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Article

Soliton Solution of the Nonlinear Time Fractional Equations: Comprehensive Methods to Solve Physical Models

1
School of Mathematical and Statistical Sciences, University of Galway, University Road, H91 TK33 Galway, Ireland
2
School of Mathematics, Iran University of Science and Technology, Narmak, Tehran 13114-16846, Iran
3
Department of Mathematics, Science Faculty, Firat University, Elazig 23119, Turkey
4
Department of Medical Research, China Medical University, Taichung 40402, Taiwan
*
Author to whom correspondence should be addressed.
Axioms 2024, 13(2), 92; https://doi.org/10.3390/axioms13020092
Submission received: 13 December 2023 / Revised: 19 January 2024 / Accepted: 22 January 2024 / Published: 30 January 2024

Abstract

:
In this paper, we apply two different methods, namely, the G G -expansion method and the G G 2 -expansion method to investigate the nonlinear time fractional Harry Dym equation in the Caputo sense and the symmetric regularized long wave equation in the conformable sense. The mentioned nonlinear partial differential equations (NPDEs) arise in diverse physical applications such as ion sound waves in plasma and waves on shallow water surfaces. There exist multiple wave solutions to many NPDEs and researchers are interested in analytical approaches to obtain these multiple wave solutions. The multi-exp-function method (MEFM) formulates a solution algorithm for calculating multiple wave solutions to NPDEs and at the end of paper, we apply the MEFM for calculating multiple wave solutions to the (2 + 1)-dimensional equation.

1. Introduction

The study of nonlinear physical models relies on the analysis of wave solutions for nonlinear equations. Recently, numerous and varied methods have been applied to solve NPDEs, such as the Trial equation method [1], functional variable method [2], Sine–Gordon expansion method [3], first integral method [4], and so on [5,6,7,8,9,10,11,12].
The objective of the present paper is to apply two methods, namely, the G G -expansion method and the G G 2 -expansion method [13], to construct new solutions for the nonlinear time fractional Harry Dym (HD) equation and the symmetric regularized long wave (SRLW) equation.
The nonlinear time fractional Harry Dym equation is given by [14]
D t α u ( x , t ) = u 3 ( x , t ) u x x x ( x , t ) , 0 < α 1 , u ( x , 0 ) = a 3 b 2 x 2 3 ,
where D α is the fractional derivative of order α in the Caputo sense.
For α = 1 , (1) reduces to the classical nonlinear Harry Dym equation
u t = u 3 u x x x ,
and the exact solution of (2) is given by
u ( x , t ) = a 3 b 2 ( x + b t ) 2 3 .
Equation (2) was presented by Harry Dym while trying to shift several results about isospectral flow to the string equation. The relation between the classical string problem and the HD, with variables springy parameter, was introduced in 1979 and the HD equation could be considered as a particular case of a broad class of NPDEs, and also the relation between Korteweg de Vries (KdV) equations and the HD equations was considered. The HD equation describes a system in which nonlinearity and dispersion are coupled together. It has an infinite number of conservation laws and does not have the Painleve property. Many authors used numerical and analytical techniques to solve the HD equation. Singh, Kumar, and Kiliman considered the HD equation by means of the homotopy perturbation Sumudu transform technique and the Adomian decomposition technique in Ref. [15] and to obtain the solution of the HD equation with approximate analysis, Saleh and Ghiasi applied the homotopy analysis technique in Ref. [16]. Mokhtari used variational iteration, power series, and direct integration to obtain exact solutions for traveling waves of the HD equation [17], and this equation was solved by Fonseca through the Lattice–Boltzmannn technique in Ref. [18]. Rawashdeh applied the fractional reduced differential transform technique to calculate the solutions to the HD equation in Ref. [19], and the q-homotopy analysis technique is used to find analytical solutions of the HD equation in Ref. [20]. Mukherij and Assabaai applied the Lie group technique to present the numerical solutions of the HD equation in Refs. [21,22], and Shunmugarajan used the homotopy analysis technique to obtain a solution that could approximate the HD equation. The homotopy perturbation technique along with the reconstruction of the variational iteration technique were applied by Khorshidi and Soltani to get the analytical solution of the HD equation in Ref. [23].
The SRLW equation is given as follows [24]:
D t 2 γ u + D x 2 γ u + u D t γ ( D x γ u ) + D x γ u D t γ u + D t 2 γ ( D x 2 γ u ) = 0 , 0 < γ 1 ,
where D γ , is the conformable derivative of order γ .
Equation (3) arises in diverse physical applications such as ion sound waves in plasma. For γ = 1 , this equation was noted to depict space-charge waves and weekly nonlinear ion acoustic and the real part of u ( x , t ) is related to the dimensionless fluid velocity with a decay condition.
The abovementioned methods are usually about traveling wave solutions of NPDEs. However, there are multiple wave solutions (MWSs) to many NPDEs, for instance, multi soliton solutions to several significant models such as the Harris–Benedict equation [25,26], and the KDV equation [27]. Thus, one is interested in presenting a method for obtaining MWSs to NPDEs and the MEFM formulates a solution algorithm for calculating MWSs to NPDEs.
At the end of the article, we apply the MEFM [28] for calculating MWSs to the following (2 + 1)-dimensional equation [29]
u y t + α u x x + β u y y + u x y = 0 , α , β C .
for the following special cases
u y t + 5 u x x + ( 1 ) 2 3 5 u y y + u x y = 0 ,
and
u y t 5 u x x 5 u y y + u x y = 0 .
We get multi classes of solutions including one, two, and triple-soliton solutions. All the computations have been performed applying the software package Maple 15. The gained solutions contain three classes of soliton wave solutions in terms of one, two, and three wave solutions, which are displayed graphically, highlighting the effects of non-linearity. Besides, the multiple soliton solutions are proposed with more arbitrary autocephalous parameters, in which the one, two, and triple solutions are localized in every direction in space. The obtained results have shown a major impact on wave behavior and can be applied in different branches of science, especially in fluid dynamics, to investigate the understanding of complex physical phenomena.
The MEFM applied by some of the powerful authors for different nonlinear equations such as the (3 + 1)-dimensional generalized KP and BKP equations [30], the nonlinear evolution equations [31], the generalized (1 + 1)-dimensional, and (2 + 1)-dimensional Ito equations [32], the new (2 + 1)-dimensional KdV equation [33], the (2 + 1)-dimensional Calogero–Bogoyavlenskii–Schiff equation [34], and a new generalization of the associated Camassa–Holm equation [35], and so on [36]. Additionally, in Ref. [33], the authors utilized the MEFM for the KdV equation, and obtained one, two, and three-soliton-type solutions with interpretations for the gained soliton solutions.

2. Algorithm for the G G 2 -Expansion, the G G -Expansion, and the Multi-Exp-Function Method

2.1. The Basic Idea of the G G 2 -Expansion Method

In this subsection, we consider the algorithm of the G G 2 -expansion method for a nonlinear fractional PDE as follows:
  • Consider the general nonlinear fractional PDE of the type:
    N ( u , D t α u , D x α u , D x β u , D x α D x β u , D t α D t β u , ) = 0 , 0 < α , β 1 ,
    where u = u ( x , t ) .
  • Convert the nonlinear PDE (6) into an ODE through the following transformation,
    ε = d x d β Γ ( 1 + β ) + c x c α Γ ( 1 + α ) , u ( x , t ) = u ( ε ) ,
    where d and c are constants and Γ ( . ) is the Gamma function defined in Ref. [3].
  • Rewrite Equation (6) as
    N ˜ ( u , u , u , u , ) = 0 .
  • Assume the general solution of (8) can be expressed in terms of G G 2 as
    u ( ε ) = a 0 + i = 1 N a i G ( ε ) G 2 ( ε ) i + b i G ( ε ) G 2 ( ε ) i ,
    where G ( ε ) satisfies the following Riccati equation:
    G ( ε ) G 2 ( ε ) = η + λ G ( ε ) G 2 ( ε ) 2 ,
    in which η 1 , λ 0 . The constants b N or a N may be zero, but both of them cannot be zero simultaneously. Also, b i , a i , i = 1 , , N , are constants to be determined in the next step. In addition, the value of N N can be computed through the homogeneous balance principle [37].
    Notice that (10) results in
    G ( ε ) = η G 4 + ( G ) 2 ( 2 G + λ ) G 2 ,
    G ( ε ) = G ( 6 G η + 2 λ η ) + ( G ) 3 G 2 ( 6 + 6 λ 1 G + 2 λ 2 1 G 2 ) .
  • Insert (9), along with (10), into (8). Collect all coefficients of the same power of G ( ε ) G 2 ( ε ) ± i for i = 1 , , N . Then, set all of the obtained coefficients to zero. Then solve the system of algebraic equations on variables a 0 , b i , a i , η , λ , c and d , for i = 1 , , N .
  • Depending on the values of η and λ , the general solutions of (10) can be separated into the following cases:
    Case 1: λ η > 0 ;
    G ( ε ) G 2 ( ε ) = η λ C cos ( η λ ε ) + D sin ( η λ ε ) D cos ( η λ ε ) C sin ( η λ ε ) ,
    Case 2: λ η < 0 ;
    G ( ε ) G 2 ( ε ) = | η λ | λ C sinh ( 2 | η λ | ε ) + C cosh ( 2 | η λ | ε ) + D C sinh ( 2 | η λ | ε ) + C cosh ( 2 | η λ | ε ) D ,
    Case 3: λ 0 , η = 0 ;
    G ( ε ) G 2 ( ε ) = C λ ( C ε + D ) ,
    where C , D 0 .
  • By substituting the obtained values of a 0 , b i , a i , η , λ , c , d and the solutions (13)–(15) into (9) with the transformation (7), the exact traveling wave solutions of (6) can be obtained.

2.2. The Basic Idea of the G G -Expansion Method

In this subsection, we present the algorithm of the G G -expansion method for a nonlinear fractional PDE as follows:
  • Consider the general nonlinear fractional PDE of the type (6).
  • Convert the nonlinear PDE (6) into an ODE through the transformation defined in (7).
  • Rewrite (6) as the NODE (8).
  • Assume the general solution of (8) can be expressed in terms of G G as
    u ( ε ) = i = 0 N a i G ( ε ) G ( ε ) i ,
    where G ( ε ) satisfies the following second order ODE:
    G ( ε ) + λ G ( ε ) + η G ( ε ) = 0 ,
    in which η , λ and a i , i = 1 , , N , are constants to be determined later.
    Notice that we can obtain the value of N by the homogeneous balance principle.
  • Insert (16), along with (17), into (8). Collect all coefficients of the same power of G ( ε ) G ( ε ) i . Then set all of the obtained coefficients to zero. Then solve the system of algebraic equations on variables a i , η , λ , c .
  • Depending on the values of η and λ , the general solutions of (17) can be separated into the following cases:
    Case 1: λ 2 4 η > 0 ;
    G ( ε ) G ( ε ) = 0.5 λ 2 4 η C cosh ( 0.5 λ 2 4 η ε ) + D sinh ( 0.5 λ 2 4 η ε ) C sinh ( 0.5 λ 2 4 η ε ) + D cosh ( 0.5 λ 2 4 η ε ) ,
    Case 2: λ 2 4 η < 0 ;
    G ( ε ) G ( ε ) = 0.5 λ 2 4 η C sin ( 0.5 λ 2 + 4 η ε ) + D cos ( 0.5 λ 2 + 4 η ε ) C cos ( 0.5 λ 2 + 4 η ε ) + D sin ( 0.5 λ 2 + 4 η ε ) ,
    Case 3: λ 2 4 η = 0 ;
    G ( ε ) G ( ε ) = D D ε + C λ 2 ,
    where C , D 0 .
  • By substituting the obtained values of a i , η , λ , c and the solutions (18), (19), and (78) into (16) with the transformation (7), the exact traveling wave solutions of (6) can be obtained.

2.3. The Basic Idea of the Multi-Exp-Function Method

In this subsection, we formulate the MEFM by considering
N ( x , t , u t , u x , ) = 0 ,
where u = u ( x , t ) .
  • Step 1: Assume that
    ε i = c i e ε i , ε i = S i x ω i t , ε i = k i x ω i t , i [ 1 , n ] ,
    in which k i , c i , and ω i are angular wave numbers, arbitrary constants, and wave frequencies, respectively. Notice that
    ε i , x = k i ε i , ε i , t = ω i ε i , i [ 1 , n ] .
  • Step 2: Assume
    u ( x , t ) : = K ( ε 1 , ε 2 , , ε n ) H ( ε 1 , ε 2 , , ε n ) , K : = r , s = 1 n i , j = 0 M P r s , i j ε r i ε s j , H : = r , s = 1 n i , j = 0 N Q r s , i j ε r i ε s j ,
    where Q r s , i j and P r s , i j are fixed to be determined from (21).
    We now get
    N ˜ ( x , t , ε 1 , ε 2 , , ε n ) = 0 .
  • Step 3: When we solve a system of algebraic equations on variables w i ,   k i ,   Q r s , i j and P r s , i j , we get the MWSs u as
    u ( x , t ) = K ( c 1 exp ( k 1 x ω 1 t ) , , c n exp ( k n x ω n t ) ) H ( c 1 exp ( k 1 x ω 1 t ) , , c n exp ( k n x ω n t ) ) .

3. Application of the G G 2 -Expansion Method

Example 1.
Assume the nonlinear time fractional Harry Dym Equation (1). where D α is the fractional derivative of order α in the Caputo sense and for a given function f : R + R is defined by
D α f ( t ) = I n α D n f ( t ) = 1 Γ ( n α ) 0 t f ( n ) ( s ) ( t s ) α n + 1 d s , n 1 < α < n N , t > 0 ,
and the Riemann–Liouville fractional integral operator I t β of order β is defined by
I t β f ( t ) = 1 Γ ( β ) 0 t ( t s ) β 1 f ( s ) d s , β > 0 , t > 0 .
Now, we employ the following transformations, which represents a new dependent variable
X = x d s u ( s , t ) , T = t α Γ ( 1 + α ) , Ξ ( X , T ) = u x ( X , T ) , t ( X , T )
where x = x ( X , T ) and t = t ( X , T ) .
We shall employ the fact that u ( x , t ) and its spatial derivative tends to zero as | x | . Then
α t α = X α X t α + T α T t α = T Ξ Ξ X X 3 2 Ξ X 2 Ξ 2 X .
Also,
x = 1 Ξ ( X , T ) X .
Therefore, (1) can be expressed as
Ξ T + Ξ X X X Ξ 2 3 Ξ X X Ξ X Ξ + 3 2 Ξ X 3 Ξ 2 = 0 .
Now consider the following transformation
ψ ( X , T ) = Ξ X Ξ .
From (28) and (30), we get the following KdV equation
ψ T 3 2 ψ 2 ψ X + ψ X X X = 0 .
Now, let
ψ ( X , T ) = ψ ( ε ) , ε = ε ( X , T ) = X c T ,
where c is constant.
Inserting (31) in (30), we get
c ψ 3 2 ψ 2 ψ + ψ = 0 .
Integration of (32) yields
c ψ 1 2 ψ 3 + ψ = 0 .
Here, we get the balancing number 3 N = N + 2 or N = 1 .
Suppose the solution of (33) can be given by
ψ ( ε ) = a 0 + a 1 G G 2 + b 1 G G 2 1 ,
in which a 0 , b 1 , a 1 are constant to be determined later.
Inserting Equation (34) into Equation (33), we have
c a 0 c a 1 G ( ε ) G 2 ( ε ) c b 1 G 2 ( ε ) G ( ε ) 1 2 a 0 3 3 2 a 0 2 a 1 G ( ε ) G 2 ( ε ) 3 2 a 0 2 b 1 G 2 ( ε ) G ( ε ) 3 2 a 0 a 1 2 ( G ( ε ) ) 2 G 4 ( ε ) 3 a 0 a 1 b 1 3 2 a 0 b 1 2 G 4 ( ε ) ( G ( ε ) ) 2 1 2 a 1 3 ( G ( ε ) ) 3 G 6 ( ε ) 3 2 a 1 2 b 1 G ( ε ) G 2 ( ε ) 3 2 a 1 b 1 2 G 2 ( ε ) G ( ε ) 1 2 b 1 3 G 6 ( ε ) ( G ( ε ) ) 3 + a 1 G ( ε ) G 2 ( ε ) 6 a 1 G ( ε ) G ( ε ) G 3 ( ε ) + 6 a 1 ( G ( ε ) ) 3 G 4 ( ε ) + 2 b 1 G 2 ( ε ) G ( ε ) ( G ( ε ) ) 3 2 b 1 G ( ε ) G ( ε ) G ( ε ) b 1 G 2 ( ε ) G ( ε ) ( G ( ε ) ) 2 + 2 b 1 G ( ε ) = 0 .
Note 1.
Making use of (10), we get
G ( ε ) = η G 4 ( ε ) + 2 ( G ( ε ) ) 2 G ( ε ) + λ ( G ( ε ) ) 2 G 2 ( ε ) ,
 and 
G ( ε ) = 6 η G ( ε ) G ( ε ) + 6 ( G ( ε ) ) 3 G 2 ( ε ) + 6 λ ( G ( ε ) ) 3 G 3 ( ε ) + 2 λ η G ( ε ) + 2 λ 2 ( G ( ε ) ) 3 G 4 ( ε ) .
Using (10), (35), and (36), and then inserting G G 2 : = X ,  and  G G 2 1 : = Y ,  we have that 
c a 1 X c b 1 Y 3 2 a 0 2 a 1 X 3 2 a 0 2 b 1 Y 3 2 a 0 a 1 2 X 2 3 2 a 0 b 1 2 Y 2 3 2 a 1 2 b 1 X 3 2 a 1 b 1 2 Y + 2 a 1 λ η X + 2 b 1 η λ Y + 2 a 1 λ 2 X 3 + 2 b 1 η 2 Y 3 1 2 a 1 3 X 3 3 a 0 a 1 b 1 1 2 b 1 3 Y 3 1 2 a 0 3 c a 0 = 0 .
By collecting all terms with the same power of X and Y and then equating each coefficients of this polynomial to zero, we get the following system of algebraic equations:
Y 3 : 2 b 1 η 2 1 2 b 1 3 = 0 , Y 2 : 3 2 a 0 b 1 2 = 0 , Y : c b 1 3 2 a 0 2 b 1 3 2 a 1 b 1 2 + 2 b 1 η λ = 0 , X 0 Y 0 : 3 a 1 a 0 b 1 1 2 a 0 3 c a 0 = 0 , X : c a 1 3 2 a 0 2 a 1 3 2 a 1 2 b 1 + 2 a 1 λ η = 0 , X 2 : 3 2 a 0 a 1 2 = 0 , X 3 : 2 a 1 λ 2 1 2 a 1 3 = 0 .
Solving the above system of nonlinear algebraic equation, we get
c = 1 2 a 0 2 , η = η , λ = λ , a 0 = a 0 , a 1 = 0 , b 1 = 0 ,
c = c , η = η , λ = λ , a 0 = 0 , a 1 = 0 , b 1 = 0 ,
c = 2 λ η , η = η , λ = λ , a 0 = 0 , a 1 = 0 , b 1 = 2 η ,
c = 2 λ η , η = η , λ = λ , a 0 = 0 , a 1 = 0 , b 1 = 2 η ,
c = 2 λ η , η = η , λ = λ , a 0 = 0 , a 1 = 2 λ , b 1 = 0 ,
c = 2 λ η , η = η , λ = λ , a 0 = 0 , a 1 = 2 λ , b 1 = 0 ,
c = 4 λ η , η = η , λ = λ , a 0 = 0 , a 1 = 2 λ , b 1 = 2 η ,
c = 8 λ η , η = η , λ = λ , a 0 = 0 , a 1 = 2 λ , b 1 = 2 η ,
c = 8 λ η , η = η , λ = λ , a 0 = 0 , a 1 = 2 λ , b 1 = 2 η ,
c = 4 λ η , η = η , λ = λ , a 0 = 0 , a 1 = 2 λ , b 1 = 2 η .
Inserting (43) and (46) in (34), we get
ψ ( ε ) = ± 2 λ G G 2 ± 2 η G G 2 1 .
Therefore, we get three types of travelling wave solutions as follows:
  • if λ η > 0 ;
    u 1 , 2 ( x , t ) = ± 2 λ ξ 1 ± 2 η ( ξ 1 ) 1 ,
    in which
    ξ 1 : = η λ C cos ( η λ ( x 4 λ η t α Γ ( 1 + α ) ) + D sin ( η λ ( x 4 λ η t α Γ ( 1 + α ) ) ) D cos ( η λ ( x 4 λ η t α Γ ( 1 + α ) ) ) C sin ( η λ ( x 4 λ η t α Γ ( 1 + α ) ) ) ,
  • if λ η < 0 ;
    u 1 , 2 ( x , t ) = ± 2 λ ξ 2 ± 2 η ( ξ 2 ) 1 ,
    in which
    ξ 2 : = | η λ | λ C sinh ( 2 | η λ | ( x 4 λ η t α Γ ( 1 + α ) ) ) + C cosh ( 2 | η λ | ( x 4 λ η t α Γ ( 1 + α ) ) ) + D C sinh ( 2 | η λ | ( x 4 λ η t α Γ ( 1 + α ) ) ) + C cosh ( 2 | η λ | ( x 4 λ η t α Γ ( 1 + α ) ) ) D ,
  • if λ 0 , η = 0 ;
    u 1 , 2 ( x , t ) = ± 2 λ ξ 3 ± 2 η ( ξ 3 ) 1 ,
    in which
    ξ 3 : = C λ ( C ( x 4 λ η t α Γ ( 1 + α ) ) + D ) ,
    where C , D 0 .
Inserting (44) and (45) in (34), we get
ψ ( ε ) = ± 2 λ G G 2 2 η G G 2 1 .
Therefore, we get three types of travelling wave solutions as follows:
  • if λ η > 0 ;
    u 3 , 4 ( x , t ) = ± 2 λ ξ 1 2 η ( ξ 1 ) 1 ,
    in which
    ξ 1 : = η λ C cos ( η λ ( x 8 λ η t α Γ ( 1 + α ) ) + D sin ( η λ ( x 8 λ η t α Γ ( 1 + α ) ) ) D cos ( η λ ( x 8 λ η t α Γ ( 1 + α ) ) ) C sin ( η λ ( x 8 λ η t α Γ ( 1 + α ) ) ) ,
  • if λ η < 0 ;
    u 3 , 4 ( x , t ) = ± 2 λ ξ 2 2 η ( ξ 2 ) 1 ,
    in which
    ξ 2 : = | η λ | λ C sinh ( 2 | η λ | ( x 8 λ η t α Γ ( 1 + α ) ) ) + C cosh ( 2 | η λ | ( x 8 λ η t α Γ ( 1 + α ) ) ) + D C sinh ( 2 | η λ | ( x 8 λ η t α Γ ( 1 + α ) ) ) + C cosh ( 2 | η λ | ( x 8 λ η t α Γ ( 1 + α ) ) ) D ,
  • if λ 0 , η = 0 ;
    u 3 , 4 ( x , t ) = ± 2 λ ξ 3 2 η ( ξ 3 ) 1 ,
    in which
    ξ 3 : = C λ ( C ( x 8 λ η t α Γ ( 1 + α ) ) + D ) ,
    where C , D 0 .
Inserting (41) and (42) in (34), we get
ψ ( ε ) = ± 2 λ G G 2 .
Therefore, we get three types of travelling wave solutions as follows:
  • if λ η > 0 ;
    u 5 , 6 ( x , t ) = ± 2 λ ξ 1 ,
    in which
    ξ 1 : = η λ C cos ( η λ ( x 2 λ η t α Γ ( 1 + α ) ) + D sin ( η λ ( x 2 λ η t α Γ ( 1 + α ) ) ) D cos ( η λ ( x 2 λ η t α Γ ( 1 + α ) ) ) C sin ( η λ ( x 2 λ η t α Γ ( 1 + α ) ) ) ,
  • if λ η < 0 ;
    u 5 , 6 ( x , t ) = ± 2 λ ξ 2 ,
    in which
    ξ 2 : = | η λ | λ C sinh ( 2 | η λ | ( x 2 λ η t α Γ ( 1 + α ) ) ) + C cosh ( 2 | η λ | ( x 2 λ η t α Γ ( 1 + α ) ) ) + D C sinh ( 2 | η λ | ( x 2 λ η t α Γ ( 1 + α ) ) ) + C cosh ( 2 | η λ | ( x 2 λ η t α Γ ( 1 + α ) ) ) D ,
  • if λ 0 , η = 0 ;
    u 3 , 4 ( x , t ) = ± 2 λ ξ 3 ,
    in which
    ξ 3 : = C λ ( C ( x 2 λ η t α Γ ( 1 + α ) ) + D ) ,
    where C , D 0 .
Inserting (39) and (40) in (34), we get
ψ ( ε ) = 2 η G G 2 1 .
Therefore, we get three types of travelling wave solutions as follows:
  • if λ η > 0 ;
    u 7 , 8 ( x , t ) = 2 η ( ξ 1 ) 1 ,
    in which
    ξ 1 : = η λ C cos ( η λ ( x 2 λ η t α Γ ( 1 + α ) ) + D sin ( η λ ( x 2 λ η t α Γ ( 1 + α ) ) ) D cos ( η λ ( x 2 λ η t α Γ ( 1 + α ) ) ) C sin ( η λ ( x 2 λ η t α Γ ( 1 + α ) ) ) ,
  • if λ η < 0 ;
    u 7 , 8 ( x , t ) = 2 η ( ξ 2 ) 1 ,
    in which
    ξ 2 : = | η λ | λ C sinh ( 2 | η λ | ( x 2 λ η t α Γ ( 1 + α ) ) ) + C cosh ( 2 | η λ | ( x 2 λ η t α Γ ( 1 + α ) ) ) + D C sinh ( 2 | η λ | ( x 2 λ η t α Γ ( 1 + α ) ) ) + C cosh ( 2 | η λ | ( x 2 λ η t α Γ ( 1 + α ) ) ) D ,
  • if λ 0 , η = 0 ;
    u 7 , 8 ( x , t ) = 2 η ( ξ 3 ) 1 ,
    in which
    ξ 3 : = C λ ( C ( x 2 λ η t α Γ ( 1 + α ) ) + D ) ,
    where C , D 0 .
The plots of u 1 , , u 4  are displayed in Figure 1, Figure 2, Figure 3, Figure 4 and Figure 5, for two different cases λ η > 0 and λ η < 0 , for specific values η = 3 , λ = 2 , α = 2 5 , D = 2 , C = 3 , and η = 3 , λ = 2 , α = 2 5 ,   D = 2 , C = 3 , respectively.
Example 2.
Here, we consider the SRLW Equation (3), where D γ is the conformable derivative of order γ , given by
D ξ γ ( ϖ ) = lim ϵ 0 ϖ ( ξ + ϵ ξ 1 γ ) ϖ ( ξ ) ϵ , ξ > 0 , 0 < γ 1 ,
in which ϖ : [ 0 , ) R is a given function.
If the above limit exists, then ϖ is called γ-differentiable. Assume 0 < γ 1 , and ϖ and ϖ be γ-differentiable at point ξ > 0 , then D γ has the following properties:
D γ ( c ϖ + d ϖ ) = c D γ ( ϖ ) + d D γ ( ϖ ) where c , d R ,
D γ ( ξ n ) = n ξ n γ , where n R ,
D γ ( χ ) = 0 ϖ ( ξ ) = χ ( is a constant ) ,
D γ ( ϖ ϖ ) = ϖ D γ ( ϖ ) + ϖ D γ ( ϖ ) ,
D γ ( ϖ ) ( ξ ) = ξ 1 γ d ϖ d ξ ( ξ ) ,
D γ ϖ ϖ = ϖ D γ ( ϖ ) ϖ D γ ( ϖ ) ( ϖ ) 2 .
Now, using the following transformation
ε = α x γ Γ ( 1 + γ ) + β t γ Γ ( 1 + γ ) , u ( x , t ) = u ( ε ) ,
Equation (3) turns into
β 2 u + α 2 u + β α u u + β α ( u ) 2 + β 2 α 2 u ( iv ) = 0 .
Integrating (60) twice yields
β 2 α 2 u + ( β 2 + α 2 + k ) u + 1 2 β α u 2 + ϑ = 0 ,
where k and ϑ are integral constants. For simplicity, we set ϑ = 0 . therefore, we get
β 2 α 2 u + ( β 2 + α 2 + k ) u + 1 2 β α u 2 = 0 .
Here, we get the balancing number 2 N = N + 2 or N = 2 .
Suppose the solution of (61) can be given by
u ( ε ) = a 0 + a 1 G G 2 + b 1 G G 2 1 + a 2 G G 2 2 + b 2 G G 2 2 ,
in which a 0 , b 1 , a 1 , b 2 , a 2 are constant to be determined later.
Inserting Equation (62) with Equation (10) into Equation (61) and collecting all terms with the same power of G G 2 , and then equating each coefficients of this polynomial to zero, we get the following system of algebraic equations:
G G 2 4 : 1 2 β α b 2 2 + 6 β 2 α 2 b 2 η 2 = 0 , G G 2 3 : 2 α 2 β 2 η 2 b 1 + α β b 1 b 2 = 0 , G G 2 2 : 1 2 β α b 1 2 + 8 β 2 α 2 b 2 λ η + β α a 0 b 2 + b 2 k + b 2 α 2 + b 2 β 2 = 0 , G G 2 1 : 2 α 2 β 2 η λ b 1 + α β a 0 b 1 + α β a 1 b 2 + α 2 b 1 + β 2 b 1 + k b 1 = 0 , G G 2 0 : β α a 1 b 1 + β α a 2 b 2 + 2 α 2 β 2 a 2 η 2 + 2 β 2 α 2 b 2 λ 2 + a 0 α 2 + a 0 β 2 + a 0 k + 1 2 β α a 0 2 , G G 2 1 : 2 α 2 β 2 η λ a 1 + α β a 0 a 1 + α β a 2 b 1 + α 2 a 1 + β 2 a 1 + k a 1 = 0 , G G 2 2 : 1 2 β α a 1 2 + 8 β 2 α 2 a 2 λ η + β α a 0 a 2 + a 2 α 2 + a 2 β 2 + a 2 k = 0 , G G 2 3 : 2 α 2 β 2 λ 2 a 1 + α β a 1 a 2 = 0 , G G 2 4 : 1 2 β α a 2 2 + 6 β 2 α 2 a 2 λ 2 = 0 .
Solving the above system of nonlinear algebraic equation, we get
η = η , k = 1 2 a 0 α β α 2 β 2 , λ = λ , a 0 = a 0 , a 1 = 0 , a 2 = 0 , b 1 = 0 , b 2 = 0 ,
η = η , k = k , λ = λ , a 0 = 0 , a 1 = 0 , a 2 = 0 , b 1 = 0 , b 2 = 0 ,
η = η , k = 16 α 2 β 2 η λ α 2 β 2 , λ = λ , a 0 = 24 λ η α β , a 1 = 0 , a 2 = 12 λ 2 α β , b 1 = 0 , b 2 = 12 η 2 α β ,
η = η , k = 16 α 2 β 2 η λ α 2 β 2 , λ = λ , a 0 = 8 λ η α β , a 1 = 0 , a 2 = 12 λ 2 α β , b 1 = 0 , b 2 = 12 η 2 α β ,
η = η , k = 4 λ η α 2 β 2 α 2 β 2 , λ = λ , a 0 = 12 λ η α β , a 1 = 0 , a 2 = 0 , b 1 = 0 , b 2 = 12 η 2 α β ,
η = η , k = 4 λ η α 2 β 2 α 2 β 2 , λ = λ , a 0 = 4 λ η α β , a 1 = 0 , a 2 = 0 , b 1 = 0 , b 2 = 12 η 2 α β ,
η = η , k = 4 λ η α 2 β 2 α 2 β 2 , λ = λ , a 0 = 12 λ η α β , a 1 = 0 , a 2 = 12 λ 2 α β , b 1 = 0 , b 2 = 0 ,
η = η , k = 4 λ η α 2 β 2 α 2 β 2 , λ = λ , a 0 = 4 λ η α β , a 1 = 0 , a 2 = 12 λ 2 α β , b 1 = 0 , b 2 = 0 .
Inserting (65) in (62), we get
u ( ε ) = 24 λ η α β 12 λ 2 α β G G 2 2 12 η 2 α β G G 2 2 ,
Therefore, we get three types of travelling wave solutions as follows:
  • if λ η > 0 ;
    u 1 = 24 λ η α β 12 λ 2 α β ( ξ 1 ) 2 12 η 2 α β ( ξ 1 ) 2 ,
    where
    ξ 1 = η λ C cos ( η λ ( α x γ Γ ( 1 + γ ) + β t γ Γ ( 1 + γ ) ) ) + D sin ( η λ ( α x γ Γ ( 1 + γ ) + β t γ Γ ( 1 + γ ) ) ) D cos ( η λ ε ) C sin ( η λ ( α x γ Γ ( 1 + γ ) + β t γ Γ ( 1 + γ ) ) ) ,
  • if λ η < 0 ;
    u 2 = 24 λ η α β 12 λ 2 α β ( ξ 2 ) 2 12 η 2 α β ( ξ 2 ) 2 ,
    where
    ξ 2 = | η λ | λ C sinh ( 2 | η λ | ( α x γ Γ ( 1 + γ ) + β t γ Γ ( 1 + γ ) ) ) + C cosh ( 2 | η λ | ( α x γ Γ ( 1 + γ ) + β t γ Γ ( 1 + γ ) ) ) + D C sinh ( 2 | η λ | ( α x γ Γ ( 1 + γ ) + β t γ Γ ( 1 + γ ) ) ) + C cosh ( 2 | η λ | ( α x γ Γ ( 1 + γ ) + β t γ Γ ( 1 + γ ) ) ) D ,
  • if λ 0 , η = 0 ;
    u 3 = 24 λ η α β 12 λ 2 α β ( ξ 3 ) 2 12 η 2 α β ( ξ 3 ) 2 ,
    where
    ξ 3 = C λ ( C ( α x γ Γ ( 1 + γ ) + β t γ Γ ( 1 + γ ) ) + D ) ,
    where C , D 0 .
The plots of (72) and (73) are displayed in Figure 6 and Figure 7, for η = 2 , λ = 3 , α = 1 2 , β = 1 3 , γ = 1 2 , D = 2 , C = 3 , and η = 2 , λ = 3 , α = 1 2 , β = 1 3 , γ = 1 2 , D = 2 , C = 3 , respectively.

4. Application of the G G -Expansion Method

Example 3.
Assume the nonlinear time fractional Harry Dym Equation (1).
Now, we employ the transformations (27), which represents a new dependent variable.
In a similar way presented in Example 1 in Section 3, we consider the ODE (33). Here, we get the balancing number 3 N = N + 2 or N = 1 .
Suppose that the solution of (33) can be given by
ψ ( ε ) = a 0 + a 1 G G ,
in which a 0 , a 1 are constants to be determined later.
Inserting Equation (75) with Equation (17) into Equation (33) and collecting all terms with the same power of G G , and then equating each coefficient of this polynomial to zero, we get the following system of algebraic equations:
G G 3 : a 1 3 2 + 2 a 1 = 0 , G G 2 : 3 2 a 0 a 1 2 + 3 a 1 λ = 0 , G G 1 : c a 1 3 2 a 0 2 a 1 + a 1 λ 2 + 2 a 1 η = 0 , G G 0 : c a 0 + a 1 η λ a 0 3 2 = 0 .
Solving the above system of nonlinear algebraic equation, we get
a 0 = λ , a 1 = 2 , c = 0.5 ( λ 2 4 η ) .
Inserting (76) in (75), we get
ψ ( ε ) = ± 2 G G ± λ .
Therefore, we get three types of travelling wave solutions as follows:
Case 1: λ 2 4 η > 0 ;
u 1 , 2 ( x , t ) = ± 2 ( 0.5 ( λ 2 4 η ) ) . i C cos ( ( 0.5 ( λ 2 4 η ) ) 2 ( x ( 0.5 ( λ 2 4 η ) ) t α Γ ( 1 + α ) ) ) + D sin ( ( 0.5 ( λ 2 4 η ) ) 2 ( x ( 0.5 ( λ 2 4 η ) ) t α Γ ( 1 + α ) ) ) i C sin ( ( 0.5 ( λ 2 4 η ) ) 2 ( x ( 0.5 ( λ 2 4 η ) ) t α Γ ( 1 + α ) ) ) + D cos ( ( 0.5 ( λ 2 4 η ) ) 2 ( x ( 0.5 ( λ 2 4 η ) ) t α Γ ( 1 + α ) ) ) ,
Case 2: λ 2 4 η < 0 ;
u 1 , 2 ( x , t ) = ± i 2 ( 0.5 ( λ 2 4 η ) ) . C sin ( ( 0.5 ( λ 2 4 η ) ) 2 ( x ( 0.5 ( λ 2 4 η ) ) t α Γ ( 1 + α ) ) ) + D cos ( ( 0.5 ( λ 2 4 η ) ) 2 ( x ( 0.5 ( λ 2 4 η ) ) t α Γ ( 1 + α ) ) ) C cos ( ( 0.5 ( λ 2 4 η ) ) 2 ( x ( 0.5 ( λ 2 4 η ) ) t α Γ ( 1 + α ) ) ) + D sin ( ( 0.5 ( λ 2 4 η ) ) 2 ( x ( 0.5 ( λ 2 4 η ) ) t α Γ ( 1 + α ) ) ) ,
Case 3: λ 2 4 η = 0 ;
u 1 , 2 ( x , t ) = ± D D ( x ( 0.5 ( λ 2 4 η ) ) t α Γ ( 1 + α ) ) + C ,
where C , D 0 .
The plots of u 1 , , u 4 are displayed in Figure 8 and Figure 9, for two different cases λ 2 4 η > 0 and λ 2 4 η < 0 , for specific values η = 3 ,   λ = 2 ,   α = 2 5 ,   D = 2 ,   C = 3 , and η = 3 ,   λ = 2 ,   α = 2 5 ,   D = 2 ,   C = 3 , respectively.

5. Comparing the G G -Expansion and the G G 2 -Expansion Methods

Here, diverse values of the solutions of (1) obtained through the G G 2 -expansion method and the G G -expansion method are presented in Table 1 and Table 2.
As you can see, the obtained solutions through the G G 2 -expansion method present a better description of Equation (1) than the obtained solutions through the G G -expansion method.
The G G 2 -expansion method and the G G -expansion method are related to traveling wave solutions of NPDEs only. As mentioned before, there exist MWSs to NPDEs. We are interested in a novel approach for obtaining MWSs to NPDEs, and the MEFM formulates a solution algorithm for calculating MWSs to NPDEs. In Section 6, we present two different examples of the MEFM.

6. Application of the Multi-Exp-Function-Method

6.1. Example 1

Here, we apply the MEFM to obtain the novel analytical solutions for (4).
  • One wave solutions for (4):
    First, consider ε 1 = ε 1 ( x , y , t ) as
    ε 1 = ϖ 1 exp ( S 1 x + R 1 y ω 1 t ) ,
    where ϖ 1 , S 1 , R 1 , and ω 1 are constants. Now, ε 1 has the following relations
    ε 1 , x = S 1 ε 1 , ε 1 , y = R 1 ε 1 , ε 1 , t = ω 1 ε 1 .
    Therefore, we assume
    K ( ε 1 ) = P 0 + P 1 ε 1 ,
    H ( ε 1 ) = Q 0 + Q 1 ε 1 ,
    where P 0 , P 1 , Q 0 , and Q 1 are fixed to be determined from (4). Thus, we get
    u ( x , t ) = K ( ε 1 ) H ( ε 1 ) = P 0 + P 1 ε 1 Q 0 + Q 1 ε 1 .
    By setting (83) into (4), we get:
    P 1 = arbitrary , ω 1 : 1 2 5 i 3 R 1 2 + 10 S 1 2 + 2 S 1 R 1 5 R 1 2 R 1 .
    By inserting (84) in (83), the one wave solutions can be presented by u 1 .
    The real part of u 1 is displayed in Figure 10 for S 1 = 7 ,   R 1 = 5 ,   Q 1 = 0.70 , Q 0 = 0.40 ,   P 0 = 0.90 ,   P 1 = 3 , (a) is three dimensional with y = 2 . Here, (b), (c), and (d) exploit the z , y , x –axis orientation, respectively. Additionally, (e) is the contour plot. In addition, the imaginary part of equation u 1 is displayed in Figure 11 for S 1 = 7 , R 1 = 5 , Q 1 = 0.70 , Q 0 = 0.40 , P 0 = 0.90 , P 1 = 3 , (a) is three dimensional with y = 2 . Here, (b), (c), and (d) exploit the z , y , x –axis, orientation, respectively. Additionally, (e) is the contour plot.
  • Two wave solutions for (4):
    Consider ε i = ε i ( x , y , t ) , i = 1 , 2 , such that
    ε i = ϖ i exp ( S i x + R i y ω i t ) , i = 1 , 2
    in which S i ,   ϖ i , R i , and ω i are fixed. Now, we have
    ε i , y = R i , ε i , x = S i ε i , ε i , t = ω i ε i , i = 1 , 2 .
    Then, we assume
    K ( ε 1 , ε 2 ) = 2 ( S 1 ε 1 + S 2 ε 2 + P 12 ( S 1 + S 2 ) ε 1 ε 2 ) ,
    H ( ε 1 , ε 2 ) = 1 + ε 1 + ε 2 + P 12 ε 1 ε 2 ,
    where P 12 is a constant to be determined from (4). Therefore, we have
    u ( x , t ) = 2 ( S 1 ε 1 + S 2 ε 2 + P 12 ( S 1 + S 2 ) ε 1 ε 2 ) 1 + ε 1 + ε 2 + P 12 ε 1 ε 2 .
    Using (89) into (4), we get:
    P 12 = 1 , ω 1 = 1 2 5 i 3 R 1 2 + 10 S 1 2 + 2 S 1 R 1 5 R 1 2 R 1 , ω 2 = 1 2 5 i 3 R 2 2 + 10 S 2 2 + 2 S 2 R 2 5 R 2 2 R 2 .
    Using (89), we can show that the two wave solutions can be presented by u 2 . The real part of u 2 is displayed in Figure 12 for S 1 = 3 , S 2 = 5 , R 1 = 2 , R 2 = 7 , (a) is three dimensional with y = 2 . Here, (b), (c), and (d) exploit the z , y , x –axis, respectively. Additionally, (e) is the contour plot. In addition, the imaginary part of equation u 2 is displayed in Figure 13 for S 1 = 3 , S 2 = 5 , R 1 = 2 , R 2 = 7 , (a) is three dimensional with y = 2 . Here, (b), (c), and (d) exploit the z , x , y –axis orientation, respectively. Additionally, (e) is the contour plot.
  • Three wave solutions for (4):
    Consider ε i = ε i ( x , y , t ) , i = 1 , 2 , 3 , such that
    ε i = ϖ i exp ( S i x + R i y ω i t ) , i = 1 , 2 , 3
    where S i ,   ϖ i , and ω i are fixed. Now, ε i has the following relations
    ε i , x = S i ε i , ε i , y = R i ε 1 , ε i , t = ω i ε i , i = 1 , 2 , 3 .
    Therefore, we assume
    K ( ε 1 , ε 2 , ε 3 ) = 2 ( S 1 ε 1 + S 2 ε 2 + S 3 ε 3 + P 12 ( S 1 + S 2 ) ε 1 ε 2 + P 13 ( S 1 + S 3 ) ε 1 ε 3 + P 23 ( S 2 + S 3 ) ε 2 ε 3 + P 12 P 13 P 23 ( S 1 + S 2 + S 3 ) ε 1 ε 2 ε 3 ) ,
    and
    H ( ε 1 , ε 2 , ε 3 ) = 1 + ε 1 + ε 2 + ε 3 + P 12 ε 1 ε 2 + P 13 ε 1 ε 3 + P 23 ε 2 ε 3 + P 12 P 13 P 23 ε 1 ε 2 ε 3 ,
    where P 12 , P 13 , and P 23 are fixed to be determined from (4). Thus, we get
    u ( x , t ) = [ 2 ( S 1 ε 1 + S 2 ε 2 + S 3 ε 3 + P 12 ( S 1 + S 2 ) ε 1 ε 2 + P 13 ( S 1 + S 3 ) ε 1 ε 3 + P 23 ( S 2 + S 3 ) ε 2 ε 3 + P 12 P 13 P 23 ( S 1 + S 2 + S 3 ) ε 1 ε 2 ε 3 ) ] / 1 + ε 1 + ε 2 + ε 3 + P 12 ε 1 ε 2 + P 13 ε 1 ε 3 + P 23 ε 2 ε 3 + P 12 P 13 P 23 ε 1 ε 2 ε 3 .
    Now, by setting (92) into (4) and solving the system of algebraic equations, we have:
    P 12 = 1 , P 13 = 1 , P 23 = 1 , ω 1 = 1 2 5 i 3 R 1 2 + 10 S 1 2 + 2 S 1 R 1 5 R 1 2 R 1 , ω 2 = 1 2 5 i 3 R 2 2 + 10 S 2 2 + 2 S 2 R 2 5 R 2 2 R 2 , ω 3 = 1 2 5 i 3 R 3 2 + 10 S 3 2 + 2 S 3 R 3 5 R 3 2 R 3 ,
    P 12 = 1 , P 13 = 1 , P 23 = 1 , R 3 = S 3 R 2 S 2 , ω 1 = 1 2 5 i 3 R 1 2 + 10 S 1 2 + 2 S 1 R 1 5 R 1 2 R 1 , ω 2 = 1 2 5 i 3 R 2 2 + 10 S 2 2 + 2 S 2 R 2 5 R 2 2 R 2 , ω 3 = 1 2 S 3 ( 5 i 3 R 2 2 + 10 S 2 2 + 2 S 2 R 2 5 R 2 2 ) R 2 S 2 ,
    P 12 = 1 , P 13 = 1 , P 23 = 1 , R 1 = S 1 R 3 S 3 , ω 1 = 1 2 S 1 ( 5 i 3 R 3 2 + 10 S 3 2 + 2 S 3 R 3 5 R 3 2 ) R 3 S 3 , ω 2 = 1 2 5 i 3 R 2 2 + 10 S 2 2 + 2 S 2 R 2 5 R 2 2 R 2 , ω 3 = 1 2 5 i 3 R 3 2 + 10 S 3 2 + 2 S 3 R 3 5 R 3 2 R 3 ,
    P 12 = 1 , P 13 = arbitrary , P 23 = arbitrary , R 1 = S 1 R 2 S 2 , R 3 = S 3 R 2 S 2 , ω 1 = 1 2 S 1 ( 5 i 3 R 2 2 + 10 S 2 2 + 2 S 2 R 2 5 R 2 2 ) R 2 S 2 , ω 2 = 1 2 5 i 3 R 2 2 + 10 S 2 2 + 2 S 2 R 2 5 R 2 2 R 2 , ω 3 = 1 2 S 3 ( 5 i 3 R 2 2 + 10 S 2 2 + 2 S 2 R 2 5 R 2 2 ) R 2 S 2 ,
    P 12 = arbitrary , P 13 = 1 , P 23 = 1 , R 2 = S 2 R 1 S 1 , ω 1 = 1 2 5 i 3 R 1 2 + 10 S 1 2 + 2 S 1 R 1 5 R 1 2 R 1 , ω 2 = 1 2 S 2 ( 5 i 3 R 1 2 + 10 S 1 2 + 2 S 1 R 1 5 R 1 2 ) R 1 S 1 , ω 3 = 1 2 5 i 3 R 3 2 + 10 S 3 2 + 2 S 3 R 3 5 R 3 2 R 3 ,
    and
    P 12 = arbitrary , P 13 = arbitrary , P 23 = arbitrary , R 2 = S 2 R 1 S 1 , R 3 = S 3 R 1 S 1 , ω 1 = 1 2 5 i 3 R 1 2 + 10 S 1 2 + 2 S 1 R 1 5 R 1 2 R 1 , ω 2 = 1 2 S 2 ( 5 i 3 R 1 2 + 10 S 1 2 + 2 S 1 R 1 5 R 1 2 ) R 1 S 1 , ω 3 = 1 2 S 3 ( 5 i 3 R 1 2 + 10 S 1 2 + 2 S 1 R 1 5 R 1 2 ) R 1 S 1 .
    Thus, the three wave solutions can be presented by u 3 , 1 , u 3 , 2 , u 3 , 3 , u 3 , 4 , u 3 , 5 , u 3 , 6 , respectively.
The real part of u 3 , 1 is displayed in Figure 14 for S 1 = 0.5 , S 2 = 0.7 , k 3 = 1.20 , R 1 = 1.50 , R 2 = 2 , R 3 = 1.50 , (a) is three dimensional with y = 2 . Here, (b), (c), and (d) exploit the z , y , x –axis, orientation. Additionally, (e) is the contour plot.
The imaginary part of equation u 3 , 1 is displayed in Figure 15 for S 1 = 0.5 , S 2 = 0.7 , k 3 = 1.20 , R 1 = 1.50 , R 2 = 2 , R 3 = 1.50 , (a) is three dimensional with y = 2 . Here, (b), (c), and (d) exploit the z , y , x –axis, orientation. Additionally, (e) is the contour plot.
The real part of u 3 , 2 is displayed in Figure 16 for S 1 = 3.50 , S 2 = 3.70 , k 3 = 1.20 , R 1 = 5 , R 2 = 2.30 , R 3 = 3 , P 23 = 3 , (a) is three dimensional with y = 2 . Here, (b), (c), and (d) exploit the z , x , y –axis, orientation. Additionally, (e) is the contour plot.
The imaginary part of equation u 3 , 2 is displayed in Figure 17 for S 1 = 3.50 , S 2 = 3.70 , k 3 = 1.20 , R 1 = 5 , R 2 = 2.30 , R 3 = 3 , P 23 = 3 , (a) is three dimensional with y = 2 . Here, (b), (c), and (d) exploit the z , y , x –axis, orientation. Additionally, (e) is the contour plot.
The real part of u 3 , 3 is displayed in Figure 18 for S 1 = 3.50 , S 2 = 3.70 , k 3 = 1.20 , R 2 = 2.30 , R 3 = 3 , P 13 = 3 , (a) is three dimensional with y = 2 . Here, (b), (c), and (d) exploit the z , y , x –axis, orientation. Additionally, (e) is the contour plot.
The imaginary part of equation u 3 , 3 is displayed in Figure 19 for S 1 = 3.50 , S 2 = 3.70 , k 3 = 1.20 , R 2 = 2.30 , R 3 = 3 , P 13 = 3 , (a) is three dimensional with y = 2 . Here, (b), (c), and (d) exploit the z , y , x -axis, orientation. Additionally, (e) is the contour plot.
The real part of u 3 , 4 is displayed in Figure 20 for S 1 = 3.50 , S 2 = 3.70 , S 3 = 1.20 , R 2 = 2.30 , P 23 = 5 , P 13 = 7 , (a) is three dimensional with y = 2 . Here, (b), (c), and (d) exploit the z , y , x –axis, orientation. Additionally, (e) is the contour plot.
The imaginary part of equation u 3 , 4 is displayed in Figure 21 for S 1 = 3.50 , S 2 = 3.70 , S 3 = 1.20 , R 2 = 2.30 , P 23 = 5 , P 13 = 7 , (a) is three dimensional with y = 2 . Here, (b), (c), and (d) exploit the z , y , x –axis, orientation. Additionally, (e) is the contour plot.
The real part of u 3 , 5 is displayed in Figure 22 for S 1 = 3.50 , S 2 = 3.70 , S 1 = 3.50 , S 3 = 1.20 , R 1 = 11 , R 3 = 13 , P 23 = 5 , P 12 = 9 , (a) is three dimensional with y = 2 . Here, (b), (c), and (d) exploit the z , y , x –axis, orientation. Additionally, (e) is the contour plot.
The imaginary part of equation u 3 , 5 is displayed in Figure 23 for S 1 = 3.50 , S 2 = 3.70 , S 1 = 3.50 , S 3 = 1.20 , R 1 = 11 , R 3 = 13 , P 23 = 5 , P 12 = 9 , (a) is three dimensional with y = 2 . Here, (b), (c), and (d) exploit the z , y , x –axis, orientation. Additionally, (e) is the contour plot.
The real part of u 3 , 6 is displayed in Figure 24 for S 1 = 3.50 , S 2 = 3.70 , S 1 = 3.50 , S 3 = 1.20 , R 1 = 11 , P 23 = 11 , P 13 = 13 , P 12 = 9 , (a) is three dimensional with y = 2 . Here, (b), (c), and (d) exploit the z , y , x –axis, orientation. Additionally, (e) is the contour plot.
The imaginary part of equation u 3 , 6 is displayed in Figure 25 for S 1 = 3.50 , S 2 = 3.70 , S 1 = 3.50 , S 3 = 1.20 , R 1 = 11 , P 23 = 11 , P 13 = 13 , P 12 = 9 , (a) is three dimensional with y = 2 . Here, (b), (c), and (d) exploit the z , y , x –axis orientation. Additionally, (e) is the contour plot.

6.2. Example 2

In this subsection, we use the MEFM to get the novel analytical solutions for (5).
  • One wave solutions for (5):
    In a similar way, we get
    P 1 = arbitrary , ω 1 : 5 S 1 2 S 1 R 1 + 5 R 1 2 R 1 .
    By inserting (93) in (83), the one wave solutions can be presented by v 1 .
    v 1 is displayed in Figure 26 for S 1 = 7 , R 1 = 5 , Q 1 = 0.70 , Q 0 = 0.40 , P 0 = 0.90 , P 1 = 3 , (a) is three dimensional with y = 2 . Here, (b), (c), and ( d) exploit the z , y , x –axis orientation. Additionally, (e) is the contour plot.
  • Two wave solutions for (5):
    In a similar way, we get
    P 12 = 1 , ω 1 = 5 S 1 2 S 1 R 1 + 5 R 1 2 R 1 , ω 2 = 5 S 2 2 S 2 R 2 + 5 R 2 2 R 2 .
    By setting the above values in (89), the two wave solutions can be presented by v 2 .
    v 2 is displayed in Figure 27 for S 1 = 3 , S 2 = 5 , R 1 = 2 , R 2 = 7 , (a) is three dimensional with y = 2 . Here, (b), (c), and (d) exploit the z-axis, y-axis, x-axis orientation, respectively. Additionally, (e) is the contour plot.
  • Three wave solutions for (5):
    In a similar way, we get
    P 12 = 1 , P 13 = 1 , P 23 = 1 , ω 1 = 5 S 1 2 S 1 R 1 + 5 R 1 2 R 1 , ω 2 = 5 S 2 2 S 2 R 1 + 5 R 2 2 R 2 , ω 3 = 5 S 3 2 S 3 R 3 + 5 R 3 2 R 3 ,
    P 12 = 1 , P 13 = arbitrary , P 23 = arbitrary , R 1 = S 1 R 2 S 2 , R 3 = S 3 R 2 S 3 , ω 1 = S 1 ( 5 S 2 2 S 2 R 2 + 5 R 2 2 ) R 1 S 2 , ω 2 = 5 S 2 2 S 2 R 2 + 5 R 2 2 R 2 , ω 3 = S 3 ( 5 S 2 2 S 2 R 2 + 5 R 2 2 ) R 2 S 2 ,
    P 12 = 1 , P 13 = arbitrary , P 23 = 1 , R 1 = S 1 R 3 S 3 , R 3 = S 3 R 2 S 3 , ω 1 = S 1 ( 5 S 3 2 S 3 R 3 + 5 R 3 2 ) R 3 S 3 , ω 2 = 5 S 2 2 S 2 R 2 + 5 R 2 2 R 2 , ω 3 = 5 S 3 2 S 3 R 3 + 5 R 3 2 R 3 ,
    and
    P 12 = arbitrary , P 13 = 1 , P 23 = 1 , R 2 = S 2 R 1 S 1 , ω 1 = 5 S 1 2 S 1 R 1 + 5 R 1 2 R 1 , ω 2 = S 2 ( 5 S 1 2 S 1 R 1 + 5 R 1 2 ) R 1 S 1 , ω 3 = 5 S 3 2 S 3 R 3 + 5 R 3 2 R 3 .
    Thus, the three wave solutions can be presented by v 3 , 1 , v 3 , 2 , v 3 , 3 , v 3 , 4 , respectively.
v 3 , 1 is displayed in Figure 28 for S 1 = 0.5 , S 2 = 0.7 , S 3 = 1.20 , R 1 = 1.50 , R 2 = 2 , R 3 = 1.50 , (a) is three dimensional with y = 2 . Here, (b), (c), and (d) exploit the z , y , x –axis orientation. Additionally, (e) is the contour plot.
v 3 , 2 is displayed in Figure 29 for S 1 = 3.5 , S 2 = 3.7 , S 3 = 1.20 , R 2 = 2.30 , P 13 = 3 7 , P 23 = 5 2 , (a) is three dimensional with y = 2 . Here, (b), (c), and (d) exploit the z , y , x –axis orientation. Additionally, (e) is the contour plot.
v 3 , 3 is displayed in Figure 30 for S 1 = 3.5 , S 2 = 3.7 , S 3 = 1.20 , R 2 = 2 , R 3 = 3 , P 23 = 5 2 , (a) is three dimensional with y = 2 . Here, (b), (c), and (d) exploit the z , y , x –axis orientation. Additionally, (e) is the contour plot.
v 3 , 4 is displayed in Figure 31 for S 1 = 3.5 , S 2 = 3.7 , S 3 = 4.20 , R 1 = 0.50 , R 3 = 0.90 , P 12 = 11 5 , (a) is three dimensional with y = 2 . Here, (b), (c), and (d) exploit the z , y , x –axis orientation. Additionally, (e) is the contour plot.
Although the MEFM can obtain the MWSs to nonlinear equations, calculating each wave solution separately takes a lot of time and this can be one of the shortcomings of this method.

7. Concluding Remarks

In this paper, we applied three different methods, namely, the G G -expansion method, the G G 2 -expansion method, and the MEFM to investigate the nonlinear time fractional Harry Dym equation in the Caputo sense and the symmetric regularized long wave equation in the conformable sense. In particular, we calculated the multiple wave solutions to (2 + 1)-dimensional equations by means of operating the MEFM, containing one, two, and triple-soliton-type solutions. It is obvious that this new technique has plenty of families of solutions, including rational exponential functions by choosing special parameters. Thus, the present paper provides encouragement for future research in soliton topics. The behaviors of the solutions for the known nonlinear equations gained via the MEFM by choosing the suitable values are cited in Figure 10 and Figure 31. Besides, numerical simulations involving the determination of the coefficients have been carried out to prove that the projected algorithm is efficient and applicable. An analytical study was performed for the solutions obtained using employing the aforementioned technique, revealing one, two, and triple-soliton-type solutions. The obtained results are beneficial for the study of wave propagation. The computations in the present paper were made with the aid of Maple.

Author Contributions

D.O., methodology, writing–original draft preparation. S.R.A., methodology, writing–original draft preparation. R.S., supervision and project administration. M.I., editing and methodology. All authors conceived of the study, participated in its design and coordination, drafted the manuscript, participated in the sequence alignment. All authors have read and agreed to the published version of the manuscript.

Funding

This research received no external funding.

Data Availability Statement

Data are contained within the article.

Conflicts of Interest

The authors declare no conflict of interest.

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Figure 1. The (ad) display the 3D, 2D and the contour plots of u 1 , 2 , for λ η > 0 .
Figure 1. The (ad) display the 3D, 2D and the contour plots of u 1 , 2 , for λ η > 0 .
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Figure 2. The (ad) display the 3D, 2D and the contour plots of u 1 , 2 , for η λ < 0 .
Figure 2. The (ad) display the 3D, 2D and the contour plots of u 1 , 2 , for η λ < 0 .
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Figure 3. The (a,b) display the 3D plots of u 3 , 4 , for λ η > 0 and λ η < 0 .
Figure 3. The (a,b) display the 3D plots of u 3 , 4 , for λ η > 0 and λ η < 0 .
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Figure 4. The (a,b) display the 3D plots of u 5 , 6 , for λ η < 0 and λ η > 0 .
Figure 4. The (a,b) display the 3D plots of u 5 , 6 , for λ η < 0 and λ η > 0 .
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Figure 5. The (af) display the 3D, 2D and the contour plots of u 7 , 8 , for λ η > 0 and λ η < 0 .
Figure 5. The (af) display the 3D, 2D and the contour plots of u 7 , 8 , for λ η > 0 and λ η < 0 .
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Figure 6. The (ad) display the 3D, 2D and the contour plots of (72).
Figure 6. The (ad) display the 3D, 2D and the contour plots of (72).
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Figure 7. The (ad) display the 3D, 2D and the contour plots of (73).
Figure 7. The (ad) display the 3D, 2D and the contour plots of (73).
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Figure 8. The (a,b) display the 3D and the contour plots of u 1 , 2 , for λ 2 4 η > 0 .
Figure 8. The (a,b) display the 3D and the contour plots of u 1 , 2 , for λ 2 4 η > 0 .
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Figure 9. The (a,b) display the plots of real and imaginery part of u 1 , 2 , for λ 2 4 η < 0 .
Figure 9. The (a,b) display the plots of real and imaginery part of u 1 , 2 , for λ 2 4 η < 0 .
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Figure 10. The (ae) display the 2D, 3D and the contour plots of the real part of u1.
Figure 10. The (ae) display the 2D, 3D and the contour plots of the real part of u1.
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Figure 11. The (ae) display the 2D, 3D and the contour plots of the imaginary part of u 1 .
Figure 11. The (ae) display the 2D, 3D and the contour plots of the imaginary part of u 1 .
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Figure 12. The (ae) display the 2D, 3D and the contour plots of the real part of u 2 .
Figure 12. The (ae) display the 2D, 3D and the contour plots of the real part of u 2 .
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Figure 13. The (ae) display the 2D, 3D and the contour plots of the imaginary part of u2.
Figure 13. The (ae) display the 2D, 3D and the contour plots of the imaginary part of u2.
Axioms 13 00092 g013aAxioms 13 00092 g013b
Figure 14. The (ae) display the 2D, 3D and the contour plots of the real part of u3,1.
Figure 14. The (ae) display the 2D, 3D and the contour plots of the real part of u3,1.
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Figure 15. The (ae) display the 2D, 3D and the contour plots of the imaginary part of u 3 , 1 .
Figure 15. The (ae) display the 2D, 3D and the contour plots of the imaginary part of u 3 , 1 .
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Figure 16. The (ae) display the 2D, 3D and the contour plots of the real part of u 3 , 2 .
Figure 16. The (ae) display the 2D, 3D and the contour plots of the real part of u 3 , 2 .
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Figure 17. The (ae) display the 2D, 3D and the contour plots of the imaginary part of u3,2.
Figure 17. The (ae) display the 2D, 3D and the contour plots of the imaginary part of u3,2.
Axioms 13 00092 g017aAxioms 13 00092 g017b
Figure 18. The (ae) display the 2D, 3D and the contour plots of the real part of u3,3.
Figure 18. The (ae) display the 2D, 3D and the contour plots of the real part of u3,3.
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Figure 19. The (ae) display the 2D, 3D and the contour plots of the imaginary part of u 3 , 3 .
Figure 19. The (ae) display the 2D, 3D and the contour plots of the imaginary part of u 3 , 3 .
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Figure 20. The (ae) display the 2D, 3D and the contour plots of the real part of u 3 , 4 .
Figure 20. The (ae) display the 2D, 3D and the contour plots of the real part of u 3 , 4 .
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Figure 21. The (ae) display the 2D, 3D and the contour plots of the imaginary part of u3,4.
Figure 21. The (ae) display the 2D, 3D and the contour plots of the imaginary part of u3,4.
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Figure 22. The (ae) display the 2D, 3D and the contour plots of the real part of u3,5.
Figure 22. The (ae) display the 2D, 3D and the contour plots of the real part of u3,5.
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Figure 23. The (ae) display the 2D, 3D and the contour plots of the imaginary part of u 3 , 5 .
Figure 23. The (ae) display the 2D, 3D and the contour plots of the imaginary part of u 3 , 5 .
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Figure 24. The (ae) display the 2D, 3D and the contour plots of the real part of u 3 , 6 .
Figure 24. The (ae) display the 2D, 3D and the contour plots of the real part of u 3 , 6 .
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Figure 25. The (ae) display the 2D, 3D and the contour plots of the imaginary part of u3,6.
Figure 25. The (ae) display the 2D, 3D and the contour plots of the imaginary part of u3,6.
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Figure 26. The (ae) display the 2D, 3D and the contour plots of v 1 .
Figure 26. The (ae) display the 2D, 3D and the contour plots of v 1 .
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Figure 27. The (ae) display the 2D, 3D and the contour plots of v 2 .
Figure 27. The (ae) display the 2D, 3D and the contour plots of v 2 .
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Figure 28. The (ae) display the 2D, 3D and the contour plots of v3,1.
Figure 28. The (ae) display the 2D, 3D and the contour plots of v3,1.
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Figure 29. The (ae) display the 2D, 3D and the contour plots of v3,2.
Figure 29. The (ae) display the 2D, 3D and the contour plots of v3,2.
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Figure 30. The (ae) display the 2D, 3D and the contour plots of v 3 , 3 .
Figure 30. The (ae) display the 2D, 3D and the contour plots of v 3 , 3 .
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Figure 31. The (ae) display the 2D, 3D and the contour plots of v 3 , 4 .
Figure 31. The (ae) display the 2D, 3D and the contour plots of v 3 , 4 .
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Table 1. Diverse values of the solutions of (1) obtained through the G G 2 -expansion method.
Table 1. Diverse values of the solutions of (1) obtained through the G G 2 -expansion method.
λ η > 0 λ η < 0
x = t u 1 , 2 ( x , t ) u 3 , 4 ( x , t ) u 5 , 6 ( x , t ) u 7 , 8 ( x , t ) u 1 , 2 ( x , t ) u 3 , 4 ( x , t ) u 5 , 6 ( x , t ) u 7 , 8 ( x , t )
0.001±10.8391±5.1739±3.0254±7.9327±0.0069±9.7979±4.9993±4.8005
0.010±11.4354±3.9987±3.0052±7.98590.0000±9.7979±4.8991±4.8988
0.100±15.5875±0.9025±1.6523±14.52470.0000±9.7979±4.8989±4.8989
1.001±16.1931±15.2886±9.8816±2.42870.0000±9.7979±4.8989±4.8989
1.010±13.5703±10.6300±33.0590±0.72590.0000±9.7979±4.8989±4.8989
1.100±18.5057±4.9848±1.4733±13.76680.0000±9.7979±4.8989±4.8989
Table 2. Diverse values of the solutions of (1) obtained through G G -expansion method.
Table 2. Diverse values of the solutions of (1) obtained through G G -expansion method.
λ 2 4 η > 0 λ 2 4 η < 0
x = t u 1 , 2 ( x , t ) u 1 , 2 ( x , t )
0.001 ± 4.1671 0.0000
0.010±4.00500.0000
0.100±4.00000.0000
1.001±4.00000.0000
1.010±4.00000.0000
1.100±4.00000.0000
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O’Regan, D.; Aderyani, S.R.; Saadati, R.; Inc, M. Soliton Solution of the Nonlinear Time Fractional Equations: Comprehensive Methods to Solve Physical Models. Axioms 2024, 13, 92. https://doi.org/10.3390/axioms13020092

AMA Style

O’Regan D, Aderyani SR, Saadati R, Inc M. Soliton Solution of the Nonlinear Time Fractional Equations: Comprehensive Methods to Solve Physical Models. Axioms. 2024; 13(2):92. https://doi.org/10.3390/axioms13020092

Chicago/Turabian Style

O’Regan, Donal, Safoura Rezaei Aderyani, Reza Saadati, and Mustafa Inc. 2024. "Soliton Solution of the Nonlinear Time Fractional Equations: Comprehensive Methods to Solve Physical Models" Axioms 13, no. 2: 92. https://doi.org/10.3390/axioms13020092

APA Style

O’Regan, D., Aderyani, S. R., Saadati, R., & Inc, M. (2024). Soliton Solution of the Nonlinear Time Fractional Equations: Comprehensive Methods to Solve Physical Models. Axioms, 13(2), 92. https://doi.org/10.3390/axioms13020092

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