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Research Article

A new study of soliton solutions for the variable coefficients Caudrey–Dodd–Gibbon equation

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Pages 763-773 | Received 30 Mar 2022, Accepted 19 Aug 2022, Published online: 06 Sep 2022

Abstract

We present a paper on the different methods for finding solutions to the Caudrey–Dodd–Gibbon equation with variable coefficients, which has wide applications in quantum mechanics and nonlinear optics. We have studied the equation analytically by using the unified method and the modified Kudryashov method. With the aid of symbolic computation and several types of auxiliary equations, we have obtained soliton solutions and other solutions. Then, we assign different values to the parameters, generating two-dimensional and three-dimensional graphics of the solutions, and discuss the interaction of several groups of solion solutions to form periodic wave solutions and kink solitary wave solutions.

1. Introduction

Nonlinear partial differential equations play a crucial role in the study of physical phenomena. Through symbolic calculation, we cannot only discover the properties of nonlinear partial differential equations [Citation1–3], but also get the exact solutions about them. Therefore, solving partial differential equations is a significant research subject. With the rapid development of the scientific society, there have been some methods proposed to deal with the nonlinear partial differential equations. For example, a history approach [Citation4], the fixed point technique [Citation5], the new method [Citation6], the modified (G/G)-expansion method [Citation7,Citation8], the novel generalized (G/G) -expansion technique [Citation9], the modified Kudryashov method [Citation10–13], the extended simplest equation [Citation14–16], the homotopy analysis transform method [Citation17] and the united method [Citation18] and so on.

In this paper, we will deal with the Caudrey–Dodd–Gibbon equation with variable coefficients (vcCDG) using the unified method and the modified Kudryashov method of the above methods. Up to now, Mickle methods are applied to Equation (Equation1) as yet, such as Hirota's bilinear method [Citation19] is used to obtain some breather wave and lumps solutions to the CDG equation, the exp-function method [Citation20] and the (G/G)-expansion method [Citation21] find generalized solitary solutions and exact solutions respectively, the invariance properties, optimal system and group invariant solutions are investigated in [Citation22], the approximate solutions are obtained by the variational iteration method [Citation23], and the improved generalized Riccati equation mapping method [Citation24] figures out exact solutions. Nevertheless, the unified method and the modified Kudryashov method have not been applied to the equation.

In fact, it has been shown that some known methods (the (G/G)-expansion method, the F-expansion method, the exp-function method and the rational expansion method and others) are special cases of the united method, which was established in 2012. The emergence of the unified method has solved a great many of equation problems, such as, the thermophoretic motion equation [Citation25], the coupled Burgers equations [Citation26], the Zakharov-Kuznetsov equation [Citation27], the Benjamin–Bona–Mahony–Peregrine equation [Citation28] and the generalized (2 + 1)-dimensional Boussinesq equation [Citation29]. Moreover, the modified Kudryashov method is also an important method for solving partial differential equation problems, the generalized Schrödinger–Boussinesq equations [Citation10], the Klein–Gordon equations [Citation11], the Benjamin–Bona–Mahony–Peregrine equation [Citation28] and the KdV–KZK equation [Citation30] are all solved by the modified Kudryashov method.

Here, the vcCDG equation [Citation31,Citation32] reads, (1) ut+σ1(t)uxuxx+σ2(t)uuxxx+σ3(t)u2ux+σ4(t)uxxxxx=0,(1) where u=u(x,t), uuxxx and uxxxxx are dispersive terms, σi(t) (i = 1, 2, 3, 4) are functions with t. As one of the fifth-order KdV, it can also describe the nonlinear phenomena in fluids or plasmas and is completely integrable [Citation32]. Compared with existing articles, breather wave and lumps solutions, solitary solutions, exact solutions, group invariant solutions, and approximate solutions have been obtained [Citation19–24]. Our primary mission is committed to using the unified method and the modified Kudryashov method to look for polynomial solutions, rational function solutions and travelling wave solutions so as to get more relevant properties of the equation. Some significant examples are given below.

When σ1(t)=σ2(t)=α,σ3(t)=α25,σ4(t)=1 [Citation33], (2) ut+αuxuxx+αuuxxx+α25u2ux+uxxxxx=0,(2) is completely integrable and has soliton solutions.

When σ1(t)=σ2(t)=30,σ3(t)=180,σ4(t)=1 [Citation34], (3) ut+30uxuxx+30uuxxx+180u2ux+uxxxxx=0,(3) are used to model nonlinear dispersive waves such as laser optics and plasma physics.

The remaining sections of this paper are textured in what follows. In Section 2, we use the unified method to receive the solutions of Equation (Equation1) and draw graphs for analysis. In Section 3, we are devoted to the utilization of the modified Kudryashov method to the vcCDG equation. Finally, conclusions will be given in Section 4.

2. The unified method

In view of the operation steps of the method, the following hypothesis is framed: (4) u=U(ξ1,ξ2),ξ1=α1x+α2t,ξ2=β1x+β2t,(4) where α1, α2, β1 and β2 are arbitrary constants. With the above travelling wave transformation, Equation (Equation1) becomes the following differential equation: (5) σ1(t)(U1α1+U2β1)α12U11+2σ1(t)(U1α1+U2β1)α1β1U12+σ1(t)(U1α1+U2β1)β12U22+σ2(t)Uα13U111+3σ2(t)Uα12β1U112+3σ2(t)Uα1β12U122+3σ2(t)Uβ13U222+α15U11111σ4(t)+5σ4(t)α14β1U11112+10σ4(t)α13β12U11122+10σ4(t)α12β13U11222+5σ4(t)α1β14U12222+U1α2+U2β2+σ3(t)(U1α1+U2β1)U2+σ4(t)β15U22222=0,(5) where U1=dUdξ1 and U2=dUdξ2.

For the given vcCDG equation with two independent variables ξ1, ξ2 and dependent variable U, the solutions of Equation (Equation5) are written (6) U(ξ1,ξ2)=p0(t)+i+j=1npi,j(t)ϕ1i(ξ1)ϕ2j(ξ2),(ϕ1(ξ1))p=r=0pkbr(t)ϕ1r(ξ1),(ϕ2(ξ2))p=r=0pkcr(t)ϕ2r(ξ2),p=1,2,(6) where pi,j(t), br(t) and cr(t) are functions that contain t. Then, by balancing condition, we need to balance U11111 and UU111 in Equation (Equation5), then we have n=2(k1), k=2,3,.

Next, we will use the unified method to find the travelling wave solutions of Equation (Equation5) in the case of n=2.

2.1. The solitary solutions

In this instance, the solutions of Equation (Equation5) are (7) U(ξ1,ξ2)=p0(t)+p1,0(t)ϕ1(ξ1)+p0,1(t)ϕ2(ξ2)+p1,1(t)ϕ1(ξ1)ϕ2(ξ2)+p2,0(t)ϕ12(ξ1)+p0,2(t)ϕ22(ξ2),(7) (8) ϕ1(ξ1)=b0(t)+b1(t)ϕ1(ξ1)+b2(t)ϕ12(ξ1),ϕ2(ξ2)=c0(t)+c1(t)ϕ2(ξ2)+c2(t)ϕ22(ξ2).(8) By taking Equations (Equation7) and (Equation8) into Equation (Equation5), we can set the coefficients of ϕj(ξj) to 0. Through symbolic computation, and making all the coefficients of ϕj(ξj)(j=1,2) equal to zero, we get (9) p1,1(t)=0,σ1(t)=σ2(t),p2,0(t)=3α1b22(t)α22Rσ2(t),p0,2(t)=120β12c22(t)α280Rσ2(t)α1,p1,0(t)=3α1b2(t)b1(t)α22Rσ2(t),p0,1(t)=3β12c2(t)c1(t)α22Rσ2(t)α1,σ3(t)=4Rσ22(t)α1α2,p0(t)=α2(c12(t)β12+8β12c0(t)c2(t)+8α12b0(t)b2(t)+α12b12(t))8Rα1σ2(t),σ4(t)=α220Rα1,(9) where R=b02(t)b22(t)α145+b0(t)b2(t)b12(t)α1410b14(t)α1480+(c0(t)c2(t)c12(t)4)2β14.We can easily work out the solutions of Equation (Equation8) are (10) ϕ1(ξ1)=b1(t)+(b12(t)4b2(t)b0(t))tanh(12(b12(t)4b2(t)b0(t))ξ1)2b2(t),ϕ2(ξ2)=c1(t)+(c12(t)4c2(t)c0(t))tanh(12(c12(t)4c2(t)c0(t))ξ2)2c2(t),(10) where b12(t)4b2(t)b0(t)>0 and c12(t)4c2(t)c0(t)>0. Then, by taking Equations (Equation9) and (Equation10) into Equations (Equation7) and (Equation8), we can receive (11) u1(x,t)=30α2cosh2(ξ2R12)(b14(t)α145β14R1216b12(t)b0(t)b2(t)α142+α14b02(t)b22(t))σ2(t)α1cosh2(2ξ1R2)×(((b14(t)α1216(b0(t)b2(t)+112)α12b12(t)2+b02(t)b22(t)α12+α12b0(t)b2(t)6+R1(R123)β1216)×cosh2(ξ2R12)β12R1216)cosh2(2ξ1R2)cosh2(ξ2R12)α12R22(b0(t)b2(t)+112)α12b12(t)2),(11) where β2=(5b02(t)b22(t)α14+5b0(t)b2(t)b12(t)α1425b14(t)α1416+(c0(t)c2(t)c12(t)4)2β14)β1α25Rα1,ξ1=α1x+α2t, ξ2=β1x+β2t, R1=c12(t)4c2(t)c0(t) and R2=b12(t)4+b2(t)b0(t).

Given the parameters of travelling wave solutions in Equation (Equation11), α1=1, α2=1, β1=1, σ2(t)=1, c0(t)=1, c1(t)=12+sin(t), c2(t)=1, b0(t)=1, b1(t)=1 and b2(t)=12, we can obtain Figure . (a) and (b) illustrate the interaction between two-soliton waves with two different velocities. And they converge into one wave at the origin and gradually split into two waves, which travel in the other direction. Moreover, we can see that except x=0 and near the origin, the values of other solutions are all greater than zero in (c). Similarly, in (d), except t=0 and near the origin, the values of other solutions are all greater than zero.

Figure 1. The solitary wave solution obtained from Equation (Equation7) with α1=1, α2=1, β1=1, σ2(t)=1, c0(t)=1, c1(t)=12+sin(t), c2(t)=1, b0(t)=1, b1(t)=1 and b2(t)=12. (a) of 3D-plot; (b) of contour plot; (c) of u-t plot; (d) of u-x plot.

Figure 1. The solitary wave solution obtained from Equation (Equation7(7) U(ξ1,ξ2)=p0(t)+p1,0(t)ϕ1(ξ1)+p0,1(t)ϕ2(ξ2)+p1,1(t)ϕ1(ξ1)ϕ2(ξ2)+p2,0(t)ϕ12(ξ1)+p0,2(t)ϕ22(ξ2),(7) ) with α1=1, α2=1, β1=−1, σ2(t)=1, c0(t)=−1, c1(t)=12+sin⁡(t), c2(t)=1, b0(t)=1, b1(t)=1 and b2(t)=−12. (a) of 3D-plot; (b) of contour plot; (c) of u-t plot; (d) of u-x plot.

2.2. The soliton solutions

In order to solve Equation (Equation5), the structure of solutions is hypothesized (12) U(ξ1,ξ2)=p0(t)+p1,0(t)ϕ1(ξ1)+p0,1(t)ϕ2(ξ2)+p1,1(t)ϕ1(ξ1)ϕ2(ξ2)+p2,0(t)ϕ12(ξ1)+p0,2(t)ϕ22(ξ2),(12) (13) ϕ1(ξ1)=ϕ1(ξ1)b0(t)+b1(t)ϕ1(ξ1)+b2(t)ϕ12(ξ1),ϕ2(ξ2)=ϕ2(ξ2)c0(t)+c1(t)ϕ2(ξ2)+c2(t)ϕ22(ξ2).(13) Substituting Equations (Equation12) and (Equation13) into Equation (Equation5), and gathering the power of ϕ1(ξ1) and ϕ2(ξ2), we have the following results: (14) p1,1(t)=0,σ1(t)=σ2(t),p2,0(t)=30α12β2b12(t)b0(t)σ2(t)β1S,c2(t)=c12(t)4c0(t),p0,2(t)=30β1β2c12(t)c0(t)σ2(t)S,p1,0(t)=60α12β2b1(t)σ2(t)β1S,p0,1(t)=60β1β2c1(t)σ2(t)S,σ3(t)=σ22(t)β1S20β2,b2(t)=b12(t)4b0(t),p0(t)=10β2(β12c0(t)+α12b0(t))σ2(t)β1S,σ4(t)=4β2β1S,(14) where S=β14c02(t)5α14b02(t).

The solutions of auxiliary equations ϕ1(ξ1) and ϕ2(ξ2) in Equation (Equation13) are (15) ϕ1(ξ1)=b0(t)b1(t)(sech(b0(t)2ξ1))2b12(t)b0(t)b2(t)(1tanh(b0(t)2ξ1))2,ϕ2(ξ2)=c0(t)c1(t)(sech(c0(t)2ξ2))2c12(t)c0(t)c2(t)(1tanh(c0(t)2ξ2))2,(15) where b0(t)>0 and c0(t)>0. Advancing, as usual, we are able to have the solution of Equation (Equation1), (16) u2(x,t)=640α2(8S34+8S33S4+S4S3+1)(8S14+8S13S2+4S2S1+1)α1(5c02(t)β14b02(t)α14)σ2(t)×(((25β12c0(t)+α12b0(t)8β12c0(t)+α12b0(t))S14+(β12c0(t)α12b0(t))S13S2(11β12c0(t)α12b0(t))S2S126c0(t)S12β12+25β12c0(t)+α12b0(t)8)S34+S4(25β12c0(t)+α12b0(t)8(β12c0(t)+α12b0(t))S146c0(t)S12β12S13×(β12c0(t)+α12b0(t))S2(11β12c0(t)α12b0(t))S2S12+25β12c0(t)+α12b0(t)8)S336S32×(S14+S13S2+12S2S1+18)b0(t)α12+12(25β12c0(t)+α12b0(t)8S4(25β12c0(t)+α12b0(t)8(β12c0(t)11α12b0(t))S146c0(t)S12β12+S2S13(β12c0(t)11α12b0(t))11(β12c0(t)+α12b0(t))S2S12+25β12c0(t)11α12b0(t)8)S3)+(β12c0(t)+25α12b0(t)8)S14+(β12c0(t)+25α12b0(t)8)S13S23c0(t)β12S124(11β12c0(t)25α12b0(t))S2S116+25β12c0(t)+25α12b0(t)64),(16) where ξ1=α1x+α2t, ξ2=β1x+β2t, α2=α1β2(5β14c02(t)α14b02(t))β1S, S1=cosh(ξ2c0(t)2), S2=sinh(ξ2c0(t)2), S3=cosh(ξ1b0(t)2) and S4=sinh(ξ1b0(t)2).

We assign values to the free variables in Equation (Equation16), α1=1, β1=1, β2=1, σ2(t)=1+2cos(2t), b0(t)=1 and c0(t)=1, and then we can receive Figure , which is periodic wave. (a) and (b) show the interaction of multiple waves, moving in the same direction and mode of propagation after a collision. Whether in the u-t plane or u-x plane, these solutions change periodically in (c) and (d).

Figure 2. The soliton wave solution gained from Equation (Equation12) for α1=1, β1=1, β2=1, σ2(t)=1+2cos(2t), b0(t)=1 and c0(t)=1. (a) of 3D-plot; (b) of contour plot; (c) of u-t plot; (d) of u-x plot.

Figure 2. The soliton wave solution gained from Equation (Equation12(12) U(ξ1,ξ2)=p0(t)+p1,0(t)ϕ1(ξ1)+p0,1(t)ϕ2(ξ2)+p1,1(t)ϕ1(ξ1)ϕ2(ξ2)+p2,0(t)ϕ12(ξ1)+p0,2(t)ϕ22(ξ2),(12) ) for α1=1, β1=−1, β2=−1, σ2(t)=1+2cos⁡(2t), b0(t)=−1 and c0(t)=−1. (a) of 3D-plot; (b) of contour plot; (c) of u-t plot; (d) of u-x plot.

2.3. The elliptic solutions

In the light of the method, we take into account the solutions of Equation (Equation5) in the form (17) U(ξ1,ξ2)=p0(t)+p1,0(t)ϕ1(ξ1)+p0,1(t)ϕ2(ξ2)+p1,1(t)ϕ1(ξ1)ϕ2(ξ2)+p2,0(t)ϕ12(ξ1)+p0,2(t)ϕ22(ξ2),(17) (18) ϕ1(ξ1)=b0(t)+b2(t)ϕ12(ξ1)+b4(t)ϕ14(ξ1),ϕ2(ξ2)=c0(t)+c2(t)ϕ22(ξ2)+c4(t)ϕ24(ξ2).(18) By a similar way, we obtain (19) p1,1(t)=0,p0,1(t)=0,p1,0(t)=0,σ1(t)=σ2(t),p0,2(t)=30σ4(t)β12c4(t)σ2(t),p2,0(t)=30σ4(t)α12b4(t)σ2(t),σ3(t)=σ22(t)5σ4(t),p0(t)=10σ4(t)(b2(t)α12+c2(t)β12)σ2(t).(19) Obviously, if the coefficients of Equation (Equation18) are (20) b0(t)=(1m12)24,b2(t)=1+m122,b4(t)=14,c0(t)=(1m22)24,c2(t)=1+m222,c4(t)=14.(20) The solutions of the auxiliary equations [Citation35] in Equation (Equation18) can be obtained (21) ϕ1(ξ1)=m1cn(ξ1,m1)+dn(ξ1,m1),ϕ2(ξ2)=m2cn(ξ2,m2)dn(ξ2,m2),(21) where 0<m1<1 and 0<m2<1.

Finally, the solution of Equation (Equation1) is (22) u3(x,t)=5σ4(t)(α12m12+β12m22+α12+β12)σ2(t)+15σ4(t)α12(m1cn(ξ1,m1)+dn(ξ1,m1))22σ2(t)+15σ4(t)β12(m2cn(ξ2,m2)dn(ξ2,m2))22σ2(t),(22) where ξ1=α1x+α2t, ξ1=β1x+β2t, α2=60α1(c0(t)c4(t)β14c22(t)β143b0(t)b4(t)α145+b22(t)α1415)σ4(t)and β2=12β1(c0(t)c4(t)β14c22(t)β1435b0(t)b4(t)α14+5b22(t)α143)σ4(t).

3. The modified Kudryashov method

In this part, we will employ the modified Kudryashov method to study and analyse the vcCDG equation. To solve Equation (Equation1), we need to make the following assumptions: (23) u=U(ξ),ξ=α1x+α2t,(23) where α1 and α2 are arbitrary constants. By above transformation, Equation (Equation1) can be transformed into ordinary differential equation (24) Uα2+σ1(t)α13UU+σ2(t)α13UU+σ3(t)α1U2U+σ4(t)α15U(5)=0,(24) where U=dUdξ.

On the basis of the method, the layout of the solutions of Equation (Equation24) can be set (25) U(ξ)=0Nqi(t)ϕi(ξ),(25) where the auxiliary equation with regard to x is (26) ϕ(ξ)=ϕ2(ξ)ϕ(ξ).(26) Therefore, the first thing we need to do is to calculate the value of N. After that we can determine the specific form of the solution of Equation (Equation24). Similarly, N can be obtained by balancing U(5) and U2U in Equation (Equation24), we compute (27) N=2.(27) Therefore, we can get the exact form of Equation (Equation25) is (28) U(ξ)=q0(t)+q1(t)ϕ(ξ)+q2(t)ϕ2(ξ).(28) According to this method, we need to bring Equations (Equation26) and (Equation28) together into Equation (Equation24). And by combining the same terms, we can get a series of equations of ϕ(ξ) and make each coefficient of ϕ(ξ) equal to zero. Finally, according to the above steps and symbolic calculation, we can acquire the following four solutions:

Case 1: (29) σ1(t)=σ22(t)+10σ3(t)σ4(t)σ2(t),q1(t)=6α12σ2(t)σ3(t),q2(t)=6α12σ2(t)σ3(t),α2=α15σ4(t)q0(t)σ2(t)α13q02(t)σ3(t)α1.(29) Then, putting Equation (Equation29) into Equation (Equation28), the solution of Equation (Equation24) can be found (30) u4(x,t)=12σ3(t)×(3tanh2(α1(tα14σ4(t)+q0(t)σ2(t)α12t+q02(t)σ3(t)tx)2)σ2(t)α12(α1(tα14σ4(t)+q0(t)σ2(t)α12t+q02(t)σ3(t)tx)2)+3α12σ2(t)+q0(t)σ3(t)).(30) Finally, we assign values to the parameters in the above solution. When the parameters α1=12cos(3t), q0(t)=12+sin(5t), σ2(t)=5+sin(4t), σ3(t)=1 and σ4(t)=1+3cos(t), we can get Figure . They show the interaction between multiple bright soliton waves in (a) and (b). Obviously, the solutions in (c) change greatly. In (d), the value of u changes greatly, and then it turns to be gradual after a sharp change.

Figure 3. The travelling wave solution given by Equation (Equation30) at α1=12cos(3t), q0(t)=12+sin(5t), σ2(t)=5+sin(4t), σ3(t)=1 and σ4(t)=1+3cos(t). (a) of 3D-plot; (b) of contour plot; (c) of u-t plot; (d) of u-x plot.

Figure 3. The travelling wave solution given by Equation (Equation30(30) u4(x,t)=12σ3(t)×(−3tanh2⁡(α1(tα14σ4(t)+q0(t)σ2(t)α12t+q02(t)σ3(t)t−x)2)σ2(t)α12(α1(tα14σ4(t)+q0(t)σ2(t)α12t+q02(t)σ3(t)t−x)2)+3α12σ2(t)+q0(t)σ3(t)).(30) ) at α1=1−2cos⁡(3t), q0(t)=12+sin⁡(5t), σ2(t)=−5+sin⁡(4t), σ3(t)=−1 and σ4(t)=1+3cos⁡(t). (a) of 3D-plot; (b) of contour plot; (c) of u-t plot; (d) of u-x plot.

Case 2: (31) σ3(t)=σ22(t)+σ1(t)σ2(t)10σ4(t),q1(t)=60α12σ4(t)σ1(t)+σ2(t),q2(t)=60α12σ4(t)σ1(t)+σ2(t),α2=α1((σ1(t)+σ2(t))σ2(t)q02(t)10+σ2(t)q0(t)α12σ4(t)+α14σ42(t))σ4(t).(31) Inserting Equation (Equation31) into Equation (Equation28), we obtain the following solution of Equation (Equation24), (32) u5(x,t)=1σ1(t)+σ2(t)×((α1(10tα14σ42(t)+10p0(t)σ2(t)α12tσ4(t)+q02(t)σ22(t)t+σ2(t)q02(t)σ1(t)t10σ4(t)x)20σ4(t))15α12σ4(t)+q0(t)(σ1(t)+σ2(t))×tanh2(α1(10tα14σ42(t)+10p0(t)σ2(t)α12tσ4(t)+q02(t)σ22(t)t+σ2(t)q02(t)σ1(t)t10σ4(t)x)20σ4(t))×(α1(10tα14σ42(t)+10p0(t)σ2(t)α12tσ4(t)+q02(t)σ22(t)t+σ2(t)q02(t)σ1(t)t10σ4(t)x)20σ4(t))(15σ4(t)α12)).(32) On the basis of the above solution, if we take α1=12tan(3t), q0(t)=12+3sin(2t), σ1(t)=12, σ2(t)=5+2sin(4t) and σ4(t)=1+8cos(3t), we obtain Figure . It shows the fluid-lattice wave solutions. We see that the rogue waves owing to the interaction between kinky and anti-kinky periodic waves in (a) and (b). The value of u varies greatly in (c). In (d), the solutions change dramatically when t=0, 5<x<5 and t=5, 10<x<0.

Figure 4. The travelling wave solution calculated by Equation (Equation32) with α1=12tan(3t), q0(t)=12+3sin(2t), σ1(t)=12, σ2(t)=5+2sin(4t) and σ4(t)=1+8cos(3t). (a) of 3D-plot; (b) of contour plot; (c) of u-t plot; (d) of u-x plot.

Figure 4. The travelling wave solution calculated by Equation (Equation32(32) u5(x,t)=1σ1(t)+σ2(t)×((α1(10tα14σ42(t)+10p0(t)σ2(t)α12tσ4(t)+q02(t)σ22(t)t+σ2(t)q02(t)σ1(t)t−10σ4(t)x)20σ4(t))15α12σ4(t)+q0(t)(σ1(t)+σ2(t))×tanh2⁡(α1(10tα14σ42(t)+10p0(t)σ2(t)α12tσ4(t)+q02(t)σ22(t)t+σ2(t)q02(t)σ1(t)t−10σ4(t)x)20σ4(t))×(α1(10tα14σ42(t)+10p0(t)σ2(t)α12tσ4(t)+q02(t)σ22(t)t+σ2(t)q02(t)σ1(t)t−10σ4(t)x)20σ4(t))(−15σ4(t)α12)).(32) ) with α1=1−2tan⁡(3t), q0(t)=12+3sin⁡(2t), σ1(t)=−12, σ2(t)=5+2sin⁡(4t) and σ4(t)=1+8cos⁡(3t). (a) of 3D-plot; (b) of contour plot; (c) of u-t plot; (d) of u-x plot.

Case 3: (33) σ4(t)=(15+849)α2546α15,σ3(t)=252(181+6849)α15σ22(t)13α2(15+849),q0(t)=(15+849)α242α13σ2(t),q2(t)=2(15+849)2α27α13σ2(t)(183+7849),σ1(t)=(3147+137849)σ2(t)390+26849,q1(t)=0.(33) We also take Equation (Equation33) into Equation (Equation28), and then we have (34) u6(x,t)=(15+849)α214α13σ2(t)(183+7849)×(48493(15+849)tanh2(α2t2+α1x2)+(302849)tanh2(α2t2+α1x2)+4648493).(34) Figure  shows that the solution of Equation (Equation24) when α1=105cos(5t), α2=1+8tanh(3t) and σ2(t)=6+5sin(5t). Figure  presents the elastic collision between multiple periodic waves in (a) and (b). In (c) when t>0, the amplitude is larger and changes faster. The value of u changes sharply near x=3 in (d).

Figure 5. The travelling wave solution given by Equation (Equation34) when α1=105cos(5t), α2=1+8tanh(3t) and σ2(t)=6+5sin(5t). (a) of 3D-plot; (b) of contour plot; (c) of u-t plot; (d) of u-x plot.

Figure 5. The travelling wave solution given by Equation (Equation34(34) u6(x,t)=(−15+849)α214α13σ2(t)(−183+7849)×(48493(−15+849)tanh2⁡(α2t2+α1x2)+(30−2849)tanh2⁡(α2t2+α1x2)+46−48493).(34) ) when α1=−10−5cos⁡(5t), α2=−1+8tanh⁡(3t) and σ2(t)=−6+5sin⁡(5t). (a) of 3D-plot; (b) of contour plot; (c) of u-t plot; (d) of u-x plot.

Case 4: (35) σ3(t)=(187+7849)σ22(t)1352σ4(t),q0(t)=13α12σ4(t)σ2(t),q1(t)=0,σ1(t)=7849σ2(t)104443σ2(t)104,q2(t)=1248α12σ4(t)σ2(t)(41+849),α2=7(15+849)α15σ4(t)8.(35) And then, we have (36) u7(x,t)=1σ2(t)(41+849)×(48tanh(105tα15σ4(t)15+7tα15σ4(t)84916+α1x2)17+849+24tanh2×(105tα15σ4(t)15+7tα15σ4(t)84916+α1x2)13σ4(t)α12).(36) In Equation (Equation36), given the parameters α1=1cos(t), σ2(t)=2+2cos(t) and σ4(t)=1+3tanh(5t), we get the Figure . It illustrates that periodic wave and solitary wave for two different velocities combine into a rogue wave in (a) and (b). It is antisymmetric, and when t=0, the value of u is also 0 in (c).

Figure 6. The travelling wave solution given by Equation (Equation36) for α1=1cos(t), σ2(t)=2+2cos(t) and σ4(t)=1+3tanh(5t). (a) of 3D-plot; (b) of contour plot; (c) of u-t plot.

Figure 6. The travelling wave solution given by Equation (Equation36(36) u7(x,t)=−1σ2(t)(−41+849)×(−48tanh⁡(105tα15σ4(t)15+7tα15σ4(t)84916+α1x2)−17+849+24tanh2×(105tα15σ4(t)15+7tα15σ4(t)84916+α1x2)13σ4(t)α12).(36) ) for α1=1−cos⁡(t), σ2(t)=−2+2cos⁡(t) and σ4(t)=1+3tanh⁡(5t). (a) of 3D-plot; (b) of contour plot; (c) of u-t plot.

4. Conclusions

Here, the vcCDG equation is studied and analysed by the unified method and the modified Kudryashov method. Compared with other methods, we receive more different travelling wave solutions and classify some solutions like solitary wave solutions, soliton wave solutions and elliptic wave solutions. These solutions contribute to a better understanding of physics phenomena in different branches of engineering science, mathematical physics, quantum mechanics and nonlinear optics, and other technical fields. By choosing appropriate parameters, 3D and 2D plots of some solutions are plotted, from which we are able to obtain periodic waves, rogue waves and kink solitary waves. Through these, we can get more physical meaning of the cvCDG equation. The unified method and the modified Kudryashov method are significant in the study of solutions of nonlinear partial differential equations, have good research prospect and also provide an idea and direction for solving other problems.

Disclosure statement

No potential conflict of interest was reported by the author(s).

Additional information

Funding

This work was supported by the Natural Science Foundation of Shanxi [grant number 202103021224068].

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