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When a viscous fluid flows steadily through a straight pipe far from the inlet, the velocity varies across the cross-section in a pattern determined by the Reynolds number. At low Reynolds numbers (Re < ∼2300) the flow is laminar: fluid moves in orderly concentric layers described by the Poiseuille equation, giving a parabolic velocity profile with maximum speed at the centreline and zero at the wall (no-slip condition).
Above Re ≈ 2300 the flow enters a transitional regime and above ∼4000 becomes fully turbulent. Turbulent eddies mix momentum vigorously across the cross-section, producing a much flatter profile well approximated by the 1/7 power law: u(r)/umax ≈ (1−r/R)1/7. Use the Compare view to see both profiles side-by-side for the same mean velocity.
The difference matters enormously in engineering: laminar flow gives exactly twice the pressure drop for the same mean velocity (Hagen-Poiseuille), turbulent flow transfers heat and mass far more efficiently, and the transition determines mixing quality in chemical reactors and heat exchangers.