Abstract

Over the last two decades, anomalous diffusion processes in which the mean squares variance grows slower or faster than that in a Gaussian process have found many applications. At a macroscopic level, these processes are adequately described by fractional differential equations, which involves fractional derivatives in time or/and space. The fractional derivatives describe either history mechanism or long range interactions of particle motions at a microscopic level. The new physics can change dramatically the behavior of the forward problems. For example, the solution operator of the time fractional diffusion diffusion equation has only limited smoothing property, whereas the solution for the space fractional diffusion equation may contain weak singularity. Naturally one expects that the new physics will impact related inverse problems in terms of uniqueness, stability, and degree of ill-posedness. The last aspect is especially important from a practical point of view, i.e., stably reconstructing the quantities of interest. In this paper, we employ a formal analytic and numerical way, especially the two-parameter Mittag-Leffler function and singular value decomposition, to examine the degree of ill-posedness of several ‘classical’ inverse problems for fractional differential equations involving a Djrbashian–Caputo fractional derivative in either time or space, which represent the fractional analogues of that for classical integral order differential equations. We discuss four inverse problems, i.e., backward fractional diffusion, sideways problem, inverse source problem and inverse potential problem for time fractional diffusion, and inverse Sturm–Liouville problem, Cauchy problem, backward fractional diffusion and sideways problem for space fractional diffusion. It is found that contrary to the wide belief, the influence of anomalous diffusion on the degree of ill-posedness is not definitive: it can either significantly improve or worsen the conditioning of related inverse problems, depending crucially on the specific type of given data and quantity of interest. Further, the study exhibits distinct new features of ‘fractional’ inverse problems, and a partial list of surprising observations is given below. (a) Classical backward diffusion is exponentially ill-posed, whereas time fractional backward diffusion is only mildly ill-posed in the sense of norms on the domain and range spaces. However, this does not imply that the latter always allows a more effective reconstruction. (b) Theoretically, the time fractional sideways problem is severely ill-posed like its classical counterpart, but numerically can be nearly well-posed. (c) The classical Sturm–Liouville problem requires two pieces of spectral data to uniquely determine a general potential, but in the fractional case, one single Dirichlet spectrum may suffice. (d) The space fractional sideways problem can be far more or far less ill-posed than the classical counterpart, depending on the location of the lateral Cauchy data. In many cases, the precise mechanism of these surprising observations is unclear, and awaits further analytical and numerical exploration, which requires new mathematical tools and ingenuities. Further, our findings indicate fractional diffusion inverse problems also provide an excellent case study in the differences between theoretical ill-conditioning involving domain and range norms and the numerical analysis of a finite-dimensional reconstruction procedure. Throughout we will also describe known analytical and numerical results in the literature.

Highlights

  • Diffusion is one of the most prominent transport mechanisms found in nature

  • Over the last two decades a large body of literature has shown that anomalous diffusion models in which the mean square variance grows faster or slower than that in a Gaussian process under certain circumstances can offer a superior fit to experimental data

  • Anomalous diffusion processes arise in many disciplines, and the physics behind is very different from normal diffusion

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Summary

Introduction

Diffusion is one of the most prominent transport mechanisms found in nature. At a microscopic level, it is related to the random motion of individual particles, and the use of the Laplace operator and the first-order derivative in the canonical diffusion model rests on a Gaussian process assumption on the particle motion, after Albert Einsteins groundbreaking work [23]. There is a well known example of backward fractional diffusion, i.e., recovering the initial condition in a time fractional diffusion equation from the final time data, which is only mildly ill-posed, instead of severely ill-posed for the classical backward diffusion problem In some sense, this example has led to the belief that ‘fractionalizing’ inverse problems can always mitigate the degree of ill-posedness, and allows a better chance of an accurate numerical reconstruction. We revisit a number of ‘classical’ inverse problems for the FDEs, e.g., the backward diffusion problem, sideways diffusion problem and inverse source problem, and numerically exhibit their degree of ill-posedness These examples indicate that the answer to the aforementioned question is not definitive: it depends crucially on the type (unknown and data) of the inverse problem we look at, and the nonlocality of the problem (fractional derivative) can either greatly improve or worsen the degree of ill-posedness. Throughout the notation c, with or without a subscript, denote a generic constant, which may differ at different occurrences, but it is always independent of the unknown of interest

Mittag-Leffler function
Wright function
Inverse problems for time fractional diffusion
Backward fractional diffusion
Sideways fractional diffusion
Inverse source problem
Inverse potential problem
Fractional derivative as an inverse solution
Inverse problems for space fractional diffusion
Inverse Sturm–Liouville problem
Cauchy problem for fractional elliptic equation
Backward problem
Sideways problem
Concluding remarks
Computation of the Mittag-Leffler and Wright functions
Time fractional diffusion
Space fractional diffusion
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