Coarsening of Vortex Ripples in Sand

Abstract

The coarsening of an array of vortex ripples prepared in an unstable state is discussed within the framework of a simple mass transfer model first introduced by K.H. Andersen et al. [Phys. Rev. E 63, 066308 (2001)]. Two scenarios for the selection of the final pattern are identified. When the initial state is homogeneous with uniform random perturbations, a unique final state is reached which depends only on the shape of the interaction function f (λ). A potential formulation of the dynamics suggests that the final wavelength is determined by a Maxwell construction applied to f (λ), but comparison with numerical simulations shows that this yields only an upper bound. In contrast, the evolution from a perfectly homogeneous state with a localized perturbation proceeds through the propagation of wavelength doubling fronts. The front speed can be predicted by standard marginal stability theory. In this case the final wavelength depends on the initial wavelength in a complicated manner which involves multiplication by factors of 2 and rational ratios such as 4/3.Unsüberfüllts. Wir ordnens. Es zerfällt. Wir ordnens wieder und zerfallen selbst.

About classical solutions for high order conserved Kuramoto-Sivashinsky type equation

“…x u = 0. (5) From a physical point of view, Equation ( 5) is deduced in [1,22,21,30,46,48,51] to model the amplitude and long-range interactions in underwater sand ripples in one dimension.…”