Soliton-mean field interaction in Korteweg-de Vries dispersive hydrodynamics

TL;DR

This paper investigates how solitons interact with large-scale waves in the Korteweg-de Vries equation, analyzing transmission and trapping phenomena through multiple analytical methods and numerical validation.

Contribution

It introduces a comprehensive analytical framework combining perturbation theory, Whitham modulation, and inverse scattering to describe soliton-mean field interactions in dispersive hydrodynamics.

Findings

Transmitted solitons experience phase shifts consistent with asymptotic analysis.

Trapped solitons lack proper eigenvalues, indicating no true soliton solution.

Analytical approaches agree with numerical simulations across interaction regimes.

Abstract

The propagation of localized solitons in the presence of large-scale waves is a fundamental problem, both physically and mathematically, with applications in fluid dynamics, nonlinear optics and condensed matter physics. Here, the evolution of a soliton as it interacts with a rarefaction wave or a dispersive shock wave, examples of slowly varying and rapidly oscillating dispersive mean fields, for the Korteweg-de Vries equation is studied. Step boundary conditions give rise to either a rarefaction wave (step up) or a dispersive shock wave (step down). When a soliton interacts with one of these mean fields, it can either transmit through (tunnel) or become embedded (trapped) inside, depending on its initial amplitude and position. A comprehensive review of three separate analytical approaches is undertaken to describe these interactions. First, a basic soliton perturbation theory is introduced that is found to capture the solution dynamics for soliton-rarefaction wave interaction in the small dispersion limit. Next, multiphase Whitham modulation theory and its finite-gap description are used to describe soliton-rarefaction wave and soliton-dispersive shock wave interactions. Lastly, a spectral description and an exact solution of the initial value problem is obtained through the Inverse Scattering Transform. For transmitted solitons, far-field asymptotics reveal the soliton phase shift through either type of wave mentioned above. In the trapped case, there is no proper eigenvalue in the spectral description, implying that the evolution does not involve a proper soliton solution. These approaches are consistent, agree with direct numerical simulation, and accurately describe different aspects of solitary wave-mean field interaction