Direct and Inverse scattering in a three-dimensional planar waveguide
Abstract
In this paper, we study the direct and inverse scattering of the Schrödinger equation in a three-dimensional planar waveguide. For the direct problem, we derive a resonance-free region and resolvent estimates for the resolvent of the Schrödinger operator in such a geometry. Based on the analysis of the resolvent, several inverse problems are investigated. First, given the potential function, we prove the uniqueness of the inverse source problem with multi-frequency data. We also develop a Fourier-based method to reconstruct the source function. The capability of this method is numerically illustrated by examples. Second, the uniqueness and increased stability of an inverse potential problem from data generated by incident waves are achieved in the absence of the source function. To derive the stability estimate, we use an argument of quantitative analytic continuation in complex theory. Third, we prove the uniqueness of simultaneously determining the source and potential by active boundary data generated by incident waves. In these inverse problems, we only use the limited lateral Dirichlet boundary data at multiple wavenumbers within a finite interval.
Keywords: Schrödinger equation, waveguide, scattering resonances, inverse scattering, uniqueness, Fourier method
1 Introduction
We consider the direct and inverse scattering problems in a three-dimensional planar waveguide. Let be an infinite slab between two parallel hyperplanes and with width . Without loss of generality, we assume that
and
Consider the following Schrödinger equation
(1) |
where is the wavenumber, is the potential function, and is the source function. Let be a two-dimensional disk and be a cylinder in the waveguide. Denote the lateral boundary of by . Assume that both and are compactly supported in . We also assume that the potential function is invariant in the -variable, i.e., . Let satisfy the Neumann and Dirichlet boundary conditions, respectively,
(2) |
An important application of this waveguide problem is to provide a simplified but effective model for the propagation of time-harmonic acoustic waves in the ocean [1, 8]. In this model, the Dirichlet boundary condition models the surface of the ocean, while the Neumann boundary condition models the seabed underneath. In this paper, we begin by analyzing the direct scattering problem to seek a resonance-free region and derive the resolvent estimates for the resolvent of the Schrödinger operator in the waveguide. These studies enable us to gain some insights into the inverse problems. As an application of the resolvent estimates, we continue to study the inverse problems of determining the source and potential functions from the knowledge of the scattered field measured on corresponding to the wavenumber given in a finite interval. The framework developed in this paper is unified and can be applied to the configuration of a tubular waveguide.
The direct scattering problems in a planar waveguide corresponding to a positive wavenumber have been well studied in the literature. In this case, resonances may occur at a sequence of special frequencies, and this fact leads to the non-uniqueness of the direct problem [2]. However, the analysis of the scattering resonances for the resolvent in this geometry remains open. In scattering theory, the resonances are considered to be the poles of the meromorphic extension of the resolvent with respect to which could be a complex number. The phenomenon of scattering resonances naturally occurs and has significant applications in a wide range of scientific and engineering areas. For instance, the properties of scattering resonances can be applied to long-time asymptotics of the wave equation, which leads to resonance expansions of waves [11]. In this paper, we analyze the direct scattering and derive a resonance-free region and resolvent estimates for the resolvent of the Schrödinger operator in a three-dimensional planar waveguide.
The existing results on the inverse source problem in a waveguide are mainly focused on the delta-type/point-like sources and numerics [6, 7, 19, 20]. In [21], the author studied the inverse problem of qualitatively recovering the support of a source function by the multi-frequency far-field pattern with certain assumptions on the source function. To our knowledge, this article makes the novel attempt to establish the theoretical foundation and provide a feasible numerical scheme for quantitatively determining a general source function in the waveguide. We refer to [13, 18] and the references cited therein for the corresponding inverse boundary value problems, where the data is the Dirichlet-to-Neumann (DtN) map and the main mathematical tool is the construction of complex geometric optics (CGO) solutions. In this paper, since multi-wavenumber data is available, our treatment does not resort to the construction of CGO solutions.
The first part of this paper is concerned with the direct problem. In our setting, the direct problem is to investigate the resolvent where could be complex. Unfortunately, as discussed above, the scattering waveguides have a special feature that is not present in free space: there may exist a sequence of scattering resonances for which the uniqueness of solutions does not hold. Another special feature is that the scattered field consists of an infinite number of exponentially decaying evanescent modes. This will bring difficulty in the analytic continuation of the resolvent to the lower-half complex plane. To resolve this issue, we assume that the source function only admits a finite number of Fourier modes with respect to the variable. As a consequence, the scattered field also consists of a finite number of Fourier modes. We derive the desired resonance-free region and resolvent estimates by studying the analytic continuation of the complex wavenumber corresponding to each mode and applying the recent results on the resolvent of the Schrödinger operator in the free two-dimensional space in [27]. As a special case, we also consider the free resolvent . In this case, we show that a larger sectorial analytic domain can be obtained in the absence of the potential function.
The study of direct scattering problems paves the way for delving into the inverse problems. The second part of this paper is devoted to three prototypical inverse scattering problems: recovering respectively the source , the potential , and the co-recovery of both and . The aforementioned analysis of the resolvent is indispensable in establishing the stability of the inverse problems. For the inverse scattering problems by using multi-wavenumber data, a key question shall be usually answered: whether one can find a resonance-free region that contains an infinite interval of the positive real axis. If this is true, then one can apply the analytic continuation principle. Based upon the analysis of the resolvent, the stability and uniqueness issues of the three inverse problems are mathematically investigated. The analysis employs the limited lateral near-field Dirichlet data on at multiple frequencies.
For the first inverse problem of determining the source with known potential, we establish the theoretical results of uniqueness and stability. For such problems, the use of multi-wavenumber is usually necessary to overcome the non-uniqueness issue [4]. We construct an orthogonal basis in and deduce integral equations that connect the scattering data and the source function. As a consequence, we derive uniqueness for the inverse source problem. Similar techniques can be found in, e.g.,[3]. In particular, in the case , we develop a numerical scheme to reconstruct the source from the multi-frequency radiated field. The proposed approach can be viewed as a novel extension of the Fourier method for solving the multi-frequency inverse source problem of acoustic wave [28]. The Fourier method has been applied to the inverse source problems for electromagnetic wave [23, 24], elastic wave [22, 26], and recently the biharmonic wave [9]. Nevertheless, it is not trivial to design the Fourier method for recovering the source in the waveguide because different Fourier modes inherently intertwine with each other. To tackle this obstruction, we adopted the variable separation strategy to first represent the radiated field via a series expression, with the expansion coefficients corresponding to the Fourier modes. Then the Fourier method can be adopted to reconstruct the Fourier modes of the source function, and thus the series expansions can be used as the reconstruction. In addition, it deserves noting that, compared with the direct problem where we assume that the source function only admits a finite number of Fourier modes for the variable, the Fourier method developed here is feasible for recovering a more general source. Furthermore, we also discuss the extension of the inverse source problem with far-field data.
Next, we consider the inverse potential problem in the absence of the source function, we prove the uniqueness and increasing stability of the inverse potential problem by the scattered field generated by incident waves. The proof relies on the resolvent estimate and does not resort to the method of constructing CGO solutions as in [13, 18] since multi-wavenumber data is available. Based on the resonance-free region and resolvent estimates, the increased stability is obtained by applying an argument of analytic continuation developed in [27].
The last inverse problem is the more challenging co-inversion from the active boundary measurements generated by both the endogenous source and the exogenous excitation waves. We show that the unknown potential and source can be uniquely determined simultaneously. For the simultaneous determination of the source and potential of the random Schrödinger equation in free space, we refer the reader to [14, 15]. We also refer to [5] for the simultaneous recovery of a potential and a point source in the Schrödinger equation from Cauchy data. Note that a promising feature of the current study is that only limited-aperture Dirichlet boundary measurements at multiple wavenumbers are needed throughout the analysis.
The rest of the paper is organized as follows. Section 2 is concerned with the direct scattering problem. An analytic domain and resolvent estimates of the resolvent in the waveguide are derived. Sections 3 to 5 are dedicated to the inverse problems with the help of the analysis of the resolvent. First, we consider theoretical uniqueness and develop a numerical method for the inverse source problem in section 3. Then, in the absence of the source function, the inverse potential scattering problem is investigated in section 4. The third inverse problem of identifying the source-potential pair is tackled in section 4. Here we present a uniqueness result of simultaneously recovering the source and potential by active measurements. Finally, we conclude this article by summarizing the contributions and shedding light on future works in section 6.
2 Direct scattering
In this section, we investigate the resolvent in the planar waveguide. Consider the following Schrödinger equation
(3) |
Denote the resolvent by
which gives
We carry out the separation of variables in and for the scattered field and the source functions, which leads to series expansions as follows
(4) |
with and the modes of and of are given by
(5) |
The modes are required to satisfy the two-dimensional Helmholtz equation
(6) |
where
and the Sommerfeld radiation condition proposed in [12]
(7) |
Denote the resolvent of the Schrödinger operator in two dimensions by
Thus, we have a formal representation of the resolvent
(8) |
In what follows, we shall delineate the analyticity of and its resolvent estimates concerning complex .
2.1 Analytic continuation
In this subsection, we would resort to the analytic continuation technique to extend the domain of from to the complex plane such that is complex analytic. Let . We have
where
(9) |
Moreover, a direct calculation yields
where
Now we extend the real analytic functions and analytically from the first quadrant to by excluding the resonance , which will lead to the complex analyticity of . First, noting that and on , we apply the even extension to and the odd extension to with respect to the variable which gives the analytic extensions of and from the first quadrant to the right half plane as follows
and
Next, noting that and on the axis , we apply the odd extension to and the even extension to with respect to the variable by
and
In this way, we analytically extend and to the left half plane . Therefore, the real part and imaginary part are both extended as real analytic functions for . As a consequence of the above extension, we can show that is complex analytic for by the Cauchy-Riemann equations
Notice that based on the above analytic extension of , the imaginary part is negative in now. Therefore, for large the kernel of satisfies
(10) |
Throughout, denotes the Hankel function of the first kind of order . The asymptotic behavior (10) implies that the series in (8) may not converge. To resolve this issue and study the analytic continuation of the resolvent , we shall make the following assumption:
-
(A)
The source function has only a finite number of modes defined in (5), i.e., there exits a positive integer such that
2.2 Resolvent estimates
Based on the preparations in the previous subsection, we are now ready to establish several crucial estimates on the resolvent. We begin with a few notations. For , denote the sectorial domain by
Hereafter, we denote by and for . We also sometimes simplify the relation “” as “” with a nonessential constant that might differ at each occurrence.
The following proposition concerns the analytic continuation of the free resolvent in two dimensions.
Proposition 2.1.
[27, Theorem 3] Let with on . The resolvent is a meromorphic family of operators in . Moreover, is analytic for with the following resolvent estimates
where . Here is defined as
where is a positive constant and satisfies . In particular, there are only finitely many poles in the domain
We represent the solution to (6)–(7) by . Let and be positive constants such that , and denote the strip by . We next show that which is complex analytic for with appropriate choices of and . From the analytic extension discussed above, is complex analytic in . For being sufficiently small and being sufficiently large, we have in (9) and then for which yields . We can also have where is specified in Proposition 2.1. Moreover, the following estimate holds
As a consequence, the resolvent is analytic for with the following resolvent estimates given a fixed
Noting
we have the following theorem which provides a resonance-free region and resolvent estimates in the geometry of a planar waveguide. It will play an important role in the subsequent study of the inverse problem.
Theorem 2.1.
Let with on and let satisfy Assumption (A). There exist and such that the resolvent is an analytic family of operators for with the following resolvent estimates
where is a positive constant.
In what follows, we consider the case that . More precisely, we investigate the free resolvent . We will see that in this case, the free resolvent has a larger analytic domain.
The following proposition concerns the analytic continuation of the free resolvent in .
Proposition 2.2.
[27, Theorem 10]The free resolvent is analytic for as a family of operators
where . Moreover, for each the free resolvent extends to a family of analytic operators for as follows
with the resolvent estimates
where .
We denote the solution to (6)–(7) when by . We next prove that the resolvent is an analytic family of bounded operators for . To achieve this goal, it suffices to show that the range of is contained in some sectorial domain for . Indeed, from the analytic extension discussed above, is complex analytic in . As a result, we have that is analytic for since is analytic for .
Since , we have that there exists some such that . Thus, the ratio of and satisfies
where is a finite positive constant. This implies that the range of is contained in some sectorial domain . Therefore, we have that is analytic for . As a consequence, the resolvent is also analytic for with the following resolvent estimates given a fixed
Noting
we have the following theorem for the free resolvent.
Theorem 2.2.
Let and let satisfy Assumption (A). The resolvent is an analytic family of operators for with . Moreover, the following resolvent estimates hold
where is a positive constant.
3 Inverse problem I: source identification
In this section, we investigate the inverse source problem. The uniqueness of the inverse source problem is established given wavenumbers only in a bounded domain. We also develop a multi-wavenumber numerical scheme to reconstruct the source term from limited aperture Dirichlet boundary measurements. Then several numerical examples are provided to verify the effectiveness of the method. This section ends with an extensional glimpse into the uniqueness in the far-field case.
3.1 Uniqueness
In this subsection, we study the unique determination of the source from multi-wavenumber boundary measurements. We further assume that is a real-valued function.
We consider the spectrum of the Schrödinger operator with the Dirichlet boundary condition in . Specifically, we let be the positive increasing eigenvalues and eigenfunctions of in , where and satisfy
Let denote the eigenfrequencies. To properly formulate the inverse source problem, we additionally require that to avoid the resonances. In fact, due to the finiteness of the resonances , this requirement could be fulfilled in certain scenarios. For instance, a large width of the waveguide would narrow down the range of the resonance distribution, such that the resonances are confined in a small vicinity of zero, and thus we may have .
Assume that is normalized such that
Since forms an orthogonal basis of the space
the orthogonality leads to the spectral decomposition of :
Let be the radiating solution to (3) with wavenumber . Noting the boundary conditions (2), multiplying both sides of (3) by and integrating by parts over gives
(11) |
where
The following lemma [17, Lemma A.2] is useful in the subsequent analysis.
Lemma 3.1.
Let be the eigensystem of in . Then it holds
where the positive constant is independent of .
If given at all eigenfrequencies , we have the following Lipschitz stability estimate.
Theorem 3.1.
The following stability estimate holds:
Proof.
The above Lipschitz stability estimate implies the uniqueness of the inverse source problem, but it requires the boundary data at all . In practical applications, however, it is more reasonable to collect data only at wavenumbers in a finite interval. By analyticity of the data proved in Theorem 2.1, we establish the following uniqueness result for the inverse source problem with wavenumbers in a finite interval.
Theorem 3.2.
Let and be an open interval, where is the constant specified in Theorem 2.1 and is any positive constant. Then the source term can be uniquely determined by the multi-frequency data .
Proof.
Let for and . It suffices to show that . Since is analytic in for , it holds that for all . As the data is also available, we have that
for all and . It follows from (11) that
which implies . ∎
3.2 Reconstruction algorithm
This subsection deals with the numerical scheme for the null-potential inverse source problem, i.e., recover in the case . Now the radiated field satisfies the Helmholtz equation
(12) |
with Let be a finite number of frequencies, then the multi-frequency inverse source problem under consideration in this subsection is to reconstruct the source function in (12) from the measurement
In terms of the series expansions (4), it is readily seen that each Fourier mode satisfies the Sommerfeld radiated condition (7) and
(13) |
where is the Fourier mode of given by (5), and with . In addition, the assumption that , without loss of generality, implies that there exists such that
Though the modal wavenumber is determined by and , from another point of view, once and are given in advance, the wavenumber can be obtained correspondingly through . This further makes it possible to choose flexibly and it is unnecessary to relate the modal wavenumber with explicitly. In this view, (13) can be rewritten as
Once the mode is recovered, the source function is correspondingly determined uniquely through (4). Thus, in the rest of this subsection, we aim to recover for from with being the set of admissible modal wavenumbers, which is defined by
Definition 3.1 (Admissible modal wavenumbers).
Let and be a small modal wavenumber such that Then the admissible set of modal wavenumbers is given by
The basic idea is to approximate by the following Fourier expansion
(14) |
where and are the Fourier basis functions. In eq. 14, are the Fourier coefficients corresponding to the index and the -th Fourier mode ,
Let be the unit outward normal to Define
(15) | ||||
(16) |
where and
3.3 Numerical verification
We shall conduct several numerical experiments to verify the performance of the Fourier method proposed for the inverse source problem arising in the waveguide. The synthetic radiated fields were generated by solving the forward problem via direct integration. Utilizing the Green’s function
(20) |
the radiating solution to the Helmholtz equation (12) is given by
where . The Gauss quadrature is adopted to calculate the volume integrals over the Gauss-Legendre points. Then the synthetic data is corrupted by artificial noise via where and are two uniformly distributed random numbers ranging from to 1, is the noise level.
Now, we specify the details of the implementational aspects of the Fourier method. Let We aim to reconstruct the true source by the Fourier expansion Throughout our numerical experiment, the Green’s function (20) is numerically truncated by Further, given the modal wavenumbers are set to be
The radiated data
are measured on with . For a visualization of the measurement surface, we refer to Figure 2 where the red points denote the receivers.

Once the radiated field is measured, the corresponding modes of the radiated data can be written as
Next, in terms of (15)–(16) with and truncation , we compute the following artificial Cauchy data of the Fourier modes
To calculate the Fourier coefficients and in (17) and (18), respectively, we use the trapezoidal rule to evaluate the surface integrals over and the volume integral over is evaluated over a grid of uniformly spaced points Finally, we compute the point-wise values by (19) with determined by (14).


Example 1.
In the first example, we test the performance of the method by considering the reconstruction of the source function which has finite Fourier modes. Specifically, the source function is given by
with
In this example, we set and . The -th Fourier mode of the exact source function is independent of and . We refer to Figure 3 for a display of . Theoretically, once a Fourier mode is recovered, the source function can be approximated by multiplying the factor . Nevertheless, we have yet to determine the precise expression of the exact source. Thus, for each we reconstruct the Fourier modes and exhibit the reconstruction of several different Fourier modes in Figure 4. The results in Figure 3 and Figure 4 demonstrate that all the Fourier modes are well recovered, and the reconstruction error is around .






Next, we reconstruct the source at different slices: , and . The reconstructions are depicted in Figure 5, which illustrate that the profile of the source function can be well captured at these locations.
This example shows that when the exact source has limited Fourier modes, these Fourier modes can be well-reconstructed. Furthermore, the source can also be recovered satisfactorily under the Fourier expansion. However, most of the source functions may not have limited Fourier expansions. So we shall reconstruct a more general source function in the next example.






Example 2.
The second example is devoted to reconstructing a mountain-shaped function described by
Different from which has limited Fourier expansion with the same Fourier mode, the source function is more general. Here the truncation is set to be with denoting the largest integer that is smaller than . In this way, the influence of the magnitude of noise is investigated in this example. For a quantitative evaluation of the inversion scheme, we compute the relative errors
First, is used and we compare and at in Figure 6. One can see from the results that the source function is well-reconstructed. For an in-depth slice view, we plot several cross-sections of them in Figure 7. We can see from Figure 7 that the reconstruction matches almost perfectly with the exact source at these typical cross sections. Especially, even if the source value is close to the reconstruction is still satisfactory (see Figure 7(b) for example).








Further, we compute the recovery errors at different locations subject to different noise levels Table 1 shows that the reconstructions are reasonably stable in the sense that the quality of the inversion improves as the noise level decreases.
3.4 The far-field case
In this last subsection, we briefly discuss the inverse source problem using the far-field data. We assume in this case. Under Assumption (A) the outgoing solution to (3) can be represented by
From the asymptotic expansion of the fundamental solution of the two-dimensional Helmholtz equation [10] as , we have
where is the observation angle. Since is exponentially decaying for those such that , we define the far-field pattern as follows
(21) |
Let be an interval such that and let be fixed such that . As can be seen in (3.4), if the multi-wavenumber far-field data is given, then
This implies that the far field of only one propagating mode corresponding to is detected which gives the following Fourier transform
Thus, by the analyticity of and the inverse Fourier transform we can determine and even derive a stability estimate by analytic continuation. Moreover, let , if is recovered and is available, in a similar manner we can determine by detecting the far-field of the corresponding single mode. Proceeding recursively in this way, we get the following uniqueness result.
Theorem 3.3.
Let be chosen such that for . The far-field uniquely determines .
Remark 3.2.
Compared with Theorem 3.2, Theorem 3.3 requires data measured at more wavenumbers. Physically speaking, a possible reason accounting for the necessity of this extra data is that part of the information is only involved in the evanescent modes which decay drastically. Hence, this information cannot be accessed or retrieved from the far-field data. Thus, more far-field data is inevitably needed to compensate for the lack of information towards establishing the uniqueness.
Remark 3.3.
We would like to highlight that the uniqueness of the inverse source problem is established by incorporating the far-field due to a single mode one by one from low to high wavenumbers. This framework of derivation has the advantage of avoiding the situation where multiple propagating modes are concurrently present. Conversely, for instance, if we only collect the data , then we are only able to find the superposed quantity . In this case, it would be difficult to separate and recover either or from the sum.
4 Inverse problem II: determining the potential
In this section, an inverse potential problem in the waveguide is considered. We assume that is real-valued and in this section. The key ingredient in the analysis is applying results in Theorem 2.1 and an argument of analytic continuation.
Let and be respectively the wavenumber and incident direction, and denote the incident field. Then the total field is given by where is the scattered field produced by and the potential . Consider the following homogeneous Schrödinger equation with satisfying the boundary conditions (2)
(22) |
We are interested in the inverse problem of determining from on . Here we employ to signify the dependence of on and .
Under the above configuration, the scattered field satisfies
(23) |
and the boundary conditions (2). Multiplying both sides of (23) by the factor with and integrating by parts over , we obtain
(24) |
where is the first Fourier mode of . As the inhomogeneous term on the right-hand side of the equation (23) has a single Fourier mode in the variable, in the last equality, we can use the resolvent estimate in Theorem 2.1 to derive
Notice that We next show that the boundary measurements uniquely determine . Here with where is specified in Theorem 2.1.
Let and be two potential functions. Assume that and are solutions to (22) corresponding to and , respectively. Denote and . Substituting and in (24) by and , respectively, and taking subtraction yields
Now it suffices to show if for all and . As is analytic for , we immediately have for all . Moreover, from the Dirichlet-to-Neumann map the normal derivative can be computed from
where are the Fourier coefficients
Thus, gives . Consequently, from (24) we have
(25) |
As on holds for all , by letting in (25) we arrive at
which yields by the inverse Fourier transform. This implies the uniqueness of the inverse problem. In summary, we have the following theorem.
Theorem 4.1.
The multi-frequency measurement uniquely determines .
Now we discuss the stability. Assume that and are the scattered field corresponding to the incident wave and potentials and , respectively. Let be an arbitrary positive constant. Define a real-valued function space
Utilizing the resolvent estimates and the estimate (24), we have the following stability estimate (the proof follows [27] in a straightforward way by applying the quantitative analytic continuation. Thus we omit it for brevity).
Theorem 4.2.
Let . The following increasing stability estimate holds
(26) |
where
and with , and .
The stability estimate (26) implies the uniqueness. It consists of two parts: the data discrepancy and the high-frequency tail. The former is of the Lipschitz type. The latter decreases as increases which makes the problem have an almost Lipschitz stability. Overall, the result reveals that the problem becomes more stable when higher-frequency data is used.
5 Inverse problem III: simultaneous recovery of source and potential
This section is devoted to the co-inversion model of simultaneously reconstructing the source and potential from active measurements. In this model, given the incident wave with incident direction , the total field satisfies the wave equation eq. 1 and the boundary conditions (2). We also assume that is real-valued and in this section.
We are interested in the inverse problem of determining both and from . To that end, we apply the method developed in [25] to the current geometry of a waveguide. We first present a preliminary result for the subsequent analysis.
Lemma 5.1.
Let and with and . Then the following estimate holds:
where is a generic constant depending on .
Proof.
Since , without loss of generality we assume that the . Using integration by parts yields
which gives by Hölder’s inequality
The proof is completed. ∎
In the case of the equation (1) with an inhomogeneous term , by multiplying both sides of (23) by with and integrating by parts over , (24) now becomes
(27) |
By applying Lemma 5.1 we have
and then (5) becomes
(28) |
As (5) is similar to (24), repeating the previous arguments we have that the active boundary data corresponding to the incident wave and source uniquely determine . Once is known, we can also recover . In summary, we have the following uniqueness result:
Theorem 5.1.
The active multi-wavenumber boundary measurements
corresponding to the incident wave uniquely determine with unknown . As a consequence of the recovery of , the source can be uniquely determined as well by the passive boundary measurements
6 Conclusion
This work presents a resonance-free region and resolvent estimates for the resolvent of the Schrödinger operator in a planar waveguide in three dimensions. As an application, theoretical uniqueness and stability for several inverse scattering problems are established. The analysis only requires the limited aperture Dirichlet data at multiple wavenumbers. Moreover, we develop an effective Fourier-based reconstruction method for the inverse source problem. We believe that the method can be applied to the biharmonic wave equation in a planar waveguide with Navier boundary conditions and the geometry of tubular waveguides. A more challenging analytic problem is the direct and inverse elastic scattering in a waveguide. In this case, we may not have a straightforward Fourier decomposition such as (6) due to the coupled pressure and shear waves. We hope to report the relevant progress elsewhere in the future.
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