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Article

Shock Waves of the Gerdjikov–Ivanov Equation Using the Adomian Decomposition Schemes

1
Department of Mathematics and Statistics, College of Science, University of Jeddah, Jeddah 23445, Saudi Arabia
2
Department of Mathematics, College of Science, University of Bisha, P.O. Box 551, Bisha 61922, Saudi Arabia
*
Author to whom correspondence should be addressed.
Mathematics 2025, 13(16), 2686; https://doi.org/10.3390/math13162686
Submission received: 6 July 2025 / Revised: 11 August 2025 / Accepted: 12 August 2025 / Published: 20 August 2025

Abstract

Analytical solutions for the complex-valued nonlinear Gerdjikov–Ivanov (GI) equation have been studied extensively using integrability-based methods. In contrast, numerical and semi-analytical exploration remains relatively underdeveloped. Thus, the present study deploys both the traditional Adomian decomposition method (ADM) and its improved version (IADM) to explore the computational relevance of the GI equation to shock waves against a benchmark exact soliton solution. The findings indicate that both methods are effective in addressing the GI equation, with the improved method demonstrating an enhancement in the stability of the convergence under specific conditions. This work offers the first systematic semi-analytic and numerical evaluation of the GI equation, introducing practical implementation guidelines.

1. Introduction

A substantial amount of research has been conducted over a considerable period of time on soliton molecules in optical fibers, metamaterials, and photonic crystal fibers (PCFs) [1]. Telecommunications advancements require a thorough understanding of soliton propagation in various waveguide structures and are governed by dissimilar nonlinear evolution equations [2,3,4,5]. Indeed, among the most outstanding models are two very important equations: the nonlinear Schrodinger equations (NLSEs) and the derivative NLSEs (DNLSEs) [6,7,8]. The DNLSEs can restore higher-order nonlinear effects in optical systems [9,10]. In addition, when accounting for higher-order nonlinear effects, the DNLSEs are regarded as a long-wave, small-amplitude model applicable in a wide array of disciplines, including quantum field theory and short light pulses [11,12]. Moreover, the categories of DNLSEs are referred to as DNLSE I, DNLSE II, and DNLSE III, respectively [13]. Moreover, the immense practical application of these systems has led to their massive development of analytical methods and a limited number of numerical methods in recent decades. Notably, DNLSE III corresponds to the Gerdjikov–Ivanov (GI) equation, which serves as the core focus of this study due to its rich structure and relevance in nonlinear wave analysis. GI equation has widespread applications in integrable systems, nonlinear optics, fluid dynamics, and quantum field theory [14,15].
In recent years, significant attention has been directed toward semi-analytic methods for solving nonlinear Schrödinger-type equations, particularly using the Adomian decomposition method (ADM) and its variants. Kapoor et al. (2022) [16] introduced the Shehu transform-based ADM (STADM) to derive analytical series solutions for multiple forms of the time fractional Schrödinger equation, demonstrating convergence without requiring discretization.
Similarly, El-Ajou et al. (2024) [17] applied an enhanced residual power series method, comparing it to the ADM, homotopy perturbation, homotopy analysis, and variational iteration techniques to solve time fractional Schrödinger equations. They showed that series-based approaches—including the ADM—remain competitive in terms of the simplicity and accuracy when benchmarked against multiple semi-analytic methods.
Although most recent ADM-based work focuses on fractional or generalized NLSEs, very few studies have extended these methods to DNLSEs such as the Gerdjikov–Ivanov equation.
In addition, the recent literature confirms that while the Gerdjikov–Ivanov (GI) equation has been thoroughly examined using integrability-based methods [18,19,20]—such as Darboux transformations, Riemann–Hilbert frameworks, and extended algebraic techniques—there is a notable absence of studies applying the Adomian decomposition method (ADM) or its improved variant (IADM) directly to GI equation or benchmarked against analytic soliton structures.
The present study is motivated precisely by this observation, which presents a numerical perspective for solving the GI equation, benchmarked against an exact one-soliton solution via Kudryshov’s method. The intended method is based upon the application of the classical Adomian decomposition method (ADM) [21,22], together with its enhanced version, the improved Adomian decomposition method (IADM) [23,24]. Certainly, the choice of ADM-based schemes for tackling the GI equation is associated with their high efficacy in effectively handling functional and integral problems.
In the same vein, the arrangement of the present study is as follows. Section 2 provides some preambles on the governing equation, Section 3 presents the outlines of the adopted decomposition methods, Section 4 supplies the numerical results and graphical representations, while Section 5 presents some concluding notes.

2. Governing Equation

The Gerdjikov–Ivanov equation arises naturally within the framework of derivative NLSE hierarchies, and its similarity reductions using Wronskian or affine Lie methods have been studied [25,26].
The dimensionless form of the governing GI equation reads as follows [27,28]:
i q t + a q x x + b q 4 q + i c q 2 q x * = 0 ,
where q = q x , t is the one-dimensional complex wave profile, together with q * = q * x , t , its conjugate. To break down the equation, the second-order dispersion term has the coefficient a , while b and c are non-zero constants for the quintic nonlinearity term and for the self-phase modulation and the derivative nonlinearity term, respectively; in addition, i is the known imaginary number.

3. Methodology

This section provides the outlines of the steps of the deployed ADM and IADM for solving the leading GI equation. Certainly, these methods possess various recompenses, including high-precision approximations to the exact analytical solution—when it exists—without resorting to perturbation, discretization, or linearization.

3.1. Adomian Decomposition Method

The present subsection provides a complete description of the ADM for the GI equation. This method was discovered by George Adomian [21,22,29] while tackling some functional equations. Remarkably, the purported Adomian polynomials are used to approximate the involved nonlinear terms arising from the equations, in the case of differential and integral equations. In addition, this method has undergone several improvements, including the IADM [23,24,30], among others.
Begin by re-expressing the partial differential equation in Equation (1) as follows:
F q x , t = g x , t ,
where F is a differential operator, which includes both nonlinear and linear terms. Hence, representing Equation (1) through operator form as
L q x ,   t + R q x ,   t + N q x ,   t = g x ,   t ,
where L is a higher-order linear differential operator defined as L = t ,   R is a linear operator in x , which is the variable of the coefficient a in Equation (1)—namely, q x x , and N is a nonlinear operator, and g is a nonhomogeneous term; in this particular case, based on the GI equation in Equation (1), g is equal to zero. Thus, rewrite Equation (3) with respect to the linear operator to get
i L q + a q x x + b q 4 q + i c q 2 q x * = 0
Accordingly, application of the inversion operator L 1 = 0 t d t to Equation (4) gives the following:
i 0 t q d t + L 1 a q x x + L 1 b q 4 q + L 1 i c q 2 q x * = 0
Note that only the first term is computed to get the solution term q x ,   t on the left-hand side and moving the other terms to the right-hand side. Simplify Equation (5) as follows:
q x ,   t =   q x , 0 +   L 1 i a q x ,   t x x + i b q x ,   t 4   q x ,   t c q x ,   t 2   q x ,   t x *
with q x , 0 as the initial condition as a result of applying the inversion operator. Recall, the solution function q ( x ,   t ) is decomposed through the ADM procedure as a series in the following form:
q ( x ,   t )   =   n = 0 q n x ,   t
Moreover, the nonlinear term is broken down using an infinite series of polynomials, referred as Adomian polynomials, as follows [21,22,29]:
A n = 1 n ! d n d λ n N i = 0 n λ i q i x , t λ = 0 ,   n   =   0 ,   1 ,   2 ,  
Accordingly, the explicit expression for the nonlinear term N in the latter formula is plainly obtained from Equation (6) as follows:
N = i b q n ( x ,   t ) 4   q n x ,   t c q n ( x ,   t ) 2 q n ( x ,   t ) x *
Next, utilize Equations (7) and (8) in Equation (6) to get
n = 0 q n x ,   t = q n x , 0 + L 1 i a n = 0 q n ( x ,   t ) x x   + n = 0 A n    
Further rewrite to form the recurrence relation. Thus, the resulting ADM scheme for the governing GI equation is obtained from the latter equation as follows:
q 0 x , t =   q 0 x , t ,
q k + 1 x ,   t = L 1 i a q k x ,   t x x + A k ,   k = 0,1 , 2 ,
Finally, upon using Equations (11) and (12), obtain the resultant approximate ADM solution for Equation (6) as follows:
q x ,   t n = 0 k q n x ,   t
With
lim k n = 0 k q n x ,   t = q x , t
In this regard, we have established a systematic approach for applying the ADM to the GI equation, demonstrating how the decomposition leads to manageable terms for computation with efficiency in generating a series solution.

3.2. Improved Adomian Decomposition Method

The method of the IADM [23,24,30] is introduced as an enhancement, designed to address some of the limitations associated with its forerunner. Thus, the present subsection provides an outline of the IADM when used on the leading GI equation.
To start, transform the complex-valued function q x , t in Equation (1) into the sum of real-valued functions q 1 ( x , t ) and q 2 ( x , t ) as follows:
q x , t = q 1 x , t + i q 2 x , t
Thus, upon substituting Equation (15) into Equation (1), obtain the following system of equations:
q 1 t + a q 2 x x + b q 2 5 + q 1 4 u 2 + 2 q 1 2 q 2 3 + c q 1 2 q 1 x q 2 2 q 1 x + 2 q 1 q 2 q 2 x = 0 ,
q 2 t + a q 1 x x + b q 1 5 + q 1 q 2 4 + 2 q 1 3 q 2 2 + c q 1 2 q 2 x q 2 2 q 2 x 2 q 1 q 2 q 1 x = 0
where
q 1 x , 0 = R q x , 0 ,
q 2 x , 0 = I q x , 0
are the related initial conditions that arise from the real and imaginary parts of the imposed initial condition in Equation (40). Moreover, based on the traditional ADM process [21,22,29], the solution for the system in Equations (16) and (17) is decomposed into an infinite summation as follows:
q 1 x , t = n = 0 q 1 n x , t ,  
q 2 x , t = n = 0 q 2 n x , t
with q 1 n ,   q 2 n ,   ( n     0 ) to be obtained recursively. Thus, perform one further re-write Equations (16) and (17) using the operator L = / t as follows:
L q 1 + a q 2 x x + b q 2 5 + q 1 4 q 2 + 2 q 1 2 q 2 3 + c q 1 2 q 1 x q 2 2 q 1 x + 2 q 1 q 2 q 2 x = 0 ,
L q 2 + a q 1 x x + b q 1 5 + q 1 q 2 4 + 2 q 1 3 q 2 2 + c q 1 2 q 2 x q 2 2 q 2 x 2 q 1 q 2 q 1 x = 0
Accordingly, carrying out the inversion process using the operator L 1 on Equations (22) and (23), obtain
0 t q 1 d t + L 1 a q 2 x x + b q 2 5 + q 1 4 q 2 + 2 q 1 2 q 2 3 + c q 1 2 q 1 x q 2 2 q 1 x + 2 q 1 q 2 q 2 x = 0 ,
0 t q 2 d t + L 1 a q 1 x x + b q 1 5 + q 1 q 2 4 + 2 q 1 3 q 2 2 + c q 1 2 q 2 x q 2 2 q 2 x 2 q 1 q 2 q 1 x = 0
Simplify them as follows:
q 1 x , t = q 1 x , 0 L 1 a q 2 x x L 1 b q 2 5 + q 1 4 q 2 + 2 q 1 2 q 2 3 + c q 1 2 q 1 x q 2 2 q 1 x + 2 q 1 q 2 q 2 x ,
q 2 x , t = q 2 x , 0 + L 1 [ a q 1 x x ]   + L 1 b q 1 5 + q 1 q 2 4 + 2 q 1 3 q 2 2 + c q 1 2 q 2 x q 2 2 q 2 x 2 q 1 q 2 q 1 x
Further, when indicating the nonlinear terms in Equations (26) and (27) as
N 2 = b q 2 5 + q 1 4 q 2 + 2 q 1 2 q 2 3 + c q 1 2 q 1 x q 2 2 q 1 x + 2 q 1 q 2 q 2 x ,
N 1 = b q 1 5 + q 1 q 2 4 + 2 q 1 3 q 2 2 + c q 1 2 q 2 x q 2 2 q 2 x 2 q 1 q 2 q 1 x ,
they tend to serve as the related Adomian polynomials in two-system equations. Thus, substituting Equations (20), (21), (28) and (29) into Equations (26) and (27) gives
n = 0 q 1 n x , t = q 1 x , 0 L t 1 n = 0 a q 2 x , t x x L t 1 n = 0 N 2 , n ,
n = 0 q 2 n x , t = q 2 x , 0 L t 1 n = 0 a q 1 x , t x x L t 1 n = 0 N 1 , n ,
where N 1 , n and N 2 , n are Adomian polynomials computed accordingly from Equation (8). Furthermore, with the help of the ADM procedure, the improved recurrent scheme for the GI equation is thus acquired through Equations (30) and (31) as follows:
q 1,0 x , t = q 1 x , 0 = R q x , 0 ,
q 2,0 x , t = q 2 x , 0 = I q x , 0 ,
q 1 ,   k + 1 x , t = L t 1 a q 2 , k + 1 x , t x x L t 1 N 2 , k + 1 ,
q 2 ,   k + 1 x , t = L t 1 a q 1 , k + 1 x , t x x + L t 1 N 1 , k + 1 .
In the same manner as in the previous subsection, obtain the resultant approximate IADM solution from Equations (16), (17) and Equations from (32)–(35), as
q x ,   t n = 0 k q 1 , n x ,   t   + i n = 0 k q 2 , n x ,   t  
with
lim k n = 0 k q 1 , n x ,   t = q 1 x , t ,
lim k n = 0 k q 2 , n x ,   t = q 2 x , t

4. Results and Graphical Illustrations

This section presents the graphical and numerical validation of the proposed ADM and IADM schemes using relevant initial conditions and exact analytical solutions for the GI equation, as outlined in [31]. Numerical simulations and visualizations are conducted using Maple 2024, which facilitates symbolic computation and high-precision plotting.
To validate the efficiency of the ADM and IADM, the following exact solution for the GI equation is adopted as a benchmark in the analysis:
q x , t = e i ϑ x κ + 1 4 a t η 2 4 κ 2 A 1 1 + d e η x t υ
where κ , η , d , υ and A 1 are non-zero constant parameters. Note that the initial condition is
q x , 0 = e i ϑ x κ A 1 1 + d e η x
Take into consideration the set of the solution
b = 3 a η 2 4 A 1 2 , c = a η 2 β κ A 1 κ A 1 ,   and   ω = 1 4 a η 2 4 κ 2
Table 1 presents the parameter values used in the numerical simulations. These values are determined through multiple preliminary iterations and subsequently held fixed to ensure consistent and valid comparisons for the ADM and IADM through the benchmarked exact solution.
Table 2 reports the resulting absolute errors from the numerical simulations, for the temporal variable at t = 0.0 , 0.1 , 0.2 , 0.3 , 0.4 , 0.5 , with the spatial variable at x = 0 and x = 2 . The corresponding numerical values are provided in Appendix A. These variations are indicative of similar behavior throughout the whole domains and thus suffice to validate the proposed methods. Utilize the absolute error, defined as ε = q a p p r o x q e x a c t , where q a p p r o x and q e x a c t denote the approximate and exact solutions, respectively. This pointwise absolute error is commonly employed in numerical analysis for assessing the local accuracy [32].
Figure 1 and Figure 2 present graphical illustrations of the ADM and IADM solutions against the exact solution across time variations. In each figure,
  • the exact solution is plotted as a solid yellow line,
  • the ADM approximations are shown with a blue line,
  • the IADM approximations are denoted by a red dotted curve.
This color-coded distinction allows the clearest visual differentiation of each method’s performance relative to the exact solution.
The ADM and the IADM are applied to the GI equation and compared with Kudryashov’s exact solution for t { 0 ,   0.1 ,   0.2 ,   0.3 ,   0.4 ,   0.5 } . The numerical results show excellent agreement between the numerical and exact profiles, with the curves being visually indistinguishable at all the tested times.
As demonstrated in Table 2, the improved ADM (IADM) consistently delivers significantly lower pointwise absolute errors compared to the classical ADM—particularly evident at ( t = 0.5 ,   x = 0 ), where the ADM’s error spikes, while the IADM maintains accuracy. This supports prior theoretical expectations that a convergence control parameter accelerates series decay and extends convergence regions, enhancing the numerical stability in challenging regimes [33].
The graphical comparisons confirm that both the ADM and IADM preserve similar behavior of maintaining tight alignment with the exact solution profile. Moreover, the error profiles indicate that both methods achieve high accuracy, with maximum absolute errors typically in the order of 10 7 or smaller.
For t = 0 , the errors vanish as expected due to the exact initial condition matching. The peak errors occur at intermediate times ( t 0.2     t 0.4 ) and align with regions of steep gradients in the exact solution, reflecting local truncation effects. Across all the cases, the IADM yields slightly smaller errors than the ADM, particularly for mid-range t , while requiring comparable computational effort. The error distributions remain smooth and symmetric, with no evidence of spurious oscillations or boundary-related growth.
These results confirm that the ADM and IADM are both robust and accurate for solving higher-order nonlinear dispersive equations, with the IADM offering a marginal accuracy improvement. Both methods preserve the stability over the spatial and temporal ranges considered, supporting their suitability for long-time wave propagation simulations. The demonstrated agreement with the exact solution validates these approaches as reliable semi-analytical tools for the GI equation and related nonlinear systems.

5. Conclusions

The Gerdjikov–Ivanov (GI) equation is a prominent derivative nonlinear Schrödinger model exhibiting strong nonlinearity and rich wave dynamics, such as shock and soliton structures. Its nonlinear nature poses significant analytical and computational challenges. The Adomian decomposition method (ADM) addresses this by decomposing the solution into an infinite series and handling nonlinear terms via Adomian polynomials. This technique avoids linearization and often yields rapidly converging semi-analytic solutions under appropriate initial and boundary conditions, with minimal computational cost. In contrast, its improved version (IADM) enhances the numerical stability, especially in problems with strong nonlinearity or complex boundary conditions.
In this study, both the ADM and IADM are applied to the GI equation. While the ADM provides a straightforward, efficient approximation framework, the IADM refines it to achieve faster convergence and higher accuracy. Importantly, both methods retain the equation’s inherent nonlinear structure without recourse to perturbation or discretization. Combined, the ADM and IADM form a versatile and robust toolkit for semi-analytical resolution of nonlinear PDEs—including the GI equation. As a future direction, we intend to implement a finite difference scheme to provide a comparative numerical study that further validates and benchmarks the performance of the proposed ADM and IADM approaches. Moreover, the extension to the 2D Gerdjikov–Ivanov equation represents an important direction that we aim to pursue in upcoming work.

Author Contributions

F.A., A.S.H.F., A.A.A. (A. A. AlQarni), A.A.A. (A. A. Alshaery) and H.O.B.: conceptualization, methodology, writing—original draft preparation, data curation, supervision. All authors have read and agreed to the published version of the manuscript.

Funding

This research received no external funding.

Data Availability Statement

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

Conflicts of Interest

The authors declare no conflicts of interest.

Appendix A

Table A1. Numerical results for specific values of the exact solution and the ADM and IADM numerical approximations.
Table A1. Numerical results for specific values of the exact solution and the ADM and IADM numerical approximations.
t x Exact ValueADM ApproximationIADM Approximation
0 0 0.007070714261 + i   0.00007070949961 0.007070714259 + i   0.00007070949959 0.007070714259 + i   0.00007070949959
0 2 0.003452404990 i   0.00003452520074 0.003452404990 i   0.00003452520074 0.003452404990 i   0.00003452520074
0.1 0 0.007070799102 + i   0.00007106378209 0.007070705422 + i   0.00007088605532 0.007070705384 + i   0.00007088605406
0.1 2 0.003452482733 i   0.00003435340595 0.003452399958 i   0.00003442017916   0.003452399962 i   0.00003442017920
0.2 0 0.007070883923 + i   0.00007141807327 0.007070696585 + i   0.00007106261106 0.007070696435 + i   0.00007106260602  
0.2 2 0.003452560470 i   0.00003418160348 0.003452394926 i   0.00003431515757 0.003452394941 i   0.00003431515772
0.3 0 0.007070968727 + i   0.00007177237300 0.007070687748   + i   0.00007123916679 0.007070687410 + i   0.00007123915545
0.3 2 0.003452638200 i   0.00003400979335 0.003452389894 i   0.00003421013599 0.003452389928 i   0.00003421013632
0.4 0 0.007071053510 + i   0.00007212668147 0.007070678911 + i   0.00007141572252 0.007070678310 + i   0.00007141570237
0.4 2 0.003452715919 i   0.00003383797552 0.003452384862 i   0.00003410511441 0.003452384922 i   0.00003410511499
0.5 0 0.007071138276 + i   0.00007248099850 0.007070670074 + i   0.00007159227825 0.007070669135 + i   0.00007159224677
0.5 2 0.003452793635 i   0.00003366615004 0.003452379830 i   0.00003400009282 0.003452379924 i   0.00003400009373
Note: Values are shown to 12 significant digits for clarity; original data contained greater precision.

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Figure 1. (af) reveal the comparisons of the exact solution, via Kudryashov’s method, and the numerical solutions obtained via the Adomian decomposition method (ADM) and the iterative Adomian decomposition method (IADM) for the Gerdjikov–Ivanov (GI) equation. At t { 0 , 0.1 , 0.2 , 0.3 , 0.4 , 0.5 } , o v e r   t h e   s p a t i a l   d o m a i n 20 < x < 20
Figure 1. (af) reveal the comparisons of the exact solution, via Kudryashov’s method, and the numerical solutions obtained via the Adomian decomposition method (ADM) and the iterative Adomian decomposition method (IADM) for the Gerdjikov–Ivanov (GI) equation. At t { 0 , 0.1 , 0.2 , 0.3 , 0.4 , 0.5 } , o v e r   t h e   s p a t i a l   d o m a i n 20 < x < 20
Mathematics 13 02686 g001aMathematics 13 02686 g001b
Figure 2. (af) present the error profiles of the Adomian decomposition method (ADM) and the iterative Adomian decomposition method (IADM) for the Gerdjikov–Ivanov (GI) equation. At t 0 , 0.1 , 0.2 , 0.3 , 0.4 , 0.5 , over the spatial domain 1 < x < 1 .
Figure 2. (af) present the error profiles of the Adomian decomposition method (ADM) and the iterative Adomian decomposition method (IADM) for the Gerdjikov–Ivanov (GI) equation. At t 0 , 0.1 , 0.2 , 0.3 , 0.4 , 0.5 , over the spatial domain 1 < x < 1 .
Mathematics 13 02686 g002aMathematics 13 02686 g002b
Table 1. Reveals the parameter values used in the resulting simulations via the Adomian decomposition method (ADM) and the iterative Adomian decomposition method (IADM), benchmarked against the exact solution via Kudryashov’s method for the Gerdjikov–Ivanov (GI) equation.
Table 1. Reveals the parameter values used in the resulting simulations via the Adomian decomposition method (ADM) and the iterative Adomian decomposition method (IADM), benchmarked against the exact solution via Kudryashov’s method for the Gerdjikov–Ivanov (GI) equation.
A 1 υ a ϑ κ η d
0.0001 0.0005 0.002 0.01 0.01 1 1
Table 2. Presents the absolute errors at specific temporal and spatial values the Adomian decomposition method (ADM) and the iterative Adomian decomposition method (IADM), benchmarked against the exact solution via Kudryashov’s method for the Gerdjikov–Ivanov (GI) equation.
Table 2. Presents the absolute errors at specific temporal and spatial values the Adomian decomposition method (ADM) and the iterative Adomian decomposition method (IADM), benchmarked against the exact solution via Kudryashov’s method for the Gerdjikov–Ivanov (GI) equation.
t x ADM Error ValuesIADM Error Values
0 0 2.000099998 × 10 12 2.000099998 × 10 12
0 2 0.0 0.0
0.1 0 2.00904 × 10 7 2.00923 × 10 8
0.1 2 1.06350 × 10 7 1.06347 × 10 7
0.2 0 4.01807 × 10 7 4.01881 × 10 7
0.2 2 2.12700 × 10 7 2.12688 × 10 7
0.3 0 6.02708 × 10 7 6.02876 × 10 7
0.3 2 3.19050 × 10 7 3.19023 × 10 7
0.4 0 8.03608 × 10 7 8.03906 × 10 7
0.4 2 4.25396 × 10 7 4.25349 × 10 7
0.5 0 1.00450 × 10 6 1.00497 × 10 6
0.5 2 5.31745 × 10 7 5.31672 × 10 7
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MDPI and ACS Style

Althrwi, F.; Farhat, A.S.H.; AlQarni, A.A.; Bakodah, H.O.; Alshaery, A.A. Shock Waves of the Gerdjikov–Ivanov Equation Using the Adomian Decomposition Schemes. Mathematics 2025, 13, 2686. https://doi.org/10.3390/math13162686

AMA Style

Althrwi F, Farhat ASH, AlQarni AA, Bakodah HO, Alshaery AA. Shock Waves of the Gerdjikov–Ivanov Equation Using the Adomian Decomposition Schemes. Mathematics. 2025; 13(16):2686. https://doi.org/10.3390/math13162686

Chicago/Turabian Style

Althrwi, Fadwa, Aisha S. H. Farhat, A. A. AlQarni, H. O. Bakodah, and A. A. Alshaery. 2025. "Shock Waves of the Gerdjikov–Ivanov Equation Using the Adomian Decomposition Schemes" Mathematics 13, no. 16: 2686. https://doi.org/10.3390/math13162686

APA Style

Althrwi, F., Farhat, A. S. H., AlQarni, A. A., Bakodah, H. O., & Alshaery, A. A. (2025). Shock Waves of the Gerdjikov–Ivanov Equation Using the Adomian Decomposition Schemes. Mathematics, 13(16), 2686. https://doi.org/10.3390/math13162686

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