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Article

Soliton Waves with the (3+1)-Dimensional Kadomtsev–Petviashvili–Boussinesq Equation in Water Wave Dynamics

1
Department of Mathematical Engineering, Yildiz Technical University, Istanbul 34349, Turkey
2
Department of Computer Engineering, Biruni University, Istanbul 34010, Turkey
*
Author to whom correspondence should be addressed.
Symmetry 2023, 15(1), 165; https://doi.org/10.3390/sym15010165
Submission received: 1 December 2022 / Revised: 24 December 2022 / Accepted: 27 December 2022 / Published: 5 January 2023
(This article belongs to the Special Issue Symmetry in Nonlinear Optics: Topics and Advances)

Abstract

:
We examined the (3+1)-dimensional Kadomtsev–Petviashvili–Boussinesq (KP-B) equation, which arises not only in fluid dynamics, superfluids, physics, and plasma physics but also in the construction of connections between the hydrodynamic and optical model fields. Moreover, unlike the Kadomtsev–Petviashvili equation (KPE), the KP-B equation allows the modeling of waves traveling in both directions and does not require the zero-mass assumption, which is necessary for many scientific applications. Considering these properties enables researchers to obtain more precise results in many physics and engineering applications, especially in research on the dynamics of water waves. We used the modified extended tanh function method (METFM) and Kudryashov’s method, which are easily applicable, do not require further mathematical manipulations, and give effective results to investigate the physical properties of the KP-B equation and its soliton solutions. As the output of the work, we obtained some new singular soliton solutions to the governed equation and simulated them with 3D and 2D graphs for the reader to understand clearly. These results and graphs describe the single and singular soliton properties of the (3+1)-dimensional KP-B equation that have not been studied and presented in the literature before, and the methods can also help in obtaining the solution to the evolution equations and understanding wave propagation in water wave dynamics.

1. Introduction

In recent years, many researchers have been interested in the physical properties of nonlinear waves. Among them, analytical solutions of nonlinear evolution equations (NLEEs), a class of nonlinear waves, are of great importance for understanding and explaining real-life problems. As important as they are, analytical solutions to these problems are often an equally troublesome process. Due to the developments in computers and software, there have also been many developments in symbolic computing such as Wolfram Mathematica, Maple, Matlab, and other symbolic programs. In this way, it can be said that the calculations and accuracy are at a very good level. Moreover, the analytical solutions of NLEEs play very important role in exposing the mechanisms in various fields, namely nonlinear optics, optical fibers, communication, data transfer, heat conduction, physics, plasma physics, chemical kinematics, quantum mechanics, mathematical biology, genetics, geochemistry, dynamic, fluid mechanics, oceanography, neural networks, wave propagation, control theory, and so on, see [1,2,3,4,5,6,7,8]. In our literature review, in recent years, many researchers and academics have proposed and developed a number of strategies, techniques, and methods to understand and analytically solve the NL phenomenon. These methods can be listed as follows: the modified tan( φ / 2 )-expansion [9], variational principles [10], the extended rational sin–cos and sinh–cosh methods, He’s variational approach and the Painleve technique [11], the residual power series [12], Lie symmetry analysis [13], the modified subequation extended method [14], improved F-expansion [15], the new compound Riccati equations rational expansion method and Fan’s subequation method [16], the Kudryashov method [17,18,19], the generalized Kudryashov method [20], the extended Kudryashov technique [21], the Jacobi elliptic function [22,23,24], the Bernoulli subequation function [25,26], the first integral method [27], the projective Riccati F-expansion [28], the Sinh Gordon Expansion (ShGEM) [29], the Sinh Gordon extended Expansion (ShGEEM) [30], the modified extended tanh function (METFM) [31], the F-expansion [32], the Improved Hirota Bilinear method [33], the Backlund transformation [34], Stable Optical Solitons for the Higher-Order Non-Kerr NLSE via the Modified Simple Equation Method [35], the modified simple equation method [36], the ansatz technique [37], the rational exponential function [38], the (G′/G)-expansion method [39], the modified trial equation method [40], Riccati equation mapping [41], the Lie group approach [42], and some recent approaches, which are the modified ( g ) , the modified ( g / g 2 ) , and the generalized simple (w/g)-expansion methods [43], an addendum to Kudryashov’s method [44], the Cole–Hopf transformation, which offers many different solutions as well as being an effective method [45], and newly introduced to the literature, the direct mapping method [46].
The (3+1)-dimensional KP-B equation that we examined in our study is given as [4,47,48,49]:
B x x x y + 3 B x B y x + B x + B y t + B t t B z z = 0 .
In (1), B ( x , y , z , t ) is a real valued potential function, which describes the height of the wave. Here, x , y , and z are independent spatial variables, and t is the temporal variable. Equation (1) is an extended form of the integrable KPE. If the term B t t is omitted, (1) degenerates to following (3+1)-dimensional generalized KPE [50],
B x x x y + 3 B x B y x + B x + B y t B z z = 0 ,
and another type of the (3+1)-dimensional generalized KPE [51],
B x x x y + 3 B x B y x + B x + B y + B z t B z z = 0 .
In addition, both the KPEs in (2) and (3) are not only related to fluid dynamics, superfluids, physics, and plasma physics, but there are also connections between hydrodynamic and optical models [52]. KPE is widely used in many fields, such as Bose–Einstein condensation [53], nonlinear optics, water wave dynamics, ferromagnetics, physics, plasma physics, and surface oceanic waves, for example, investigations of nonlinear ion acoustic waves in magnetized dusty plasma [54], acoustic waves studies in an elastic circular rod [55], nonlinear wave propagation in a fluid and elastic tube covering turbulence, small bubbles [56,57], the traveling of tsunami waves in the inhomogeneous zone on the bottom of the ocean [58,59], and so on. Moreover, by using the KPE it is possible to investigate quasi one dimensional shallow water waves, if the effects of the viscosity and surface tension are very small or negligible [60]. Therefore, although it is thought that Equation (1) can be obtained as a result of adding the term B t t to Equation (2), in a sense, it is also possible to evaluate it as a combination of Equation (2) and the following generalized Boussinesq ((4)) or generalized KP-B equation-like equation in (5) [61,62,63],
B x x x y + 3 B x B y x + B t t B z z = 0 ,
B x x x y + 3 B x B y x + B x + B y t + B t t B z z = 0 .
To be clear, if we consider (4), the presented model in (1) not only allows for the modeling of waves traveling in both directions (both left and right going waves), but (1) also does not require the zero mass assumption that is required during many applications of the KPE, and it allows more precise results to be obtained in many physics and engineering applications.
With the aim of establishing many physical models, researchers have studied the KP-B equation and have obtained many results about the soliton behavior of the KP-B equation, for example, by using Lie symmetry reductions and direct integration by invoking the ( G / G ) expansion method [42], one and two soliton solutions and multi-soliton solutions [4,47,48,49,50,51,52,53,54,55,56,57,58,59,60,61,62,63], by giving only one type of exponential solution. Multiple-order rogue waves for the generalized (2+1)-dimensional KPE were studied in [64,65], the nonautonomous and mixed lump–stripe soliton solutions of a variable-coefficient KPE were studied in [66], the solitary, shock, and and singular wave solutions of the (3+1)-dimensional KPE and the generalized Boussinesq equations were investigated using the solitary wave method in [67], and the (3+1)-dimensional generalized nonlinear evolution equation of shallow water waves was investigated in [68]; in addition (3+1)-dimensional KPE and its integrability, multiple-solitons, breathers, and lump waves were presented in [69], multi-order rogue wave solutions of the generalized (3+1)-dimensional KPE through its bilinear form and symbolic computation were given in, and localized nonlinear waves on spatiotemporally controllable backgrounds of a KP-B model in water waves were studied in [70].
Our motivation is that there has not been any previous study for both the (3+1)-KP-B equation and the different soliton types of the singular solutions of this equation. In addition, singular soliton solutions play an important role in the multi-soliton solutions of the KP-B equation.
Therefore, our main purpose in this article is to search for and obtain single-wave and singular solutions of the KP-B equation that will help researchers working in the field.

2. Mathematical Analysis and Obtaining a Nonlinear Ordinary Differential Form

Let we remember (1) and take into account the following transformation:
B = B x , y , z , t = B ζ , ζ = x + α y + β z ω t ,
in which α , β , and ω are real values. Considering Equations (6) and (1) together, the result is the following equation:
ω 2 ω ( α + 1 ) β 2 d B ζ d ζ + 3 α d B ζ d ζ 2 + α d 3 B ζ d ζ 3 = 0 .
Accepting d B ζ d ζ = Γ ζ , we derive the nonlinear ordinary differential form of (1).
ω 2 ω ( α + 1 ) β 2 Γ ζ + 3 α Γ ζ 2 + α d 2 Γ ζ d ζ 2 = 0 .
In (8), using the balance rule between the terms Γ ζ and Γ 2 ζ , we reach m = 2 , and that m is called the balancing constant.

3. Quick View of the Methods and Implementation of the KP-B Equation

3.1. Modified Extended tanh Function Method

In order to achieve the solution of (8), we propose the solution in the following truncated series:
Γ ζ = A 0 + i = 1 m A i κ i ( ζ ) + i = 1 m B i κ i ( ζ ) ,
where A 0 , , A m , B 1 , , B m are real constants ( A m and B m should not be zero, simultaneously), m is a positive integer balancing constant, which was calculated as m = 2 ; so, (9) takes the following form:
Γ ( ζ ) = A 0 + A 1 κ ( ζ ) + A 2 κ 2 ( ζ ) + B 1 κ 1 ( ζ ) + B 2 κ 2 ( ζ ) ,
where κ ( ζ ) fulfills the following equation:
d κ ( ζ ) d ζ w + κ ( ζ ) 2 = 0 ,
in which w is a real constant, and Equation (11) produces the following solutions:
κ ( ζ ) = w tan ( w ζ + ζ 0 ) ; w < 0 , w cot ( w ζ + ζ 0 ) ; w < 0 , 1 / ζ + ζ 0 ; w = 0 , w tanh ( w ζ + ζ 0 ) ; w > 0 , w coth ( w ζ + ζ 0 ) ; w > 0 ,
where w and ζ 0 are real free parameters. Substitution of (10) and (11) into (8) results in the polynomial in powers of κ ( ζ ) . Applying algebraic polynomial operations to the coefficients of κ ( ζ ) will produce the following algebraic equation system:
κ 4 ( ζ ) : 3 α B 2 2 w 2 + B 2 = 0 , κ 3 ( ζ ) : 2 α B 1 w 2 + 3 B 2 = 0 , κ 2 ( ζ ) : 8 w ω + 6 A 0 α β 2 + ω 2 ω B 2 + 3 α B 1 2 = 0 , κ 1 ( ζ ) : 2 w ω + 6 A 0 α β 2 + ω 2 ω B 1 + 6 α A 1 B 2 = 0 , κ 0 ( ζ ) : 3 A 0 2 A 0 ω + 2 w 2 + 6 B 2 A 2 + 6 A 1 B 1 + 2 B 2 α A 0 β 2 ω 2 + ω = 0 , κ 1 ( ζ ) : 2 w ω + 6 A 0 α β 2 + ω 2 ω A 1 + 6 α B 1 A 2 = 0 , κ 2 ( ζ ) : 8 w ω + 6 A 0 α β 2 + ω 2 ω A 2 + 3 α A 1 2 = 0 , κ 3 ( ζ ) : 2 α A 1 3 A 2 + 1 = 0 , κ 4 ( ζ ) : 3 α A 2 A 2 + 2 = 0 .
In (13) A 0 , A 1 , A 2 , B 1 , B 2 , ω , α , β , and w are unknowns to be calculated. The solution of this system yields the possible solution sets as follows:
C S e t 1 = { w = ω 2 + α 1 ω β 2 4 α , A 0 = ω 2 + α 1 ω β 2 6 α , A 1 = 0 , A 2 = 2 , B 1 = 0 , B 2 = 0 } ,
C S e t 2 = { w = 2 2 B 2 , ω = α 2 + 1 2 + 1 2 8 α 2 B 2 + α 2 + 4 β 2 + 2 α + 1 , A 0 = 2 B 2 , A 1 = 0 , A 2 = 0 , B 1 = 0 , B 2 = B 2 } ,
C S e t 3 = { ω = α + 1 2 + 1 2 α 2 + 16 w + 2 α + 4 β 2 + 1 , A 0 = 2 w 3 , A 1 = 0 , A 2 = 2 , B 1 = 0 , B 2 = 0 } ,
C S e t 4 = { w = ω 2 + α 1 ω β 2 4 α , A 0 = ω 2 + α 1 ω β 2 6 α , A 1 = 0 , A 2 = 0 , B 1 = 0 , B 2 = α ω + β 2 ω 2 + ω 2 8 α 2 } ,
C S e t 5 = { w = 2 2 B 2 , ω = α + 1 2 1 2 32 α 2 B 2 + α 2 + 4 β 2 + 2 α + 1 , A 0 = 2 2 3 B 2 , A 1 = 0 , A 2 = 2 , B 1 = 0 , B 2 = B 2 } ,
C S e t 6 = { ω = α + 1 2 + 1 2 α 2 + 64 w + 2 α + 4 β 2 + 1 , A 0 = 4 w 3 , A 1 = 0 , A 2 = 2 , B 1 = 0 , B 2 = 2 w 2 } .
Selecting any solution set and solution function given in (12) for ζ 0 = 0 , then substituting them together into (10) by considering B ( ζ ) = Γ ( ζ ) d ζ and (6), the solutions of (1) are achieved as in (14)–(18).
Case-1: for κ ( ζ ) = W 2 tan ( W 2 ζ ) :
B 1 ( x , y , z , t ) = A 0 ζ A 1 2 ln 1 + tan w ζ 2 A 2 w tan w ζ 1 w + A 2 w arctan tan w ζ 1 w + B 1 w ln tan w ζ B 1 2 w ln 1 + tan w ζ 2 + B 2 w 1 w tan w ζ 1 + B 2 w w arctan tan w ζ ,
or κ ( ζ ) = W 2 cot ( W 2 ζ ) :
B 2 ( x , y , z , t ) = A 0 ζ A 1 2 ln cot w ζ 2 + 1 + B 1 w ln cot w ζ B 1 2 w ln cot w ζ 2 + 1 + A 2 w cot w ζ 1 w A 2 w π 2 w + A 2 w w arccot cot w ζ B 2 π 2 w w + B 2 w w arccot cot w ζ B 2 w w cot w ζ 1 .
Case-2: κ ( ζ ) = W 1 tanh ( W 1 ζ ) :
B 3 ( x , y , z , t ) = A 0 ζ A 1 2 ln tanh ψ 1 A 1 2 ln tanh ψ + 1 A 2 w tanh ψ A 2 2 w ln tanh ψ 1 + A 2 2 w ln tanh ψ + 1 + B 1 w ln tanh ψ B 1 2 w ln tanh ψ 1 B 1 2 w ln tanh ψ + 1 B 2 2 ln tanh ψ 1 w 3 2 B 2 w 3 2 tanh ψ 1 + B 2 2 ln tanh ψ + 1 w 3 2 ,
or κ ( ζ ) = W 1 coth ( W 1 ζ ) :
B 4 ( x , y , z , t ) = A 0 ζ A 1 2 ln coth ψ 1 A 1 2 ln coth ψ + 1 A 2 w coth ψ A 2 2 w ln coth ψ 1 + A 2 2 w ln coth ψ + 1 B 1 2 w ln coth ψ 1 + B 1 w ln coth ψ B 1 2 w ln coth ψ + 1 B 2 2 ln coth ψ 1 w 3 2 + B 2 2 ln coth ψ + 1 w 3 2 B 2 w 3 2 coth ψ 1 ,
where ψ = W 1 ζ , W 1 = ω , and W 2 = ω .
Case-3: κ ( ζ ) = 1 / ζ :
B 5 ( x , y , z , t ) = A 0 ζ + A 1 ln ζ A 2 ζ + B 1 ζ 2 2 + B 2 ζ 3 3 .
In (14)–(18), ζ = x + α y + β z ω t .

3.2. Kudryashov Method

In order to derive the solution of (8), we suggest the solution in the following form:
Γ ζ = i = 0 m a i κ i ( ζ ) ,
where a m 0 , and in (19), a 0 , , a m are real constants, and m is also a balancing constant. From the previous section, remembering that m = 2 , (19) turns into the following form:
Γ ( ζ ) = a 0 + a 1 κ ( ζ ) + a 2 κ 2 ( ζ ) ,
where κ ( ζ ) satisfies the following equation [71]:
d κ ζ d ζ δ κ ζ κ ζ 1 = 0 ,
where δ is a nonzero real free parameter, and (21) gives the following solution:
κ ζ = 1 1 η e δ ζ ,
in which η is a nonzero arbitrary real constant to be found later. Unlike its general usage, we take the expression in (22) as follows.
By considering
s i n h ( x ) = e x e x 2 , c o s h ( x ) = e x + e x 2 , e x = s i n h ( x ) + c o s h ( x ) , η = 1 ,
one can easily obtain the following two forms:
κ ζ = 1 2 1 tanh δ 2 ζ ,
κ ζ = 1 2 1 coth δ 2 ζ .
Substitution of (20) and (21) into (8) provides us a polynomial in powers of κ ( ζ ) . Applying polynomial operations based on κ ( ζ ) , we obtain the following algebraic equation system:
κ 0 ( ζ ) : a 0 α ω + 3 α a 0 2 a 0 β 2 + a 0 ω 2 a 0 ω = 0 , κ 1 ( ζ ) : α δ 2 a 1 α ω a 1 + 6 α a 0 a 1 β 2 a 1 + ω 2 a 1 ω a 1 = 0 , κ 2 ( ζ ) : 3 α δ 2 a 1 + 4 α δ 2 a 2 α ω a 2 + 6 α a 0 a 2 + 3 α a 1 2 β 2 a 2 + ω 2 a 2 ω a 2 = 0 , κ 3 ( ζ ) : 2 α δ 2 a 1 10 α δ 2 a 2 + 6 α a 1 a 2 = 0 , κ 4 ( ζ ) : 6 α δ 2 a 2 + 3 α a 2 2 = 0 .
In (26) a 0 , a 1 , a 2 , α , β , ω , and δ are real values to be found. The solution of this system gives us the following solution sets:
C S e t 7 = δ = 1 2 2 a 2 , α = 2 β 2 2 ω 2 + 2 ω a 2 + 2 ω , a 0 = a 2 6 , a 1 = a 2 , a 2 = a 2 ,
C S e t 8 = β = α δ 2 α ω + ω 2 ω , a 0 = 0 , a 1 = 2 δ 2 , a 2 = 2 δ 2 .
Selecting any solution set and then substituting it into (20) by considering B ( ζ ) = Γ ( ζ ) d ζ and (6), the solution of NLPDE (1) is found, as given in (27) and (28). We consider Equation (24):
B 6 , 1 ( x , y , z , t ) = a 0 ϑ + a 1 ϑ 2 + a 1 2 δ ln tanh δ ϑ 2 1 + a 1 2 δ ln tanh ϑ 2 + 1 a 2 2 δ tanh δ ϑ 2 + a 2 δ ln tanh δ ϑ 2 + 1 ,
and we consider Equation (25):
B 6 , 2 ( x , y , z , t ) = a 0 ϑ + a 1 ϑ 2 + a 1 2 δ ln coth δ ϑ 2 1 + a 1 2 δ ln coth ϑ 2 + 1 a 2 2 δ coth δ ϑ 2 + a 2 δ ln coth δ ϑ 2 + 1 ,
where ϑ = α y + β z ω t + x .

4. Results and Discussion

In this part, some of the graphical illustrations are presented for the soliton solution functions given in (14), (15), (17), (27), and (28). The simulations of these solutions are given in order, from Figure 1, Figure 2, Figure 3, Figure 4, Figure 5, Figure 6, Figure 7 and Figure 8, according to the appropriate selection of parameters. Although we obtained many solution sets from the solution of (13) and (26) according to different parameter values, in order to not occupy unnecessary pages, only some selected solution sets of C s e t 1 ,…, C s e t 8 are used for graphical representations.
Figure 1, Figure 2, Figure 3, Figure 4, Figure 5, Figure 6, Figure 7 and Figure 8 generally show the graphical representations of the singular solutions of the KP-B equation. Although the graphs generally express the singular wave representation, there are still some differences between these representations. Figure 1 represents the periodic singular solution graph. The values taken by the function are given in different signs on the left and right where the singularity occurs. In Figure 2, there is a graph of the periodic singular soliton solution. However, if we pay attention to this graph, the wave takes a step-like appearance at the point where the singularity occurs, just before diverging to negative or positive infinity. In Figure 3, there is a graph of a periodic singular solution. In this graph, the wave has a bending point on an axis that can be considered a vertical symmetry point. Then, in a sense, the concavity diverges to different infinities after its direction changes. Figure 4 is a graph that gives a different image among these graphs. It represents a singular behavior, which can be called a smooth kink, albeit partially. The graph of Figure 5 is yet another singular graph, and it gives an image of the soliton here with inclined wings to the left and right. The singular soliton graphs in Figure 6 and Figure 7 are representations of step-shaped physical formations. Although the soliton given with the Figure 8 graph is similar to the graphical expression given in Figure 3, there is a vertical distance between its left and right skirts. In other words, although the singular soliton graphs represented by Figure 3 and Figure 8 are categorically the same, they do not represent exactly the same physical behavior. In this sense, in any soliton representation of the problem modeling a physical event, even if the same type of soliton is formed, the physical representations of such solitons can express different physical phenomena. All solution functions obtained in the study have also been confirmed by careful examination to satisfy (1), which is the nonlinear form of the main problem.
When the METFM and Kudryashov methods we used in the article are taken into account, it is easily seen that these methods are easy to apply, effective, and give direct results. However, it is important to emphasize the following: what is important here is the researcher’s purpose and the method one chooses for this purpose. When evaluated from this point of view, these two methods, which are widely used and effective, were chosen in our study, especially as we wanted to work on single wave and singular solutions. Therefore, it is also possible to obtain different types of solitons by using methods other than those mentioned here. For example, in the article [43], there were various and different soliton solutions obtained by using modified ( g ) , the modified ( g / g 2 ) , and the generalized simple (w/g)-expansion methods. Similarly, it is obvious that Wang’s direct algebraic method [46], which has just been introduced to the literature, is an effective method based on an easily applicable auxiliary equation and can give different singular solutions. In addition, it seems possible that this method could be applied to the equation in our study, similar to the different types of solitons obtained from the problems using the Cole–Hopf transformation [45]. It is possible to add other techniques, such as the Hirota bilinear form [33,47], to examine multiwave solutions or soliton types such as breather, lump, and rouge. In addition, it would be appropriate to emphasize two points. All of the solution functions obtained in the study were determined to satisfy the main equation Equation (1). In our study, both the solution functions we obtained and the graphic representations we presented do not have any contradictions with the studies in this field and the generally accepted concepts in this field.

5. Conclusions

In this study, we examined in detail the KP-B equation that widely appears in the models of physical phenomena, such as fluid dynamics, superfluids, physics, plasma physics, and hydrodynamic and optical models. Moreover, the KP-B equation provides for the modeling of waves traveling in both directions and more accurate approximations than the KPE. We applied two well-known analytical methods, the METFM function and the Kudryashov method. For this purpose, we obtained the solution functions by taking the Riccati equation as given in (11), while applying the modified extended tanh expansion method and by taking the solution functions as hyperbolic given in (24) and (25) instead of the exponential form in the application of the Kudryashov function method. The scientific contributions of this study are to show that different singular solutions of the multi-soliton solutions of the KP-B equation can be obtained with two easy-to-apply and effective methods. We obtained and exhibited a plethora of solutions, such as anti-kink, singular, periodic, and singular periodic. In this study, we covered some topics that can be studied prospectively, such as detailed examinations of the step-shaped formations observed in singular soliton solutions, examining the equations of different fractional forms of this structure, and investigating the effects of the results obtained from single-wave solutions on multiwave solutions and different soliton types. In addition to effective and different methods, such as the Hirota and Cole–Hopf, we aim to obtain further different solutions to the problem examined here, with new methods such as Wang’s direct algebraic method. In addition, considering that the single-wave and singular solutions of the KP-B equation have a significant effect on obtaining multi-soliton solutions, we believe that the results obtained in the study will be useful for research in this field.

Author Contributions

Conceptualization, M.O. and M.B.; methodology, A.S.; software, A.S.; validation, M.B., M.O. and A.S.; formal analysis, A.S.; investigation, M.B.; resources, A.S.; data curation, M.O.; writing—original draft preparation, M.B.; writing—review and editing, M.O.; visualization, M.B.; supervision, A.S.; project administration, M.O.; funding acquisition, M.B. All authors have read and agreed to the published version of the manuscript.

Funding

This research received no external funding.

Institutional Review Board Statement

The corresponding author declares that this manuscript is original, has not been published before, and is not currently being considered for publication elsewhere. The corresponding author confirms that the manuscript has been read and approved by all the named authors, and there are no other persons who satisfied the criteria for authorship. I further confirm that the order of authors listed in the manuscript has been approved by all of us. We understand that the corresponding author is the sole contact for the editorial process and is responsible for communicating with the other authors about progress, submissions of revisions, and final approval of proofs.

Data Availability Statement

All data generated or analyzed during this study are included in this published article.

Conflicts of Interest

The authors declare no conflict of interest.

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Figure 1. 3D and 2D projections of B 1 ( x , y , z , t ) in (14), selecting the C S e t 1 and α = 0.5 , β = 0.5 , ω = 2 , and z = t = 1 .
Figure 1. 3D and 2D projections of B 1 ( x , y , z , t ) in (14), selecting the C S e t 1 and α = 0.5 , β = 0.5 , ω = 2 , and z = t = 1 .
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Figure 2. 3D and 2D depictions of B 1 ( x , y , z , t ) in (14), selecting the C S e t 2 and B 2 = 2 , α = 0.5 , β = 0.5 , and z = t = 1 .
Figure 2. 3D and 2D depictions of B 1 ( x , y , z , t ) in (14), selecting the C S e t 2 and B 2 = 2 , α = 0.5 , β = 0.5 , and z = t = 1 .
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Figure 3. 3D and 2D silhouettes of B 1 ( x , y , z , t ) in (14), selecting the C S e t 3 and w = 0.1 , α = 0.5 , β = 0.75 , and z = t = 1 .
Figure 3. 3D and 2D silhouettes of B 1 ( x , y , z , t ) in (14), selecting the C S e t 3 and w = 0.1 , α = 0.5 , β = 0.75 , and z = t = 1 .
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Figure 4. 3D and 2D views of B 4 ( x , y , z , t ) in (17), selecting the C S e t 4 and α = 0.5 , β = 0.5 , ω = 2 , and z = t = 1 .
Figure 4. 3D and 2D views of B 4 ( x , y , z , t ) in (17), selecting the C S e t 4 and α = 0.5 , β = 0.5 , ω = 2 , and z = t = 1 .
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Figure 5. 3D and 2D presentations of B 4 ( x , y , z , t ) in (17), selecting the C S e t 5 for the selected parameters w = 0.1 , α = 0.5 , β = 0.75 , and z = t = 1 .
Figure 5. 3D and 2D presentations of B 4 ( x , y , z , t ) in (17), selecting the C S e t 5 for the selected parameters w = 0.1 , α = 0.5 , β = 0.75 , and z = t = 1 .
Symmetry 15 00165 g005
Figure 6. 3D and 2D plots of B 6 , 1 ( x , y , z , t ) in (27), selecting the C S e t 6 and α = 0.5 , β = 0.75 , ω = 2 , and z = t = 1 .
Figure 6. 3D and 2D plots of B 6 , 1 ( x , y , z , t ) in (27), selecting the C S e t 6 and α = 0.5 , β = 0.75 , ω = 2 , and z = t = 1 .
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Figure 7. 3D and 2D portraits of B 6 , 2 ( x , y , z , t ) in (28), selecting the C S e t 7 and a 2 = 0.5 , β = 0.5 , ω = 2 , and z = t = 1 .
Figure 7. 3D and 2D portraits of B 6 , 2 ( x , y , z , t ) in (28), selecting the C S e t 7 and a 2 = 0.5 , β = 0.5 , ω = 2 , and z = t = 1 .
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Figure 8. 3D and 2D portraits of B 6 , 2 ( x , y , z , t ) in (28), selecting the C S e t 8 and δ = 1 , α = 0.5 , ω = 2 , and z = t = 1 .
Figure 8. 3D and 2D portraits of B 6 , 2 ( x , y , z , t ) in (28), selecting the C S e t 8 and δ = 1 , α = 0.5 , ω = 2 , and z = t = 1 .
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Ozisik, M.; Secer, A.; Bayram, M. Soliton Waves with the (3+1)-Dimensional Kadomtsev–Petviashvili–Boussinesq Equation in Water Wave Dynamics. Symmetry 2023, 15, 165. https://doi.org/10.3390/sym15010165

AMA Style

Ozisik M, Secer A, Bayram M. Soliton Waves with the (3+1)-Dimensional Kadomtsev–Petviashvili–Boussinesq Equation in Water Wave Dynamics. Symmetry. 2023; 15(1):165. https://doi.org/10.3390/sym15010165

Chicago/Turabian Style

Ozisik, Muslum, Aydin Secer, and Mustafa Bayram. 2023. "Soliton Waves with the (3+1)-Dimensional Kadomtsev–Petviashvili–Boussinesq Equation in Water Wave Dynamics" Symmetry 15, no. 1: 165. https://doi.org/10.3390/sym15010165

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