What you are looking at
Steady, smooth (laminar) flow of a viscous fluid down a straight pipe, driven by a pressure difference ΔP
between the ends. The tracer dots move at the local fluid speed: quick along the axis, frozen against the
wall. Their envelope is the gold
velocity profile — and it is exactly a parabola.
Why a parabola
Viscosity means each cylindrical shell of fluid drags on its neighbour. Balancing the pressure force on a
cylinder of radius r against the viscous shear on its surface, and applying the
no-slip
condition (fluid touching the wall doesn't move), gives
v(r) = ΔP·(R² − r²) / (4ηL)
Speed peaks on the axis (r = 0) and falls to zero at r = R. The centre-line maximum and the cross-sectional
average are
vmax = ΔP·R² / 4ηL v̄ = vmax / 2
The fourth-power law
Integrate that parabola over the pipe's area and the total volume flow rate is the
Hagen–Poiseuille result:
Q = πΔP·R⁴ / 8ηL
The R⁴ is the headline. Widen a pipe by just 19% and you double its throughput; halve a radius and flow
collapses to one-sixteenth. This is why a modest narrowing of an artery sharply raises the pressure the
heart must supply, and why a slightly wider fire hose delivers vastly more water.
Staying laminar
Poiseuille's parabola only holds while the flow is orderly. The Reynolds number compares inertia to
viscosity:
Re = ρ·v̄·(2R) / η
Below roughly 2000 the flow is laminar and the formulas above are exact; push Re higher (wide pipe, thin
fluid, big ΔP) and the stream eventually turns turbulent, at which point flow rate grows much more slowly
than this ideal law predicts.
Things to try
Nudge the radius up and down and watch Q swing wildly while ΔP barely moves the profile's shape — R⁴ versus
linear. Crank the viscosity up to model blood or oil: the profile keeps its parabola but every speed drops
in proportion. Then raise ΔP with a thin fluid until Re climbs past 2000 and the readout warns that real
flow would break into turbulence.