The Last Spin
A coin spun on a table eventually comes to rest. In the final moments, the coin tilts nearly flat, its edge tracing a rapid circle, the frequency of the rattling increasing until it stops. The sound accelerates. The visual blur intensifies. Then silence.
The idealized model — a rigid disk on a frictionless surface — predicts a finite-time singularity. The angular velocity diverges to infinity at a definite time. The disk reaches infinite speed and then stops. The singularity is mathematical, clean, and physically impossible.
What prevents it? The dominant dissipation mechanism has been debated for decades. Rolling friction, sliding friction, air resistance — each has been proposed, each has supporters, and the answer matters because it determines the scaling law that governs the disk's final moments.
The authors use high-speed stereoscopic imaging to track disks of different masses, sizes, and shapes on different surfaces. They vary the air pressure. They change the geometry. They measure the scaling exponents.
The answer is air. In the final phase, as the disk tilts nearly flat against the surface, a thin layer of air is trapped and sheared between the disk and the table. The viscous drag from this boundary layer dominates all other dissipation. The evidence is clean: reducing air pressure extends the spinning time. Changing disk mass has a specific scaling consistent with air drag. The surface material barely matters.
Earlier in the motion, rolling friction dominates, and its scaling with mass is sublinear — suggesting adhesion-based resistance rather than the linear dependence that simple models assume. Two dissipation mechanisms, two regimes, one crossover as the disk approaches its end.
The singularity is prevented by a film of air thinner than a hair. The infinite spin is killed by the thing the disk barely touches.
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