/ / Article

Research Article | Open Access

Volume 2017 |Article ID 3204959 | 7 pages | https://doi.org/10.1155/2017/3204959

# Numerical Inversion for the Multiple Fractional Orders in the Multiterm TFDE

Accepted02 Jul 2017
Published17 Aug 2017

#### Abstract

The fractional order in a fractional diffusion model is a key parameter which characterizes the anomalous diffusion behaviors. This paper deals with an inverse problem of determining the multiple fractional orders in the multiterm time-fractional diffusion equation (TFDE for short) from numerics. The homotopy regularization algorithm is applied to solve the inversion problem using the finite data at one interior point in the space domain. The inversion fractional orders with random noisy data give good approximations to the exact order demonstrating the efficiency of the inversion algorithm and numerical stability of the inversion problem.

#### 1. Introduction

The partial differential equations of fractional order have played an important role in modeling of the anomalous phenomena and in the theory of the complex systems during the last two decades; see, for example, . The so-called time-fractional diffusion equation (TFDE) that is obtained from the classical diffusion equation by replacing the first-order time derivative by a fractional derivative of order with has to be especially mentioned. On the other hand, by the attempts to describe some real processes with the equations of the fractional order, several researches were confronted with the situation that the order of the time-fractional derivative from the corresponding models did not remain constant and changed, say, in the interval from to , from to , or even from to . To manage these phenomena, several approaches were suggested. One of them introduces the fractional derivatives of the variable order, that is, the derivatives with the order that can change with the time or/and depending on the spatial coordinates , and the other way is to employ the distributed order TFDE, or the multiterm TFDE in discretization. Let be a bounded domain in () with smooth boundary , and let ; the multiterm homogeneous TFDE with variable coefficient in is given as where denotes the state variable at space point and time , denotes the principal fractional order, and are the multiterm fractional orders of the time derivatives, which satisfy the condition and are positive constants, and is the smooth diffusion coefficient tensor. All of the above time-fractional derivatives are defined in the sense of Caputo; for example, the fractional derivative of the order is given by See, for example, Podlubny  and Kilbas et al.  for the definition and properties of Caputo’s derivative.

There are still a few research works reported on the multiterm TFDE like (1). On theoretical analysis and analytical methods for the forward problem, we refer to Daftardar-Gejji and Bhalekar , Luchko [15, 16], Jiang et al. , Ding et al. [18, 19], and Li et al. , and for numerical methods and simulations we refer to , and so on.

However, for real problems, the fractional orders, the initial distribution, the diffusion coefficient, or the source term cannot be obtained directly and we have to determine them by some additional measurements, which contributes to inverse problems arising in the fractional diffusion models. There are still some researches on inverse problems for the one-term TFDE; see, for example, Murio , Liu et al. [25, 26], Sakamoto and Yamamoto , Tuan , Chi et al. , Yamamoto and Zhang , Luchko et al. , Wei et al. [32, 33], and Liu et al. ; also see Jin and Rundell  for a tutorial review on inverse problems for anomalous diffusion processes.

It is noted that the research works stated above are almost related to coefficient identification problems in the one-term time/space fractional diffusion equations. However, it is also important to deal with inverse problems of determining the fractional orders in the fractional differential equations since the fractional order is an essential index characterizing the anomalous diffusion. As for inverse problems of determining fractional orders in the single-term time/space fractional diffusion models, we refer to , and so on. On the other hand, there are few literatures concerned with the inverse problems in the multiterm TFDEs to our knowledge. Li and Yamamoto  studied an inverse problem of identifying the multiple fractional orders in the multiterm TFDE, and they gave the uniqueness result using Laplace transform and analytical method, and later they considered the similar model , and also the uniqueness of determining the fractional orders, the number of the fractional terms, and the spatially varying coefficient simultaneously is proved. Recently, Sun et al.  considered a simultaneous inversion problem for determining the space-dependent diffusion and source coefficients in the multiterm TFDE using the optimal perturbation regularization algorithm, and quite a few numerical inversions are presented.

Based on the above analysis, we are to deal with the inverse problem of determining the multiple fractional orders in the multiterm TFDE with the additional measurements at the interior point from numerics. The uniqueness results for such kind of inverse problems have been obtained (c.f. [39, 42], e.g.), but numerical inversions are still open to be implemented. Based on the difference solution to the forward problem, we perform numerical inversions by utilizing the homotopy regularization algorithm not only with the accurate data but also with random noisy data. The inversion fractional orders approximate to the exact orders as the noise level gets smaller demonstrating a numerical stability of the inverse problem here.

The rest of the paper is organized as follows. In Section 2, an implicit finite difference solution to the forward problem is given and the inverse problem of determining the fractional orders is formulated. In Section 3, the homotopy regularization algorithm is introduced to solve the inversion problem and numerical inversions are presented, and concluding remarks are given in Section 4.

#### 2. The Forward Problem and the Inverse Problem

Consider the forward problem given by (1) with the initial condition and the homogeneous Dirichlet boundary condition where the initial function is smooth enough and satisfies the consistency condition with the boundary condition. Let the diffusion coefficient be -class and take positive values on ; then the forward problem (1), (4)-(5) has a unique solution for suitable initial functions (c.f. , e.g.). Here we focus our attention on the finite difference solution to the forward problem. For completeness of the paper, we give an implicit finite difference scheme in 1D case for solving the forward problem. For further details, see [22, 23], and so on.

##### 2.1. The Difference Scheme to the Forward Problem

Let for . For given integer numbers and , discretizing the space domain by and the time domain by , we have by definition (3) for , respectively; here is the space mesh step and is the time mesh step.

Let and for . By discretizing the term using the ordinary integer-order difference method and denoting and , we getwhere is the truncated term. Denoting , dividing by on two sides of (7), and ignoring the truncated term, we get the following: where for . The initial boundary value conditions are discretized as Let and , where is defined by for .

Thus, we have the implicit finite difference scheme in the matrix form given as

Theorem 1. The implicit difference scheme (13) has only one solution, and it is of unconditional stability and convergence for any finite time .

Proof. By the assumptions for the diffusion coefficient , we have and for . So the coefficient matrix of (13) is strictly diagonally dominant; then the difference equation (13) has only one solution. Moreover, thanks to the equality and with a similar method as used in , we get the unconditional stability and convergence of the difference scheme for any given finite time .

##### 2.2. The Inverse Problem

For the forward problem (1), (4)-(5), if the fractional orders and () in (1) are unknown, we encounter the inverse problem of determining these multiple fractional orders. Suppose that there are some measured points in the space domain; for example, let be the measured point, and we have the additional information given as and the inverse problem is to determine and using the overposed condition (14) based on (1) and the initial boundary conditions (4) and (5).

As stated in Section 1, the general uniqueness results have been proved in [39, 42] by Dr. Li and Professor Yamamoto. We give the following lemma for the completeness of the paper.

Lemma 2 (see ). Suppose that the fractional orders and , the diffusion coefficient tensor , and the coefficients in (1) satisfy the conditions given in Section 1, and the initial function is smooth enough, and and for . Then all the fractional orders can be determined uniquely by the additional data for .

The uniqueness result is very important for inverse problems in theory. By Lemma 2 we need to utilize the additional data measured at for ; however, in concrete computations, we find that the numerical inversions can also be performed only employing a few of the additional data. So it is still meaningful to study inverse problems from numerics.

#### 3. The Inversion Algorithm and Numerical Inversions

In this section, we present numerical inversions for the inverse problem of (1), (4)-(5) with (14). The inversion algorithm we utilize is the homotopy regularization algorithm (see [43, 44], e.g.), which is a combination of the homotopy method with the optimal perturbation algorithm. We give a sketch for the inversion algorithm in the following.

##### 3.1. The Homotopy Regularization Algorithm

For the fractional orders and satisfying the order condition (2), let . We denote a vector and equip the Euclidean norm

For any given , denote as the unique solution to the forward problem. Combined with the additional information (14), solving the inverse problem is equivalent to a minimization problem where .

Following the homotopy regularization idea, it turns out that the following minimization problem is solved instead of (17): where is the homotopy parameter which takes values from near decreasingly approximating to . By linearization and numerical differentiation approximations, solving (18) is transformed to solve a normal equation combined with an iteration process via where is a perturbation vector for any given , denotes the iterative number, and is the initial iteration, and here is the numerical differential step and is the unit basis vector in , and

The algorithm can be terminated as long as an optimal perturbation satisfies the condition ; here eps is the given convergent precision. Like that done in [43, 44], we employed the homotopy parameter by where is the number of iterations, is a preestimated number, and is an adjusted parameter.

In the following, we will take two-term case () and three-term case () as example to perform the inversion algorithm in 1D case. We set the model parameters , , and and if there is no specification. In addition, we choose and in (22) to determine the homotopy parameter and utilize the grid steps and in the computation of the forward problem by the difference scheme (13).

##### 3.2. Inversion for

In the case of , let , and the fractional orders we have to determine are and , and is the exact solution of the fractional orders. By the exact fractional orders, we compute the forward problem to get the additional data at with which we reconstruct the fractional orders. It is noticeable that the dimension of the additional data is related to the discretization of the time domain; that is, there are for ; here is the time at which the measurement is made, and we have a -dimensional vector representing the additional data given as However, the inversion could be performed using a few of the additional data, and it is meaningful to investigate the influence of the number (dimension) of the additional data on the inversion algorithm.

###### 3.2.1. Inversion with Accurate Data

Taking two additional datasets at the time of and and choosing the initial iteration as , the inversion results are listed in Table 1, where is the inversion solution, denotes the solutions error, and is the number of iterations.

 Err (0.9, 0.1) (0.900000, 0.100000) 30 (0.8, 0.2) (0.800000, 0.200000) 30 (0.7, 0.3) (0.700000, 0.300000) 30 (0.6, 0.4) (0.600000, 0.400000) 32 (0.4, 0.3) (0.400000, 0.300000) 34 (0.3, 0.2) (0.300000, 0.200000) 34 (0.2, 0.1) (0.200000, 0.100000) 33

Without loss of generality, choosing the exact fractional orders as and , we implement the inversion algorithm using different number of the additional data. The inversion results are listed in Table 2, where denotes the number (dimension) of the additional data and denotes the measured time to get the additional data.

 2 (0.800000, 0.400000) 30 3 (0.800000, 0.400000) 28 4 (0.800000, 0.400000) 26 5 (0.800000, 0.400000) 25 6 (0.800000, 0.400000) 24 7 (0.800000, 0.400000) 23 8 (0.800000, 0.400000) 22 9 (0.800000, 0.400000) 22

From Table 1, it can be seen that the inversion can be realized only utilizing two additional datasets, and the inversion solutions are good approximations to the exact solutions. From Table 2, we can see that there are some influences for choosing the number of the additional data on the inversion algorithm, and the inversion results become a little better as the number of the additional data increases and the number of the iterations decreases. Moreover, if using much more additional data in the above, for example, taking all of the measured data given by (23), the inversion solution is still , and the solutions error is , but the number of iterations decreases to .

###### 3.2.2. Inversion with Noisy Data

It is difficult to perform an inversion algorithm in the case of using random noisy data, especially for inverse problems arising from the fractional diffusion. Noting computational errors and data noises, the additional information utilized for real inversions is often given as where is the noise level and is a random vector ranging within .

Also we take the exact fractional orders as and ; that is, the exact solution of the inverse problem here is given as . It is noticeable that the inversion with data noises could always fail if still using the above inversion parameters, and we perform the inversion using the completely additional data at for and choosing the initial iteration as nonzero vector of . The average inversion results with continuous ten-time inversions are listed in Table 3, where is the average inversion solution of the ten-time inversions and is the relative average error in the solutions.

 rr 5% (0.789840, 0.422128) 14.6 1% (0.799757, 0.401140) 14.3 0.1% (0.799990, 0.400094) 13.9 0.01% (0.799999, 0.400009) 15.0 0.001% (0.800000, 0.400001) 16.0

From Table 3, we find that the inversion is satisfactory in the case of using random noisy data, and the inversion errors become small when reducing the noise level.

##### 3.3. Inversion for

In the case of , the fractional orders we are to determine are and , and is the exact solution in this case. Let , and also choose as the measured point. We utilize nine additional datasets at the time of for and choose the initial iteration as here. The inversion results with accurate data are listed in Table 4.

 Err (0.9, 0.7, 0.5) (0.900000, 0.700000, 0.500000) 41 (0.8, 0.6, 0.4) (0.800000, 0.600000, 0.400000) 40 (0.7, 0.5, 0.3) (0.700000, 0.500000, 0.300000) 39 (0.6, 0.5, 0.4) (0.600000, 0.500000, 0.400000) 45 (0.5, 0.4, 0.3) (0.500000, 0.400000, 0.300000) 45 (0.4, 0.3, 0.2) (0.400000, 0.300000, 0.200000) 45 (0.3, 0.2, 0.1) (0.300000, 0.200000, 0.100000) 45

As done for , we can also realize the inversion in the case of using noisy data for although the ill-posedness of the inversion becomes more serious than that of . Taking as an example and using as the initial iteration, the average results also with continuous ten-time inversions are listed in Table 5, where , , and rr are all the same as those used in Table 3. It is important to note that we perform the inversion algorithm with convergent precision as for and and for and , respectively.

 rr 1% (0.853161, 0.762050, 0.411797) 0.1% (0.878925, 0.716188, 0.520835) 0.01% (0.900086, 0.699732, 0.500985) 0.001% (0.900007, 0.699989, 0.500042)

From Tables 3 and 5, we can see that the inversion solutions with random noisy data approximate to the exact solutions as the noise level gets smaller. Although the inversion results for with large noises are not so good as that for , they are still satisfactory and show a numerical stability for the inverse problem.

#### 4. Conclusions

The numerical determination problem for the fractional orders in the multiterm TFDE is investigated using some measurements at the interior point of the space domain. The inversion problem is unique, and numerical inversions with random noisy data are performed successfully by using the homotopy regularization algorithm. The homotopy regularization algorithm can also be utilized to determine the multiple fractional orders in the multidimensional case as long as a solution to the forward problem can be worked out.

It is noted that numerical inversions can be implemented smoothly in the case that the fractional orders satisfy the order condition (2) given in Section 1, which is just a necessary condition for the uniqueness of the inverse problem. The inversion results are very satisfactory if coping with accurate data; however, they become a little bad in the case of when using noisy data with noises greater than . Therefore, we can say that the stability of the inverse problem here with more fractional derivatives, that is, , could be severely ill-posed in spite of the fact that uniqueness is valid. We will deal with the inverse problem in the multidimensional case and we have to seek more effective inversion algorithms for the multiterm TFDE with in the future work.

#### Conflicts of Interest

The authors declare that there are no conflicts of interest regarding the publication of this paper.

#### Acknowledgments

This work is supported by the National Natural Science Foundation of China (nos. 11371231, 11071148).

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