Increasing stability of the inverse source problem for one dimensional domain
Shahah Almutairi, Ajith Gunaratne

TL;DR
This paper demonstrates that using multi-frequency waves at the endpoints of a one-dimensional domain enhances the stability of the inverse source problem for the Helmholtz equation, balancing data discrepancy and high-frequency effects.
Contribution
The paper introduces a stability estimate for the inverse source problem that incorporates multi-frequency data at domain endpoints, improving stability analysis.
Findings
Stability improves with multi-frequency data at endpoints.
The stability estimate accounts for data discrepancy and high-frequency tail.
Multi-frequency approach enhances inverse problem robustness.
Abstract
Here we are investigating the one dimensional inverse source problem for Helmholtz equation where the source function is compactly supported in our domain. We show that increasing stability possible using multi-frequency wave at the two end points. Our main result is a stability estimate consists of two parts: the data discrepancy and the high frequency tail.
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Taxonomy
TopicsNumerical methods in inverse problems · Microwave Imaging and Scattering Analysis · Ultrasonics and Acoustic Wave Propagation
Increasing stability of inverse source problem for one dimensional domain
Shahah Almutairia Ajith Gunaratne b
(March 2019)
Abstract.
Here we are investigating the one dimensional inverse source problem for Helmholtz equation where the source function is compactly supported in our domain. We show that increasing stability possible using multi-frequency wave at the two end points. Our main result is a stability estimate consists of two parts: the data discrepancy and the high frequency tail.
Keywords: Inverse source problems, scattering theory, Helmholtz equation
Mathematics Subject Classification: 35R30; 78A46
1 Introduction and statement of problem
We consider the one dimensional Helmholtz equation in a one layered medium:
[TABLE]
where the wave field is required to satisfy the outgoing wave conditions:
[TABLE]
Given , it is well-known that the problem (1)-(2) has a unique solution:
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where is the Green function given as follows
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This work concerns the inverse source problem when the source function is a complex function with a compact support contained in . here our goal is to recover the source function using the boundary data and with where is a positive constant.
Inverse source problem arises in many area of science. It has numerous applications in acoustical and biomedical/medical imaging, antenna synthesis, geophysics, and material science ([2, 3]). It has been known that the data of the inverse source problems for Helmholtz equations with single frequency can not guarantee the uniqueness ([13], Ch.4). On the other hand, various studies, for instance in [4], showed that the uniqueness can be regained by taking multifrequency boundary measurement in a non-empty frequency interval noticing the analyticity of wave-field on the frequency [13, 17]. On the other hand, various studies, for instance in [12], showed that the uniqueness can be regained by taking multi-frequency boundary measurement in a non-empty frequency interval (0,K) noticing the analyticity of wave-field on the frequency. Because of the wide applications, these problems have being attracted considerable attention. These kinds of problems have been extensively investigated by many researchers (see, for example, [1, 5, 6, 7, 8, 9, 10, 14, 15, 16, 18, 19, 20]). We also note that these type of problem and technique can apply to systems. For example, in [11], inverse source problems was considered for classical elasticity system. In this paper, we intended to prove
Theorem 1.1**.**
There exists a generic constant depending on the domain such that
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for all solving (1) with . Here
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* and M=\max\big{\{}\parallel f\parallel_{(1)}^{2}(-1,1),1\big{\}} where is the standard Sobolev norm in .*
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**Remark 1.1: ** The estimate in (5) consists of two parts: the data discrepancy and the high frequency part. The first part is of the LIpschitz type. The second part is of logarithmic type. The second part decrease as increases which makes the problem more stable. The estimate (5) also implies the uniqueness of the inverse source problem.
2 Proof of Theorem 1.1
2.1 Increasing Stability of Continuation to higher frequencies
Let
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where
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using (3) and a simple calculation shows that
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where . Functions and are both analytic with respect to the wave number and play important roles in relating the inverse source problems of the Helmholtz equation and the Cauchy problems for the wave equations.
Lemma 2.1**.**
Let and . Then
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[TABLE]
Proof.
Since we have is complex analytic on the set , where is the sector arg with . Since the integrands in (6) are analytic functions of in , their integrals with respect to can be taken over any path in joining points [math] and in the complex plane. Using the change of variable , in the line integral (3), the fact that .
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and
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Noting
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using the Schwartz inequality and integrating with respect to , using the bound for in , we complete the proof of (8). Using the same technique, we can prove the (9).
∎
Noticing that functions are analytic functions of and . The following steps are essential to link the unknown and for to the known value in (1). Obviously
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where M=\max\big{\{}\parallel f\parallel_{(0)}^{2}(-1,1),1\big{\}}. With the similar argument bound (12) is true for . Observing that
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Let be the harmonic measure of the interval in then as known (for example see [13], p.67), from two previous inequalities and analyticity of the function and we conclude that
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when . Similarly it also yields for
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consequently
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To achieve a lower bound of the harmonic measure , we use the following technical lemma. The proof can be found in [7].
Lemma 2.2**.**
Let be the harmonic measure of the interval in , then
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Lemma 2.3**.**
Let source function with , then
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Proof.
Using the result of [19] by applying the Green function (4) and letting . ∎
Lemma 2.4**.**
Let source function , then
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[TABLE]
Proof.
It follows from (7) and . ∎
2.2 Increasing stability for inverse source problem
To continue the estimate for reminders in (10) and (11) for , we need the following lemma.
Lemma 2.5**.**
Let be a solution to the forward problem (1) with with , then
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Proof.
Using (7), we obtain
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[TABLE]
Using integration by parts and the fact that and , we have
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and
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consequently for the first and second terms in (19) we obtain
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[TABLE]
utilizing the same argument for the second term in (19) and integrating with respect to the proof is complete. ∎
Now, we are ready to proof Theorem 1.1.
Proof.
We can assume that and , otherwise the bound (1.1) is obvious. Let
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if , then , using the (13) and (15), we can conclude
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If , we can assume that , otherwise and hence and the bound (5) is straightforward. From (20), Lemma 2.2, (13) and the equality we obtain
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[TABLE]
using the trivial inequality for and our assumption at the beginning of the proof, we obtain
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Due to the (10), (21), (22), and Lemma 2.5. we can conclude
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[TABLE]
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Using the inequalities in (23) and Lemma 2.3., we finally obtain
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Due to the fact that for , the proof is complete.
∎
3 Concluding Remarks
In this paper, we studied the inverse source problem with many frequencies in a one dimensional domain. The result showed that if grows the estimate improves. It also showed that if we have date exists for all wave number , the estimate will be a Lipschitz estimate.
Acknowledgment: We wish to thank Dr. M.N. Entekhabi for her support and encouragement.
The reference list from the paper itself. Each links out to its DOI / PubMed record.
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- 2[2] Ammari H, Bao G and Fleming J 2002 Inverse source problem for Maxwell’s equation in magnetoencephalography SIAM J. Appl. Math. 62 1369-82
- 3[3] Balanis C 2005 Antenna Theory - Analysis and Design (Wiley, Hoboken, NJ)
- 4[4] Bao G, Lin J, Triki F 2010 A multi- frequency inverse source problem J. Differential Equations 249 3443-3465.
- 5[5] Bao G, Lin J, Triki F 2011 An inverse source problem with multiple frequency data Comptes Rendus Mathematique 349 855-859.
- 6[6] Bao G, Lu S, Rundell W, and Xu B 2015 A recursive algorithm for multifrequency acoustic inverse source problems SIAM Journal on Numerical Analysis 53 (3), 1608-1628
- 7[7] Cheng J, Isakov V and Lu S 2016 Increasing stability in the inverse source problem with many frequencies, J. Differential Equations 260 4786-4804
- 8[8] Entekhabi M N, 2018 Increasing stability in the two dimensional inverse source scattering problem with attenuation and many frequencies Inverse Problems 34 115001
