Abstract
In this paper, we primarily use the inverse operator method to find a unique series solution to a time–fractional wave equation with variable coefficients based on the Mittag–Leffler function. In addition, we also derive the series and integral convolution solutions to the Klein–Gordon equation using the Fourier transform and Green’s functions. Furthermore, our series solutions significantly simplify the process of finding solutions with several illustrative examples, avoiding the need for complicated integral computations.
Keywords:
Mittag–Leffler function; time–fractional wave equation; inverse operator method; Fourier transform; time–fractional Klein–Gordon equation MSC:
35A02; 35C15; 47N20; 26A33
1. Introduction
The induction will proceed through six small subsections: preliminaries, motivation, a review of the literature, the Klein–Gordon equation and research methods, the importance of the Klein–Gordon equation, and further discussion and examples.
1.1. Preliminaries
Time–fractional wave equations with variable coefficients play a significant role in both theoretical and applied mathematics, as well as in physics and engineering, due to their ability to model complex phenomena that classical wave equations cannot adequately capture. Moreover, the Fourier transform serves as a fundamental tool in the analysis of such equations. To initiate this process, we define the n-dimensional Fourier transform as
and the inverse Fourier transform;
where . In particular, we write .
Clearly, from , we have
where Δ is the Laplace operator given by
Let and . Then
is the well-known multivariate Mittag–Leffler function [1,2], which is an entire function on the complex plane , with
When , it reduces to the following two-parameter Mittag–Leffler function:
If , we obtain the classical Mittag–Leffler function defined by
The gamma function, denoted by for , is an extension of the factorial function, given by
The partial Liouville–Caputo fractional derivative of order () with respect to t is defined in [1] as
In particular, for ,
In addition, we define the fractional partial integral operator of a function for as
In particular,
1.2. Motivation
Fractional partial integrals and derivatives are fundamentally non-local operators, meaning they incorporate information over an entire domain rather than just a neighborhood of a point (like classical derivatives). This nonlocality is crucial for modeling systems where long-range interactions, memory effects, or spatially distributed dependencies play a key role.
In this paper, we will study the following equation with initial conditions and variable coefficients for and :
which, to the best of our knowledge, has not been previously studied.
This equation is essential in applications due to the following factors:
(a) The equation involves a Caputo fractional derivative of order , which generalizes the classical second-order time derivative. This allows it to model systems that exhibit memory and hereditary effects, which classical diffusion or wave equations cannot capture.
(b) This is a fractional diffusion–wave equation, interpolating between diffusion () and wave () dynamics. It is applicable in anomalous diffusion, viscoelastic materials, signal processing, and finance.
(c) The function introduces time-dependent diffusivity, making the model more realistic for non-homogeneous media where the material properties evolve with time.
(d) Solving such equations requires advanced tools, like the inverse operator method, especially when or are not constant. These methods help to establish the existence, uniqueness, and even series representations of solutions.
Furthermore, the time–fractional wave equation has emerged as a central topic in the study of anomalous diffusion and wave propagation phenomena, particularly where memory and hereditary properties simulate. Unlike classical wave equations, time–fractional models incorporate nonlocality in time, typically via the Caputo or Riemann–Liouville fractional derivatives, enabling them to describe complex physical processes more accurately. This model generalizes the classical wave and heat equations, allowing for the description of anomalous diffusion and memory-dependent processes in complex systems. The presence of variable coefficients makes the equation suitable for real-world applications in heterogeneous media, while also introducing significant analytical challenges. The inclusion of first- and second-order initial conditions further enhances its applicability to physical problems involving memory and inertia. The inverse operator method applied in this paper offers a robust approach to establishing the existence and uniqueness of a series solution, making this study both mathematically rich and practically relevant.
1.3. Literature Review
One of the foundational contributions is made by Mainardi [3,4], who investigated the fundamental solutions of the time–fractional diffusion–wave equation, revealing its intermediate nature between parabolic and hyperbolic dynamics. Gorenflo et al. [5] further analyzed these fundamental solutions using Fox H-functions, providing insights into their analytical structures. Podlubny [6] provided a comprehensive mathematical framework for fractional differential equations, laying the groundwork for further theoretical advancements.
Theoretical studies have focused on the existence, uniqueness, and regularity of solutions. Eidelman and Kochubei [7] analyzed the Cauchy problem for fractional diffusion–wave equations, providing integral representations and exploring the properties of fundamental solutions. Similarly, Luchko [8] established maximum principles and uniqueness theorems for time–fractional PDEs, extending classical results to the fractional setting.
Spectral methods and eigenfunction expansions have been employed for analytical solutions, especially in bounded domains. Li and Liu [9] investigated eigenfunction expansions for multi-term time–fractional wave equations, contributing to the spectral theory of fractional models. Moreover, Kilbas et al. [1] provided detailed theoretical insights into the mathematical properties of fractional operators and their applications to linear and nonlinear PDEs.
In 2022, Abuomar et al. [10] studied the following fractional wave equation with certain conditions for :
based on the Laplace transform and fractional series method.
Very recently, Li and Liao [11] studied the generalized time–fractional diffusion–wave equation for using the inverse operator method for all constants and :
based on the multivariate Mittag–Leffler function and a newly constructed space.
Huang and Yamamoto [12] established existence, uniqueness, and regularity estimates for fractional diffusion–wave equations (fractional order in ) with time-dependent coefficients, via Fredholm and Galerkin methods. Li et al. [13] derived a unique series solution to a multiple time–fractional convection diffusion equation with a non-homogenous source term based on an inverse operator, a newly constructed space, and the multivariate Mittag–Leffler function. Ge and Zhang [14] investigated the exponential/polynomial stability of wave equations with boundary fractional damping and spatially variable coefficients.
There are both analytical approaches [15]—such as convolution and fractional Green’s functions, various types of integral transforms, separation of variables, the Adomian decomposition method, and the homotopy analysis method—and numerical methods [6], including finite difference methods, finite element methods, spectral methods, and meshless methods, for solving fractional partial differential equations.
1.4. The Klein–Gordon Equation and Research Methods
The motivation for using the Mittag–Leffler function and the inverse operator method in this paper stems from the fact that Equation (1) is not easily handled by any currently existing theoretical methods—including Laplace and Fourier transforms—due to the presence of the variable coefficient , which is independent of any spatial variable. In addition, this approach is also useful for finding analytical solutions to fractional partial differential equations and partial integro-differential equations under various conditions [11]. As a demonstration, we first apply this technique to the following Klein–Gordon equation, as a preparatory step toward solving Equation (1).
Let S be the subspace of , given by
Theorem 1.
Let . We assume that is continuous over in t and . Then, the following time–fractional Klein–Gordon equation for and is a smooth function over with respect to x:
where is a constant (mass parameter) that admits a unique solution,
if and are in S. Furthermore, there is an integral solution:
where the Green’s functions are defined by
and
Proof.
Clearly, for ,
provided is continuous over in t and . Then,
Applying the operator to both sides of Equation (2) yields
which implies that
by using the initial conditions.
To find the inverse operator of , we define an operator V as
which is well defined over the space S. Indeed, for any , we have
for any non-negative integer . Thus,
for each . Furthermore,
It follows that
Similarly,
and the uniqueness of V is clear. Hence,
Using the Fourier transform, we get
Since
we deduce that
Let the Green function be defined as
Then,
On the other hand,
using
Let the Green function be defined as
Then,
The uniqueness of solutions follows immediately from the uniqueness of the inverse operator V. This completes the proof. □
1.5. The Importance of Klein–Gordon Equation
The time–fractional Klein–Gordon Equation (2) is a significant generalization of the classical Klein–Gordon equation, which serves as a cornerstone in relativistic quantum mechanics and field theory. The fractional formulation is important for a variety of reasons—spanning mathematical, physical, and applied contexts:
(a) The key difference lies in the Caputo fractional derivative of order in time, as follows: . This operator introduces memory effects, meaning that the future evolution of depends not just on its current state but also on its entire history. This is critical for viscoelastic materials, non-Markovian processes in quantum mechanics, and anomalous diffusion (where the mean square displacement grows nonlinearly in time).
(b) The classical Klein–Gordon equation () models relativistic wave propagation. Replacing the second-order time derivative with a fractional derivative allows the model to capture memory effects and non-local temporal behavior—features typical of complex or disordered media. In addition, the time–fractional Klein–Gordon equation offers new insights in mathematical physics, especially in the study of non-local and fractional dynamics, and it drives the development of new analytical and numerical methods [16].
(c) Fractional PDEs like (2) open new avenues in functional analysis (especially in fractional Sobolev spaces), existence, uniqueness, and regularity of solutions, and spectral theory, especially for the fractional Laplacian and damping/memory terms. Theorem 1 asserts the well-posedness (existence and uniqueness under smooth initial conditions) of the problem, which is critical for building further analysis.
(d) The time–fractional Klein–Gordon equation appears in quantum field models with temporal dispersion or dissipation, acoustics in lossy media, plasma physics, where wave propagation is not purely classical, and geophysics (e.g., seismic wave attenuation).
In addition, the mass parameter m is typically taken to be real and non-negative for physical reasons: The Klein–Gordon equation describes spin-0 particles (scalar or pseudoscalar bosons) in quantum field theory, and the parameter m corresponds to the rest mass of the particle, which is a measurable physical quantity. Mass is conventionally non-negative in classical and quantum physics.
1.6. Further Discussion and Examples
Remark 1.
(a) Clearly, the solution u given in Equation (3) satisfies the conditions that and by noting that .
(b) In addition, in order to prove the equivalence between Equation (1) and Equation (3), we used the identity for
if . Indeed, we are able to provide the following distributional proof directly. Let
In particular, in the distributional sense, and
where ϕ is a smooth function with compact support [17]. Using
implies that
Thus,
by using the identity
Since w is continuous, the identity
holds point-wise on the interval .
Remark 2.
Following the similar technique, we are able to find the unique series or integral solution for the time–fractional non-homogeneous Klein–Gordon equation:
with a slight modification of the space S and certain conditions on g:
Then,
where the Green’s functions and are defined above, and
which is the fundamental solution to equation:
Example 1.
The following time–fractional Klein–Gordon equation for ,
has a unique solution:
Evidently, and 1 are in the space S. From Theorem 1, we have
Applying the identity
we arrive at
which satisfies the initial conditions
by noting that .
Clearly, this series approach is much simpler than using the integral solution which contains complicated computations.
In general, the Klein–Gordon equation
has the solution
using the identities [6]:
2. The Fractional Wave Equation with Variable Coefficients
In this section, we mainly work on Equation (1) based on the inverse operator method, the Mittag–Leffler function and a new space , with two illustrative examples.
Theorem 2.
We assume that is continuous over in t and . Let and and ψ be in the space defined by
Then, the solution to Equation (1), being a smooth function over with respect to x, admits a unique series solution:
In particular, if (constant), then
where
Proof.
By applying the operator to both sides of Equation (1), we have
which implies that
To find a unique inverse operator of over , we define
which is well defined over . Indeed, for , we get
and
using
Therefore,
by noting that . Moreover, is a unique inverse operator of since
In fact,
Similarly,
and the uniqueness of follows easily. Hence,
If , then
Firstly, we consider , which is
by using
As for
Finally,
From the solution
we clearly see that
since . This completes the proof. □
Example 2.
The following is a fractional wave equation with a variable coefficient and initial conditions:
where a is a constant and
is the Bessel function of the first kind, which admits a unique solution:
In , the Laplace operator in polar coordinates is
For a radially symmetric function , we obtain
We now consider the eigenfunction equation for the Laplacian:
For a redial solution , this becomes
which is Bessel’s equation for order , and its solution is . This implies that
Thus, applying the Laplacian k times gives
This identity also deduces that . On the other hand,
which claims that
From Theorem 2, we get
Using
we have
by noting that and are in the space and
for all .
Remark 3.
We should note that the series
converges. Indeed,
and
Hence,
Remark 4.
If and , then Equation (1) becomes a non-homogeneous wave equation:
with the solution
Li and Liao [11] showed that if and , then
This is d’Alembert’s formula for a one-dimensional homogeneous wave equation.
Furthermore, if and , then
which is the well-known Kirchoff formula [18], and where denotes the surface area of the ball and is the boundary of .
We can use Kirchhoff’s formula for the solution of the wave equation in three dimensions to derive the solution of the wave equation in two dimensions. This technique is known as the method of descent. A similar result also holds for .
Moreover, if and n is odd, then the series solution given is
where
and the average value of ϕ over is defined as
A similar conclusion follows if and n is even.
Example 3.
The following wave equation in with the initial conditions,
has a unique solution:
Clearly,
for all and
which implies that
From Theorem 2, we get
Using the identities
we get
which claims that
Therefore,
which is a simple function.
3. Conclusions
By applying an inverse operator method, we studied the time–fractional wave equation (1) and the time–fractional Klein–Gordon equation (2), utilizing a multivariate Mittag–Leffler function and newly constructed function spaces. Moreover, we derived both series and integral solutions. In particular, our series-based technique provides a simpler process for finding solutions. This approach is also applicable to a wide range of fractional partial differential equations, such as the fractional Euler–Bernoulli beam equation:
where .
This equation has good applications in viscoelastic beam vibrations with key features that combine fractional damping and stiffness.
Funding
This research was supported by the Natural Sciences and Engineering Research Council of Canada (Grant Number 2019-03907).
Data Availability Statement
Data sharing is not applicable to this article as no new data were created or analyzed in this study.
Acknowledgments
The author is thankful to the reviewers and editor for providing valuable comments and suggestions.
Conflicts of Interest
The author declares no conflicts of interest.
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