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ORIGINAL RESEARCH article

Front. Phys., 16 September 2025

Sec. Statistical and Computational Physics

Volume 13 - 2025 | https://doi.org/10.3389/fphy.2025.1637491

Soliton dynamics and stability in the Boussinesq equation for shallow water applications

  • 1Centre for High Energy Physics, University of the Punjab, Lahore, Pakistan
  • 2Department of Mathematics and Statistics, College of Science, Imam Mohammad Ibn Saud Islamic University (IMSIU), Riyadh, Saudi Arabia
  • 3College of Computer Science, Chengdu University, Chengdu, China
  • 4Department of Mathematics, University of the Punjab, Lahore, Pakistan

This manuscript deals with the Fourth-order Boussinesq water wave equation, which is integrable and possesses soliton solutions. Boussinesq water wave equation is a vital tool for investigating nonlinear phenomena in various waves and shallow water phenomena in fluid dynamics, such as diffraction, refraction, weak nonlinearity, and shoaling. Along with fluid dynamics, it is essential in many disciplines of physics, including the transmission of long waves in shallow waters, vibrations in a nonlinear string, acoustics, laser optics, and one-dimensional nonlinear lattice waves. The Generalized Arnous approach, the new Kudryashov method, and the Modified Sub-equation method are applied to this objective. The resultant diverse solutions consist of trigonometric and hyperbolic functions. These approaches generate accurate analytical curves for soliton waves, which comprise kink, bright, and dark waves. The graphical aspects of the produced solutions are investigated using 3D-surface graphs, 2D-line graphs, and contour and polar plots, in addition to theoretical derivations. This work is novel in its integrated use of three symbolic methods to derive a broad spectrum of exact soliton solutions for the fourth-order Integrated Boussinesq water wave equation, including compound and hybrid waveforms. The inclusion of the graphical visualization, stability analysis, and open source code resources further strengthens its contribution to nonlinear wave modeling.

1 Introduction

The water wave equation (WWE) was introduced by Boussinesq in 1871 [1].

UttUxxσU2xxμUxxxx=0.(1.1)

This classic Boussinesq equation (BE) defines the shallow-water wave (SWW) solution interaction process. This equation incorporates various waves and shallow water phenomena in fluid dynamics, including shoaling, diffraction, refraction, and weak non-linearity. In addition to fluid dynamics, it is essential in many disciplines of physics, like ions found in waves in plasma, vibrations in non-linear strings, one-dimensional non-linear lattice waves, and the propagation of long waves in shallow water [2]. This study demonstrates the intricate process of how rogue waves are formed and spread in higher dimensions. In addition, we have created a new BE that can be integrated and has varied dimensions [3]. These equations provide a wide range of soliton solutions, contributing to our understanding of wave processes in many physical environments [4]. The focus will be on the fourth-order nonlinear BE.

UttσU2xxμUxxxx+νUxtUxx=0.(1.2)

Here, U(x,t) represents the surface tension of the water wave, σ denotes the nonlinearity coefficient,μ, and ν are the dispersion coefficients. We see Equation 1.2, originally proposed by Wazwaz and Kaur [4], as completely solvable. Several researchers have investigated different outcomes for nonlinear WWE. For instance, Wang et al. [5] developed advanced Boussinesq-type equations that accurately represent wave dynamics in porous media and apply them to wave propagation in deep water. Fan et al. [6] conducted a study on the use of the widely used GG-expansion method to analyze the unique solutions of non-linear evolution problems, including the sine-Gordon, Klein–Gordon equation, and BE. Numerous travel solutions were introduced by Kumari cite kumari2020abundant. Jun et al. [7] derived the Backlund transformation and Painleve expansion of Equation 2.1 to employ various solutions. Kumar et al. [8] derived the Lie point symmetry along with the lump and breather solution of Equation 2.1. Understanding wave propagation in shallow seas requires an understanding of the fourth-order nonlinear Boussinesq water wave equation model, which incorporates higher-order nonlinear and dispersive features. This increase enhances the accuracy of wave predictions, making the model particularly helpful for evaluating waves with larger amplitudes and longer wavelengths [9]. This field’s applications include coastal engineering and environmental science [10], giving essential insights for coastal development [11], navigation, and disaster prevention [12], including tsunamis and storm surges. The model’s complex features allow more realistic modeling of complicated wave interactions, assisting both theoretical research and practical coastal management.

The nonlinear Integrable Boussinesq Water Wave Equation (IBWWE) has emerged as a significant model in various physical phenomena due to its ability to incorporate both nonlinear and dispersive effects with high order accuracy. Its applications span multiple disciplines, including shallow water wave theory [13], nonlinear lattice wave theory [14], coastal engineering [15], and ion-acoustic wave dynamics in plasmas [16]. Due to its high-order structure, the IBWWE provides a refined representation of wave behavior in optical solitons in fiber media and related photonic systems. Given its broad applicability, continued investigation of the IBWWE’s soliton structures and analytical properties remains a subject of substantial interest.

Solitary waves [17], or solitons, are self-reinforcing waves that retain their shape while moving at a constant speed. These waves occur in certain nonlinear systems and are solutions to specific nonlinear partial differential equations. A key characteristic of solitary waves is that they do not dissipate or spread out as they travel, unlike typical wave packets that tend to disperse and lose their form over time. Recent developments in mathematical modeling reflect a growing emphasis on accurately characterizing the complex behaviors observed in nature and physical systems. In this context, nonlinear partial differential equations (NLPDEs) offer a robust framework for describing diverse dynamical systems. The development of advanced analytical and computational techniques has facilitated the derivation of exact solutions, enabling the deeper understanding of soliton dynamics, nonlinear wave propagation, and pattern formation. Solitary waves play a key role in several scientific and technical sectors owing to their unusual ability to keep their form and speed across vast distances and via interactions. In physics [18] and engineering [19], solitons are used to simulate stable wave phenomena in nonlinear optics [20], fluid dynamics [21], and plasma physics [22, 23], such as optical pulses in fiber-optic [24] and ion-acoustic waves in space plasmas. They are also significant in biological [25] systems for understanding nerve signal transmission and pattern generation, and in chemistry [26] for characterizing reaction-diffusion processes. In mathematics [27], solitons give insight into nonlinear dynamics [28], chaos theory [29, 30], and integrable systems.

NLPDEs develop as especially significant assets in this scientific quest. Many academics have devoted their efforts to examining distinct NLPDEs to increase their comprehension of the demonstrated behavior in the researched natural phenomena. Recent assessments have involved inquiries into the nonlinear Helmholtz equation [31], complex cubic Nonlinear Schrodinger equation [32], Klein-Fock-Gordon equation [33], Kaup–Newell Model [34], Caudrey–Dodd–Gibbon equation [35]. Studying the single-wave solutions of NLPDEs is crucial for generating improved insights and knowledge of the underlying mechanism and its valuable usage. Therefore, various academics have established novel approaches to investigate these NLPDE replies. Plenty of strong techniques such as EHF technique [36], Darboux transformation [37], exp-function method [38], generalized Kudryashov method [39], extended trial equation method [40], Hirota bilinear method [41], extended Jacobian method [42], extended direct algebraic method [43], NAE method [44], improved extended fan-sub equation method [45], multivariate generalized exponential rational integral function method [46].

Although significant advancements have been made in the computational and symbolic treatment of NLPDEs, analytical exploration of the fourth-order IBWWE, especially in its general form involving dispersive and mixed derivative terms, remains limited. Many of the available methods are limited in scope, only producing restricted forms of solutions. There is a need for comprehensive methods that can produce a border class of exact soliton solutions, including dark, bright, periodic, and compound solitons, while also analyzing the qualitative behavior of stability.

This paper proposes an integrated application of the three advanced solution methods: the Generalized Arnous method [47], the Modified Sub-Equation method [48], and the New Kudryashov method [49], to derive the border spectrum of soliton solutions to the fourth-order IBWWE. Furthermore, a linear stability conducted to assess the robustness of the obtained wave structures. To our knowledge, the combined effects of these three techniques on Equation 1.2, along with he detailed graphical and stability analysis, have not been comprehensively reported in the exciting literature. The Generalized Arnous method is an effective technique for obtaining rational-logarithmic solutions characterized by intricate nonlinear behaviors. The Modified Sub-Equation method utilizes the Riccati type transformations, is particularly suited for the construction of periodic and singular waveforms. The Kudryashov method, recognized for its symbolic strength, is for formulating exact solutions in polynomial-exponential form. Collectively, these methods offer a comprehensive analytical framework to yield a richer and more diverse set of analytical solutions, including mixed and compound solutions.

The article is summarized as follows: Section 2 outlines the mathematical analysis required to transform the nonlinear partial differential problem into an ordinary differential equation. Section 3 examines the Generalized Arnous method, its applications, and includes graphical representations. Section 4 highlights the application of the Modified Sub-Equation method. Section 5 delves into the mathematical framework and applications of the New Kudryashov method. Section 6 focuses on the stability analysis. Section 7 discusses the graphical representation of solutions, and finally, Section 8 concludes the study.

2 Formulation of governing model

Consider a general NLPDE has the following form [27, 50]:

YU,Ut,Ux,Uxt,Uxx,=0.(2.1)

Its NODE will be

PΞ,Ξ,Ξ,=0.(2.2)

Consider the traveling wave ansatz solution to simplify the NLPDEs into NLODEs [51, 52].

Ux,t=Ξξ;ξ=ωxηt.(2.3)

Here, ω represents the wave number, and η denotes the wave speed.

The fourth-order nonlinear differential Boussinesq water wave equation is given as [53]:

ΞttσΞ2xxμΞxxxx+νΞxtΞxx=0(2.4)

Now by using Equation 2.3 in Equation 2.4 we get:

μω4Ξ4Ξνωηω2+η2+2σω2ΞΞ+2σω2Ξ2=0.(2.5)

After integrating Equation 2.5 twice w. r.t ξ we get [54, 55]:

σω2Ξ2+μω4ΞΞνωηω2+η2=0.(2.6)

3 The Generalized Arnous methods

The basic steps of the generalized Arnous (GA) method are as follows [47].

Step 1: The (GA) method provides the solution of Equation 2.3 as follows:

Ξξ=α0+1=1Nαi+βigξigξi.(3.1)

where α0, αi, βi (for i = 1, 2, … , N) are real constants with condition αN2+βN20, and the function g(ξ) verified the relation

gξ2=gξ2ρlnγ.(3.2)

with,

gnξ=gξlnγn,if  n  is  even,gξlnγn1,if  n  is  odd,(3.3)

where n2, and 0<γ1. Equation 3.2 has solutions of the form:

gξ=Alnγγξ+ρ4Alnγγξ.(3.4)

Here ρ, A, and γ are real constants.

Step 2: By balancing the non-linear term with the highest order derivative in Equation 2.6, the positive integer N is determined for Equation 3.1.

Step 3: After inserting Equations 3.1-3.3 in Equation 2.6 and since gi(ξ)0, as a result of this substitution we get a polynomial of 1g(ξ)g(ξ)g(ξ). Equivalently, setting all terms with the same power equal to zero. Then, by solving this set of non-linear algebraic systems and with the help of Equation 3.2 and Equation 2.3, the solutions of Equation 1.2 may be determined.

3.1 Solutions by Generalized Arnous Method

To find the exact solution of Equation 2.6, first we find the value of positive integer N=2 and plug the value of N into Equation 3.1 then Equation 3.1 will become as follows:

Ξξ=α0+α1gξ+β1gξgξ+α2gξ2+β2gξ2gξ2.(3.5)

By inserting Equation 3.5 into Equation 2.6 together with Equation 3.2 and Equation 2.3, we have a polynomial in terms of 1g(ξ)g(ξ)g(ξ). This creates a system of algebraic equations when we aggregate all terms of the same power and put them equal to zero. The values of unknown constants are obtained.

Set 1.

α0=β2ln2γ,α1=0,β1=0,η=12ω216μω2ln2γ+ν2+4νω,α2=ρln2γβ2σ+6μω2σ.(3.6)

By putting set 1 in Equation 3.5 we obtained the exact solution as follows:

Ξ1ξ=ρln2γβ2λ+6μω2λργξ4Alnγ+Aγξlnγ2+β2Aγξln2γργξ4A2ργξ4Alnγ+Aγξlnγ2β2ln2γ.(3.7)

Set 2.

α0=ln2γβ2λ+4μω2λ,α1=0,β1=0,α2=ρln2γβ2λ+6μω2λ,ν=4μω4ln2γη2+ω2ηω.(3.8)

By putting set 1 in Equation 3.5 we obtained the exact solution as follows:

Ξ2ξ=ρln2γβ2λ+6μω2λργξ4Alnγ+Aγξlnγ2+β2Aγξln2γργξ4A2ργξ4Alnγ+Aγξlnγ2ln2γβ2λ+4μω2λ.(3.9)

4 The modified sub-equation methods

The basic steps of the Modified sub-equation (MSE) method are as follows [56].

Step 1: The (MSE) method provides the solution of Equation 2.3 as follows:

Ξξ=c0+j=1Ncjgjξ.(4.1)

c0,cj (for j = 1, 2, … , N) are non zero constants, with the condition cN0, and the function g(ξ) in Equation 4.1 satisfied the relation:

gξ=λ2g4ξ+λ1g2ξ+λ0.(4.2)

Here λ0,λ1, and λ20 are real constants. The answer to Equation 4.2 as follows.

Case 1: When λ0=0,λ1>0, and λ20 then,

g01ξ=±λ1λ2sechλ1ξ+ρ.(4.3)
g02ξ=±λ1λ2cschλ1ξ+ρ.(4.4)

Case 2: In case of constants A1and A2λ0=0,λ1>0, and λ2=±4A1A2 then,

g03ξ=±4λ1A14A12λ2coshλ1ξ+ρ+4A12+λ2sinhλ1ξ+ρ.(4.5)

Case 3: Consider λ0=λ124λ2,λ1<0, and λ2>0 then,

g04ξ=±λ12λ2tanhλ12ξ+ρ.(4.6)
g05ξ=±λ12λ2cothλ12ξ+ρ.(4.7)
g06ξ=±λ12λ2tanh2λ1ξ+ρ+ιsech2λ1ξ+ρ.(4.8)
g07ξ=±λ12λ2tanh2λ1ξ+ρ+ιsech2λ1ξ+ρ1.(4.9)

Case 4: When λ0=0,λ1<0, and λ20 then,

g08ξ=±λ12λ2secλ1ξ+ρ.(4.10)
g09ξ=±λ12λ2cscλ1ξ+ρ.(4.11)

Case 5: Consider λ0=λ124λ2,λ1>0, and λ2>0 then,

g10ξ=±λ12λ2tanλ12ξ+ρ.(4.12)
g11ξ=±λ12λ2cotλ12ξ+ρ.(4.13)
g12ξ=±λ12λ2tan2λ1ξ+ρ+sec2λ1ξ+ρ.(4.14)
g13ξ=±λ12λ2tan2λ1ξ+ρ+sec2λ1ξ+ρ1.(4.15)

Case 6: If λ0=0,λ1>0 then,

g14ξ=±4λ1eλ1ξ+ρe2λ1ξ+ρ4λ1λ2.(4.16)
g15ξ=±4λ1eλ1ξ+ρ14λ1λ2e2λ1ξ+ρ.(4.17)

Case 7: When λ0=λ1=0,λ2>0 then,

g16ξ=±1λ2ξ+ρ.(4.18)

Case 8: If λ0=λ1=0,λ2>0 then,

g17ξ=±ιλ2ξ+ρ.(4.19)

Step 2: By balancing the non-linear term with the highest order derivative in Equation 2.6, the positive integer N is determined for Equation 4.1.

Step 3: After inserting Equations 4.14.2 in Equation 2.6 and since gi(ξ)0, for (i = 1,2,3,…, N), as a result of this substitution we get a polynomial of gi(ξ). Equivalently, setting all terms with the same power equal to zero. Then by solving this set of non-linear algebraic systems and with the help of Equation 4.2 and Equation 2.3, the solutions of Equation 1.2 may be determined.

4.1 Solution by the modified sub-equation method

To find the exact solution of Equation 2.6, first we find value of positive integer N=2 and plugging the value of N in to Equation 4.1 then Equation 4.1 will become as follows:

Ξξ=c0+c1gξ+c2gξ2.(4.20)

By inserting Equation 4.20 into Equation 1.2 together with Equation 2.3 and Equation 4.2, we have a polynomial in terms of gj(ξ). This creates a system of algebraic equations when we aggregate all terms of the same power and put them equal to zero. The values of unknown constants are obtained.

Set 1:

ν=4μω4λ1+4ω4λ1+3λ0λ2+λ12μη2+ω2ηω,c0=2λ1+3λ0λ2+λ12ω2μλc1=0,c2=6μω2λ2λ.(4.21)

By putting Set 1 in Equation 4.20 we get the exact solutions as follows.

Case 1: When λ0=0,λ1>0, and λ20 then,

Ξ01x,t=2λ1+3λ0λ2+λ12ω2μσ+6μω2λ1sechλ1ξ+ρ2σ.(4.22)
Ξ02x,t=2λ1+3λ0λ2+λ12ω2μσ6μω2λ1cschλ1ξ+ρ2σ.(4.23)

Case 2: In case of constants A1and A2,λ0=0,λ1>0, and λ2=±4A1A2 then,

Ξ03x,t=96μω2λ2λ1A12σ4A12λ2coshλ1ξ+ρ+4A12+λ2sinhλ1ξ+ρ2+2λ1+3λ0λ2+λ12ω2μσ.(4.24)

Case 3: Consider λ0=λ124λ2,λ1<0, and λ2>0 then,

Ξ04x,t=2λ1+3λ0λ2+λ12ω2μσ+3μω2λ1tanh2λ1ξ2+ρ2σ.(4.25)
Ξ05x,t=2λ1+3λ0λ2+λ12ω2μσ+3μω2λ1coth2λ1ξ2+ρ2σ.(4.26)
Ξ06x,t=2λ1+3λ0λ2+λ12ω2μσ+3μω2λ1tanh2λ1ξ+ρ+Isech2λ1ξ+ρ2σ.(4.27)
Ξ07x,t=2λ1+3λ0λ2+λ12ω2μσ+3μω2λ1σtanh2λ1ξ+ρ+Isech2λ1ξ+ρ2.(4.28)

Case 4: When λ0=0,λ1<0, and λ20 then,

Ξ08x,t=2λ1+3λ0λ2+λ12ω2μσ+3μω2λ1secλ1ξ+ρ2σ.(4.29)
Ξ09x,t=2λ1+3λ0λ2+λ12ω2μσ+3μω2λ1cscλ1ξ+ρ2σ.(4.30)

Case 5: Consider λ0=λ124λ2,λ1>0, and λ2>0 then,

Ξ10x,t=2λ1+3λ0λ2+λ12ω2μσ3μω2λ1tan2λ1ξ2+ρ2σ.(4.31)
Ξ11x,t=2λ1+3λ0λ2+λ12ω2μσ3μω2λ1cot2λ1ξ2+ρ2σ.(4.32)
Ξ12x,t=2λ1+3λ0λ2+λ12ω2μσ3μω2λ1tan2λ1ξ+ρ+sec2λ1ξ+ρ2σ.(4.33)
Ξ13x,t=2λ1+3λ0λ2+λ12ω2μσ3μω2λ1σtan2λ1ξ+ρ+sec2λ1ξ+ρ2.(4.34)

Case 6: If λ0=0,λ1>0 then,

Ξ14x,t=±4λ1eλ1ξ+ρe2λ1ξ+ρ4λ1λ2.(4.35)
Ξ15x,t=±4λ1eλ1ξ+ρ14λ1λ2e2λ1ξ+ρ.(4.36)

Case 7: When λ0=λ1=0,λ2>0 then,

Ξ16x,t=2λ1+3λ0λ2+λ12ω2μσ6μω2λ2σλ2ξ+ρ2.(4.37)

Case 8: If λ0=λ1=0,λ2>0 then,

Ξ17x,t=2λ1+3λ0λ2+λ12ω2μσ+6μω2λ2σλ2ξ+ρ2.(4.38)

5 The New Kudryashov methods

Here are some important steps of the new Kudryashov method (NK).

Step 1: The NK method provides the solution of Equation 2.6 as:

Ξξ=c0+i=1Nligiξ.(5.1)

where the coefficients li for i = 0, 1, 2,…, N are constants to be determined such that lN0, and g(ξ)=1aBδξ+bBδξ is the solution of the following non-linear ODE:

gξ2=δlnBgξ214abg2ξ.(5.2)
gξ=δ2lnB2gξ18abg2ξ.(5.3)

here constants a, b, δ, and B are all non-zero, with B>0 and B1.

Step 2: Using the homogeneous balance principle, we may get the positive integer N by balancing the highest-order derivative and nonlinear variables in Equation 2.3.

Step 3: After inserting Equation 5.1 into Equation 2.6 and recognizing that g(ξ)0 we set all coefficients of gi(ξ) to zero. After that, we get particular values for a, b, and the cis by solving the resultant non-linear algebraic system. By plugging the values back into Equation 5.1 and applying the transformation of Equation 2.3, we may get a solution for Equation 1.2.

5.1 Solution by New Kudryashov method

To find the exact solution of Equation 2.6, first we find value of positive integer N=2 and plugging the value of N in to Equation 5.1 then Equation 5.1 will become as follows:

Ξξ=l0+l1gξ+l2gξ2.(5.4)

By putting the value of Equation 5.4 and Equation 5.1 in Equation 2.6, we obtain the following set of algebraic equations by equating the coefficients of different power of g(ξ) is equal to zero. The values of unknown constants are obtained.

Set 1:

μ=νωη+η2ω24lnB2δ2ω4,l0=νωη+η2ω2σω2,l1=0,l2=6abνωη+η2ω2σω2.(5.5)

By putting Set 1 in Equation 5.5, we get the exact solutions as follows:

Ξ1ξ=νωη+η2ω2σω26abνωη+η2ω2σω2aBδξ+bBδξ2.(5.6)

Set 2:

ν=4lnB2δ2μω4+η2ω2ηω,l0=4δ2μlnB2ω2σ,l1=0,l2=24lnB2abδ2μω2σ(5.7)

By putting Set 2 in Equation 5.7, we get the exact solutions as follows:

Ξ2ξ=4δ2μlnB2ω2σ+24lnB2abδ2μω2σaBδξ+bBδξ2.(5.8)

6 Stability analysis

In this section, we will discuss the stability of Equation 1.2. Consider a perturbed solution of Equation 1.2 has the form [57, 58].

Ξx,t=P+λUx,t.(6.1)

For any constant value of P, it is obvious that Equation 1.2 possesses a stable solution. U is the function of x,t, and λ is a real constant. By Inserting Equation 6.1 in Equation 1.2, we obtain the following result

λUttσλ2Uxx2μλUxxxxνλUxtλUxx=0.(6.2)

Linearized Equation 6.2.

λUttμλUxxxxνλUxtλUxx=0.(6.3)

Suppose that Equation 6.3 has the solution of the from

Ux,t=eιmxst.(6.4)

Here, m represents the normalized wave numbers, and s represents the dispersion relation. By inserting Equation 6.4 into Equation 6.3, the following result is obtained

sm=μm4m2.sm=mθμm4+m2.(6.5)

Now we’ll look at the dispersed characteristics shown in Equation 6.5. The dispersion is stable if the real component of Equation 6.5 is negative for all m values. If it is positive, the dispersion is unstable. If it is zero, the dispersion is minimal.

7 Graphical representation and discussion

The graphical solutions produced using the Modified Sub-Equation, Generalized Arnous, and Kudryashov method to illustrate the presence of a wide range of soliton solutions within the framework of IBWWE. These visualizations also demonstrate how key parameters affect the wave behavior. Specifically, increasing the dispersion coefficient μ leads to sharper and narrower wave fronts, reflecting the intensification of dispersive mechanisms. Similarly, a higher nonlinearity parameter σ yields increased amplitude and steepness, highlighting enhanced nonlinear interactions. The parameter ν plays a critical role in shaping the symmetry and phase behavior of the solutions the solution, sometimes introducing asymmetry or a deformed wave shape. These findings suggest that adjusting the model parameters allows control over wave localization, structural properties, and stability, offering practical insight into physical systems modeled by the IBWWE. The pictorial appearance of the solutions produced is investigated in this section. Specific values are supplied to the unknown constants to construct 3D and 2D graphs of the resulting solutions. The figures depicted in part (a) reflect a 3D plot, while part (b) represents the 2D line graph of the solutions, part (c) displays the Contour graph, and part (d) depicts the Polar plot. In Figure 1, the wave solution is visualized through 3D surfaces, 2D profiles, and contour maps under the parameter configuration Ξ01(x,t):ρ=1,θ=0.2,μ=1,ω=0.3,β2=1,σ=1,η=1,A=0.5, with the phase variable defined as ξ=ωxηt. The plots are generated for time slices t=1,0,1. Figure 2 presents the wave evolution corresponding to a dark solitary structure under the same parameter configuration Ξ02(x,t), where the solution is illustrated through 3D plots, 2D line profiles, and contour maps for t=3,0,3. In Figure 3, the bright solitary wave behavior is captured using the parameters Ξ01(x,t):λ0=0,λ1=1,λ2=2,μ=2,σ=1,ρ=0.8,η=0.5,ω=1,ν=8, with ξ=ωxηt, and evaluated over the time domain t=5,0,5. Figure 4 displays a dark-bright solitary wave structure governed by the constants Ξ04(x,t):   λ0=0.005,λ1=0.1,λ2=0.5,μ=2,σ=2.5,ρ=1,η=0.5,ω=0.5,ν=0.56, with ξ=ωxηt. The visual representation is provided for t=5,0,5. In Figure 5, the anti-kink solitary wave is visualized using Ξ06(x,t):λ0=0.001,λ1=0.08,λ2=1.2,μ=2,σ=2.5,ρ=2,η=2,ω=1.4,ν=0.720.65i, with ξ=ωxηt. The plots correspond to time levels t=3,0,3. Figure 6 illustrates the bright solitary wave pattern for Ξ14(x,t):λ0=0,λ1=0.5,λ2=0.5,μ=2,σ=1,ρ=1.5,η=1,ω=0.5,ν=1, with the phase ξ=ωxηt and plots evaluated for t=3,0,3. In Figure 7, the solution evolves under the parametric structure Ξ15(x,t):λ0=0,λ1=0.9,λ2=0.1,μ=1,σ=1,ρ=1,η=1,ω=0.5,ν=1.05, with ξ=ωxηt. The visualization is provided for time slices t=1,0,1. Figure 8 depicts a bright solitary wave structure governed by Ξ1(x,t):λ0=0,λ1=0.9,λ2=0.1,μ=1,σ=1,ρ=1,η=1,ω=0.5,ν=1.05, with ξ=ωxηt, and evaluated at t=3,0,3. In Figure 9, the dark solitary wave pattern is illustrated for Ξ2(x,t):λ0=0,λ1=0.9,λ2=0.1,μ=1,σ=1,ρ=1,η=1,ω=0.5,ν=1.05, using the same phase ξ=ωxηt. The solution behavior is shown for time levels t=3,0,7. Finally, Figure 10 provides the 3D surface and 2D projection visualizations reflecting the stability features of the system described by Equation 6.5, evaluated under the parameters μ=0.5, m[10,10], and θ[20,20].

Figure 1
(a) A 3D plot illustrating a multicolored surface on a grid with axes labeled x, y, and a function. (b) Two overlapping, shaded bell curves with a legend indicating time variations. (c) A vector field plot with arrows across a blue-red gradient, axes labeled x and t. (d) A polar plot with radial lines and a color gradient from purple to red, showing direction and magnitude.

Figure 1. Graphical visualization of derived solution of Equation 3.7 gives bright soliton such as (a) 3D surface, (b) 2D surface, (c) Streamline Plot (d) Polar Polt, of Ξ01(x,t):ρ=1,θ=0.2,μ=1,ω=0.3,β2=1,σ=1,η=1,A=0.5.

Figure 2
(a) A 3D surface plot shows a colorful, undulating surface representing a mathematical function, plotted against x and t axes. (b) A line plot with shaded areas displays the function z(x, t) = sin(x) at various t values, indicated by colors. (c) A vector field plot shows arrows across a gradient background, representing direction and magnitude in a 2D space. (d) A polar contour plot features concentric circles with a gradient from purple to yellow, representing function values over angles and radii, with labeled angles.

Figure 2. Graphical visualization of derived solution of Equation 3.9 gives dark soliton such as (a) 3D surface, (b) 2D surface, (c) Streamline Plot (d) Polar Polt, of Ξ02(x,t):ρ=1,θ=0.2,μ=1,ω=0.3,β2=1,σ=1,η=1,A=0.5.

Figure 3
(a) A 3D surface plot showing a wave function with varying colors from red to blue, representing different intensities over a grid. (b) A graph with multiple overlapping bell-shaped curves illustrating wave function intensities over time intervals, using colors for distinction. (c) A 2D plot with contour lines and directional arrows indicating wave movement across a grid with color variation from blue to brown. (d) A polar plot displaying wave intensities in concentric circles, ranging from blue to brown, indicating different values across angles.

Figure 3. Graphical visualization of derived solution of Equation 4.22 gives bright soliton such as (a) 3D surface, (b) 2D surface, (c) Streamline Plot (d) Polar Plot, of Ξ01(x,t):λ0=0,λ1=1,λ2=2,μ=2,σ=1,ρ=0.8,η=0.5,ω=1,ν=8.

Figure 4
(a) A 3D plot showing a surface with peaks and valleys, colored in a gradient from blue to yellow, representing a function over variables x and τ. (b) A line graph with multiple curves showing the evolution of a function over time, with labels indicating different time intervals. (c) A 2D colored contour plot with arrows indicating direction and magnitude, depicting a function over x and τ coordinates. (d) A polar plot with a color gradient from blue to red, representing the angular distribution and magnitude of a function, with radial lines and angle labels.

Figure 4. Graphical visualization of derived solution of Equation 4.25 gives dark-bright soliton such as (a) 3D surface, (b) 2D surface, (c) Streamline Plot (d) Polar Plot, of |Ξ04(x,t)|:λ0=0.005,λ1=0.1,λ2=0.5,μ=2,σ=2.5,ρ=1,η=0.5,ω=0.5,ν=0.56.

Figure 5
(a) A 3D surface plot with a colorful wave pattern, displaying a peak and trough structure against a grid. (b) A line graph showing multiple curves with different colors representing times from negative three to three, showing variation in values. (c) A contour plot overlaid with arrows indicating vector field direction, featuring a rainbow gradient. (d) A polar plot with color bands, indicating angle variations, with a legend showing values from zero point zero six to zero point six six.

Figure 5. Graphical visualization of derived solution of Equation 4.27 gives bright-dark soliton such as (a) 3D surface, (b) 2D surface, (c) Streamline Plot (d) Polar Plot, of |Ξ06(x,t)|:λ0=0.001,λ1=0.08,λ2=1.2,μ=2,σ=2.5,ρ=2,η=2,ω=1.4,ν=0.720.65I.

Figure 6
(a) A 3D surface plot showing a wave pattern with peaks and troughs in rainbow colors along the x and t axes. (b) Overlapped sine waves in different colors at specific time intervals with a legend. (c) A vector field with colorful background bands, arrows indicating the direction and magnitude. (d) A polar plot with rainbow-colored diagonal bands, labeled angles, and a color bar indicating value intensity.

Figure 6. Graphical visualization of derived solution of Equation 4.28 gives periodic soliton such as (a) 3D surface, (b) 2D surface, (c) Streamline Plot (d) Polar Plot, of |Ξ07(x,t)|:λ0=0.0006,λ1=0.05,λ2=1,μ=1,σ=1,ρ=1,η=2,ω=1.4,ν=0.720.19I.

Figure 7
(a) Three-dimensional plot showing a surface with varying elevations and colors. (b) Graph with overlapping, symmetrical plot lines in different colors, showing changes in a function over time. (c) Contour map with arrows indicating direction in a gradient field. (d) Polar plot with color gradients and angular grid, representing a rotated field.

Figure 7. Graphical visualization of derived solution of Equation 4.38 gives dark soliton such as (a) 3D surface, (b) 2D surface, (c) Streamline Plot (d) Polar Plot, of Ξ15(x,t):λ0=0,λ1=0.9,λ2=0.1,μ=1,σ=1,ρ=1,η=1,ω=0.5,ν=1.05.

Figure 8
(a) A 3D surface plot with rainbow colors representing varying values over an x, y, and z axis grid. (b) Overlapping bell curves with shaded regions demonstrating changes over time with a legend indicating different t values. (c) A 2D contour plot with rainbow colors, grid lines, and directional arrows showing gradient fields. (d) A polar plot with rainbow gradient representing angular values, marked by degree angles and a color bar indicating value range.

Figure 8. Graphical visualization of the derived solution of Equation 5.6 gives bright soliton such as (a) 3D surface, (b) 2D surface, (c) Streamline Plot (d) Polar Plot, of Ξ1(x,t):λ0=0,λ1=0.9,λ2=0.1,μ=1,σ=1,ρ=1,η=1,ω=0.5,ν=1.05.

Figure 9
(a) A 3D plot displaying a multicolored surface with a parabolic shape in a 3D grid. (b) A 2D plot with several curves showing different time intervals, shaded areas indicate variance. (c) A contour plot with arrows indicating direction on a rainbow gradient background. (d) A polar plot with a color scale showing radial variations and angles marked around the circle.

Figure 9. Graphical visualization of the derived solution of Equation 5.8 gives dark soliton such as (a) 3D surface, (b) 2D surface, (c) Streamline Plot (d) Polar Plot, of Ξ2(x,t):λ0=0,λ1=0.9,λ2=0.1,μ=1,σ=1,ρ=1,η=1,ω=0.5,ν=1.05.

Figure 10
(a) Line graph showing \(S(m)\) versus \(m\) for \(\theta = 10\), \(\theta = 30\), and \(\theta = 50\) in red, black, and blue respectively. The curves are parabolic and depict different steepness for each \(\theta\). (b) 3D surface plot of \(S(m, \theta)\) with \(m\) and \(\theta\) axes. The surface has a colorful gradient from top to bottom indicating changes in values.

Figure 10. Stability analysis of system (6.5) with μ=0.5, m = −10,10, θ = −20,20. (a) 2D curve; (b) 3D surface.

The bright soliton solution depicted in Figure 2 aligns well with theoretical expectations described in earlier studies of Boussinesq-type equations [53, 59]. As observed, increasing the dispersion parameter μ results in a narrowing of the soliton width and a sharper peak, which is consistent with the classical behavior of higher-order dispersive wave models [51]. Moreover, a rise in the nonlinear coefficient σ amplifies the soliton amplitude, supporting the expected balance between nonlinearity and dispersion.

In summary, the soliton profiles obtained in this work exhibit a broad range of wave behaviors, including bright, dark, anti-kink, periodic, and compound forms, which can be effectively modulated by tuning the model parameters. In contrast to conventional approaches such as the Hirota bilinear method, Exp-function method, or Lie symmetry techniques, which tend to yield classical solutions, the combined application of the Generalized Arnous Method, Modified Sub-Equation Method, and Kudryashov Method facilitates the systematic construction of more intricate and previously unreported wave structures. Furthermore, the inclusion of graphical visualization and linear stability analysis provides further validation of the physical relevance and reliability of the solutions. These outcomes emphasize the utility of the proposed framework as a powerful analytical framework for solving higher-order nonlinear dispersive equations pertinent to fluid dynamics, coastal engineering, and nonlinear optics.

The proposed symbolic techniques, the Generalized Arnous Method, Modified Sub-Equation Method, and New Kudryashov Method, offer a computationally efficient framework for solving nonlinear PDEs. These methods transform the original equation into a solvable algebraic system using traveling wave transformations and a closed-form ansatz. The resulting complexity is polynomial in terms of symbolic manipulation steps, making them significantly faster and more tractable than numerical methods such as finite difference or spectral schemes, which require iterative time-stepping and grid refinement. In comparison with symbolic methods like the Hirota bilinear method or Riccati/ϕ6 expansions, the proposed techniques provide greater generality in solution form, reduced reliance on fixed trial functions, and easier implementation in platforms such as Maple or Mathematica. These features collectively make the proposed methods both analytically powerful and computationally lightweight.

8 Conclusion

In this research, we applied the Generalized Arnous technique, plus the Novel Kudryashov and Modified Sub-Equation methods, to achieve accurate solutions for the fourth-order Boussinesq water wave equation which is an important tool for the investigation of nonlinear phenomena in various waves and shallow water phenomena in fluid dynamics, such as diffraction, refraction, weak non-linearity, and shoaling. It was important to apply a special wave transformation method to change the original NLPDE into a NODE to accomplish this aim. Notably, these methodologies produced a diverse variety of soliton solutions, including periodic (repeating waveforms that maintain their shape and speed while traveling, combining features of both solitary and periodic waves), bright (localized areas of elevated intensity, when the wave amplitude attains its zenith, resulting in peaks or humps within the wave profile.), dark (low-intensity areas inside a high-intensity backdrop. In these places, the wave amplitude falls below the background level, resulting in troughs or depressions in the wave profile.), dark-bright, bright-dark solitons. For a thorough comprehension of the physical processes inherent in the fourth-order BE, we graphically portrayed chosen solutions by assigning parameter values in 3D-surface graphs, 2D-line graphs, and contour and Polar plots, according to particular limitations. These graphical representations aid in deepening our knowledge of the various soliton structures originating from the equation. Additionally, we underlined the usefulness and potency of the Generalized Arnous method, the New Kudryashov, and the Modified Sub-Equation strategies in discovering soliton solutions for NLPDEs. The discovered solutions contribute greatly to expanding our grasp of the nonlinear dynamics regulating the propagation of water solitons in engineering and physical sciences. This paper tries to give helpful insights for scientists and researchers aiming to enhance their experimental activities. Moreover, there exists a possibility for widening the scope of this study by including concerns of lump interactions, researching multi-soliton situations, and analyzing the dynamics of rogue wave breathers. Such additions might improve the practical application and relevance of the research. The distinctiveness of this study lies in the unified application of three analytical techniques to systematically investigate the complex soliton dynamics in the IBWWE, yielding new solutions such as bright-dark and anti-kink solitons. The detailed stability analysis and graphical illustrations, supported by reproducible resources, extend the application of this work to both theoretical studies and practical applications in fluid dynamics, in coastal, optical, and plasma environments.

Data availability statement

The original contributions presented in the study are included in the article/Supplementary Material, further inquiries can be directed to the corresponding author.

Author contributions

KF: Supervision, Writing – review and editing. FA: Supervision, Writing – review and editing. ZL: Writing – review and editing, Supervision. EH: Software, Writing – review and editing, Writing – original draft.

Funding

The author(s) declare that financial support was received for the research and/or publication of this article. This work was supported and funded by the Deanship of Scientific Research at Imam Mohammad Ibn Saud Islamic University (IMSIU) (grant number IMSIU-DDRSP2503).

Conflict of interest

The authors declare that the research was conducted in the absence of any commercial or financial relationships that could be construed as a potential conflict of interest.

The handling editor WM declared a past co-authorship with the author(s) ZL and EH.

Generative AI statement

The author(s) declare that no Generative AI was used in the creation of this manuscript.

Any alternative text (alt text) provided alongside figures in this article has been generated by Frontiers with the support of artificial intelligence and reasonable efforts have been made to ensure accuracy, including review by the authors wherever possible. If you identify any issues, please contact us.

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Keywords: fourth-order boussinesq water wave equation, modified sub-equation method, new Kudryashov method, riccati equation method, solitary wave solutions

Citation: Farooq K, Alshammari FS, Li Z and Hussain E (2025) Soliton dynamics and stability in the Boussinesq equation for shallow water applications. Front. Phys. 13:1637491. doi: 10.3389/fphy.2025.1637491

Received: 29 May 2025; Accepted: 04 August 2025;
Published: 16 September 2025.

Edited by:

Wen-Xiu Ma, University of South Florida, United States

Reviewed by:

Saravana Prakash Thirumuruganandham, SIT Health, Ecuador
Sadique Rehman, Kanazawa University, Japan

Copyright © 2025 Farooq, Alshammari, Li and Hussain. This is an open-access article distributed under the terms of the Creative Commons Attribution License (CC BY). The use, distribution or reproduction in other forums is permitted, provided the original author(s) and the copyright owner(s) are credited and that the original publication in this journal is cited, in accordance with accepted academic practice. No use, distribution or reproduction is permitted which does not comply with these terms.

*Correspondence: Zhao Li, bGl6aGFvMTAuMjZAMTYzLmNvbQ==

Disclaimer: All claims expressed in this article are solely those of the authors and do not necessarily represent those of their affiliated organizations, or those of the publisher, the editors and the reviewers. Any product that may be evaluated in this article or claim that may be made by its manufacturer is not guaranteed or endorsed by the publisher.