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Original Articles

Application of the Exp (−φ(ζ))-expansion method for solitary wave solutions

, , , ORCID Icon, &
Pages 376-384 | Received 26 Aug 2018, Accepted 29 Jun 2019, Published online: 16 Jul 2019

Abstract

The solution of nonlinear mathematical models has much importance and in soliton theory its worth has increased. In present article, a research has been conducted of Caudrey-Dodd-Gibbon and Pochhammer-Chree (PC) equations, to discuss physics of these equations and to attain soliton solutions. Exp (φ(ζ))-expansion technique is used to construct solitary wave solutions. Wave transformation is applied to convert problem in the form of ordinary differential equation. The drawn-out novel type outcomes play an essential role in the transportation of energy. It is noticed that under the study, the approach is extremely dependable and it may be prolonged to further mathematical models signified mostly in nonlinear differential equations.

1. Introduction

Recently solitary wave theory got some great improvements. Soliton wave occurrence enticed a number of researchers for its comprehensive applications in engineering and mathematical physics. First, J S Russell (by profession an engineer) contemplated on the solitary wave in 1834. In the form of differential equations, various physical occurrences in nature are modelled. The scientists made big efforts to get solution of such differential equations. To get soliton solutions, different attempts have been made by scientists. Modeling of various physical, biochemical and biological occurrences are in forms of nonlinear PDEs. The vigorous attainment is the headway for exact soliton solutions of mathematically modelled differential equations. Different mathematical techniques are developed. For the observation of physical activities of problem, exact solutions are vital. We have more applications and ability to examine the number of properties of mathematical model by utilizing the exact solution.

NLE equations play a very vital part in innumerable engineering and scientific arenas, such as, the heat flow, quantum mechanics, solid state physics, chemical kinematics, fluid mechanics, optical fibres, plasma physics, the wave proliferation phenomena, proliferation of shallow water waves, etc.

Therefore, different techniques for finding exact solutions are used for a diversified field of partial differential equations like, homogenious balance technique for example (Wang, Citation1995; Zayed et al., Citation2004), Hirota’s bilinear approach (Hirota, Citation1973; Hirota & Satsuma, Citation1981), Auxiliary equivalence technique (Sirendaoreji, Citation2004), Trial task technique (Inc & Evans, Citation2004), Jacobi elliptic task system (Ali, Citation2011), Tanh-function technique (Abdou, Citation2007), and method of sine-cosine (Wazwaz, Citation2004), truncated Painleve expansion technique (Weiss et al., Citation1983), variational iteration method (VIM) (Abbasbandy, Citation2007), Exp-function technique (He & Wu, Citation2006; Akbar & Ali, Citation2012), (G/G)-expansion approach (Wang et al., Citation2008; Akbar et al., Citation2012; Zayed, Citation2010; Zayed & Gepreel, Citation2009; Shehata, Citation2010; Zhang et al., Citation2010), Exact soliton solution (Khan & Akbar, Citation2013; Liping et al., Citation2009; Zhang et al., Citation2013). Several theoretical and experimental works for solitons includes (Wang et al., Citation2017; Dai et al., Citation2018; Wang et al., Citation2016; Wang et al., Citation2018; Ding et al., Citation2017). On exact solution, some novel results and computational methods involved to travelling-wave transformation, see the references (Yang, Citation2016; Yang et al., Citation2016, Citation2017; Saad et al., Citation2017; Yang & Feng, Citation2017; Feng et al., Citation2017). Some recent studies on exact soliton solutions are (Hu & Li, Citation2018; Islam et al., Citation2017; Kaplan & Akbulut, Citation2018; Zayed & Al-Nowehy, Citation2017).

In this paper, our basic motive is to discuss physics of nonlinear CDG and PC equation, and also to obtain soliton like solutions of these equation through a much authentic and productive method that is notable in literature as exp (φ(ζ))-expansion technique. The analytical results are very stimulated. From the technique, the solution procedure is quite simple, clear and all types of NLEEs are easily expanded. This technique simply emphasises to obtain the solution of PDE that is indicated in the kind of polynomial in exp (φ(ζ)), and (φ(ζ)) must satisfies the ODE. (1.1)   φ(ζ)=exp(φ(ζ))+μexp(φ(ζ))+λ.(1.1)

We know ζ=x+y+zωt.

By homogenous principle, the degree of polynomial is obtained. We accomplish a set of algebraic equation by balancing the highest order derivative with nonlinear terms. The article is divided in to various segments. In the next segment, we study analysis of method to obtain the soliton waves solution. The third segment is appropriate to discuss physics of nonlinear equations and for application of exp (φ(ζ))-expansion method. In the last section, we drew some conclusions by discussing the results.

2. Analysis of method

In general, nonlinear partial differential equation (NPDE) can be written as: (2.1) Fη,ηx,ηy,ηz,ηxx,ηxy,ηxz,=0.(2.1)

Where ηx,y,z,t is to be unknown, F is the polynomial in η(x,y,z,t) and different derivatives of η(x,y,z,t) involving nonlinear terms and highest order differential. Using Exp (φ(ζ))-expansion method, we follow steps given below in detail,

Step1: Invoking a wave transformation: (2.2) ζ=x+y+zωt.(2.2)

Here ω represent wave speed. Applying wave transformation into Equationequation (2.1) we got an ODE: (2.3) G(η,η,η,η,)=0.(2.3)

In Equation(2.3), derivative w.r.t ζ are symbolized by prime. If it is needed, integrate Equationequation (2.3) and set constant of integration equal to zero.

Step 2: Solution of Equationequation (2.3) is expressed in the form of a polynomial in exp (φ(ζ)) as: (2.4) η(ζ)=an(exp(φ(ζ)))n+an1(exp(φ(ζ)))n1+,(2.4)

In the Equationequation (2.4) an,an1, are the arbitrary constants which are to be evaluated such that an0. Also φ(ζ) satisfies Equationequation (1.1).

Step 3: In this step, we calculate value of n by using homogeneous balance principle.

Case 1:

For λ24μ>0 and μ0, (2.5) φ(ζ)=ln{12μ(λ24μtanh(λ24μ2(ζ+c1))λ)}.(2.5)

Where c1 is constant of integration.

Case 2:

For λ24μ<0 and μ0, (2.6) φ(ζ)=ln{12μ(λ+4μλ2(4μλ22(ζ+c1)))}.(2.6)

Case 3:

For λ0 and μ=0, (2.7) φ(ζ)=ln{λ(exp(λ(ζ+c1))1)}.(2.7)

Case 4:

For λ24μ=0 and μ0, λ0, (2.8) φ(ζ)=ln{2(λ(ζ+c1))+2λ2(ζ+c1)}.(2.8)

Case 5:

For λ=0 and μ=0, (2.9) φ(ζ)=ln(ζ+c1).(2.9)

Step 4: In this step, we insert polynomial given in Equation(2.4) into ODE Equation(2.3) and then use Equationequation (1.1). The left-hand side of nonlinear ODE is converted in the form of a polynomial in Exp-(φ(ζ)). We put each coefficient of polynomial equal to zero, results in attain a set of algebraic equations for an,,ω,λ and μ.

Step 5: In this step, with the help of symbolic computation software like Maple 18, the values of the constants an,, ω,λ,μ are computed. Replacing values of these constants into Equationequation (2.4), we obtain soliton wave solutions.

3. Applications of method

This section is divided into two sub sections. Both Caudrey-Dodd-Gibbon (CDG) and Pochhammer-Chree (PC) equations are studied physically, then exp (φ(ζ))-expansion technique is applied to attain solitary wave solutions of these nonlinear differential equations. The attained results are quite efficient and motivating.

3.1. Solution of Caudrey-Dodd-Gibbon Equation

The general form of the fifth order KdV equation is written as: (3.1) ηt+αηxxxxx+σηηxxx+γηxηxx+δη2ηx=0.(3.1)

In above equation α,σ,γ and δ are arbitrary real parameters. By setting α=1,σ=β,γ=β and δ=15β2 we obtain, (3.2) ηt+15β2η2ηx+βηxηxx+βηηxxx+ηxxxxx=0.(3.2)

Which is known as CDG equation. This equation describes the evolution of quasi one-dimensional shallow water waves when it affects the surface tension; and the viscosity are negligible. Shallow water waves are produced when depth of water is less than one half of the wavelength of wave. Their speed is independent of their wavelength too. It depends, however, on the depth of the water. Shallow water waves show no dispersion.

Introducing a transformation as ζ=x+y+zωt. (3.3) ωη+15β2η2η+βηη+βηη+η(v)=0.(3.3)

On integrating we have, (3.4) Aωη+115β2η3+βηη+η(iv)=0.(3.4)

Here A is the constant of integration and prime symbolizes the derivative w.r.t. ζ. Now for value of n, we balance the highest order linear term with the highest order non-linear term of Equationequation (3.4). We attain n=2. So Equationequation (2.4) reduces to: (3.5) η(ζ)=a0+a1eφ(ζ)+(eφ(ζ))2.(3.5)

Here a0 and a1, a2 are the constants which are to be calculated.

By making use of Equation(3.5) into Equation(3.4), we transformed the left-hand side into a polynomial in eφ(ζ). We put each coefficient of this polynomial equal to zero and attain a set of algebraic equations for a0,a1,a2,λ,μ,A and ω as follow: ωa1+15β2a2a1+22a1μλ2+120a2μ2λ+30a2λ3μ+6βa0a2μλ+βa0a1λ2+2βaa1μ+2βa1a2μ2+βa12μλ+16a1μ2+a1λ4=0. 15β2a02a2+15β2a12a0+2βa12μ+60a1μλ+232a2λ2μ+2βa22μ2+βa12λ2+7βa1a2μλ+8βa0a2μ+3βa0a1λ+4βa0a2λ2+136a2μ2+16a2λ4ωa2+15a1λ3=0. 440a2μλ+2βa0a1+3βa12λ+25β2a0a1a2+10βa1a2μ+6βa22μλ+10βa0a2λ+5βa1a2λ2+115β2a13+40a1μ+130a2λ3+50a1λ2=0. 15β2a0a22+15β2a12a2+8βa22μ+6βa0a2+4βa22λ2+13βa1a2λ+240a2μ+330a2λ2+2βa12+60a1λ=0. 15β2a1a22+8βa1a2+10βa22λ+336a2λ+24a1=0. 6βa22+115β2a23+120a2=0. Aωa0+115β2a03+a1μλ3+8a1μ2λ+14a2μ2λ2+16a2μ3+βa0a1μλ+2βa0a2μ2=0.

With the help of symbolic computation software like Maple 18 algebraic equations are solved. Finally, we obtain the following solution set:

1st Solution Set:

Consider the solution set of the form ω=15β2a02+βa0λ2+22μλ2+76μ2+λ4+8βa0μ, a0=a0, a1=30λβ, a2=30β, A=115β2β3a03+15β2a02λ2+780a0λ2μβ+2040a0μ2β+15βa0λ4+120β2a02μ+450μλ4+9900μ2λ2+7200μ3.

By using above values into Equationequation (3.5), we obtain: (3.6) η=βa0+30eφ(ζ)λ+30e2φ(ζ)β.(3.6)

Where ζ=x+y+zωt.

Inserting the solutions of Equation(1.1) in Equation(3.6), we attain five cases of soliton wave solutions for CDG equation.

Case 1:

When λ24μ>0 and μ0, we attain solution, (3.7) η11=1ββa0(60μλ)λ24μtanh12λ24μζ+c1λ (120μ2)λ24μtanh12λ24μζ+c1λ2 .(3.7)

Case 2:

When λ24μ<0 and μ0, then we have, (3.8) η12=1ββa0(60μλ)λ2+4μtan12λ2+4μζ+c1λ (120μ2)λ2+4μtanh12λ2+4μζ+c1λ2 .(3.8)

Case 3:

When μ=0 and λ0, we attain, (3.9) η13=1ββa030λ2expλζ+c1130λ2expλζ+c112.(3.9)

Case 4:

When λ24μ=0, μ=0 and λ0, (3.10) η14=1ββa0+30λ3ζ+c14+2ζ2c1λ+30λ4ζ+c124+2ζ2c1λ2.(3.10)

Case 5:

When μ=0 and λ=0, we attain the solution as, (3.11) η15=1ββa030e2lnζ+c1.(3.11)

Where ζ=x(15β2a02+βa0λ2+22μλ2+76μ2+λ4+8βa0μ)t.

2nd Solution Set:

Consider the solution set of the form: ω=λ48μλ2+16μ2, a0=5λ2+8μβ, a1=60λβ, (3.12) a2=60β, A=103βλ648μ2λ2+64μ3+12μλ4μ.(3.12)

Using values given in Equationequation (3.12) into Equationequation (3.5), we obtain (3.13) η=5λ2+8μ+12eφ(ζ) λ+12e2φ(ζ)β.(3.13)

Where ζ=x+y+zωt.

Replacing the solutions of Equationequation (1.1) into equation Equation(3.13), we get five cases of soliton wave solutions for the Caudrey-Dodd-Gibbon (CDG) equation:

Case 1:

When λ24μ>0 and μ0, we attain solution, (3.14) η21= 1β5λ240μ120μλλ24μtanh12λ24μζ+c1λ  240μ2λ24μtanh12λ24μζ+c1λ2 .(3.14)

Case 2:

When λ24μ<0 and μ0, we attain the solution, (3.15) η22=1β5λ240μ120μλλ2+4μtan12λ2+4μζ+c1λ  (240μ2)λ2+4μtanh12λ2+4μζ+c1λ2 .(3.15)

Case 3:

When μ=0 and λ0, we obtain the solution, (3.16) η23=1β5λ260λ2expλζ+c1160λ2expλζ+c112.(3.16)

Case 4:

When λ24μ=0, μ=0 and λ0, we have the solution, (3.17) η24=1β5λ2+8μ+12λ3ζ+c14+2ζ2c1λ+12λ4ζ+c124+2ζ2c1λ2.(3.17)

Case 5:

When μ=0 and λ=0, we attain the solution, (3.18) η25=60βζ+c12 .(3.18)

Here ς=x(λ48μλ2+16μ2)t

3.2. Solution of Pochhammer-Chree Equation

The generalized Pochhammer-Chree (PC) equation is given by, ηttηttxxaηbηn+1γη2n+1xx=0.

Taking n = 2, we have, ηttηttxxaηbη3γη5xx=0.

Where a,b and γ are arbitrary non-zero constants, while the exponent n>1 is the power law nonlinearity parameter. This equation represents a nonlinear model of longitudinal wave propagation of elastic rods. Longitudinal waves are waves in which the displacement of the medium is in the same direction as, or the opposite direction to, the direction of propagation of the wave. Longitudinal waves include sound waves and particle velocity propagated in an elastic medium.

Let us consider  γ=0, the above equation becomes, (3.19) ηttηttxxaηbη3xx=0.(3.19)

Introducing a transformation as ξ=x+y+zωt Equationequation (3.19) can be converted to an ordinary differential equation. ω2ηω2η″″aη+6bηη2+3bη2η=0.

Integrating twice, we have, (3.20) A+Bξ+ω2ηaη+bη3ω2η=0.(3.20)

Here A and B are the constants of integration and prime symbolizes the derivative w.r.t. ζ. Now for value of n, we balance the highest order linear term with the highest order non-linear term of Equationequation (3.20). We attain n=1. So Equationequation (2.4) reduces to, (3.21) η(ζ)=a0+a1eφ(ζ).(3.21)

Here a0 and a1 are the constants which are to be calculated.

By making use of Equation(3.21) into Equation(3.20), we transformed the left-hand side into a polynomial in eφ(ζ). We put each coefficient of this polynomial equal to zero, and attain a set of algebraic equations for a0,a1,a2,λ,μ,A,B and ω as follow: a1ω2aa1+3ba02a12a1ω2μa1ω2λ2=0. 3ba12α03a1ω2λ=0. ba132a1ω2=0. A+Bζ+a0ω2aa0+ba03a1ω2μλ=0.

After solving these algebraic equations with the help of computer software like Maple 18, we obtain the solution set: (3.22) ω=42λ2+8μa2λ2+4μ,A=Bζ,B=B,a0=aλb2λ2+4μ,a1=2 b2λ2+4μab2λ2+4μ(3.22)

By using Equation(3.22) in Equation(3.21), we obtain, (3.23) η=λ+2eφ(ζ)ab2λ2+4μa .(3.23)

Where ζ=x+y+zωt.

Relieving the solutions of Equation(1.1) into Equationequation (3.23), we get five cases of travelling wave solutions for the PC Equationequation (3.19).

Case 1:

When λ24μ>0 and μ0, we attain the soliton wave solution, (3.24) η1=1b2λ2+4μaλ+4μλ24μtanh12λ24μζ+c1λa.(3.24)

Case 2:

When λ24μ<0 and μ0, we attain solution, (3.25) η2=1b2λ2+4μaλ+4μλ24μtan12λ2+4μζ+c1λa.(3.25)

Case 3:

When μ=0 and λ0, we attain, (3.26) η3=ab2+λ2aλ+2λexpλ ζ+c11.(3.26)

Case 4:

When λ24μ=0, μ=0 and λ0, we attain, (3.27) η4=2λab2λ2+4μaλ ζ+c1+2.(3.27)

Case 5:

When μ=0 and λ=0, we attain the travelling wave solution, (3.28) η5=a2ζ+c1ba.(3.28)

Here ζ=x+42λ2+8μa2λ2+4μt.

4. Discussion on results

The construction of soliton waves by solving nonlinear Caudrey-Dodd-Gibbon (CDG) and Pochhammer-Chree (PC) equations have been examined via an analytical technique, Exp (φ(ζ))-expansion method. The findings are mentioned and discussed as under:

Solitary waves arise due to indirect balance of nonlinear effects with the dispersive effects. From the above graphs, we are able to judge that soliton is a wave which preserves its shape after it strikes with another wave of the similar kind. The waves produced by linear description tend to experience dispersion and create localized disturbance to spread. The solitary waves can intuitively be anticipated to be the outcome of two effects of steepening and spreading with marginally nonlinear amplitude. The waves of various types of wave-number, there speeds and amplitude as they rely upon the process of dispersion being generated without changing their actual shapes. We have observed that media go under strong dispersion process and can generate high amplitude waves and oppositely weak dispersive media generate such waves of small amplitude.

We attain the desired solution through rational functions. The hyperbolic and trigonometric function travelling wave solutions of nonlinear Caudrey-Dodd-Gibbon equation are represented in and respectively for different values of physical parameters. and show soliton solutions for various physical parameters through exponential and rational functions. shows rational function solution for different values of λ, μ  and c1. In these graphical results, it is taken β=30. By changing the values of physical and additional free parameters, the velocity and amplitude of solitary waves are controlled. It is observed that the displacement potential η becomes sharp at leading and trailing edges. Amplitude is proportional to the velocity of propagation also taller solitary waves are thinner and move faster.

Figure 1. Represents 3 D plot for λ=0.2, μ=1, c1=2, a0=1,30x30, 0t5.

Figure 1. Represents 3 D plot for λ=0.2, μ=1, c1=2, a0=1,−30≤x≤30, 0≤t≤5.

Figure 2. Represents 3 D plot for λ=0.2, μ=1, c1=2, a0=1,30x30, 0t5.

Figure 2. Represents 3 D plot for λ=0.2, μ=1, c1=2, a0=1,−30≤x≤30, 0≤t≤5.

Figure 3. Signifies 3 D plot for λ=1, μ=1, c1=0.1, a0=2,30x30, 0t4.

Figure 3. Signifies 3 D plot for λ=1, μ=−1, c1=0.1, a0=2,−30≤x≤30, 0≤t≤4.

Figure 4. Signifies 3 D plot for λ=1, μ=1, c1=0.1, a0=2,30x30,0t4.

Figure 4. Signifies 3 D plot for λ=1, μ=−1, c1=0.1, a0=2,−30≤x≤30,0≤t≤4.

Figure 5. Shows 3 D plot for λ=1, μ=2, c1=1,30x30,0t5.

Figure 5. Shows 3 D plot for λ=−1, μ=2, c1=1,−30≤x≤30,0≤t≤5.

Next, and show hyperbolic and trigonometric function travelling wave solutions of Pochhammer-Chree (PC) equation respectively by setting suitable values of physical parameters which control the solitary wave amplitude. Also, and show exponential and rational function solutions respectively. shows rational function solution for different values of a,c1 and b. The solitary wave moves toward right if the velocity is positive and left directions if the velocity is negative, and the amplitudes and velocities are controlled by various physical parameters. Solitary waves show more complicated behaviours which are controlled by various physical and additional free parameters. Figures indicate graphical solutions for altered values of physical parameters. Arbitrary functions can be affected by the solitary wave solution. It is concluded that various constraint can be selected as an input to our simulation. Solitary waves for various values of physical and additional free parameters are being pointed out by the graphic illustration. From above discussed graphical cases it has been observed that solution of soliton waves does not rely completely upon the additional free parameters. The soliton waves of different types are clearly described by the graphic outcomes.

Figure 6. Represents 3 D plot for λ=1, μ=2, c1=0.1,a=3,b=1,30x30, 0t5.

Figure 6. Represents 3 D plot for λ=−1, μ=2, c1=0.1,a=3,b=1,−30≤x≤30, 0≤t≤5.

Figure 7. Represents 3 D plot for λ=1, μ=2, c1=0.1,a=3,b=1,30x30, 0t5.

Figure 7. Represents 3 D plot for λ=−1, μ=2, c1=0.1,a=3,b=1,−30≤x≤30, 0≤t≤5.

Figure 8. Signifies 3 D plot for λ=1, μ=2, a=0.1,c1=1,b=3,30x30, 0t4.

Figure 8. Signifies 3 D plot for λ=1, μ=2, a=0.1,c1=1,b=3,−30≤x≤30, 0≤t≤4.

Figure 9. Signifies 3 D plot for λ=1, μ=2,a=0.1, c1=1,b=3,30x30, 0t4.

Figure 9. Signifies 3 D plot for λ=1, μ=2,a=0.1, c1=1,b=3,−30≤x≤30, 0≤t≤4.

Figure 10. Shows 3 D plot for a=0.1, b=1, c1=2,30x30,0t4.

Figure 10. Shows 3 D plot for a=0.1, b=1, c1=2,−30≤x≤30,0≤t≤4.

5. Conclusion

In this paper, the main focus is to find, test and analyze the new travelling wave solutions and physical properties of nonlinear Caudrey-Dodd-Gibbon (CDG) and Pochhammer-Chree (PC) equations by applying reliable mathematical technique. It is noted that soliton type solution is allowed by the under study nonlinear differential equation. The applied algorithm is helpful to verify the results that are acquired by the exact solution. The closeness among the outcome discloses that for solving differential equation it behaves like a powerful tool. CDG and PC equations have very important part in solitary wave’s theory as it opens up the various natures of soliton wave solution, and to handgrip these equations we use an expansion technique as a tool which is proper and authentic. The conclusion is very clear to check the physical behaviour of solitary waves, we use valuable way under study method. The method has been applied directly without requiring linearization, discretization or perturbation. The obtained results demonstrate the reliability of the algorithm and give it a wider applicability to nonlinear differential equations. Although using Maple software it permits us more solution sets, less computational work and less computer memory.

Disclosure statement

No potential conflict of interest was reported by the authors.

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