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32 (
1
); 48-53
doi:
10.1016/j.jksus.2017.12.006

Exact solutions for a generalized Higgs equation

Department of Mathematics, Universidad Nacional de Colombia, Bogotá, Colombia
Disclaimer:
This article was originally published by Elsevier and was migrated to Scientific Scholar after the change of Publisher.

Peer review under responsibility of King Saud University.

Abstract

In this paper, the improved tanh-coth method is used for construct exact traveling wave solutions for a new coupled nonlinear system. Variable coefficients and a forcing term are considered. As particular case, new exact solutions for the classical Higgs field equation are obtained. The results show us the generation and evolutions of new traveling waves with several interesting structure, which can be used in physical applications. The method can be used to analyze a wide class of coupled nonlinear evolutions equations.

Keywords

Coupled Higgs equation
Traveling wave solutions
Improved tanh-coth method
Forcing term
35Q53
PubMed
1

1 Introduction

The coupled nonlinear partial differential equations have been subject of intense study in the recent years, due to the wide variety of applications in several branches of the physics. Since the soliton theory came into being in last century, the classification as well as the study of the different fields of applications of them are a relevant task for many researches today. In particular, the rich structures of the solitons systems is used for mathematicians to compare, in many cases, the numerical results obtained with the exact solutions and by physicists because the structure of the solutions can be help to them to understand in a better way the physical phenomenon that the model represent. In many cases, for instance in models of shallow water wave, the structure of the traveling wave solutions can be help to engineers to design structures in the coasts that can support certain type of waves. Due to complexity of the coupled nonlinear partial differential systems, does not exist a general theory for solving them, so that, a suitable ansatz methods are necessary. Some methods are design to obtain certain type of solutions, for instance the following: the Hirota bilinear method (Hirota, 1980), the inverse scattering transform method (Ablowitz and Clarkson, 1991), the Painlevé expansion method (Yan, 2004) and the Lie group Analysis method (Olver, 1980). However, in many other (computational) methods, the solutions of special ordinary differential equation is used. In this last class of methods, we can mentioned the following: The tanh method (Baldwin et al., 2004), the extended tanh method (Fan, 2000), the projective Riccati equation method (Conte and Musette, 1992), the generalized projective Riccati equation method (Yan, 2003), the Exp. function method (He and Wu, 2006), the tanh-coth method (Wazwaz, 2007), the Exp( - ϕ ( ξ ) ) method (Hafez et al., 2015; Hafez, 2016; Ali et al., 2016; Alam et al., 2015a,b; Hafez and Akbar, 2015), the improved tanh-coth method (Gomez S and Salas H, 2008), the extended trial equation method (Pandir, 2014; Bulut et al., 2014), He’s semi-inverse method and the G / G - expansion method (Jabbari et al., 2011). The main objective of this work is to use the improved tanh-coth method to obtain exact solutions for the following generalized model with variable coefficients and forcing term

(1.1)
u tt - u xx - δ ( t ) u + ρ ( t ) | u | 2 u - 2 uv = 0 , v tt + v xx - ρ ( t ) ( | u | 2 ) xx = G ( t ) , where u ( x , t ) , v ( x , t ) are the unknown function, δ ( t ) , ρ ( t ) , and G ( t ) functions depending only on variable t. In the case δ ( t ) > 0 , ρ ( t ) > 0 are arbitrary constant and G ( t ) = 0 , the classic coupled Higgs equation (Kumar et al., 2012; Tang and Xia, 2011)
(1.2)
u tt - u xx - δ u + ρ | u | 2 u - 2 uv = 0 , v tt + v xx - ρ ( | u | 2 ) xx = 0 .
is derived. The system given by (1.2) represents a nonlinear model with great interests in physic associated with the so called Higgs mechanism. It describes a system of conserved scalar nucleons interacting with neutral scalar mesons. However, in the case δ < 0 , ρ < 0 , the model is called the coupled nonlinear Klein–Gordon equation. Here, v ( x , t ) represent a complex scalar nucleon field and u ( x , t ) a real scalar meson field. The Hirota bilinear method (Hirota, 1980) have been used to show the existence of N-soliton solutions for (1.2) (Hu et al., 2003). In the same way, N-soliton solutions have obtained by the authors in Tajiri (2277). Now, in the case that δ ( t ) = 0 and ρ ( t ) = 1 , from (1.2) we have the following particular system
(1.3)
u tt - u xx + | u | 2 u - 2 uv = 0 , v tt + v xx - ( | u | 2 ) xx = 0 ,
studied by some authors. More exactly, traveling wave solutions for (1.3) have been derived in Hafez et al. (2015) and Manafian and Zamanpour (2013), using the Exp-function method and the Exp(- ϕ ( ξ ) ) method respectively.

The importance of the work with Eq. (1.1) can be described by the following reasons: First, is a generalized model from which new soliton solutions for (1.2) and (1.3) can be derived as particular cases. From of mathematical point of view this is a relevant fact. Second, the use of variable coefficients and forcing term, give us a variety of new traveling waves with several interesting structure that can may also be important of significance for the explanation of some practical physical problems. Third, the models with variable coefficients and forcing term, are an area of very interest for researches due to recent applications in physic, as can be seen in the works (Miura, 1968; Nirmala et al., 1986; Liu, 2012). The paper is organized as follows: in Section 2 we made a review of the improved tanh-coth method for solving systems; in Section 3 we obtain exact traveling wave solutions to (1.1) and as particular case, solutions to (1.2) and (1.3). Finally, we compare the method used here with the Exp( - ϕ ( ξ ) ) method used in Hafez et al. (2015) and the G / G -expansion method used by the authors in Kumar et al. (2012) and Jabbari et al. (2011).

2

2 The improved tanh-coth method

As we mentioned early, some methods use the solutions of special ordinary differential equation. This is the case of the improved tanh-coth method (Gomez S and Salas H, 2008) which can be described as follows: Given the system of nonlinear partial differential equations in the variables x and t

(2.1)
P ( u , v , u x , v x , u t , v t , u xt , v x , t , u xx , v xx , ) = 0 , Q ( u , v , u x , v x , u t , v t , u xt , v x , t , u xx , v xx , ) = 0 , where u and v are the unknowns, and the coefficients of the system are functions depending only of variable t, the transformation ξ = x + λ t + ξ 0 , converts it to a system of ordinary differential equations in the new unknowns u ( ξ ) , v ( ξ )
(2.2)
P 1 ( u , v , u , v , u , v , ) = 0 , Q 1 ( u , v , u , v , u , v , ) = 0 ,
where “′” denote the ordinary derivation respect to ξ , u ( ξ ) = du d ξ . The improved tanh-coth method use the following expansion
(2.3)
u ( ξ ) = i = 0 M a i ( t ) ϕ ( ξ ) i + i = M + 1 2 M a i ( t ) ϕ ( ξ ) M - i , w ( ξ ) = i = 0 N b i ( t ) ϕ ( ξ ) i + i = N + 1 2 N b i ( t ) ϕ ( ξ ) N - i ,
as solutions for (2.2), where M , N are a positive integer that will be determined later and ϕ = ϕ ( ξ ) satisfies the following Riccati equation
(2.4)
ϕ ( ξ ) = γ ϕ 2 ( ξ ) + β ϕ ( ξ ) + α .

Is well know that the general solution for (2.4) is given by Gomez S and Salas H (2010)

(2.5)
ϕ ( ξ ) = - β 2 - 4 α γ tanh 1 2 β 2 - 4 α γ ξ + ξ 0 - β 2 γ .

Clearly, varying the parameter ξ 0 in (2.5), we can obtain other type of solutions, and depending of the sign of β 2 - 4 α γ we can obtain, for instance, periodic solutions (Gomez S and Salas H, 2010). Substituting (2.3) into (2.2) and balancing the linear terms of highest order in the resulting equations with the highest order nonlinear term we obtain M , N . With the respective expressions and using (2.4) we obtain an algebraic system of equations in the variables α ( t ) , β ( t ) , γ ( t ) , λ ( t ) , a 0 ( t ) , , a 2 M , b 0 ( t ) , , b 2 N ( t ) . Solving it, and reversing the used transformations, we obtain exact solutions to (1.1) in the original variables.

3

3 Traveling wave solutions for (1.1)

First, we consider the transformation

(3.1)
u ( x , t ) = e ı ( x + rt ) u ( ξ ) , v ( x , t ) = v ( ξ ) + G ( t ) dt , ξ = x + λ t + ξ 0 .

By simplicity, we have used the same variables u and v. Substituting (3.1) into (1.1) and taking r = 1 λ , we have the following system

(3.2)
( λ ( t ) - 1 ) u ( ξ ) + 1 - 1 λ ( t ) 2 - δ ( t ) u ( ξ ) + ρ ( t ) u 3 ( ξ ) - 2 u ( ξ ) v ( ξ ) - 2 u ( ξ ) G ( t ) dt = 0 , ( λ ( t ) 2 + 1 ) v ( ξ ) - ρ ( t ) ( u ( ξ ) 2 ) = 0 .

Now, substitution of (2.3) into (3.2) and after balancing, we have 3 M = M + 2 in the first equation and N + 2 = 2 M + 2 in the second, so that M = 1 , N = 2 .

With this values, (2.3) reduces to

(3.3)
u ( ξ ) = a 0 ( t ) + a 1 ( t ) ϕ ( ξ ) + a 2 ( t ) ϕ ( ξ ) - 1 , v ( ξ ) = b 0 ( t ) + b 1 ( t ) ϕ ( ξ ) + b 2 ( t ) ϕ ( ξ ) 2 + b 3 ( t ) ϕ ( ξ ) - 1 + b 4 ( t ) ϕ ( ξ ) - 2 .

Now, substituting this last expressions into (3.2) we obtain an algebraic system in the variables α ( t ) , β ( t ) , γ ( t ) , λ ( t ) , a 0 ( t ) , a 1 ( t ) , a 2 ( t ) , b 0 ( t ) , b 1 ( t ) , b 2 ( t ) , b 3 ( t ) , b 4 ( t ) . For sake of simplicity, we omit here. Using the Mathematica we obtain the following solutions:

First case:

(3.4)
a 2 ( t ) = a 3 ( t ) = a 4 ( t ) = b 3 ( t ) = b 4 ( t ) = 0 , b 0 ( t ) = 1 2 ( - δ ( t ) - 2 ( G ( t ) dt ) + ρ ( t ) a 0 ( t ) 2 ) , b 1 ( t ) = ρ ( t ) a 0 ( t ) a 1 ( t ) , b 2 ( t ) = ρ ( t ) a 1 ( t ) 2 2 , λ ( t ) = ± 1 .

Reversing the respective transformations, respect to (3.4) we have the following solutions for (1.1)

(3.5)
u ( x , t ) = e ı ( x + t ) a 0 ( t ) + a 1 ( t ) - β 2 ( t ) - 4 α ( t ) γ ( t ) tanh [ 1 2 β 2 ( t ) - 4 α ( t ) γ ( t ) ξ ] - β ( t ) 2 γ ( t ) , v ( x , t ) = 1 2 - δ ( t ) - 2 G ( t ) dt + ρ ( t ) a 0 2 ( t ) + ρ ( t ) a 0 ( t ) a 1 ( t ) - β 2 ( t ) - 4 α ( t ) γ ( t ) tanh 1 2 β 2 ( t ) - 4 α ( t ) γ ( t ) ξ - β ( t ) 2 γ ( t ) + ρ ( t ) a 1 2 ( t ) 2 - β 2 ( t ) - 4 α ( t ) γ ( t ) tanh 1 2 β 2 ( t ) - 4 α ( t ) γ ( t ) ξ - β ( t ) 2 γ ( t ) 2 + G ( t ) dt , where ξ = x + t + ξ 0 , and α ( t ) , β ( t ) , γ ( t ) , a 0 ( t ) , a 1 ( t ) arbitrary functions depending only of the variable t. ξ 0 arbitrary constant.

Second case:

(3.6)
a 0 ( t ) = β ( t ) - 1 - λ 2 ( t ) 2 β ( t ) , a 2 ( t ) = a 3 ( t ) = a 4 ( t ) = b 3 ( t ) = b 4 ( t ) = 0 , b 0 ( t ) = - 2 + 2 λ 2 ( t ) - 2 δ ( t ) λ 2 ( t ) - 4 ( G ( t ) dt ) λ 2 ( t ) - β 2 ( t ) λ 4 ( t ) ± 2 2 β ( t ) α ( t ) λ 2 ( t ) a 1 ( t ) - 1 - λ 2 ( t ) 2 2 β ( t ) α ( t ) λ 4 ( t ) a 1 ( t ) - 1 - λ 2 ( t ) 4 λ 2 ( t ) , b 1 ( t ) = 2 β ( t ) β ( t ) a 1 ( t ) - 1 - λ 2 ( t ) , b 2 ( t ) = β ( t ) a 1 2 ( t ) 1 + λ 2 ( t ) , γ ( t ) = β ( t ) a 1 ( t ) 2 - 1 - λ 2 ( t ) .

With respect to this set of values, let

(3.7)
ϕ ( ξ ) = - β 2 ( t ) - 4 α ( t ) β ( t ) a 1 ( t ) 2 - 1 - λ 2 ( t ) tanh 1 2 β 2 ( t ) - 4 α ( t ) β ( t ) a 1 ( t ) 2 - 1 - λ 2 ( t ) ξ - β ( t ) 2 β ( t ) a 1 ( t ) 2 - 1 - λ 2 ( t ) .

Then, in this case, the respective solution for (1.1) is given by

(3.8)
u ( x , t ) = e ı ( x + 1 λ t ) β ( t ) - 1 - λ 2 ( t ) 2 β ( t ) + a 1 ( t ) ϕ ( ξ ) , v ( x , t ) = - 2 + 2 λ 2 ( t ) - 2 δ ( t ) λ 2 ( t ) - 4 ( G ( t ) dt ) λ 2 ( t ) - β 2 ( t ) λ 4 ( t ) ± 2 2 β ( t ) α ( t ) λ 2 ( t ) a 1 ( t ) - 1 - λ 2 ( t ) 2 2 β ( t ) α ( t ) λ 4 ( t ) a 1 ( t ) - 1 - λ 2 ( t ) 4 λ 2 ( t ) + 2 β ( t ) β ( t ) a 1 ( t ) - 1 - λ 2 ( t ) ϕ ( ξ ) + β ( t ) a 1 2 ( t ) 1 + λ 2 ( t ) ϕ 2 ( ξ ) + G ( t ) dt , where ϕ ( ξ ) is given by (3.7), ξ = x + λ ( t ) t + ξ 0 , a 1 ( t ) , λ ( t ) , β ( t ) and α ( t ) are arbitrary functions depending on t.

Third case:

(3.9)
a 1 ( t ) = a 2 ( t ) = a 4 ( t ) = b 2 ( t ) = b 2 ( t ) = 0 , b 0 ( t ) = 1 2 - δ ( t ) - 2 G ( t ) dt + ρ ( t ) a 0 ( t ) 2 , b 3 ( t ) = ρ ( t ) a 0 ( t ) a 3 ( t ) , b 4 ( t ) = ρ ( t ) a 3 ( t ) 2 2 , λ ( t ) = ± 1 .

With respect to (3.9) we have the following solutions for (1.1)

(3.10)
u ( x , t ) = e ı ( x ± t ) a 0 ( t ) + a 3 ( t ) - β 2 ( t ) - 4 α ( t ) γ ( t ) tanh 1 2 β 2 ( t ) - 4 α ( t ) γ ( t ) ξ - β ( t ) 2 γ ( t ) - 1 , v ( x , t ) = 1 2 - δ ( t ) - 2 ( G ( t ) dt ) + ρ ( t ) a 0 2 ( t ) + ρ ( t ) a 0 ( t ) a 3 ( t ) - β 2 ( t ) - 4 α ( t ) γ ( t ) tanh 1 2 β 2 ( t ) - 4 α ( t ) γ ( t ) ξ - β ( t ) 2 γ ( t ) - 1 + ρ ( t ) a 3 2 ( t ) 2 - β 2 ( t ) - 4 α ( t ) γ ( t ) tanh 1 2 β 2 ( t ) - 4 α ( t ) γ ( t ) ξ - β ( t ) 2 γ ( t ) - 2 + G ( t ) dt , where ξ = x ± t + ξ 0 , and α ( t ) , β ( t ) , γ ( t ) , a 0 ( t ) , a 3 ( t ) arbitrary functions depending only of the variable t. ξ 0 arbitrary constant. We can note that, the solution (3.10) is similar to (3.5) (with a 3 ( t ) instead of a 1 ( t ) and ϕ ( ξ ) - 1 instead of ϕ ( ξ ) ). In the same way, a similar solutions to (3.6) and (3.8) can be obtain, however for sake of simplicity we omit here.

4

4 On the solutions for (1.2) and (1.3)

Can be verified that taking G ( t ) = 0 in (3.5), (3.8) and (3.10) we obtain expressions that are solutions for (1.2). If furthermore, we take δ ( t ) = 0 and ρ ( t ) = 1 , solutions to (1.3) are obtained. The authors of Hafez et al. (2015), have derived solutions to (1.3) using the Exp(- ϕ ( ξ ) ) method. The ordinary differential equation used by them is Φ ( ξ ) = e - Φ ( ξ ) + μ e Φ ( ξ ) + λ , but with the substitution e Φ ( ξ ) we obtain the equation ϕ ( ξ ) = μ ϕ ( ξ ) 2 + λ ϕ ( ξ ) + 1 which is a particular case of (2.4). The expansion used by them is i = 0 N A i ( e - Φ ( ξ ) ) i , however, with Φ ( ξ ) = ln ϕ ( ξ ) , the last expression is clearly a particular case of (2.3).

On the other hand, the ordinary differential equation considered by the G ( ξ ) G ( ξ ) -expansion method used by the authors in Jabbari et al. (2011) and Kumar et al. (2012) can be reduced to particular case of (2.4), as well as, the expansion used for the solutions. More exactly, the equation used in this method is given by G ( ξ ) + λ G ( ξ ) + μ G ( ξ ) . The change of variable ϕ ( ξ ) = G ( ξ ) G ( ξ ) reduce it to ϕ ( ξ ) = - ϕ 2 ( ξ ) - λ ϕ ( ξ ) - μ which again, is a particular case of (2.4). In the same way, the expansion used by this method i = 0 m a i ( G ( ξ ) G ( ξ ) ) i reduces to a particular case of (2.3).

In the following graphs, we show the evolution of the traveling wave solutions for particular cases of the system (1.1), however, for sake of simplicity, we consider only the solutions given by (3.10). As we mentioned early, if we take δ ( t ) = 0 , G ( t ) = 0 and ρ ( t ) = 1 we obtain the system (1.3), so that substituting this values in (3.10), solutions for (1.3) are obtained. Fig. 1.

Solution for (1.3).
Fig. 1
Solution for (1.3).

Figures | u 1 | and v 1 , represent the evolution of the soliton solution corresponding to (1.3), with a 0 ( t ) = 1 , a 3 ( t ) = 1 , β ( t ) = 3 , α ( t ) = 1 , γ ( t ) = 1 , ( x , t ) [ - 10 , 10 ] × [ - 10 , 10 ] . In the same way, if we take G ( t ) = 0 in (3.10), we obtain solutions to (1.2).Fig. 2.

Solutions for (1.2).
Fig. 2
Solutions for (1.2).

Figures | u 2 | and v 2 , represent the evolution of the soliton solution corresponding to (1.2), with δ ( t ) = 1 , ρ ( t ) = 1 , a 0 ( t ) = 1 , a 3 ( t ) = 1 , β ( t ) = 3 , α ( t ) = 1 , γ ( t ) = 1 , ( x , t ) [ - 10 , 10 ] × [ - 10 , 10 ] .Fig. 3.

Solutions of (1.1).
Fig. 3
Solutions of (1.1).

Now, using (3.10) again, we can obtain the following figures, corresponding to solutions of (1.1) in the case that the coefficients are constants, but with a forcing term: Fig. 4.

Solutions to (1.1).
Fig. 4
Solutions to (1.1).

Figures | u 3 | and v 3 , represent the evolution of the soliton solution corresponding to (1.1), with δ ( t ) = 1 , ρ ( t ) = 1 , a 0 ( t ) = 1 , a 3 ( t ) = 1 , β ( t ) = 3 , α ( t ) = 1 , γ ( t ) = 1 , G ( t ) = sin t , ( x , t ) [ - 10 , 10 ] × [ - 10 , 10 ] .

Now, using variable coefficients and forcing term, we have the following figures:

Figures | u 4 | and v 4 , represent the evolution of the soliton solution corresponding to (1.1), corresponding to following values: δ ( t ) = t , ρ ( t ) = t 3 , a 0 ( t ) = 1 , a 3 ( t ) = 1 , β ( t ) = 3 , α ( t ) = 1 , γ ( t ) = 1 , G ( t ) = sin t , ( x , t ) [ - 10 , 10 ] × [ - 10 , 10 ] .

5

5 Conclusions

A new model with variable coefficients and forcing term have been studied from the point of view of it traveling wave solutions. Exact solutions for it have been derived by means of the improved tanh-coth method. As a consequence, new exact solutions for the classical Higgs Eq. (1.2), (1.3) have been obtained. We have showed that the used method here, is more general that the Exp - ( Φ ( ξ ) ) -method and that the G ( ξ ) G ( ξ ) -method used by several authors to handle (1.2) and (1.3). With the aim of make a comparison between the two models (variable coefficients and constants coefficients) we have made the graph of solutions in both cases. The solution are stable, at least, in the intervals considered for its graphs.

Acknowledgement

The author is grateful to referees for the helpful suggestions given with the aim to improve this paper.

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