Contact Line Catch Up by Growing Ice Crystals
arXiv:2110.14299 · doi:10.1103/PhysRevLett.128.254501
Abstract
The effect of freezing on contact line motion is a scientific challenge in the understanding of the solidification of capillary flows. In this letter, we experimentally investigate the spreading and freezing of a water droplet on a cold substrate. We demonstrate that solidification stops the spreading because the ice crystals catch up with the advancing contact line. Indeed, we observe the formation and growth of ice crystals along the substrate during the drop spreading, and show that their velocity equals the contact line velocity when the drop stops. Modelling the growth of the crystals, we predict the shape of the crystal front and show that the substrate thermal properties play a major role on the frozen drop radius
arXiv commentPhysical Review Letters, 22 juin 2022
References in corpus (8)
- Initial spreading of low-viscosity drops on partially wetting surfaces
- Solidification dynamic of an impacted drop
- Fast-freezing kinetics inside a droplet impacting on a cold surface
- Solidification of liquid metal drops during impact
- Freezing-damped impact of a water drop
- A criterion for the pinning and depinning of an advancing contact line on a cold substrate
- Freezing a rivulet
- Solidification of a rivulet: shape and temperature fields
Cited by in corpus (5)
- Enhanced bubble growth near an advancing solidification front
- The macroscopic contact angle of water on ice
- Flat-cupped transition in freezing drop impacts
- Vertical-supercooling-controlled interfacial instability for a spreading liquid film
- Marangoni-driven freezing dynamics of supercooled binary droplets