Frost propagation on breath figures
Event details
| Date | 13.11.2024 |
| Hour | 14:00 › 15:00 |
| Speaker | David Paulovics |
| Location | |
| Category | Conferences - Seminars |
| Event Language | English |
Abstract :
The formation of frost on surfaces is ubiquitous in cold and humid environments. The various mechanisms that take place during frost formation are still under active scrutiny, both from a fundamental point of view and for their applications to frost control.
Breath figures form by dropwise condensation on surfaces colder than the dew temperature. Frost propagates through breath figures by means of the solidification of droplets and the formation of inter-droplet ice bridges. We take a novel experimental approach using infrared microscopy to follow the propagation of the frosted area. Starting from a first nucleation event, a frost front propagates radially at a constant speed for a given experiment. The droplet size distribution was varied systematically and we found that the front speed is a non-monotonous function of droplet size with a maximum speed of 70 micrometer per second, for a characteristic drop radius of 300 micrometers.
The dynamics are governed by three timescales: the freezing time of individual droplets, their cooling time, and the inter-droplet bridge formation time. We present a mean-field model that without any free parameters is in very good agreement with both experimental and numerical data.
The formation of frost on surfaces is ubiquitous in cold and humid environments. The various mechanisms that take place during frost formation are still under active scrutiny, both from a fundamental point of view and for their applications to frost control.
Breath figures form by dropwise condensation on surfaces colder than the dew temperature. Frost propagates through breath figures by means of the solidification of droplets and the formation of inter-droplet ice bridges. We take a novel experimental approach using infrared microscopy to follow the propagation of the frosted area. Starting from a first nucleation event, a frost front propagates radially at a constant speed for a given experiment. The droplet size distribution was varied systematically and we found that the front speed is a non-monotonous function of droplet size with a maximum speed of 70 micrometer per second, for a characteristic drop radius of 300 micrometers.
The dynamics are governed by three timescales: the freezing time of individual droplets, their cooling time, and the inter-droplet bridge formation time. We present a mean-field model that without any free parameters is in very good agreement with both experimental and numerical data.
Practical information
- General public
- Free
Organizer
Contact
- Prof. François Gallaire