honey, a household pipe, an artery, a swimmer and a wing — and why the 2 300 threshold belongs to pipe flow alone.

The formula, and a check that the units really cancel

Re = ρvL/μ. Rather than take the word dimensionless on trust, put the units in. Density ρ is kg·m⁻³, speed v is m·s⁻¹, length L is m, so the numerator ρvL carries kg·m⁻³ × m·s⁻¹ × m = kg·m⁻¹·s⁻¹. Dynamic viscosity μ is measured in pascal-seconds, and a pascal is a newton per square metre, so Pa·s = (kg·m·s⁻² / m²)·s = kg·m⁻¹·s⁻¹ — the same combination. Numerator and denominator carry identical units, they cancel, and what is left is a bare number with no unit at all. That is why a Reynolds number of 14 900 means the same thing in every laboratory on Earth, and why writing it with a unit attached is always a mistake.

Work one case end to end. Water at 20 °C has ρ = 998.2 kg/m³ and μ = 1.002 × 10⁻³ Pa·s. Push it at 1.0 m/s through a pipe of 15 mm internal diameter and the numerator is 998.2 × 1.0 × 0.015 = 14.973 kg·m⁻¹·s⁻¹; divide by 1.002 × 10⁻³ kg·m⁻¹·s⁻¹ and you get 14 943, which most engineers would report as 1.5 × 10⁴. The second form of the formula is often quicker: kinematic viscosity ν = μ/ρ = 1.002 × 10⁻³ / 998.2 = 1.0038 × 10⁻⁶ m²/s, so Re = vL/ν = 1.0 × 0.015 / 1.0038 × 10⁻⁶ = 14 943 again. The units there cancel just as cleanly, since m·s⁻¹ × m ÷ m²·s⁻¹ = 1. Use whichever form matches the viscosity your table gives, and never mix the two.

2 300 belongs to a pipe: thresholds come with a geometry attached

The Reynolds number is only defined once you say what L is, because L is not a fixed property of the object — it is the length scale you choose to characterise the flow. For flow inside a pipe, L is the internal diameter, and it is for that choice that the familiar numbers hold: below roughly 2 300 the flow stays laminar, above roughly 4 000 it is turbulent, and in between it is transitional and depends on inlet disturbances and wall roughness. In the 15 mm pipe above, 2 300 corresponds to 0.154 m/s, about 1.6 L/min, and 4 000 to 0.268 m/s. Open the tap any further and you are in turbulent flow.

Change the geometry and the threshold changes with it. On a flat plate in an unbounded stream, the usual figure for transition is Re ≈ 5 × 10⁵ with L measured as the distance from the leading edge, which in air at 50 m/s is reached only 0.152 m back from the edge, and in water at 1.5 m/s at 0.335 m. Flow past a cylinder starts shedding a regular vortex street from about Re ≈ 47, and a sphere goes through the drag crisis near Re ≈ 3 × 10⁵. None of those numbers is 2 300, and none of them contradicts it — they are different problems with different characteristic lengths. Any Reynolds number quoted without naming L, and any threshold quoted without naming a geometry, is unfinished information.

What the number is actually for: comparing flows that are not the same size

The Reynolds number is not a verdict on whether a flow is good or bad; it is a statement about which physics dominates. At low Re, viscosity wins and inertia is negligible, which is why a bacterium at Re = 6 × 10⁻⁵ coasts nowhere: stop the flagellum and it stops within a fraction of its own body length. At high Re, inertia wins, small disturbances grow instead of being damped, and the flow becomes turbulent. The eleven orders of magnitude in the table above are not a scale of quality — they are a map of which term in the Navier–Stokes equations you are allowed to neglect.

The practical payoff is dynamic similarity. Two flows with the same Reynolds number and the same geometry behave the same way, whatever their absolute size — the streamline pattern and the drag coefficient carry across. That is the entire basis of wind-tunnel and towing-tank testing, and also its central difficulty. To match the 4.9 × 10⁶ of the full-size wing with a one-tenth-scale model in ordinary air, you would need ten times the speed, 500 m/s, which is Mach 1.46 and no longer the same physics at all. The standard escape is to raise the density instead: pressurising the tunnel tenfold matches Re at the original 50 m/s, Mach 0.15, which is why serious aerodynamic tunnels are pressure vessels rather than large fans.

Reynolds numbers across eleven orders of magnitude — water at 20 °C (ρ = 998.2 kg/m³, μ = 1.002 × 10⁻³ Pa·s), air at 20 °C (ρ = 1.204 kg/m³, μ = 1.825 × 10⁻⁵ Pa·s), blood (ρ = 1 060 kg/m³, μ = 3.5 × 10⁻³ Pa·s)
SituationCharacteristic length L and speed vReRegime, and which threshold applies
A swimming bacterium in waterL = 2 µm, v = 30 µm/s6 × 10⁻⁵Creeping flow: inertia is irrelevant, and stopping the flagellum stops the cell instantly
Blood in a capillaryL = 8 µm, v = 0.5 mm/s1.2 × 10⁻³Creeping flow: viscosity dominates completely, thousands of times below the pipe threshold
Honey in a 15 mm pipeL = 15 mm, v = 0.10 m/s (ρ ≈ 1 400 kg/m³, μ ≈ 10 Pa·s)0.21Laminar with room to spare — same pipe, same speed, ten thousand times the viscosity
Water trickling in a household pipeL = 15 mm, v = 0.15 m/s (about 1.6 L/min)2 240Laminar, just under the 2 300 pipe threshold — the one case where that number is the right one
Blood in the aorta, mean flowL = 25 mm, v = 0.40 m/s3 030Between 2 300 and 4 000, but the flow is pulsatile and the steady-pipe rule is a weak guide
Water in the same 15 mm household pipeL = 15 mm, v = 1.0 m/s (about 10.6 L/min)14 900Fully turbulent, well past 4 000 — an ordinary open tap is not a laminar flow
A person swimmingL = 2.0 m body length, v = 1.5 m/s3.0 × 10⁶External flow: the 5 × 10⁵ flat-plate figure is the relevant one, not 2 300
Air over a light-aircraft wingL = 1.5 m chord, v = 50 m/s4.9 × 10⁶Turbulent over most of the chord; L here is the chord, and saying so is part of the answer

Worked with our own calculator

Reynolds number calculator

Given

Flow geometry
Pipe / internal (laminar < 2300)
Flow velocity
1
Velocity unit
m/s
Characteristic length (pipe diameter)
25
Length unit
m
Fluid density (kg/m³)
499
Dynamic viscosity μ (cP)
0.501

Result

Reynolds number Re
24,900,200

These figures are produced by the calculator below, not typed in by hand — they are recomputed whenever the tool changes.

Run it on your own figures

Frequently asked questions

Is a high Reynolds number good or bad?
Neither — it is a description, not a score. A high Reynolds number means inertia dominates and the flow is likely turbulent, which raises friction losses in a pipe but improves mixing and heat transfer, and on a wing can delay separation and reduce drag. A low number means viscosity dominates and the flow is orderly and predictable, which is excellent for a lubricating film and useless for stirring a reactor. Ask what you want the flow to do before deciding which end of the scale is desirable.
Which length do I use for L?
The one the threshold you plan to compare against was defined with. Inside a circular pipe, use the internal diameter; for a non-circular duct, use the hydraulic diameter, four times the cross-sectional area divided by the wetted perimeter. Along a flat plate, use the distance from the leading edge, so Re grows as you move downstream. For a wing, use the chord; for a sphere or a cylinder in cross-flow, use the diameter; for a swimming body, the body length. The number is meaningless in isolation, so state L whenever you report Re.
What is the difference between dynamic and kinematic viscosity?
Dynamic viscosity μ measures a fluid's resistance to shear and is expressed in pascal-seconds; kinematic viscosity ν is that resistance divided by the density, ν = μ/ρ, and is expressed in square metres per second. Water at 20 °C has μ = 1.002 × 10⁻³ Pa·s and ν = 1.0038 × 10⁻⁶ m²/s; air at the same temperature has a far smaller μ, 1.825 × 10⁻⁵ Pa·s, yet a fifteen-times larger ν, 1.5158 × 10⁻⁵ m²/s, because air is so much less dense. Use Re = ρvL/μ with the first and Re = vL/ν with the second — both give the same answer, but mixing them gives an error of a factor of ρ.

Articles you may find interesting

All guides
ExplainerHow Buoyancy Works: Archimedes' Principle, and Why Ice Floats With 10.5 % Above WaterThe upward force equals the weight of the fluid pushed aside. That one sentence decides whether something floats, and if it floats, exactly how much of it stays under.ExplainerHow the Doppler Effect Works: The Formula, the Sign Convention, and Why Moving the Source Is Not the Same as Moving the ListenerFor sound, f' = f(v + v_o)/(v − v_s) — and getting the signs backwards is the classic error. Here is the convention spelled out, a 440 Hz source computed at four speeds, and why light needs a different equation entirely.ExplainerWhat Is Kinetic Energy? The KE = ½mv² Formula ExplainedKinetic energy is the energy of motion, given by KE = ½mv². Learn what the formula means, why speed matters most, and see worked examples in joules.ExplainerHooke's Law Explained: F = kx, Real Spring Constants, and Where It Stops HoldingHooke's law says force is proportional to stretch — but only below the elastic limit. Here is F = kx with worked numbers, what a 200 N/m spring actually feels like, and how springs combine.GuideThe Four Kinematics Equations: Which One to Use, and What Each One Leaves OutFive variables, four equations, and each equation is missing exactly one of them. Choose by looking at the variable the question never mentions.ExplainerProjectile Motion Explained: Range, Height, Flight Time — and Why 45° Is Not Always BestThree formulas cover the whole of projectile motion on level ground. The catch is level ground: the moment launch and landing heights differ, the 45° result stops being true.

Related tools

Sources

Spotted a mistake in this article?