Abstract
We consider the inverse problem of reconstructing the boundary curve of a cavity embedded in a bounded domain. The problem is formulated in two dimensions for the wave equation. We combine the Laguerre transform with the integral equation method and we reduce the inverse problem to a system of boundary integral equations. We propose an iterative scheme that linearizes the equation using the Fréchet derivative of the forward operator. The application of special quadrature rules results to an ill-conditioned linear system which we solve using Tikhonov regularization. The numerical results show that the proposed method produces accurate and stable reconstructions.
Keywords:
boundary reconstruction; Laguerre transform; modified single layer potential; non-linear boundary integral equation; quadrature rules; Tikhonov regularization MSC:
33C45; 35R30; 45E05; 47A52
1. Introduction
The inverse problem of reconstructing part of a boundary of an object from overdetermined measurements on the accessible part of the boundary has attracted a great deal of attention in different research areas because of its importance in various applications [1,2,3,4]. This problem is related to the solution of partial differential equations (PDEs) and, because of its non-linearity and ill-posedness, is rather complicated in both theoretical and numerical aspects.
Most numerical methods for such kind of problems provide iterative methods with regularization techniques. However, the use of integral equations for the numerical solution of the boundary reconstruction problem is still possible in various ways. One possibility is to reduce the inverse boundary value problem directly to a system of non-linear integral equations using the reciprocity gap method (see for example [5,6,7]). Another approach is to apply potential theory and reduce the inverse problem for the PDE to a system of non-linear integral equations, see [8,9,10] and references therein. Then, a Newton type iteration method with regularization is applied in both cases. Note that the integral equation technique can be also used as a numerical tool for the corresponding direct problems [11].
In the case of time-dependent inverse problems, there exist additional difficulties because of the presence of the independent time variable. For the heat equation, the time-boundary integral equations were used for the reconstruction of the interior curve of a planar doubly connected domain in [12] (see also [13,14]). Here, the inverse parabolic problem is interpreted as a non-linear operator equation. For its approximate solution, the regularized Newton method is used, which requires in every step the numerical solution of the direct problem. These well-posed time-dependent direct problems are reduced to integral equations using heat potentials.
In [15], the authors used a different integral based approach. Firstly, the Laguerre transform was applied for the semi-discretization in time of the inverse parabolic boundary problem. This resulted to a sequence of inverse boundary problems for an elliptic PDE. Then, a special potential representation of the solution led to a sequence of non-linear integral equations. In this paper, we extend this approach to an inverse boundary problem for a hyperbolic PDE.
Problem formulation The domain is doubly connected in with smooth boundary of class We assume that consists of two disjoint curves and , meaning with such that is contained in the interior of (see Figure 1).
Figure 1.
The domain geometry and the notation used throughout this paper.
We consider the following initial boundary value problem for the wave equation
subject to the homogeneous initial conditions
and the boundary conditions
Here, for , a represents the wave speed, denotes the outward unit normal vector to , and g is a given and sufficiently smooth function. We refer to [16] for the well-posedness of the direct problem to find the solution given the domain and the flux g.
In this work, we are interested in the numerical solution of the inverse problem to determine the interior boundary curve from the knowledge of the Cauchy data on the exterior boundary meaning given g and
We note here that the formulated inverse problem can be interpreted as an optimization problem and can be solved using shape optimization tools [17].
An outline of the paper is as follows: in Section 2, we describe the combination of the Fourier–Laguerre transform with the non-linear boundary integral equation method for the hyperbolic inverse boundary problem. We derive a sequence of systems of non-linear boundary integral equations, which are transformed into -periodic integral equations. Then, we present an iterative scheme to recover the unknown boundary shape.
In Section 3, we discuss the numerical implementation of the proposed scheme. Given an initial approximation of the unknown boundary curve, we solve the system of equations on the boundary using a quadrature method. The correction of the boundary of the cavity is the solution of the linearized integral equation on the exterior boundary, which we discretize with a trigonometrical collocation method. The Tikhonov regularization is applied to the derived system of linear equations.
Numerical results are presented in Section 4, confirming that the outlined approach is a feasible way of reconstructing the boundary shape of a cavity.
2. A Two-Step Approach for Dimension Reduction
We first describe the solution u of (1)–(4) using a scaled Fourier expansion with respect to the Laguerre polynomials. Then, we represent the solution of the stationary problem using a single-layer ansatz.
2.1. Semi-Discretization in Time
We consider the expansion
where
for using the Laguerre polynomials of order n.
It is easy to show (see for example [15,18]) that u (sufficiently smooth) is the solution of the time-dependent problem (1)–(4) if and only if its Fourier–Laguerre coefficients satisfy the following sequence of mixed problems
with boundary conditions
Here , and
In order to apply the non-linear integral equation method, we need the sequence of fundamental solutions of Equation (5).
Definition 1.
The sequence of functions , for is called the fundamental solution for the sequence of Equation (5) if it satisfies
We consider the modified Bessel functions
and the modified Hankel functions
of order zero and one, respectively. Here, we set and
and denotes the Euler constant [19]. We define the polynomials and by
with the convention The coefficients are given by the relations
for .
2.2. A Boundary Integral Equation Method
A modified single-layer approach is proposed to solve the sequence of stationary problems. We represent the solutions of the problem (5) and (6) in the doubly-connected domain using the following single layer potential form
with the unknown densities and , , defined on the boundary curves and , respectively, and is given by (10).
We let x tend to the boundary and, using the boundary conditions (6) and the standard jump relations, we obtain the following system of equations:
for the right-hand sides
This is a system of three equations for the three unknowns: the two densities and the boundary curve The integral operators are singular and linear on the densities but act non-linearly on the boundary curve. We consider the Fréchet derivative of the integral operators for linearizing them.
Before presenting the iterative method, we consider the parametrization of the system (12)–(14). We assume the following parametric representation of the boundary
and we define
The kernels are given by
for , and . The functions are defined in (10).
2.3. The Iterative Scheme
We solve the derived systems of equations iteratively by splitting them to their well- and ill-posed parts. Following [20], we first solve the well-posed subsystem to obtain the corresponding densities and then we linearize (with respect to the boundary) the ill-posed subsystem to be solved for the update of the radial function.
In the following, we assume for simplicity a star-like interior curve with parametrization
where is a periodic function representing the radial distance from the origin.
- Step 1.
- Step 2
- Keeping now the densities fixed, we linearize the ill-posed integral Equation (17) resulting towhere q is the radial function of the perturbed boundary. We solve the N equations for the radial function q of the perturbed and we update as
Equation (20) contains the Fréchet derivative of the integral operator with kernel with respect to This is a linear operator on q, and its form is obtained by the formal differentiation of the kernel with respect to We get
with kernel
where
for the polynomials
Note that the Fréchet derivative operator is injective at the exact solution [15].
3. Numerical Implementation
The numerical implementation of the iterative scheme has been well examined in [15] for a system similar to (15)–(17). Thus, in this section, we give just a brief description of it. We refer to (15) as the “field” equations and to (16) as the “data” equations.
With the given current approximation of the interior boundary , we consider the “field” Equation (15). Firstly, we handle the singularity of the parametrized kernels. More precisely, the kernel in (18) admits logarithmic singularity. After lengthy but straightforward calculations, we derive the following decomposition:
where
and
with diagonal terms
Furthermore, the kernels have logarithmic singularities
where
and
with diagonal terms
Here, we introduce the function
Clearly the kernels and are smooth for , .
Thus, we have to solve the sequence of systems of well-posed periodical integral Equation (15) with logarithmic singularities. We use for it the Nyström method with trigonometrical quadrature rules (see for details [15,21]).
For the “data” Equation (16), we apply the collocation method and, due to its ill-posedness, the received sequence of linear systems is solved by Tikhonov regularization.
4. Numerical Results
We approximate the function q by a trigonometric polynomial of the form
with
We substitute (23) in the linearized “data” equations and at the nodal points
we obtain a linear system of the form
for the unknown coefficients , where and describe the left- and right-hand side of the linearized “data” equations, respectively.
The above equation is ill-posed, and thus we apply Tikhonov regularization
The regularization parameter is chosen initially by trail and error and decreases at every iteration step as
This is a heuristic approach to compute but provides satisfactory reconstructions, as we can see later. There exist more sophisticated techniques, but this investigation is out of the scope of this work.
We simulate the Cauchy data by solving the sequence (5) with boundary conditions
for given boundary functions To avoid an inverse problem, we consider double the amount of nodal points for the direct problem, and afterwards we add noise to the Cauchy data on the boundary with respect to the norm. We use the boundary functions
We consider two examples with different boundary curves:
Example 1.
The interior boundary curve is a rounded rectangle with radial function
and is a circle with center and radius
Example 2.
Here, both boundary curves are apple-shaped with parametrizations
for the radial functions
In both examples, the initial guess is a circle with center and radius We set and we use Fourier coefficients and we solve at the nodal points with In the following figures, the brown solid line represents the boundary the green dotted line shows the initial guess, the red dashed line is the exact boundary and its reconstruction is the blue solid line.
In the first example, the initial radius is given by and we use In Figure 2, we see the reconstructions for exact (left) and noisy (right) data. The presented results are, with the initial regularization parameter after 21 and 12 iterations, respectively.
Figure 2.
Reconstructions of the boundary of the rounded rectangle for exact data (left) and data with noise (right).
For the second example, we set and We consider for the reconstructions presented in Figure 3. The algorithm terminated after 10 and 7 iterations, for the noise-free and noisy data, respectively.
Figure 3.
Reconstructions of theapple-shaped boundary for exact data (left) and data with noise (right).
We observe that we obtain accurate and relative stable reconstructions of the boundary curve. However, we have to stress that the results are sensitive with respect to the initial guess.
5. Conclusions
We extended the integral equation method to the inverse hyperbolic problem of the reconstruction of the interior boundary curve given the Cauchy data on the exterior boundary of a doubly connected planar domain. We applied the Laguerre transform in time, and we derived a sequence of stationary inverse boundary problems. These problems were reduced to a sequence of non-linear boundary integral equations by the application of modified single layer potentials. The Nyström method is used for the well-posed system of linear integral equations, and the collocation method together with Tikhonov regularization is applied to the the ill-posed sub-system. This technique can be extended to the case of three-dimensional domains for similar but more involved fundamental sequences.
Author Contributions
Formal analysis, R.C.; Investigation, R.C. and L.M.; Methodology, L.M.; Writing–original draft, R.C. and L.M. All authors have read and agreed to the published version of the manuscript.
Funding
L.M. was supported by the Austrian Science Fund (FWF) in the project F6801-N36 within the Special Research Programme SFB F68: “Tomography Across the Scales”.
Institutional Review Board Statement
Not applicable.
Informed Consent Statement
Not applicable.
Data Availability Statement
Not applicable.
Acknowledgments
L.M. acknowledges the support by the Austrian Science Fund (FWF) in the project F6801-N36 within the Special Research Programme SFB F68: “Tomography Across the Scales”. Open Access Funding by the Austrian Science Fund (FWF).
Conflicts of Interest
The authors declare no conflict of interest.
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