Model for self-organized Leidenfrost rotating polygons as cnoidal waves
A. S. Carstea, A. Ludu
TL;DR
The study tackles the formation of self-organized rotating polygonal patterns in shallow Leidenfrost rings by deriving a nonlinear contour evolution equation for the inner free surface under the Euler equations in a Boussinesq shallow-convection regime. The model incorporates a rolling poloidal vortex and detailed capillary pressure via mean curvature, yielding $cn$-type cnoidal wave solutions in a co-rotating frame, and also presents a reduced KdV-type description through pressure averaging. Two complementary routes are used: a full nonlinear equation that fits experimental polygons (4–8 edges) and a KdV-like reduced model that explains both standard and peaked polygons, with exact and approximate cnoidal-wave forms. Experimental data from liquid nitrogen Leidenfrost rings validate the theoretical predictions, showing good agreement and revealing the crucial roles of rolling vortices and surface tension, while identifying avenues for 3D thermo-convective extensions and stability analyses.
Abstract
The remarkable appearance of self-organized regular and peaked polygonal rotating patterns in shallow Leidenfrost rings is investigated as a balance between surface tension geometry and nonlinear terms of Euler equation. Using the Boussinesq shallow convection approximation and a specialized expansion of the Laplace equation solutions, we derive a nonlinear equation that can be integrated in terms of elliptic functions. The model rigorously accounts for surface tension, the contribution of the poloidal rolling vortex, and the interplay between buoyancy-driven and thermocapillary flows. We obtain cnoidal waves solutions describing the dynamics of the inner free surface of the Leidenfrost ring, to predict polygonal patterns in liquid nitrogen. These predictions are compared with experimental observations.Additionally, we introduce a simplified model based on poloidal averaging of the capillary pressure, leading to a Korteweg-de Vries-type equation. This simplified model not only reproduces the cnoidal wave solutions but also predicts new trigonometric solutions, offering insights into the formation of peaked polygons.
