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3.2  Savart–Plateau–Rayleigh instability of a water column

Author
Stéphane Popinet
Command
gerris3D -m plateau.gfs | gfsview-batch3D
Version
100529
Required files
plateau.gfs (view) (download)
plateau.gfv white.gfv closeup.gfv
Running time
2 hours

As observed by Félix Savart and Joseph Plateau, and confirmed theoretically by Lord Rayleigh, a column of liquid spontaneously breaks up into droplets under the influence of surface tension. An example of this process is given in the animation of Figure 13 for a column of water in air. The solution is computed using a 3D Volume-Of-Fluid (VOF) representation of the interface. The interface in Figure 13 is represented using the VOF-reconstructed fragments. This explains the narrow gaps which can sometimes be seen between fragments in the animation.


Figure 13: Evolving interface for a Savart–Plateau–Rayleigh instability.

Adaptivity is used to track the regions with high curvature which are created during breakup. The evolution of spatial resolution along the interface is illustrated in Figure 14 where the resolution doubles for each change in colour. A detail of the adaptive mesh close to the point of breakup is shown in Figure 15.


Figure 14: Evolving interface coloured according to the local spatial resolution.


Figure 15: Detail of the interface reconnection.

For this particular example, using adaptivity leads to orders-of-magnitude gains compared to an equivalent simulation on a regular Cartesian mesh (Figure 16).


Figure 16: Total number of grid points as a function of time. A regular Cartesian grid with an equivalent maximum spatial resolution would require 230≈ one billion grid points.

A more detailed study of these simulations is given in Popinet (2009), Journal of Computational Physics, 228.


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