Atomisation — where it appears
Named by 3 essays across one field — each of them below, with the objects they name alongside it.
Where a jet stops being a jet
A tap makes drops a few centimetres down, a garden hose makes a stream that carries, a sprayer makes a mist and a diesel injector makes fog. Same liquid, same mechanism, four regimes — and the number that separates them is not the jet's inertia but the surrounding air's.
Viscosity lets a jet break, later and into bigger drops
A thread of honey falls for metres before it breaks, and a thread of water for centimetres, which suggests that viscosity holds a jet together. It does not: it cannot stop any ripple longer than the jet's circumference from growing. It slows them, the short ones most, so the ripple that wins is longer, it takes the viscous time rather than the capillary one to win, and each drop it makes is bigger. The wavelength grows as the square root of the Ohnesorge number and the drop as its sixth root.
The air shortens a jet's fastest ripple, and the drops follow
A jet in a vacuum breaks into drops nearly twice its own width, whatever its speed. A jet in air does not, and the reason is a pressure the air puts on its surface: flowing over a rippled jet it is faster over the crests and its pressure lower there, which pulls them further out. That pull lets ripples shorter than the jet's circumference grow, shortens the fastest one, shrinks the drops, and puts a ceiling on how long a fast jet can be — at the gas Weber number where the measured break-up regimes change.
Named alongside it
The objects these essays reach for when they reach for this one.
InstabilityModel limitSurface tensionDropOhnesorge numberRegimeWeber numberCorrelationDimensionlessDispersion relationGrowth rateJet