Reconstruction of a source domain from the Cauchy data
Masaru Ikehata

TL;DR
This paper presents a method to reconstruct the shape of a polygonal source support in a Helmholtz equation from boundary Cauchy data, advancing inverse boundary value problem techniques.
Contribution
It introduces a way to compute the support function of polygonal sources using boundary data, providing a new approach for inverse source reconstruction.
Findings
Support function can be calculated from boundary Cauchy data for polygonal shapes.
Method applies to inverse boundary value problems involving Helmholtz equations.
Reconstruction is feasible for polygonal supports, aiding inverse problem solutions.
Abstract
We consider an inverse source problem for the Helmholtz equation in a bounded domain. The problem is to reconstruct the shape of the support of a source term from the Cauchy data on the boundary of the solution of the governing equation. We prove that if the shape is a polygon, one can calculate its support function from such data. An application to the inverse boundary value problem is also included.
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Reconstruction of a source domain from the Cauchy data
Masaru IKEHATA111 Department of Mathematics, Faculty of Engineering, Gunma University, Kiryu 376-8515, JAPAN
Abstract
We consider an inverse source problem for the Helmholtz equation in a bounded domain. The problem is to reconstruct the shape of the support of a source term from the Cauchy data on the boundary of the solution of the governing equation. We prove that if the shape is a polygon, one can calculate its support function from such data. An application to the inverse boundary value problem is also included.
1 Introduction
In this paper, we consider an inverse source problem, which is more general than traditional inverse potential problem described in [5], initiated by Novikov [7].
We consider the weak solution of the Helmholtz equation with a source term in a two-dimensional bounded domain with Lipschitz boundary:
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Here is a fixed non-negative number and known. We denote by the unit outward normal to . Throughout this paper we assume that
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Take such that in a neighbourhood of . Define
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This bounded linear functional on does not depend on the choice of such . Using it, we can define the Neumann derivative of on as an element of the dual space of by the formula
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where and is a lifting of in .
We call the Cauchy data of on . Roughly speaking, our problem is to extract some information about the support of from the Cauchy data of on . When and is a three-dimensional domain, this problem is related to the inverse source problem in geophysics since the restriction of the gravitational potential to satisfies the Poisson equation.
The purpose of this paper is to present a simple idea for the reconstruction of the support of the source in the two-dimensional case because of the simplicity of the situation. In a subsequent paper we will consider the three-dimensional case. We consider the special type of the source:
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or
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Here is a function defined on an open subset of and is a non-zero constant vector. We assume that , and are all unknown and Cauchy data , are known. We also assume that
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and for each vertex on there exist an open disk centred at with radius , and a function such that
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and
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Recall the support function for :
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Definition (regular direction). is regular with respect to if and only if the set
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consists of only one point.
The main result is as follows.
Theorem 1.1.* Assume that has the form (1.2) or (1.3). One can calculate for regular with respect to from the Cauchy data of on .*
The proof contains how to calculate for regular . See (2.12) of Proposition 2.3 in the next section. Furthermore, since is continuous with respect to and the set of directions which are not regular with respect to are at most a finite set, from the uniqueness of we automatically obtain two uniqueness theorems about the reconstruction of the convex hull of .
Corollary 1.* Assume that and are two pairs satisfying (1.4)-(1.8). Let have the form (1.2) for . Let be the weak solution of (1.1) for . Then*
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implies
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Corollary 2.* Assume that (D_{1},\rho_{1},\mbox{\boldmatha}_{1}) and (D_{2},\rho_{2},\mbox{\boldmatha}_{2}) are two pairs satisfying (1.4)-(1.8). Let have the form (1.3) for (D,\rho,\mbox{\boldmatha})=(D_{j},\rho_{j},\mbox{\boldmatha}_{j}). Let be the weak solution of (1.1) for . Then*
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implies
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Of course, as a direct consequence of Corollaries 1 and 2, we obtain two uniqueness theorems in the inverse potential problem and they seem to be new. See [5] for several uniqueness theorems.
Badia and Duong [1] considered a similar inverse source problem for the Poisson equation with a product source in a cylindrical geometry. Using the method of separation of variables, they find a reconstruction procedure for the shape of the support of the product source under additional information: the volume or one of the first-order moments of the bottom domain is known.
The method for the proof of Theorem 1.1 is similar to the idea discovered in [4] and does not require a cylindrical structure of the domain. Therein we considered two variants of the inverse conductivity problem proposed by Calderón [2]. The first is to reconstruct the surface of discontinuity of the coefficient of the equation in from the Dirichlet-to-Neumann map; the second is to reconstruct the shape of on which the Dirichlet data of the solution of the Helmholtz equation in vanish, from the Dirichlet-to-Neumann map. Note that is fixed. We found a new application of the so-called complex plane wave
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to these problems. Using it and an energy inequality, we reduced the problems to study the asymptotic behaviour of the integral
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as for each fixed . We succeeded in calculating the support function for the surface from the Dirichlet-to-Neumann map.
The argument in this paper, in contrast, is based on studying the asymptotic behaviour of the integral
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as for each fixed . Note that this integral is a kind of oscillatory integral and has a different character from (1.9).
Notice that Badia-Duong never made use of the complex plane wave. Instead, they used constant, first- and second-order harmonic polynomials and separated variable harmonic functions.
We think that there should be several applications of our method to the inverse source problems for other equations and maybe the inverse conductivity problem with a single set of Cauchy data (see [6] and the references therein). In fact, in the final section of this paper we present an example of one of the applications in such a direction.
2 Proof of Theorem 1.1
Proposition 2.1.* Let be the weak solution of (1.1) with . Then*
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This is justfrom the definition of the Neumann derivatives of and .
Now we substitute a special solution of in into (2.1):
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Here and are parameters and satisfy . Using indicated above, we have the following definition.
Definition (indicator function).
(i) Let be the weak solution of (1.1) with . Define
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(ii) Let be the weak solution of (1.1) with . Define
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These indicator functions satisfy the following.
Proposition 2.2.**
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Proof. Recall that for any
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if ;
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if F=\nabla\cdot\{\rho(x)\chi_{D}(x)\mbox{\boldmatha}\}.
A combination of these facts and (2.1) yields (2.2) and (2.3). Now (2.4) and (2.5) are trivial.
Lemma 2.1.* Assume that is regular with respect to and denote by the only one point on the set . Then there exists a non-zero complex number such that*
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as .
Proof. Take and such that (1.7) and (1.8) hold. Since is a vertex of and is regular, there exists and two linear functions and on such that
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Set
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Then
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We get
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Since there exists a constant such that, for any ,
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one gets
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This thus yields
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On the other hand, integration by parts yields
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We note that and since both and are linear functions. Thus
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Needless to say, we have the estimate for similar to (2.10). A combination of these estimates, (2.8) and (2.9) gives the desired conclusion. Notice that is given by the formula
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Theorem 1.1 is just a consequence of the following proposition.
Proposition 2.3 (reconstruction formula of ).* Assume that is regular for . Then for any *
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Proof. From (2.4) we have
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A combination of (2.5), (2.6) and (2.13) gives (2.12).
We point out a remarkable fact which is also derived from (2.13) and (2.6). Assume that , and that is . We denote by the surface measure on . Then
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Note that this is not a formal expression. Give an arbitrary . Then the Cauchy data of on the set
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decays exponentially as . This thus yields the following.
Proposition 2.4.* Assume that is regular for . Then holds if and only if*
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Proof. From (2.13) and (2.14) one gets
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Now from (2.6) we get the desired conclusions.
Proposition 2.4 means that to decide whether we need only the Cauchy data of on the set
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3 Remark
The key point for the proof of Theorem 1.1 is to prove the exact algebraic decay of
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as . When is smooth, it is not true. In this section, we describe an example for such a phenomenon. Let be the open disk with radius centred at . Then we have the following.
Proposition 3.1.* For any *
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where is the Bessel function of order zero.
Proof. This is nothing but a consequence of the mean value theorem for the Helmholtz equation (see, e.g, [3]) but for the reader’s convenience we present a direct proof. Change of variables yields
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and
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By elementary calculation, we know that the residue of
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at is
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Combining this with (3.2) to (3.4), we get (3.1).
Now assume that , and is small eneough. From (3.1) we conclude that decays exponentially as . More precisely,
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Note that . When is a general domain with smooth boundary, what can one extract from ?
4 Application to an inverse boundary value problem
We consider the strong solution of the equation
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Here , and we assume that satisfies (1.4), (1.5), (1.7) and (1.8) of Section 1 and that
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The problem is to reconstruct from the Cauchy data . It is closely related to the inverse scattering problem of a time-harmonic plane wave by an absorbing inhomogeneous medium. In this section we prove that one can reconstruct the convex hull of from such data.
More precisely, let be regular with respect to and denote by the only one point in the set . By the Sobolev imbedding theorem, one may assume that for any
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and thus one can consider the value of at . The result is as follows.
Theorem 4.1.* Assume that*
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Then one can calculate from the Cauchy data of on .
Also from the uniqueness of we automatically obtain the following.
Corollary 3.* Assume that and are two pairs satisfying (1.4), (1.5), (1.7) and (1.8). Let be the strong solution of (4.1) with . Assume that both and never vanish everywhere in . Then*
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implies
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The non-vanishing of everywhere in can be realized in several situations. For example, when one consideres the restriction to of the total field of the scattering solution by the incident plane wave , of the equation in , never vanishes for sufficiently small.
Proof of Theorem 4.1. Let be the strong solution of the Helmholtz equation in . Integration by parts yields
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Set . From (1.7), (1.8), (4.2) and (4.3) we know that satisfies (1.7) and (1.8). Now take
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and define
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On account of (4.3) a combination of (2.6) and (4.4) as in Proposition 2.3 gives
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and also
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if and only if .
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Acknowledgments
The author thanks the referees for several suggestions for the improvement of the manuscript.
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The reference list from the paper itself. Each links out to its DOI / PubMed record.
- 1[1] Badia, A. El. and Duong, T. Ha., Some remarks on the problem of source identification from boundary measurements, Inverse Problems, 14 (1998), 883-891.
- 2[2] Calderón, A. P., On an inverse boundary value problem, Seminar on Numerical Analysis and its Applications to Continum Physics, ed. W. H. Meyer and M. A. Raupp (Rio de Janeiro: Brzilian Mathematical Society), pp.65-73, 1980.
- 3[3] Courant, R. and Hilbert, D., Methoden der Mathematischen Physik, vol. 2., Berlin, Springer, 1937.
- 4[4] Ikehata, M., Reconstruction of the support function for inclusion from boundary measurements, J. Inverse Ill-Posed Problems, submitted .
- 5[5] Isakov, V., Inverse Source Problems, Mathematical Surveys and Monographs, vol. 2, Providence, RI: American Mathematical Society, 1990.
- 6[6] Kang, H. and Seo, J. K., The layer potential technique for the inverse conductivity problem, Inverse Problems, 12 (1996), 267-278.
- 7[7] Novikov, P., Sur le probleme inverse du potential, Dokl. Akad. Nauk, 18 (1938), 165-168.
