# Exact traveling wave solutions for system of nonlinear evolution equations

- Kamruzzaman Khan
^{1}Email author, - M. Ali Akbar
^{2}and - Ahmed H. Arnous
^{3}

**Received: **18 March 2015

**Accepted: **22 April 2016

**Published: **26 May 2016

## Abstract

In this work, recently deduced generalized Kudryashov method is applied to the variant Boussinesq equations, and the (2 + 1)-dimensional breaking soliton equations. As a result a range of qualitative explicit exact traveling wave solutions are deduced for these equations, which motivates us to develop, in the near future, a new approach to obtain unsteady solutions of autonomous nonlinear evolution equations those arise in mathematical physics and engineering fields. It is uncomplicated to extend this method to higher-order nonlinear evolution equations in mathematical physics. And it should be possible to apply the same method to nonlinear evolution equations having more general forms of nonlinearities by utilizing the traveling wave hypothesis.

### Keywords

Generalized Kudryashov method Nonlinear evolution equation Variant Boussinesq equation Breaking soliton equations Exact traveling wave solutions### Mathematics Subject Classification

35K99 35P05 35P99## Background

The study of autonomous nonlinear evolution equations has a rich and long history, which has continued to attract attention in more recent years. The exact solutions to nonlinear evolution equations are the key tool to understand the various physical phenomena that govern the real world today. Hence searching for exact traveling wave solutions to nonlinear evolution equations plays an important role in the study of nonlinear physical phenomena in many fields such as fluid dynamics, water wave mechanics, meteorology, electromagnetic theory, plasma physics and nonlinear optics.

In the past several decades, there has been significant progress in the development of various methods for finding exact traveling wave solutions to nonlinear evolution equations, such as the Bäcklund transformation (Wahlquist and Estabrook 1973; Luo 2011), the F-expansion method (Liu and Yang 2004; Islam et al. 2014), the tanh method (Wazwaz 2004), the exp-function method (Yusufoglu 2008; Khan and Akbar 2014a), the (G′/G)-expansion method (Wang et al. 2008; Zayed and Al-Joudi 2010; Kim and Sakthivel 2012; Khan and Akbar 2014b; Islam et al. 2013), the functional variable method (Zerarka et al. 2010; Khan and Akbar 2014c; Zayed et al. 2013a), the exp(−Φ(ξ))-expansion method (Khan and Akbar 2014d, 2015), the modified simple equation method (Jawad et al. 2010; Khan and Akbar 2013, 2014e; Ahmed et al. 2013), the homotopy perturbation method (Mohiud-Din 2007; Mohyud-Din and Noor 2009), the Kudryashov method (Kudryashov 2012; Lee and Sakthivel 2013), and the Riccati equation mapping method (Zayed and Arnous 2013a, b).

The aim of this work is to demonstrate the efficiency of the generalized Kudryashov method for finding exact traveling wave solutions transmutable to the solitary wave solutions for system of nonlinear evolution equations. For this purpose, we consider the one dimensional variant Boussinesq equations, and the (2 + 1)-dimensional breaking soliton equations.

## Algorithm of the generalized Kudryashov method

*x*and

*t*:

The main steps of generalized Kudryashov method are as follows (Demiray et al. 2014a, b; Baskonus and Bulut 2015):

###
**Step 1:**

Equation (2) may be successively integrated as many times as possible. Remaining to the boundary conditions \( u(\xi ) \to 0 \) and \( \frac{{d^{m} u(\xi )}}{{d\xi^{m} }} \to 0\,(m = 1,\,2,\,3,\, \ldots ) \) for \( \xi \to \pm \infty \), \( \xi = x - \omega \,t \), the constants of integration, if any, should be set to zero (Malfliet and Hereman 1996; Wazwaz 2009).

###
**Step 2:**

*A*is a constant of integration.

###
**Step 3:**

*N*and

*M*appearing in Eq. (3) can be determined by considering the homogeneous balance between the highest order derivatives and the nonlinear terms come out in Eq. (1) or Eq. (2). Moreover precisely, we define the degree of \( u(\xi ) \) as \( D(u(\xi )) = N - M \) which gives rise to the degree of other expression as follows:

Therefore, we can find the value of *N* and *M* in Eq. (3).

###
**Step 4:**

Substituting Eqs. (3) and (4) into Eq. (2), we obtain a polynomial in \( Q^{i - j} \), (\( i,j = 0,\,1,\,2, \ldots \)). In this polynomial equating the coefficients of all terms of the same powers of *Q* to zero, we obtain a system of algebraic equations which can be solved by using Maple or Mathematica to get the unknown parameters \( a_{i} (i = 0,\,1,\,2, \ldots ,N) \), \( b_{j} (j = 0,\,1,\,2, \ldots ,M) \), and \( \omega \). Consequently, we obtain the exact solutions of Eq. (1).

## Applications

In this section, we will apply the generalized Kudryashov method to construct the exact traveling wave solutions transmutable to the solitary wave solutions for the following two nonlinear evolution equations:

###
*Example 1. The variant Boussinesq equations:*

*ξ*, choosing the constant of integration as zero (under the boundary conditions described in “Algorithm of the generalized Kudryashov method” section (Step 1) and using similar boundary conditions for H(ξ)), we obtain the following ordinary differential equations respectively:

Now balancing the highest order derivative \( u^{{\prime \prime }} \) and nonlinear term \( u^{3} \), we get \( 3N - 3M = N - M + 2 \) or equivalent to \( N = M + 1 \).

###
*Remark*

*H*(

*x,t*) must be a non-negative and real physical quantity. Solutions (17)–(22) of the variant Boussinesq equations are significant both mathematically and physically for their positive sign for

*H*(

*x, t*). Besides solutions (15) and (23) are valid mathematically and physically for their positive and negative signs for

*u*(

*x, t*) but their corresponding solutions (16) and (24) are valid only mathematically. Solutions (25) and (26) are complex solutions, therefore although they are logically true but they have no physical significance (Figs. 1, 2).

We can obtain some traveling wave solutions since A is an arbitrary constant of integration, for example.

*A*= 1 into Eqs. (19) and (20) and considering

*u*(

*x*,

*t*) > 0 as well as a wave moving to the right, i.e., in the positive direction of

*x*-axis, we obtain

###
*Example 2: The (2* *+* *1)-dimensional breaking soliton equations*:

Considering the homogeneous balance between \( u^{{\prime \prime }} \) and \( u^{2} \) in Eq. (34), we obtain \( N = M + 2 \).

### Comparisons

- 1.
Khan and Akbar (2013) studied the variant Boussinesq equations by means of the modified simple equation method and found only four solutions (see “Appendix 1”). On the other hand, by using the generalized Kudryashov method we have found twelve solutions. Moreover, if we put

*A*= 1 into our solutions Eqs. (19) and (20), then these solutions coincide with the solutions (42) and (44) obtained by Khan and Akbar (2013) for the value of \( \omega = - 1 \) and \( \omega = 1 \) (see “Appendix 1”). Similarly, if we put A = −1, then our solutions Eqs. (19) and (20) coincide with the solutions (43) and (45) for the values of \( \omega = - 1 \) and \( \omega = 1 \) obtained by Khan and Akbar (2013).

- 2.
Zayed et al. (2013b) investigated exact traveling wave solutions to the (2 + 1)-dimensional breaking soliton equation by means of the functional variable method and found only one solution (see “Appendix 2”). On the other hand, by using the generalized Kudryashov method we found four solutions from which one of our solutions coincides with the solution of Zayed et al. If we set \( c = \alpha \) into the solution (46) (see “Appendix 2”) obtained by Zayed et al. (2013b), then our solution (41) coincides with that solution.

From the above discussion, we conclude that the generalized Kudryashov method is a more reliable technique, in principle, than the modified simple equation method and the functional variable method.

## Conclusions

In this article, we have successfully presented a mathematical tool named the generalized Kudryashov method for finding exact traveling wave solutions to the variant Boussinesq equations, and the (2 + 1)-dimensional breaking soliton equations. The obtained results will serve as a very important milestone in the study of plasma physics and water waves phenomena. We also have demonstrated that the generalized Kudryashov method is an effective tool for obtaining exact analytical solutions for large classes of system of nonlinear evolution equations.

## Declarations

### Authors’ contributions

This work was carried out in collaboration among the authors. KK, MAA and AHA have a good contribution to design the study, and to perform the analysis of this research work. All authors read and approved the final manuscript.

### Acknowledgements

Authors are thankful to the respected reviewers for their valuable suggestions to improve the quality of this article. Authors would like to thank to Professor Dr. Abdul-Majid Wazwaz, Department of Mathematics, Saint Xavier University, Chicago, IL 60655, USA, who has expanded his helping hands for developing this article. Besides no study sponsor is involved with this work.

### Competing interests

The authors declare that they have no competing interests.

**Open Access**This article is distributed under the terms of the Creative Commons Attribution 4.0 International License (http://creativecommons.org/licenses/by/4.0/), which permits unrestricted use, distribution, and reproduction in any medium, provided you give appropriate credit to the original author(s) and the source, provide a link to the Creative Commons license, and indicate if changes were made.

## Authors’ Affiliations

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