Abstract
A mathematical model consisting of weakly coupled time fractional one parabolic PDE and one ODE equations describing dynamical processes in porous media is our physical motivation. As is often performed, by solving analytically the ODE equation, such a system is reduced to an integro-parabolic equation. We focus on the numerical reconstruction of a diffusion coefficient at finite number space-points measurements. The well-posedness of the direct problem is investigated and energy estimates of their solutions are derived. The second order in time and space finite difference approximation of the direct problem is analyzed. The approach of Lagrangian multiplier adjoint equations is utilized to compute the Fréchet derivative of the least-square cost functional. A numerical solution based on the conjugate gradient method (CGM) of the inverse problem is studied. A number of computational examples are discussed.
1. Introduction
The second-order hyperbolic and parabolic systems of partial differential equations, as well as coupled PDE-ODE systems, are a substantial theoretical foundation for many mathematical and engineering problems [1,2,3,4,5,6,7,8,9,10]. In the present paper, we concentrate on the features of a parabolic PDE-ODE system.
Recently, because of the the many applications, fractional integro-differential equations are the focus of a large body of results. The classical integer order derivative is a local operator, which is not adequate for a description of many processes in physics, mechanics, industrial finance, etc. The fractional derivative is a nonlocal operator, which is often used to model phenomena in heat mass transfer [4,5,11], medicine [12], viscoelastic materials [8,13], porous media [1,5,7,10,14,15], mathematical biology and in particularly the honeybee population [16], mathematical finance and economics—see [17,18] and references therein—and atmosphere pollution [6,19].
In [4], analytical exact solutions to the neutron fractional parabolic PDE-ODE system are derived. The inverse problems (IPs) of differential equations with time fractional derivatives concern the recovery of a variety unknown parameters, such as source term, fractional order, coefficients, etc. For instance, Georgiev and Vulkov [16] present a numerical study of the inverse problem for coefficient determination in honeybee population models with Caputo and Caputo–Fabrizio time fractional derivative, and in [13] a parameter identification inverse problem is studied.
In this work, we numerically recover the unknown diffusion coefficient for a time fractional integro-diffusion convection reaction equation, obtained from a model system of differential equations.
A System of a Parabolic and a Ordinary Differential Equation
As a simple physical motivation, we consider a model of non-Darcian flow in transport media used to describe different real processes, see, e.g., [3,5,7,8,10,20].
Suppose that diffusion and solute transport initiate within the mobile phase, while the change in solute concentration within the immobile phase is a dynamic process influenced by the porous media’s low permeability and significant heterogeneity. The fractional calculus has been introduced as an efficient tool for modeling. A general form of a differential equation system that describes such processes reads as follows [3,5,7,20]:
with the initial condition and appropriate boundary conditions. Here, and
is the pointwise Caputo derivative [13,21,22,23]. With u and w are denoted the concentration of a contaminant in the relevant phases. The authors of [24] using Equation (2) write an integral formula for and placed it in (1) to obtain an integro-differential equation for , . On this basis, we consider a more general equation:
The remainder of the paper is constructed as follows. In Section 2, we give some notations and discuss the well-posedness of the direct problem. Section 3 is devoted to the numerical solution of the direct problem. In Section 4, we introduce the IP and study its quasisolution. In Section 5, we introduce a finite difference method, combined with the conjugate gradient method (CGM) to solve the IP. Section 6 presents computational results that validate the analysis and demonstrate the efficiency of the proposed algorithm. Some comments and conclusions finalized this paper.
2. Well-Posedness of the Direct Problem
In the IP, it is assumed in advance that the corresponding direct problem is well-posed. The main purpose of this section is the discussion of this question. In this section, our main focus is on the discussion of this question. We consider the Equation (4), , and with no loss of generality, zero Dirichlet boundary conditions
and initial condition
2.1. Notations and Preliminaries
In the following, we assume classical interpretations of fractional calculus and equations and will refer to monographs [22,23]. Further, let
with and
where the norms are conventionally established by
In view of the Young inequality on the convolution, it could be directly established that the classical Caputo derivative (3) could be well-defined for
The Riemann–Liouville left and right integrals of fractional order are defined as follows [22,23]:
and the corresponding Riemann–Liouville left and right fractional derivatives for are defined as
Further, the notations and will be used instead of and , respectively, etc.
Let us recall the integration by parts formula, see, e.g., [25] (Proposition 2.19). Let and assume that , , and , where
with and being the classes of continuous and absolutely continuous functions in [22,23].
Then, we have the integration by parts formula
The subsequent Gronwall-type inequality is established in [26].
Lemma 1.
Let the absolutely continuous function satisfy the inequality
for almost all t in , where is a positive constant and is an integrable function on . Then,
where
are the Mittag–Leffler functions.
Further, we also use the relation between Caputo and Rieamann–Liouville derivatives
2.2. Solution of the Direct Problem
Now, following the results of Section 3 in [24] we show first the forward (direct) problem (4)–(6) and present a priory estimates for the corresponding solutions.
Theorem 1.
Suppose that the smoothness conditions hold:
and
Then,
and the a priori estimate holds
where is a constant, which does not depend on and f.
Here, we use standard notations [23,27]
as well as for the Hölder spaces , .
The proof of Theorem 1 resembles the one of Theorem 1 in [24], namely, first we take the scalar product of Equation (4) with u. Then, we use Lemma 3 from [26] (continuous version of Lemma 3 in the current study). Next, we apply several times the -Cauchy inequality to estimate the terms of the scalar product and to obtain a basic inequality. Further, we act with integral operator to both sides of this inequality and obtain (8).
3. Numerical Solution of the Direct Problem
Here we construct a monotone finite difference discretization for (4)–(6) and investigate the stability and convergence.
3.1. Difference Scheme
We construct a second-order monotone Samarskii-type [28] finite difference scheme for the discretization in space and scheme [29] of order for the temporal approximation.
On the rectangle , we build the uniform mesh
where
Further, we set , .
To build a monotone scheme for (4)–(6), that satisfies the maximum principle for arbitrary mesh step sizes, we consider the perturbation of Equation (4), see [28]
We write as a sum
and approximate in space as follows:
where
Thus, the resulting semidiscretization
achieves a second-order of convergence in space, as is proved in [28], since
The temporal derivative is discretized by formula of order at , , , , derived in [29].
where, for and for
Using (9), the —weighted finite difference discretization of the Equation (4) is
, where
and similarly for , and .
The approximation (11) is obtained in the same fashion as the discretization of the fractional integral operator.
Further, the integrals in (11) can be computed by the trapezoidal rule, midpoint rule or exactly, depending on the function .
The Dirichlet boundary conditions (5) and initial condition (6) are incorporated into the numerical scheme straightforwardly:
Lemma 2
([30]). Suppose that the non-negative , , fulfill the inequalities
where are constants. Then, there exists , such that: for , we have
where .
Further, we use the difference scheme inequality as well.
Lemma 3
([29]). For every mesh function , defined on , the inequality holds:
where , where .
3.2. Solvability and Convergence
Theorem 2.
Proof.
We apply the energy method of Samarskii [28] for the case . With this aim, we introduce the scalar product along with its corresponding norms:
We obtain the scalar product of with (10):
We estimate each term of the equality (14) using Lemma 3:
Finally, inserting the last estimates in (14), we obtain
Then, taking , we obtain
Now, the application of Lemma 1 to the last inequality results in
where the constant does not depend on h and .
In view of the expression for , we restate the last inequality in the following:
Letting we obtain from the last inequality
where
The inequality (13) provides the unicity and stability of the difference scheme (10), (12) with respect to the right-hand side and initial data.
Further, again using Theorem 1, we will obtain an accuracy estimate for the difference problem (10), (12). Let , where and is the solution of the differential problem (4)–(6), while is the solution of the difference problem (10), (12). Then, inserting in (10), (12), for the mesh function V, we derive the following discrete problem:
with approximation error .
Applying Theorem 1 to the problem (17), we find
where the constant is independent on h and . From this inequality follows the convergence of the discretization (10), (12) towards the solution of the differential problem (4)–(6) on the each time level, so that there exists s.t. for the estimate holds
4. Quasi Solution of the IP
For the ease of simplicity we further consider space space-dependent coefficient in the Equation (4). Then, the IP is to reconstruct under the measurements
We employ the Lagrange multiplier technique [2,27,31] to obtain the Fréchet gradient of the least-squares discrepancy functional associated with the quasisolution of the IP (4)–(6), (18). Because of the instability of their solutions with respect to (18), these IPs are ill-posed [2,27,31].
Moreover, in our case, the solution’s uniqueness of the IP is dependent on the placement of the points in (18) along with the initial and boundary conditions.
Consider the operator form of the problem (4)–(6), (18). Here, denotes an injective operator, represents the admissible set and , where G is Euclidian space. Our IP is reformulated as a minimization problem:
with being the solution to the problem (4)–(6).
In order to numerically investigate the recovering of the diffusion coefficient from the observations at interior points, we employ the conjugate gradient method (CGM). It is grounded in the utilization of the Fréchet gradient of the objective functional (19). The increment of the functional could be express as follows [2,27,31,32]:
where with we denote the scalar product in . Therefore, . We use the adjoint operator
Theorem 3.
The proof resembles the one of Theorem 3 in [24]. A key role has the so-called sensitivity problem. By we denote that depends on the parameter . Assume that for and , .
Hence, the deviation fulfills the next IBVP with an accuracy up to terms of order :
5. Conjugate Gradient Steepest Descent Method
We explore the CGM [2,24,27,31,33] in developing a numerical algorithm to solve the IP for recovering the diffusion coefficient from interior concentration observations in porous media. As is common knowledge, the Fréchet gradient (20) plays a key role.
The iterative procedure is implemented by applying the CGM (see, e.g., [2,27,31,33])
where k denotes the number of iteration, and correspond to consecutive approximations of the minimizer, and and refer to the search direction and the search step size, respectively.
At each step, the search direction is computed as a linear combination of the steepest descent direction at the current approximation and the search direction from previous iterations, namely,
with being the conjugation coefficient. An often-used choice of is as follows [2,27,32]:
first proposed by Fletcher and Reeves [34]. The coefficient is determined through the use of line search, which involves minimizing along the specified search direction, . Applying the sensitivity problem (24)–(26), a method similar to [35] can be employed to linearize the objective functional with respect to and obtain the search step size
where and are the corresponding direct and sensitivity problems solutions and , .
6. Numerically Solving the Inverse Problem
In this section, we will develop numerical discretizations for solving the IP. To this aim, we need to approximate adjoint problem (21)–(23), sensitivity problem (24)–(26), gradient of the functional (20), etc.
6.1. Discretization of the Adjoint Problem
Now, we consider (21)–(23). Applying the temporal inversion in (21), we obtain a forward problem with an initial instead of terminal condition and , , , , . With the fractional derivative , we deal as in [14], applying also the variable change , namely,
Next, in view of (7), considering , we obtain
We take , since in this case (22), (23) are satisfied for .
We treat the time integral in (21) similarly
where , .
Then, we approximate the adjoint problem in the same fashion as the direct problem and derive
where , , ( and
For Dirichlet boundary conditions (23), we have
6.2. Discretization of the Sensitivity Problem
6.3. Discretization of the Gradient of the Functional and
For the approximation of the gradient of the functional at spatial grid node , , we apply central second order discretization and the trapezoidal rule:
where and .
In order to obtain the conjugate coefficient at iteration number , we need to solve the integral
6.4. Realization
The CGM for solving the IP is realized by the Algorithm 1.
| Algorithm 1 Inverse problem |
7. Computational Results
Here, we provide numerical results from computations for both direct and inverse problems in order to illustrate the effectiveness and accuracy of the suggested numerical method. The computational domain is .
We consider (4)–(6), with r.h.s , initial and boundary conditions, such that , is the exact solution. The other model parameters are
Example 1
In Table 1, we illustrate the order of convergence in space and time. As a benchmark test, we also include the case of integer time derivative, namely . The computations are conducted for . Results show that the order of convergence is .
Table 1.
Errors and spatial convergence rate of the solution of the direct problem.
Example 2
(Inverse problem). With this test, we demonstrate the efficiency in recovering the diffusion coefficient and solution u of the IP. The initial guess for the diffusion coefficient is generated by [36]
where is a uniformly distributed random function in the interval and is the exact diffusion coefficient. In the same fashion, we generate noisy data
where is the exact solution at points of measurements .
The measurements are located at grid nodes; namely, we take seven spatial nodes , at and all time layers. The initial data are regularized by smoothing the function using fifth-degree polynomial curve fitting. The stopping accuracy is . Actually, for all presented experiments at the first 2–3 iterations, the functional J decreases more rapidly and then, the decreasing is very small. On Figure 1 and Figure 2, we plot the true (exact) and restored diffusion coefficient and error of the computed by the inverse problem solution U for , and , , .
Figure 1.
Exact (solid line) and restored (line with circles) diffusion coefficient (left) and solution u (right), , , .
Figure 2.
Exact (solid line) and restored (line with circles) diffusion coefficient (left) and solution u (right), , , .
In Figure 3, we depict the exact and restored diffusion for , and , and . We observe that for both values of the fractional order, the accuracy of the restored function is very close.
Figure 3.
Exact (solid line) and restored (line with circles) diffusion coefficient , (left) and (right), , .
The results show that the main factor for the accuracy of the solution is the deviation of the measurements, rather than the fractional order.
Next, we take initial function, right-hand side
and generate perturbed data from (34), (35), replacing the exact solution u with a numerical solution of the direct problem, computed for the exact diffusion coefficient. Then, the solution of the discrete inverse problem U will be compared with the corresponding numerical solution of the direct problem. The computations are performed for and the same points of measurements as in previous test. On Figure 4 (left), we illustrate the impact of the fractional order on the accuracy for , . As before, we deduce that it is not so significant. On Figure 4 (right), we examine the impact of the perturbation on the accuracy for . We observe that the deviation has a larger impact on accuracy than the fractional order. On Figure 5, we plot the error of the solution for and two sets of perturbation and . In spite of the noise affecting the accuracy of the solution, it is evident that the precision of the solution is quite satisfactory when employing the recovered diffusion coefficient.
Figure 4.
Dependence on the fractional order (left): exact (solid line) and restored diffusion coefficient , (line with triangles), (line with squares), (line with circles), , ; dependence on the perturbation (right): Exact (solid line) and restored diffusion coefficient , , (line with triangles), , (line with circles), , (line with squares), , (line with stars).
Figure 5.
Error of the solution for (left) and (right).
The computational simulations, presented in this section to test the proposed approach are implemented by MATLAB® R2022a.
8. Conclusions
In this paper, we have solved a single fractional parabolic integro-differential equation, derived by reducing a coupled fractional parabolic PDE-ODE system. First, we discussed the well-posedness of the Dirichlet problem and then we performed an analysis for stability and convergence of Alikhanov’s scheme [29]. We have developed an approach for numerical recovering of the space-dependent diffusion coefficient using a finite number of space points observations. We have experimentally illustrated the efficacy of the suggested method. The order of the fractional derivative does not significantly affect the results. The numerical tests with perturbed data showed the accurate recovery of the diffusion coefficient with a satisfactory error.
We intend to expand the investigation presented in this paper to other inverse problems of type [37,38,39,40,41,42] for one and multidimensional systems of fractional differential equations.
Author Contributions
Conceptualization, L.G.V.; methodology, M.N.K. and L.G.V.; investigation, M.N.K. and L.G.V.; resources, M.N.K. and L.G.V.; writing—original draft preparation, M.N.K. and L.G.V.; writing—review and editing, L.G.V.; visualization, M.N.K. All authors have read and agreed to the published version of the manuscript.
Funding
This research was supported by the Bulgarian National Science Fund under the Project KP-06-N 62/3 “Numerical methods for inverse problems in evolutionary differential equations with applications to mathematical finance, heat-mass transfer, honeybee population and environmental pollution”, 2022.
Data Availability Statement
Not applicable.
Acknowledgments
The authors express their gratitude to the anonymous reviewers, whose valuable comments and suggestions have improved the quality of the paper.
Conflicts of Interest
The authors declare no conflict of interest.
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