Splash crown formation from a falling drop
When a drop or stone hits a liquid surface fast enough, why does the splash form a crown of regularly-spaced spikes, and how does the crown height depend on impact speed and drop size?
History and references
Partly settled. Some of it is understood, some is still argued about.
Kapitza's problem #65 in the 1966 collection asks students to explain how a splash forms and how splash height scales with impact velocity and stone/drop size, in the spirit of Worthington's 1877 photographic studies of splashes. High-speed imaging (Edgerton's famous 'milk-drop coronet' photos) made the crown-and-spike geometry iconic well before it was theoretically understood. Since the 1990s-2000s, groups led by Zaleski, Thoroddsen, Deegan and others identified air-film entrapment and Rayleigh-Taylor-type rim instabilities as key mechanisms, but a fully predictive theory linking impact parameters to spike number and crown height is still incomplete, especially for thin films and low-viscosity regimes.
A puddle splash looks chaotic yet organizes itself into an almost perfectly periodic crown of spikes, and nobody has a complete first-principles formula for how many spikes appear.
Explanations that circulated
- The splash is caused simply by the drop pushing liquid outward like a solid piston (ignores the trapped-air / thin-film instability mechanisms now known to matter)
- Crown finger number is set only by the Weber number (shown insufficient; film thickness and viscosity also matter)
References
- Experimental investigation of splash and crown formation during single drop impact on wetted surfaces, C. Josserand, S. Zaleski et al. (various groups), Experiments in Fluids, 2003
- Crown-forming instability phenomena in the drop splash problem, Krechetnikov & Homsy (and related groups), Journal of Colloid and Interface Science, 2009
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