Abstract

The improved Boussinesq equation is solved with classical finite element method using the most basic Lagrange element k = 1, which leads us to a second order nonlinear ordinary differential equations system in time; this can be solved by any standard accurate numerical method for example Runge-Kutta-Fehlberg. The technique is validated with a typical example and a fourth order convergence in space is confirmed; the 1- and 2-soliton solutions are used to simulate wave travel, wave splitting and interaction; solution blow up is described graphically. The computer symbolic system MathLab is quite used for numerical simulation in this paper; the known results in the bibliography are confirmed.

Highlights

  • The improved Boussinesq equation (IBq) was proposed in Bogolyubsky’s work [1], like a correct modification to solve the bad Boussinesq equation (BBq) which describes a large group of nonlinear dispersive wave phenomena, such as propagation of long waves on the surface of shallow water in both directions, propagation of ion-sound waves in a uniform isotropic plasma, and so on [2]

  • Bogolyubsky has shown that the BBq equation describes an unphysical instability of short wave lengths and the Cauchy problem for this partial differential equation is incorrect

  • Which is the IBq and will be the principal study equation of this paper; it is convenient for computer simulation of the dynamics of different nonlinear waves with weak dispersion; in our case the IBq equation will help to formulate the finite element discretization in the spatial direction with the primal L2-Galerkin finite element formulation [4] [5]; this due to the correction in the fourth order derivative term which leads us to the integral of a discontinuous function over a set of measure zero

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Summary

Introduction

The improved Boussinesq equation (IBq) was proposed in Bogolyubsky’s work [1], like a correct modification to solve the bad Boussinesq equation (BBq) which describes a large group of nonlinear dispersive wave phenomena, such as propagation of long waves on the surface of shallow water in both directions, propagation of ion-sound waves in a uniform isotropic plasma, and so on [2]. Which is the IBq and will be the principal study equation of this paper; it is convenient for computer simulation of the dynamics of different nonlinear waves with weak dispersion; in our case the IBq equation will help to formulate the finite element discretization in the spatial direction with the primal L2-Galerkin finite element formulation [4] [5]; this due to the correction in the fourth order derivative term which leads us to the integral of a discontinuous function over a set of measure zero (for the Lagrange finite element k = 1 ). Wave break up, inelastic and elastic head-on collision, and blow-up solution are modeled and graphics representations are done [14]

The Classical Finite Element Method
The Finite Element Computational Aspects
The Initial Value Problem
Numerical Examples
Conclusion
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