Long time behavior of solutions to the generalized Boussinesq equation
Amin Esfahani, Gulcin M. Muslu
TL;DR
The paper analyzes the Cauchy problem for the generalized Boussinesq equation $u_{tt} = {(u - \alpha u_{xx} + u_{tt} - \kappa u_{xxtt} + f(u))}_{xx}$ arising in surface-tension–driven water waves, addressing long-time behavior via a multi-space well-posedness theory, decay estimates, and solitary-wave analysis. It develops local well-posedness in Sobolev, Bessel potential, and modulation spaces, derives linear decay and dispersive bounds, and establishes asymptotic decay in various norms. The study proves nonexistence of solitary waves for several parameter regimes using Pohozaev identities, and simultaneously constructs solitary waves numerically with the Petviashvili iteration, complemented by a Fourier pseudo-spectral time-evolution scheme. Numerical experiments illuminate gap-interval dynamics between global existence and blow-up, revealing threshold amplitudes that separate global persistence from finite-time blow-up and demonstrating how higher-order dispersion and nonlinearity shape long-time behavior.
Abstract
In this paper, we study the generalized Boussinesq equation as a model for the water wave problem with surface tension. Initially, we investigate the initial value problem within Sobolev spaces, deriving conditions under which solutions are either global or experience blow-up in time. Subsequently, we extend our analysis to Bessel potential and modulation spaces, determining the asymptotic behavior of solutions. We establish the non-existence of solitary waves for certain parameters using Pohozaev-type identities. Additionally, we numerically generate solitary wave solutions of the generalized Boussinesq equation through the Petviashvili iteration method. To further examine the time evolution of solutions, we propose employing the Fourier pseudo-spectral numerical method. Our investigation extends to the gap interval, where neither global existence nor blow-up results have been theoretically established. We find that our numerical results effectively fill these gaps, supplementing the theoretical findings.
