Laminar/Turbulent Flow

Flow is smooth (laminar) or chaotic (turbulent) depending on the Reynolds number. Learn Re, transition, velocity profiles, boundary layers and why turbulence matters for mixing, heat transfer and pressure loss.

Watch smoke rising from a candle: it starts as a smooth thread (laminar) and then breaks into swirls (turbulent). The same transition happens in pipes, over wings and around cars, and it changes friction, heat transfer and noise dramatically.

One dimensionless number, the Reynolds number, predicts which regime you're in.

An analogy

Laminar flow is a disciplined marching band in neat lanes; turbulent flow is a crowd rushing out of a stadium — the same average direction but constant mixing and jostling.

Inertia vs viscosity

Re compares inertial forces (which amplify disturbances) with viscous forces (which damp them). Low Re (slow, small, viscous) = laminar; high Re = turbulent. Most engineering water and air flows are turbulent.

Velocity profiles

Laminar pipe flow has a parabolic profile; turbulent flow is much flatter in the core with steep gradients near the wall — which is why turbulent flow has higher wall friction and heat transfer.

Boundary layers

Near any surface a thin layer slows to zero velocity at the wall (no-slip). On a flat plate it transitions at Re_x ≈ 5 × 10⁵. Adverse pressure gradients can make it separate, causing stall on wings and drag behind bluff bodies.

Modelling turbulence

Turbulence contains eddies from the pipe size down to the Kolmogorov scale. Direct simulation (DNS) is extremely costly, so engineering CFD uses RANS models (k-ε, k-ω SST) or LES. Dimples on golf balls deliberately trip turbulence to delay separation and cut drag.

Formulas

Worked example: Water in a pipe

Given: V = 1 m/s, D = 50 mm; ρ = 998, μ = 1.0 × 10⁻³ Pa·s

Find: Reynolds number and regime.

Answer: Re ≈ 5 × 10⁴ (turbulent)

Worked example: Oil in a hydraulic line

Given: V = 0.5 m/s, D = 25 mm; ν = 1 × 10⁻⁴ m²/s

Find: Regime.

Answer: Laminar

Common mistakes

Applications

Key takeaways

Going further