1. Introduction
By applying an inverse operator and the multivariate Mittag–Leffler function, we obtain a unique series solution to the following time-fractional convection–diffusion equation with an initial condition and a source term, for constants
:
where
,
and the partial Liouville–Caputo fractional derivative
of order
with respect to
t is defined as
We note that
b is the diffusion coefficient,
is the velocity field of the fluid, and
denotes the sources.
In particular, we have the non-homogeneous convection equation, given below, if
and
:
and the non-homogeneous heat equation:
if
.
Equation (
1) is a multi-term time-fractional differential equation that describes the transport of a scalar quantity—such as concentration, temperature, or momentum—in a fluid medium due to the combined effects of convection (bulk motion) and diffusion (random molecular motion). It is widely used in fields such as fluid dynamics, heat transfer, and environmental modeling [
1,
2,
3]. Moreover, practical applications of the studied fractional differential equation include modeling contaminant transport in soils and groundwater, where heterogeneous pore structures cause trapping, delays, and the slow release of pollutants from binding sites. It is also used to model non-Fourier heat transfer, particularly in materials such as polymers, biological tissues, and porous media. The use of multiple fractional time derivatives of different orders allows for more accurate modeling of complex memory effects and anomalous diffusion behaviors than single-order models. Each fractional derivative term, with an order between 0 and 1, captures a distinct memory kernel characterized by a specific decay rate. When combined, these terms model systems with multiple relaxation times or heterogeneous memory behaviors. Lower-order derivatives (e.g.,
) correspond to strong memory effects and slower diffusion, while higher-order derivatives (closer to 1) indicate weaker memory and faster system responses. Together, they enable the modeling of transitional behaviors between different anomalous diffusion regimes. In materials or media with multiple trapping mechanisms, binding sites, or structural heterogeneity, different fractional orders naturally reflect the various types of obstructions or delays experienced by transported particles.
Physical scenarios where multi-term fractional equations are particularly relevant include heat conduction in composite or porous materials and drug diffusion in biological tissues, where complex temporal dynamics and structural variability play a significant role.
Generally speaking, there are many analytic approaches [
4] (fractional Green’s function, separation of variables, integral transforms, adomian decomposition method, and homotopy analysis method) and numerical methods [
2] (finite difference methods, finite element methods, spectral methods, and meshless methods) dealing with fractional partial deferential equations. In 2024, Chertovskih et al. [
5] studied an optimal control problem for a stochastic differential equation related to the Fokker–Planck–Kolmogorov equation in the space of probability measures and proposed a rapidly converging numerical algorithm to address the fundamental nature of diffusion processes. In 1997, Tannehill et al. [
6] studied numerical schemes (e.g., upwind, SUPG) for convection–dominated flows. In 2008, Roos et al. [
7] addressed stabilization techniques for singularly perturbed convection–diffusion equations. In 2007, Lin and Xu [
8] considered the numerical resolution for the following time-fractional diffusion equation for
:
subject to the initial and boundary conditions:
and proved that the full discretization is unconditionally stable, and the numerical solution converges to the exact one with the order
, where
, and
m are the time-step size, polynomial degree, and regularity of the exact solution, respectively. However, we believe that applying a numerical approach to Equation (
1) presents significant challenges due to the unbounded domain and the presence of complex terms. To use the inverse operator method, it is necessary to represent the inverse operator as an infinite series, which must be well-defined within an appropriate function space.
On the application side, Bear [
9] applied convection–diffusion equations to model groundwater flow and contaminant transport. LeVeque [
10] discussed finite volume methods for conservation laws, including convection–diffusion systems.
Variants of Equation (
1) with a distributed order have been successfully analyzed in various contexts, and it has been shown that these variants can lead to different diffusion regimes. For example, Luchko [
11] investigated the maximum principle for several types of generalized time-fractional diffusion equations—including multi-term and distributed-order diffusion equations—and applied it to establish the uniqueness of solutions to various initial-boundary value problems. Additionally, Kilbas et al. [
12] constructed a solution to Equation (
1) for the case
, using the Laplace transform, multivariate Mittag–Leffler functions, and Green’s functions. In contrast, our current work employs inverse operators to derive a unique and novel series solution, offering a significantly simpler computational approach that avoids the complex integrals and convolutions typically required when using Green’s functions.
In summary, the multi-term time-fractional convection–diffusion equation extends classical transport models by incorporating memory effects and multi-scale dynamics through fractional derivatives of distinct orders. This equation is indispensable for modeling systems in which transport processes exhibit anomalous behavior or long-range temporal dependencies.
Let
and
. Then
is the well-known multivariate Mittag–Leffler function [
12,
13,
14], which is an entire function on complex plane
. When
, it reduces to the following two-parameter Mittag–Leffler function:
If
, we obtain the classical Mittag–Leffler function defined by
The partial fractional integral operator
(
) is defined as
In particular,
.
The inverse operator method is a powerful tool for studying the uniqueness, existence, and stability of differential equations with various conditions and variable coefficients [
15]. In addition, it is also useful for finding analytic solutions to partial fractional-differential equations or partial integro-differential equations. As an example, we present the following theorem to demonstrate applications of inverse operators in fractional partial differential equations, thereby laying the groundwork for Equation (
1). In addition, we show that the inverse operator method is also applicable to equations with variable coefficients.
Theorem 1. The following equation with a variable coefficient for all () and in the space :wherehas a solution Proof. Applying the operator
to both sides of Equation (
4), we have
using the initial conditions given. This implies that
We are going to show that the inverse operator (unique) of
is
in the space
. In fact, for any
,
where
Hence, the operator
is well-defined in the space
. Furthermore,
Clearly,
Similarly,
. Assuming
is another inverse operator. Then
and applying
to both sides of the above implies that
.
From Equation (
5), we derive
which converges under the norm of the space
. This completes the proof. □
Very recently, Li [
16] considered the following fractional differential equation using the inverse operator method:
where
and obtained
in a subspace of
.
In particular, if
, then Equation (
1) reduces to
which is similar to Equation (
6), except for the difference in the fractional order and the fact that
is a more general operator than
.
The remainder of the paper is structured as follows.
Section 2 derives a unique series solution to Equation (
1) based on a new space
S, an inverse operator, and the multivariate Mittag–Leffler function.
Section 3 discusses a time-fractional non-homogenous convection equation, which is the particular case for Equation (
1), and show that our solution is consistent with the existing integral convolution solution using the Fourier transforms and Taylor’s expansion of the two-parameter Mittag–Leffler function.
Section 4 works on a time-fractional non-homogenous convection equation obtained from Equation (
1) in detail with an illustrative example showing applications of our results.
Section 5 proves that our series solution derived in
Section 2 coincides with the classical integral solution. Finally. we summarize the entire work in
Section 6.
3. The Solution to the Time-Fractional Non-Homogenous Convection Equation
Clearly, if
, then the fractional convection equation:
has a unique solution for
from Theorem 2
In the following, we show that solution (
10) can be written as the following convolution solution for
(the AI model DeepSeek-
finds this integral solution):
where
and
are Green’s functions, given by
and
respectively.
We begin defining the
n-dimensional Fourier transform as
and the inverse Fourier transform
where
. In particular, we write
. Then, we have
, and thus,
So, we have
On the other hand, we have
It is not difficult to see that
So, we have
Substituting (
12) and (
13) into (
10) results in the desired convolution expression (
11).
Furthermore, if
,
and
, then the equation:
has a unique solution by noting that
which represents a wave travelling to the right if
or left if
.
On the other hand, if
and
, then we obtain Equation (
2) with a unique solution
Example 1. The following time-fractional convection equation:has a unique solution for Clearly, we haveandwhere . Thus, We should note that it would be complicated to use the following integral formula to find the solution:
and our method is much easier and faster.
Remark 2. (a) It would be interesting to see how DeepSeek-R1 finds the solution (11). When the problem (9) is entered in LaTeX code form, DeepSeek-R1 first converts the fractional partial differential equation into the partial differential equationby performing the Laplace transform . Here, and . Then DeepSeek-R1 points out that Equation (16) can be solved by using the Fourier transform method. After applying the inverse Laplace transform and inverse Fourier transform, it obtains the solution (11). The authors also employ DeepSeek-R1 to find series solutions of (9), but it fails to reach our expression (10). The reason is that DeepSeek AI can generally be used to solve many fractional partial differential equations (FPDEs) analytically by leveraging known techniques such as Laplace and Fourier transforms, separation of variables, Green’s functions for fundamental solutions, eigenfunction expansions, and series expansions with re-summation. However, our series solution method differs from the approaches mentioned above. (b) The experience of using DeepSeek in this specific case has been notably effective. It not only presented integral convolution solutions but also offered detailed steps mentioned above that accelerated our understanding of the existing theoretical framework. By streamlining the literature review process, DeepSeek allowed us to focus more deeply on the key materials of the problem, ensuring that our work builds directly upon them.