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Research Article

Soliton solutions to generalized (3 + 1)-dimensional shallow water-like equation using the (ϕ'/ϕ,1/ϕ)-expansion method

, , , , , , & ORCID Icon show all
Pages 121-131 | Received 28 Oct 2023, Accepted 29 Jan 2024, Published online: 06 Feb 2024

Abstract

The (3 + 1)-dimensional generalized shallow water equation is a significant mathematical framework for analyzing the dynamic behavior of waves in ocean physics. The purpose of this article is to investigate some more generic soliton solutions of the generalized shallow water-like model in three dimensions. The investigation is conducted utilizing the sophisticated mathematical methodology known as the double variables (ϕ/ϕ,1/ϕ) expansion technique. With this approach, we produce new propagating wave solutions for this model in the form of hyperbolic, trigonometric, and rational functions. In addition, we offer two- and three-dimensional graphical representations to help visualize the intricate physical phenomena of the system. We have constructed many soliton solutions, such as kink shape soliton solutions, anti-bell shape solutions, single periodic solutions, singular soliton solutions, and anti-kink shape solutions for different values of the free parameters involved in the obtained solutions. These graphical representations are predicated on certain parameter selections, which facilitate the understanding of the complicated general behavior for this model. Through the presentation of new findings in the field of soliton solutions for the aforementioned equation, this paper offers fresh perspectives and highlights hitherto overlooked aspects of this fascinating mathematical challenge. The paper illuminates new results on soliton solutions with different geometrical structures for the given equation, revealing hitherto overlooked facets of this intriguing mathematical challenge.

1. Introduction

In a wide range of scientific, engineering, and technological areas, mathematical solutions are superior to experimental results in terms of understanding physical phenomena (Fang, Nadeem, Habib, Karim, & Wahash, Citation2022; He, Nadeem, Habib, Sedighi, & Huang, Citation2022; Nadeem & He, Citation2021). As a result, physical phenomenon emerging in scientific and technological areas are mathematically represented using differential equations. Nonlinear evolution equations, often deployed in modeling phenomena, have emerged as a particularly captivating domain of inquiry for researchers. By formulating and solving these equations, we can gain a deeper understanding of complex systems and develop more accurate predictions about their behavior.

The (3 + 1)-dimensional shallow water equation is a useful model for studying waves in a variety of ocean science. It is used to explain the motion of water under the assumption that the depth of the water is small in comparison to the wavelength of the waves. The shallow water equation is a nonlinear evolution equation with traveling wave solutions, which are significant for different reasons. Soliton solutions to the aforementioned equation can reveal information about the behavior of waves in various physical systems, such as the formation and propagation of tsunamis, storm swells, and tidal waves. The shallow water equation and its traveling wave solutions are critical for the study of wave energy, which is a quickly expanding field.

There are some studies on this equation. Some academics obtained the solutions for Equationequation (3.1) by the improved Bernouli’s sub-equation method (Dusunceli, Citation2019), the generalized bilinear operator (Zhang, Dong, Zhang, & Yang, Citation2017), the Hirota bilinear form (Tang, Ma, & Xu, Citation2012; Tian & Gao, Citation1996), the tanh method (Zayed, Citation2010), and the (G/G) expansion method (Sadat, Kassem, & Ma, Citation2018).

Solving nonlinear evolution equation is not an easy task. There are many useful methods have been represented such as the generalized method (Boakye, Hosseini, Hinçal, Sirisubtawee, & Osman, Citation2024), the exp-function method (Bekir, Citation2009; He & Wu, Citation2006; Yusufoglu, Citation2008), the (G′/(G′+ G + A))-expansion method (Ganie et al., Citation2023), the generalized Kudryashov method (Kumar, Park, Tamanna, Paul, & Osman, Citation2020), the sine cosine method (Wazwaz, Citation2004), the Jacobi elliptic method (Chen & Wang, Citation2005; Liu, Fu, Liu, & Zhao, Citation2001; Lü, Citation2005), the homogeneous balance method (Radha & Duraisamy, Citation2021), the tanh function method (Abdou, Citation2007; Fan, Citation2000), the Sardar sub-equation method (Rehman, Akber, Wazwaz, Alshehri, & Osman, Citation2023), the first integral method (Martínez, Aguilar, & Atangana, Citation2018), the Backlund transformation method (Rogers & Shadwick, Citation1982), (G′/G)-expansion method (Abazari & Abazari, Citation2011; Borhanifar & Moghanlu, Citation2011; Elagan, Sayed, & Hamed, Citation2011; Feng, Li, & Wan, Citation2011; Islam, Al-Amin, Akbar, Wazwaz, & Osman, Citation2023; Jabbari, Kheiri, & Bekir, Citation2011; Naher, Abdullah, & Akbar, Citation2011; Öziş & Aslan, Citation2010; Wang, Li, & Zhang, Citation2008), the central finite difference approximations (Khalid et al., Citation2022), the two variables (G/G,1/G)-expansion method (Demiray, Ünsal, & Bekir, Citation2014, Citation2015; Mamun, Shahadat, Akbar, & Wazwaz, Citation2017; Miah, Iqbal, & Osman, Citation2023; Shakeel & Mohyud-Din, Citation2014), and many more (Abdel-Gawad & Osman, Citation2013; Citation2014; Baskonus et al., Citation2021; El-Sherif & Shoukry, Citation2007; Fahim, Kundu, Islam, Akbar, & Osman, Citation2022; Fetoh, Asla, El-Sherif, El-Didamony, & El-Reash, Citation2019; He, Hou, He, Saeed, & Hayat, Citation2021; He et al., Citation2023; He & Liu, Citation2023; Soliman, Amin, El-Sherif, Sahin, & Varlikli, Citation2017).

In this article, we shall endeavor to explore soliton solution of the generalized (3 + 1) shallow water equation utilizing the two variables  (ϕ/ϕ,1/ϕ) expansion method, which is an advancement of the (G/G)-expansion method, was originally introduced by Li et al. in 2010 to derive precise solutions for the Zakharov equation. Subsequently, this technique has exhibited remarkable efficacy in resolving a wide range of nonlinear partial differential equations. However, to the best of our knowledge, the (ϕ/ϕ,1/ϕ)-expansion method has not yet been employed to derive the soliton solution of the generalized (3 + 1) shallow water equation. Thus, this study has the potential to illuminate the behavior of this equation and the proficiency of the (ϕ/ϕ,1/ϕ)-expansion method in solving other nonlinear evolution equations.

2. Methodology

The (ϕ/ϕ,1/ϕ)-expansion technique, which provides a precise method of solving nonlinear equations, is the first thing we shall look at. Consider about a second-order LODE (linear ordinary differential equation). (2.1) ϕ(ξ)+λϕ(ξ)=μ,(2.1)

Afterward, consider the relationships that follows (2.2) ϕ=ϕϕ and ψ=1/ϕ.(2.2)

The above relationships allow for its derivation. (2.3) ϕ=ϕ2+μψλ,ψ=ϕ ψ.(2.3)

Three different sorts of solutions can be discovered for the EquationEquation (2.1) for various values of λ.

Remark 1:

When the value of  λ > 0, the EquationEquation (2.1) has a generic solution, which is expressed as follows. (2.4) ϕ(ξ)=m1 sinh(λ ξ)+m2cosh(λ ξ)+μλ.(2.4) (2.5) Thus, it is obtained ψ2=λ(ϕ22μψ+λ)λ2β+μ2,(2.5)

Wherein β=m12m22 and m1, m2 are arbitrary constants.

Remark 2:

The generic solution of EquationEquation (2.1) has the following form for λ > 0, (2.6) ϕ(ξ)=m1sin(λ ξ)+m2cos(λ ξ)+μλ,(2.6) (2.7) And it is obtained ψ2=λ(ϕ22μψ+λ)λ2βμ2,(2.7)

Wherein,  β=m12+m22.

Remark 3:

Again, assume λ = 0, then the solution of EquationEquation (2.1) is of the form, (2.8) ϕ(ξ)=μ2ξ2+m1ξ+m2,(2.8) (2.9) And thus, it is obtained, ψ2=(ϕ22μψ)m122 μm2.(2.9)

Step 1: Let us consider a nonlinear evolution equation involving two independent variables, namely x and t, in the following context. (2.10) Q(u,ut,ux,utt,uxt,uxx,.)=0.(2.10)

Here F is a polynomial in u(x,t) and its partial derivatives. We present the independent variables x and t, along with the wave variable ξ, which is related to them as follows: (2.11) u(ξ)=u(x,t),ξ=xvt,(2.11)

Where, v is the traveling wave velocity. Applying Equation(2.10) into Equation(2.9) produces an ODE for u(ξ) (2.12) F(u,u,u,)=0.(2.12) Step 2: Assume that the solution of the ODE Equation(2.12) can be described as a polynomial in ϕ and  ψ (2.13) u(ξ)=i=0naiϕi(ξ)+i=1nbiϕi1(ξ)ψi(ξ),(2.13)

Where ϕ=ϕ(ξ) satisfies a second-order linear differential equation, and ϕ and ψ are defined in EquationEquation (2.2). In this context, the constants ai(i=0,1,2,,N), bi(i=0,1,2,,N),λ, and μ are arbitrary, while N is a positive integer that can be regarded as the homogeneous balance number. The condition of homogeneous balance is applied by equating the highest-order derivatives with the nonlinear terms in the ODE Equation(2.12). Utilizing the double (ϕ/ϕ,1/ϕ) expansion approach, the values of these arbitrary constants can be determined.

Step 3: By substituting EquationEquation (2.13) into EquationEquation (2.12) while utilizing EquationEquations (2.3) and Equation(2.5), we derive a polynomial that involves both ϕ and ψ. Notably, the degree of ψ in this polynomial does not exceed one. By equating the coefficients of ϕ and ψ to zero, we establish a system of algebraic equations encompassing variables such ai(i=0,1,2,,N), bi(i=0,1,2,,N), v, λ, μ, m1, and m2.

Step 4: The algebraic equations given in Step 3 can be solved using Maple, a mathematical program. The final accumulation of the exact solution for EquationEquation (2.12) can then be achieved by determining the consequent values for  ai,bi,c,λ,μ,m1,m2.

3. Application to SWL equation

In this specific section, our objective is to elucidate the precise soliton solutions for the generalized (3 + 1)-dimensional shallow water-like equation, employing the two variables (ϕ/ϕ,1/ϕ)-expansion method. Here the (3 + 1) shallow water-like equation is (3.1) uxxy+3uxxuy+3uxuxyuytuxz=0.(3.1)

Let us assume that the wave function has the following arrangement (3.2) u(x,y,z,t)=u(ξ),(3.2)

With the transformation  ξ=x+ky+mzvt, where v is the traveling wave speed.

Using the above transformation in the EquationEquation (3.1), we get the nonlinear ordinary differential equation as follows, (3.3) ku+6kuu+(kvm)u=0.(3.3)

Now, integrating the above Equation (3.3.3), we have the nonlinear ODE in the form, (3.4) ku+3k(u)2+(kvm)u=0.(3.4)

To obtain the traveling wave solution, we resolve the EquationEquation (3.4). By the method of homogeneous balance principle, here we get the balance number  N+2=3N. Hence N=1.

So, the solutions of the (3 + 1)-dimensional generalized shallow water like equation with the scheme of the two variables (ϕ/ϕ,1/ϕ)-expansion method takes form, (3.5) u(ξ)=a0+a1ϕ(ξ)+b1ψ(ξ),(3.5)

Where a0,a1,b1 are arbitrary constants are to be determined. Here there are three cases to be discussed to examine the nonlinear evolution equation for the sign of λ. Putting the above solutions Equation(3.5), in the EquationEquation (3.4), we illustrated the solutions, that are given below

Case 1: For hyperbolic function solutions is (when λ<0)

EquationEquation (3.4)’s left side transforms into a polynomial when Equation(3.5), Equation(2.3), and Equation(2.5) are added. EquationEquation (3.4) then becomes a system of algebraic equations when the coefficients of this polynomial are put to zero.

Using the mathematical application Maple, we were able to solve the aforementioned algebraic problems and arrive at a0=a0, a1=1,b1=±λ(λ2β+μ2)λ,v=m+kλk.

Putting these values into EquationEquation (3.5) and using EquationEquation (3.2), we obtain the exact solution of the shallow water like EquationEquation (3.2) as follows (3.6) u(ξ)=a0+{λ (m1cosh(λ ξ)+m2sinh(λ ξ))}(m1sinh(λ ξ)+m2cosh(λ ))+μλ±λ(λ2β+μ2)λ(m1sinh(λ ξ)+m2cosh(λ ξ)+μλ)(3.6) where ξ=x+ky+mzvt and β=m12m22.

In particular if m10 and m2=0 and μ=0, the above solution takes form (3.7) u(x,y,z,t)=a0+λ coth(λ(x+ky+mzvt))±λ(λ2β+μ2)λcosechλ(x+ky+mzvt))(3.7)

And if m1=0 and m20 and μ=0, then the above solution turns out, (3.8) u(x,y,z,t)=a0+λ tanh(λ(x+ky+mzvt))±λ(λ2β+μ2)λ sechλ(x+ky+mzvt))(3.8)

Case 2: For Trigonometric solution (when λ>0)

When the value of λ is greater than zero, if we substitute EquationEquation (3.5) into EquationEquation (3.4) while making use of EquationEquations (2.3) and Equation(2.7), the left-hand side of EquationEquation (3.5) undergoes a transformation resulting in a polynomial that involves the variables ϕ and ψ. By setting the coefficients of this polynomial to zero, we derive a system of algebraic equations.

Using the mathematical program Maple, it is obtained by solving those mentioned algebraic equations. a0=a0, a1=1,b1=±λ(λ2β+μ2)λ,v=m+kλk.

By substituting these specified values into EquationEquation (3.5) and combining it with EquationEquation (3.2), we are able to derive the exact solution of the shallow water-like EquationEquation (3.1) in the following manner. (3.9) u(ξ)=a0+{λ (m1cos(λ ξ)+m2sin(λ ξ))}(m1sin(λ ξ)+m2cos(λ ξ))+μλ±λ(λ2β+μ2)λ(m1sin(λ ξ)+m2cos(λ ξ)+μλ)(3.9)

Where β=m12+m22, λ>0 and ξ=x+ky+mzvt.

For m10 and m2=0 and μ=0, the attain solution becomes (3.10) u(x,y,z,t)=a0+λ cot(λ(x+ky+mzvt))±λ(λ2β+μ2)λcosecλ(x+ky+mzvt))(3.10)

Thus for m1=0 and m20 and μ=0, the solution Equation(3.9) takes the following form, (3.11) u(x,y,z,t)=a0+λ tan(λ(x+ky+mzvt))±λ(λ2β+μ2)λsecλ(x+ky+mzvt))(3.11)

Case 3: For rational function solution (when λ=0)

The left-hand side of EquationEquation (3.4) changes to a polynomial in ϕ and ψ and if λ=0, putting EquationEquation (3.5) into EquationEquation (3.4), using Equation(2.3) and Equation(2.9), and so on. This polynomial’s values can be set to zero to produce an algebraic system of equations.

Using Maple, the aforementioned algebraic equations are solved, and the result is received a0=a0, a1=1,b1=±(m122μm2),v=mk.

Substituting these values into EquationEquation (3.5), in addition to using EquationEquation (3.2), we obtain the exact solution of the shallow water like EquationEquation (3.1) as follows (3.12) u(ξ)=a0+μξ+m1μ2ξ2+m1ξ+m2±(m122μm2)μ2ξ2+m1ξ+m2,(3.12)

Where m1 and m2 are arbitrary constants and ξ=(x+ky+mzvt).

4. Graphical representation and result discussion

In this section, we present the graphical representation of the traveling wave solutions obtained for the generalized (3 + 1)-dimensional shallow water-like (SWL) equation. The graph, generated using MATLAB, offers a clear illustration of the soliton solutions obtained in the previous section. Due to the influence of graphical morphology on the dynamics of traveling wave solutions, we have depicted various types of soliton solutions such as kink-shaped soliton solution, anti-bell-shaped solution, singular periodic solution, singular soliton solution, anti-kink-shaped solution, etc., in both three-dimensional and two-dimensional formats.

We mention that a singular wave solution is very important for investigating many physical phenomena, for example when a sudden force is applied, such as an earthquake that might cause a devastating tsunami wave, a singular wave is created. Furthermore, for a porous media, an abrupt temperature shock may potentially cause a thermal tsunami (He & Liu, Citation2023).

Here, the solution Equation(3.7) represents a kink shape soliton solution for the suitable parameters of values μ=0,λ=0.5,v=0.2,y=2.5,z=0.5,10x10,0t10  and equivalents 2D plots depicts for t=1,t=4,t=7 which shown in the . Again we observe from the , the solution Equation(3.7) represents a kink shape soliton solution for the suitable parameters choose values  μ=0,λ=0.25,v=0.3,y=3,z=2.75,10x10,0t5 and in a 2D representation, there are three spatial progressions associated with time points 1, 3, and 5. Next, we plot the of solution Equation(3.7) from which we obtain the kink shape soliton solution for the values of parameters described as μ=0,λ=0.1,v=0.3,y=4,z=2.9,10x10,0t5 and for t=1,t=3,t=5, the corresponding 2D graphs are shown.

Figure 1. 3-D And 2-D graphical illustration of the solution Equation(3.7) for values  μ=0,λ=0.5,v=0.2,y=2.5,z=2,10x10,0t10.

Figure 1. 3-D And 2-D graphical illustration of the solution Equation(3.7)(3.7) u(x,y,z,t)=a0+−λ coth(−λ(x+ky+mz−vt))±−λ(λ2β+μ2)λcosech−λ(x+ky+mz−vt))(3.7) for values  μ=0,λ=−0.5,v=0.2,y=2.5,z=2,−10≤x≤10,0≤t≤10.

Figure 2. 3-D And 2-D graphical illustration the solution Equation(3.7) for values  μ=0,λ=1,v=1,y=3,z=3,5x5,0t5.

Figure 2. 3-D And 2-D graphical illustration the solution Equation(3.7)(3.7) u(x,y,z,t)=a0+−λ coth(−λ(x+ky+mz−vt))±−λ(λ2β+μ2)λcosech−λ(x+ky+mz−vt))(3.7) for values  μ=0,λ=−1,v=1,y=3,z=3,−5≤x≤5,0≤t≤5.

Figure 3. 3-D And 2-D graphical illustration the solution Equation(3.7) for values  μ=0,λ=0.5,v=2,y=1,z=1,5x5,0t5.

Figure 3. 3-D And 2-D graphical illustration the solution Equation(3.7)(3.7) u(x,y,z,t)=a0+−λ coth(−λ(x+ky+mz−vt))±−λ(λ2β+μ2)λcosech−λ(x+ky+mz−vt))(3.7) for values  μ=0,λ=−0.5,v=2,y=1,z=1,−5≤x≤5,0≤t≤5.

Now, the of the solution Equation(3.8) for the values of described parameter μ=0,λ=2,v=2,y=2,z=2,5x5,0t5 with analogous plots can be seen in 2D graphical representations for t=1,t=3,t=5  and it represents anti-bell shape soliton solution. The solution Equation(3.8) represents a kink shape soliton solution for the suitable parameters of values  μ=0,λ=1,v=1,y=3,z=3,5x5,0t5 and in 2D graphical representations, we can observe analogous plots for time instances 3, 4, and 5, which depicted in the . Solution Equation(3.8) describes a kink shape soliton solution which illustrated in the and the graph depicted for the values μ=0,λ=0.5,v=1,y=1,z=1,5x5,0t5 and two-dimensional charts illustrate corresponding representations at t=3,t=4,t=5.

Figure 4. 3-D And 2-D graphical illustration the solution Equation(3.8) for values μ=0,λ=2,v=2,y=2,z=2,5x5,0t5.

Figure 4. 3-D And 2-D graphical illustration the solution Equation(3.8)(3.8) u(x,y,z,t)=a0+−λ tanh(−λ(x+ky+mz−vt))±−λ(λ2β+μ2)λ sech−λ(x+ky+mz−vt))(3.8) for values μ=0,λ=−2,v=2,y=2,z=2,−5≤x≤5,0≤t≤5.

Figure 5. 3-D And 2-D graphical illustration the solution Equation(3.8) for values  μ=0,λ=1,v=1,y=3,z=3,5x5,0t5.

Figure 5. 3-D And 2-D graphical illustration the solution Equation(3.8)(3.8) u(x,y,z,t)=a0+−λ tanh(−λ(x+ky+mz−vt))±−λ(λ2β+μ2)λ sech−λ(x+ky+mz−vt))(3.8) for values  μ=0,λ=−1,v=1,y=3,z=3,−5≤x≤5,0≤t≤5.

Figure 6. 3-D And 2-D graphical illustration the solution Equation(3.8) for values  μ=0,λ=0.5,v=1,y=1,z=1,5x5,0t5.

Figure 6. 3-D And 2-D graphical illustration the solution Equation(3.8)(3.8) u(x,y,z,t)=a0+−λ tanh(−λ(x+ky+mz−vt))±−λ(λ2β+μ2)λ sech−λ(x+ky+mz−vt))(3.8) for values  μ=0,λ=−0.5,v=1,y=1,z=1,−5≤x≤5,0≤t≤5.

The solution Equation(3.10) represents a singular periodic soliton solution for the suitable parameters of values  μ=0,λ=2,v=1,y=3,z=3,5x5,0t5  and for t=1,3,5 in 2D images and displayed in the . The of the solution Equation(3.10) represents singular periodic soliton solution for the values of parameter μ=0,λ=1,v=1,y=4,z=4,5x5,0t5 and for the time points t=1,t=3,and t=5,a 2D graph displaying the same information is constructed. Next, we illustrated the of solution Equation(3.10) from which we obtain the singular soliton solution for the values of parameters described as μ=0,λ=0.5,v=2,y=4,z=4,5x5,0t5 and in 2D we choose t=1,t=3,and t=5.

Figure 7. 3-D And 2-D graphical illustration the solution Equation(3.10) for values  μ=0,λ=2,v=1,y=3,z=3,5x5,0t5.

Figure 7. 3-D And 2-D graphical illustration the solution Equation(3.10)(3.10) u(x,y,z,t)=a0+λ cot(λ(x+ky+mz−vt))±−λ(−λ2β+μ2)λcosecλ(x+ky+mz−vt))(3.10) for values  μ=0,λ=2,v=1,y=3,z=3,−5≤x≤5,0≤t≤5.

Figure 8. 3-D And 2-D graphical illustration the solution Equation(3.10) for values μ=0,λ=1,v=1,y=4,z=4,5x5,0t5.

Figure 8. 3-D And 2-D graphical illustration the solution Equation(3.10)(3.10) u(x,y,z,t)=a0+λ cot(λ(x+ky+mz−vt))±−λ(−λ2β+μ2)λcosecλ(x+ky+mz−vt))(3.10) for values μ=0,λ=1,v=1,y=4,z=4,−5≤x≤5,0≤t≤5.

Figure 9. 3-D And 2-D graphical illustration the solution Equation(3.10) for values μ=0,λ=0.5,v=2,y=4,z=4,5x5,0t5.

Figure 9. 3-D And 2-D graphical illustration the solution Equation(3.10)(3.10) u(x,y,z,t)=a0+λ cot(λ(x+ky+mz−vt))±−λ(−λ2β+μ2)λcosecλ(x+ky+mz−vt))(3.10) for values μ=0,λ=0.5,v=2,y=4,z=4,−5≤x≤5,0≤t≤5.

gives the singular periodic soliton solutions for the solution Equation(3.11) where the values of the parameters are μ=0,λ=1.5,v=2,y=3,z=3,10x10,0t5 and the 2D propagations are shown for t=1,t=3,and t=5, in that order and λ=1,v=2,y=2,z=2,10x10,0t5 and for a 2D graph exhibiting the same information is presented for time units t=3,t=4,t=5 and μ=0,λ=0.5,v=1,y=1,z=1,10x10,0t5 also The 2D visualizations represent at t=1,t=3,and t=5  time intervals respectively.

Figure 10. 3-D And 2-D graphical illustration the solution Equation(3.11) for μ=0,λ=1.5,v=2,y=3,z=3,10x10,0t5.

Figure 10. 3-D And 2-D graphical illustration the solution Equation(3.11)(3.11) u(x,y,z,t)=a0+λ  tan (λ(x+ky+mz−vt))±−λ(−λ2β+μ2)λsec λ(x+ky+mz−vt))(3.11) for μ=0,λ=1.5,v=2,y=3,z=3,−10≤x≤10,0≤t≤5.

Figure 11. 3-D And 2-D graphical illustration of the solution Equation(3.11) for values  μ=0,λ=1,v=2,y=2,z=2,10x10,0t5.

Figure 11. 3-D And 2-D graphical illustration of the solution Equation(3.11)(3.11) u(x,y,z,t)=a0+λ  tan (λ(x+ky+mz−vt))±−λ(−λ2β+μ2)λsec λ(x+ky+mz−vt))(3.11) for values  μ=0,λ=1,v=2,y=2,z=2,−10≤x≤10,0≤t≤5.

Figure 12. 3-D And 2-D graphical illustration the solution Equation(3.11) for values μ=0,λ=0.5,v=1,y=1,z=1,10x10,0t5.

Figure 12. 3-D And 2-D graphical illustration the solution Equation(3.11)(3.11) u(x,y,z,t)=a0+λ  tan (λ(x+ky+mz−vt))±−λ(−λ2β+μ2)λsec λ(x+ky+mz−vt))(3.11) for values μ=0,λ=0.5,v=1,y=1,z=1,−10≤x≤10,0≤t≤5.

The of the solution Equation(3.12) for the values of described parameter m1=4,m2=1 and μ=1,λ=0,v=2,y=2,z=2,5x5,0t5 and The same information is shown on a 2D graph for t=3,t=4,t=5 and it represents anti-kink shape soliton solution and lastly the solution Equation(3.12) represents a parabolic shape soliton solution for the suitable parameters of values m1=4,m2=2 and μ=3,λ=0,v=1,y=3,z=4,10x10,0t10 and an analogous two-dimensional diagram is drawn to represent data at t=7,t=8,t=9 as both are shown in .

Figure 13. 3-D And 2-D graphical illustration the solution Equation(3.12) for values  m1=4,m2=1 and μ=1,λ=0,v=2,y=2,z=2,5x5,0t5.

Figure 13. 3-D And 2-D graphical illustration the solution Equation(3.12)(3.12) u(ξ)=a0+μξ+m1μ2ξ2+m1ξ+m2±(m12−2μm2)μ2ξ2+m1ξ+m2,(3.12) for values  m1=4,m2=1 and μ=1,λ=0,v=2,y=2,z=2,−5≤x≤5,0≤t≤5.

Figure 14. 3-D And 2-D graphical illustration the solution Equation(3.12) for values m1=1,m2=1 and μ=3,λ=0,v=1,y=3,z=2,10x10,0t10.

Figure 14. 3-D And 2-D graphical illustration the solution Equation(3.12)(3.12) u(ξ)=a0+μξ+m1μ2ξ2+m1ξ+m2±(m12−2μm2)μ2ξ2+m1ξ+m2,(3.12) for values m1=1,m2=1 and μ=3,λ=0,v=1,y=3,z=2,−10≤x≤10,0≤t≤10.

5. Comparison

Now, in this part, we will try to compare the solutions obtained by Dusunceli et al. (Nadeem & He, Citation2021) with the aid of improved Bernouli’s sub-equation method and result which we got by using the double variables (ϕ/ϕ,1/ϕ)-expansion method of the generalized (3 + 1) shallow water like equation (SWL). The (ϕ/ϕ,1/ϕ)-expansion method has used to describe in this article to find thesoliton solutions of the generalized (3 + 1)-dimensional shallow water like equation (SWL). Different values of full of nonlinearity parameter gives us different types of solution, Dusunceli has derived total four solutions of the generalized (3 + 1)-dimensional shallow water like equation by of improved Bernouli’s sub-equation method which are given in the table and all the solutions are in tan function. In this article we derived five soliton solutions (3.7)(3.8),(3.10)(3.12) of the mentioned EquationEquation (3.1) where each of the solutions are unique from solution Dusunceli’s solution and here all the solution are derived in terms of hyperbolic, trigonometric and rational functions. In particular, if we set m1=0, m20 and μ=0, then we get the solution in terms of hyperbolic functions of tanh and sech and in terms of trigonometric function we get secant and tangent functions. Similarly, if we set m10, m2=0 and μ=0, then we get other types of solution in terms hyperbolic functions in coth and cosech and cosec or cot in terms of trigonometric functions.

6. Conclusion

In this article we have found the soliton solutions of the (3 + 1)-dimensional shallow water equation by using the two variables (ϕ/ϕ,1/ϕ)-expansion method which will be able to understand the physical phenomenon in ocean physics in a better way. Different types of soliton solutions have been obtained in this study like kink shape soliton solution, anti-bell shape solution, singular periodic solution, singular soliton solution, anti-kink shape solution etc. The solutions which we got in this study are capable of discussing the system’s complex behavior than the mentioned article. The computer program MATLAB is employed to visually demonstrate the three-dimensional (3-D) and two-dimensional (2-D) graphical depictions of the derived solutions. Moreover, this research has the capacity to have significant implications for the future of nonlinear partial differential equations (NPDEs). By demonstrating the efficacy of the two variables (ϕ/ϕ,1/ϕ)-expansion method for solving the mentioned equation, in near future our work could serve as an impetus for other researchers to apply this method to other NPDEs, potentially leading to groundbreaking discoveries in the field. Additionally, when the aforementioned model’s coefficients are not constants, we will use this method to analyze it in a future work.

Disclosure statement

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

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