H\"older Stable Recovery of Time-Dependent Electromagnetic Potentials Appearing in a Dynamical Anisotropic Schr\"odinger Equation
Yavar Kian, Alexander Tetlow

TL;DR
This paper establishes a H"older stability result for recovering time- and space-dependent electromagnetic potentials in a Schr"odinger equation on a Riemannian manifold, removing previous smallness constraints.
Contribution
It proves H"older stability for the inverse problem of determining electromagnetic potentials, extending prior work by removing the smallness assumption on the magnetic potential.
Findings
H"older stability of potential recovery from Dirichlet-to-Neumann data
Recovery of electric and magnetic potentials without smallness constraints
Extension to general Riemannian manifolds with boundary
Abstract
We consider the inverse problem of H\"oldder-stably determining the time- and space-dependent coefficients of the Schr\"odinger equation on a simple Riemannian manifold with boundary of dimension from knowledge of the Dirichlet-to-Neumann map. Assuming the divergence of the magnetic potential is known, we show that the electric and magnetic potentials can be H\"older-stably recovered from these data. Here we also remove the smallness assumption for the solenoidal part of the magnetic potential present in previous results.
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Hölder Stable Recovery of Time-Dependent Electromagnetic Potentials Appearing in a Dynamical Anisotropic Schrödinger Equation
Yavar Kian
and
Alexander Tetlow
(Date: Compiled )
Abstract.
We consider the inverse problem of Höldder-stably determining the time- and space-dependent coefficients of the Schrödinger equation on a simple Riemannian manifold with boundary of dimension from knowledge of the Dirichlet-to-Neumann map. Assuming the divergence of the magnetic potential is known, we show that the electric and magnetic potentials can be Hölder-stably recovered from these data. Here we also remove the smallness assumption for the solenoidal part of the magnetic potential present in previous results.
1. Introduction
1.1. Statement of the Problem
Let , let be a compact, connected, smooth Riemannian manifold of dimension , and denote by its boundary. Further assume that is simple (see definition 1). Let be given by , and consider the magnetic Laplacian given by
[TABLE]
where and . If , this is just the usual Laplace-Beltrami operator . For and we consider the initial boundary value problem (IBVP)
[TABLE]
with inhomogeneous Dirichlet data . For all and or define the spaces with the associated norm
[TABLE]
We further define the space
[TABLE]
The problem (1.1) admits a unique solution for (see [10, Proposition 2.1]). Further, the Dirichlet-to-Neumann (D-to-N map in short) map
[TABLE]
where denotes the unit outward normal to with respect to the metric , is a bounded operator from to . For , let , and . We call and gauge equivalent if there exists such that , and and let be the solution of (1.1) with potentials and . If is as above, we recall that the D-to-N map is invariant under this gauge transformation. More precisely, we have
[TABLE]
and we deduce that and
[TABLE]
which then implies that . This obstruction to uniqueness notwithstanding, the aim of this paper is to prove Hölder-stable recovery of the time-dependent electric and magnetic potentials from knowledge of the D-to-N map .
1.2. History of the Problem
In the case of the dynamic Schrödinger equation with time-independent potentials, Hölder-stable recovery of the magnetic field from knowledge of the Dirichlet-to-Neumann map was shown in [3], and stable recovery of the electric potential of the Schrödinger equation on a Riemannian manifold was proved in [4]. This latter result is extended to stable determination of the electromagnetic potentials on a Riemannian manifold from the D-to-N map in [2]. We mention also the recent work of [5], where such results have been extended to unbounded cylindrical domain.
Literature dealing with the inverse problem of recovering time-dependent potentials of the Schrödinger equation is rather sparse. To the best of the authors’ knowledge, the only results establishing recovery of time-dependent potentials of the Schrödinger equation from the D-to-N map deal with Euclidean domains. In particular, it was proved in [8] that the time-dependent electric and magnetic potentials are uniquely determined by the D-to-N map. Logarithmic-stable determination was shown for the electric potential in [7]. This result was extended to the full electromagnetic potential in [6], provided that the time-independent part of the magnetic potential is sufficiently small. Indeed, it was only recently shown in [10] that the electromagnetic potential in a Euclidean domain can be Hölder-stably recovered from knowledge of the D-to-N map.
In the current work, we show that it is possible to Hölder-stably recover the time-and-space-dependent coefficients of the dynamic Schrödinger equation on a simple Riemannian manifold.
1.3. Main Results
Here and in the rest of this paper we write for the norm of an operator in \mathcal{B}\big{(}H^{\frac{9}{4},\frac{3}{2}}_{0}((0,T)\times\partial\mathcal{M}),L^{2}((0,T)\times\partial\mathcal{M})\big{)}. In this paper we aim to prove the following:
Theorem 1**.**
(Uniqueness):For , let and . Assume also that
[TABLE]
Then the condition implies that and are gauge equivalent.
Theorem 2**.**
(Stable Recovery of the Magnetic Potential): Let the condition of Theorem 1 be fulfilled and, for , let be such that
[TABLE]
Assume also that there exists a constant such that
[TABLE]
Then we have
[TABLE]
where is a general constant, a constant depending only on , , and is the solenoidal part of the Hodge decomposition of , given in Lemma 1.
Theorem 3**.**
(Stable Recovery of the Electric Potential): Let the condition of Theorem 2 be fulfilled with
[TABLE]
Fix also and assume that the condition
[TABLE]
is fulfilled. We also assume that there exists a constant such that
[TABLE]
Then we have
[TABLE]
where depends only on , , and , and is a general constant.
As far as the authors are aware, the present work is the first dealing with recovery of time-dependent potentials appearing in a Schrödinger equation with variable coefficients of order two. In fact, the above estimates are the first showing Hölder-stable recovery of a coefficient dependent on all variables of a second order partial differential equation with variable coefficients of order two. The only other work where similar results have been obtained is [10], where the authors consider the case of a bounded subset of with the Euclidean metric.
Furthermore, stable recovery of a magnetic potential appearing in a Schrödinger equation on a manifold with non-Euclidean metric has, thus far, relied upon the a priori assumption that the magnetic potential is small in some appropriate norm, even in the time-independent case (see, for example, [2]). This smallness assumption is also utilized when recovering the magnetic potential of the wave equation (as seen in [12]). In fact, it happens that this assumption is not necessary when dealing with the Schrödinger equation, even when the magnetic potential is allowed to depend on time, as we shall demonstrate herein.
In Section 2, we introduce the geodesic ray-transforms for -forms and for functions. In Section 3 we construct geometric optics solutions to the equation (1.1). We devote Section 4 to the proof of Theorem 1, using the geometric optics solutions as the main tool. The estimate of Theorem 2 is proved in Section 5, whereas the estimate of Theorem 3 is proved in Section 6.
2. Notations
In this section, we list some notation used in the rest of the paper. We denote by the inner product with respect to on , that is for and given by , we have
[TABLE]
Similarly, we denote by the inner product with respect to on , that is for given by , we have
[TABLE]
We denote by the Riemannian volume on , which is given in local coordinates by . We further define on the surface measure such that for we have
[TABLE]
where \textrm{div}_{g}(X)=\sum_{j=1}^{n}\left\lvert g\right\rvert^{-\frac{1}{2}}\partial_{x_{j}}\big{(}\left\lvert g\right\rvert^{\frac{1}{2}}X^{j}\big{)}. Additionally, we recall the Riemannian gradient operator given by \nabla_{g}f=\big{(}g^{j1}\partial_{x_{j}}f,\cdots,g^{jn}\partial_{x_{j}}f\big{)}.
We recall the coderivative operator is the operator sending the 1-form to the function given in local coordinates by
[TABLE]
We recall also the definition of a simple manifold. Let be the Levi-Civita connection on . For we consider the second quadratic form of the boundary
[TABLE]
We say that is strictly convex if the form is positive-definite for every .
Definition 1**.**
We say that is simple if is strictly convex, is simply connected, and for any the exponential map is a diffeomorphism.
We write for the unique geodesic in with initial point and initial direction . We define the sphere bundle of by
[TABLE]
and likewise the submanifold of inner vectors by
[TABLE]
Given that is assumed to be simple, we can also define to be the maximal time of existence in of the geodesic for , that is
[TABLE]
We also introduce here the geodesic ray transforms on a simple Riemannian manifold .
Definition 2**.**
The geodesic ray transform for -forms is the linear operator which is defined by
[TABLE]
Definition 3**.**
The geodesic ray transform for functions is the linear operator which is given by
[TABLE]
3. Geometric Optics Solutions
We now seek to construct GO solutions of the magnetic Schrödinger equation in . We fix , and assume that
[TABLE]
We consider the equations
[TABLE]
We seek to find, for , , solutions of (3.2) of the form
[TABLE]
In (3.3) above, satisfy the following eikonal and transport equations:
[TABLE]
[TABLE]
[TABLE]
Taken together, equations (3.4) - (3.6) yield
[TABLE]
We also assume that there exists \tau\in\big{(}0,\frac{T}{4}) such that are supported in and further assume that , whence . Thus we can choose solving
[TABLE]
Since is simple, the eikonal equation (3.4) can be solved globally on . To see this, we first extend the simple manifold to a simple, compact manifold with contained in the interior of . We pick and consider polar normal coordinates on given by for and . Letting denote the outward unit normal to with respect to the metric , we define . According to the Gauss Lemma (see e.g. [15, Chapter 9, Lemma 15]), in these coordinates the metric takes the form with a metric on depending smoothly on . In polar normal coordinates , where and is the usual spherical volume form on . For a function extended by zero to , we can extend to a volume form on and get
[TABLE]
We choose
[TABLE]
where denotes the Riemannian distance function. Since , we can easily check that solves the eikonal equation (3.4).
We now look towards solving the transport equations (3.5)-(3.6). First, note that
[TABLE]
Therefore, we rewrite the transport equations (3.5)-(3.6) in polar normal coordinates based at to obtain
[TABLE]
[TABLE]
where denotes and denotes .
Applying [17, Section 3, Theorem 5], we find such that for the support of is contained in the interior of , and we have on and , where depends only on . Then for all we put:
[TABLE]
Then according to (3.1), and
[TABLE]
Similarly, for , we consider such that for the support of is contained in the interior of , and we have on and . Note that here we do not impose that and should coincide on .
For any , the functions
[TABLE]
[TABLE]
are solutions to the transport equations (3.10). In the same way, for , we fix
[TABLE]
which is a solution of (3.11). Here we fix satisfying on , and with independent of .
Let us now consider the remainder terms , . In view of (3.12)-(3.14), we deduce the following bounds:
[TABLE]
[TABLE]
[TABLE]
where depends only on , and . Then applying [10, Lemma 2.1], we see that problem (3.7) admits unique solutions for with . On the other hand, from the a priori estimate [11, (10.10), page 324], we deduce that
[TABLE]
Moreover, applying [10, Lemma 2.1] we find that
[TABLE]
and by interpolation between this estimate and (3.18) we deduce
[TABLE]
Combining this with (3.18) we obtain
[TABLE]
In a similar manner, we derive the estimate
[TABLE]
This completes our construction of the geometric optics solutions of (3.2).
4. Unique Determination of the Potentials Modulo Gauge Invariance
We recall that any -form , with admits a Hodge decomposition via , where is the solenoidal part of which satisfies (see (2.1) for the definition of coderivative operator ) and . Let us first prove an extension of this Hodge decomposition for the -form given by the following:
Lemma 1**.**
Let . Then we can decompose into
[TABLE]
where, for any , , and , we have and .
Proof.
We fix to be the solution for all of the boundary value problem
[TABLE]
Since , according to [9, Theorem 2.5.1.1], this problem admits a unique solution . Moreover, since , we also deduce that . In the same way, using the fact that , we prove that . We then use the Sobolev embedding theorem to deduce that . We fix and by the Sobolev embedding theorem, deduce that . Moreover, we see that
[TABLE]
Thus (4.1) is the Hodge decomposition of and the proof of the lemma is complete. ∎
We start by considering the implication
[TABLE]
where is the solenoidal part of the Hodge decomposition (4.1) of . For this purpose, we establish the following intermediate result.
Lemma 2**.**
Let satisfy the matching condition (1.3), and fix extended by [math] on . In particular, for the extension of to introduced in the previous section, we have . Assuming these conditions are fulfilled, we find that
[TABLE]
Proof.
We fix , the solutions for respectively of (3.2) taking the form (3.3). We write also . We consider solving
[TABLE]
and consider which solves
[TABLE]
where . Multiplying this equation by and integrating by parts yields
[TABLE]
Moreover,
[TABLE]
[TABLE]
Here is a generic constant which depends only on , and . On the other hand, we have that
[TABLE]
We then divide (4.5) by and apply (3.19)-(3.20) to obtain
[TABLE]
Using polar normal coordinates in the left hand side of the above gives us
[TABLE]
Using now the fact that , we conclude that
[TABLE]
We use this last estimate together with (4.3) and (4.4) to obtain (4.2).∎
Armed with the above, we are now in a position to complete the proof of the uniqueness result.
Proof of Theorem 1.
Let us assume that , and begin by proving that this condition implies that . We recall also Definition 2 of , the geodesic ray transform for -forms given by (2.2). According to s-injectivity of the transform (consult e.g. [1] or [16, Theorem 4]), it is enough to show that . Then, sending in (4.2) we obtain
[TABLE]
On the other hand, notice that, due to (3.9), for we have
[TABLE]
Thus we deduce that
[TABLE]
Using this identity in (4.6) and applying Fubini’s theorem, we get
[TABLE]
Since is arbitrary, we deduce that
[TABLE]
But since is arbitrary and for , we see that
[TABLE]
and hence deduce that for all , . Since one can check that . Then since for all it holds that is connected, we conclude that the map is constant. On the other hand, note that on , so that for any there exists such that for all we have . Therefore we conclude that .
We can then use the Hodge decomposition (4.1), to deduce the existence of satisfying such that . Thus the proof will be completed if we show that . Since we can put and by gauge invariance we have . Thus, by assumption it follows that
[TABLE]
Therefore, the proof will be complete if we prove that condition (4.7) implies that . For this purpose, we let , . We consider the solution of (3.2) for taking the form (3.3), and the solution of (3.2) but with replaced by and replaced by , again taking the form (3.2). Note that , so this construction is still valid. In particular, taking in (4.3) we obtain
[TABLE]
Fixing extended by [math] on , we get
[TABLE]
Then, we argue similarly to the proof of Lemma 2. Using polar normal coordinates and (3.19)-(3.20) we get
[TABLE]
And we send to obtain
[TABLE]
Let us recall the definition of the geodesic ray transform acting on functions, given by (2.3). In light of (4.8), we allow and to be arbitrary, whence we deduce that
[TABLE]
Now, since is arbitrary and on , we conclude that for all . Then by injectivity of on (e.g. [16, Theorem 3]) implies that , whence . This completes the proof of Theorem 1.∎
5. Stable Determination of the Magnetic Potential
In this section we establish the stability estimate in the recovery of the magnetic potential stated in Theorem 2. For , we assume that fulfill (1.4). Then, for extended by [math] on we have . We will also assume for the moment that for some small it holds that
[TABLE]
Before proving Theorem 2, let us recall some facts about the geodesic ray transform .
Firstly, according to [14, Theorem 4.2.1], the ray transform for -forms extends to a bounded linear operator . Fixing , we can also extend to a bounded linear operator , where is the space with respect to the weighted measure , and thus define as the adjoint of . By condition (1.3) we have with for . Moreover, according to [16, Section 8], the operator , is an elliptic pseudodifferential operator of order . Together with condition (1.5), we have for
[TABLE]
Also according to [16, Section 8], we can find constants such that for
[TABLE]
.
Proof of Theorem 2 subject to (5.1).
Following the work of the previous section, we allow to depend on . We can rewrite inequality (4.2) in the form
[TABLE]
We can use the Taylor expansion to see that
[TABLE]
and using this identity in (5.4) yields
[TABLE]
Combining this with the fact that
[TABLE]
and the definition of , we deduce that
[TABLE]
This implies that
[TABLE]
Since extends to a bounded linear operator , we can choose and then integrate (5.5) with respect to the volume form of . Using the compactness of we deduce that
[TABLE]
Moreover, using (5.2) we can further simplify (5.6) in order to obtain
[TABLE]
Since we also have
[TABLE]
we obtain the estimate
[TABLE]
We now set \gamma_{\ast}=\min\big{(}(\frac{T}{4})^{44},1\big{)}. Let . For , we can choose , and deduce that
[TABLE]
By the Sobolev embedding theorem, interpolation, and condition (1.5), we observe that
[TABLE]
Then, using (5.3) and condition (1.5), interpolation also yields the estimate
[TABLE]
Finally we combine (5.10), (5.11) and (5.12) to obtain
[TABLE]
Thus for small we deduce that
[TABLE]
Similarly for , we have
[TABLE]
Thus the proof of Theorem 2 is complete, subject to the smallness assumption (5.1).∎
We will now show that the assumption that (5.1) holds a priori is unnecessary. Define by
[TABLE]
where is chosen so that . We further define the function
[TABLE]
Note that approximates the Dirac delta distribution on as . Arguing as we did in (5.8), we use the estimate (5.4) to deduce that
[TABLE]
Since is extended by [math] to , it follows that is compactly supported in . We can find a finite open cover of so that for all we can choose the same spherical coordinates on in such a way that gives coordinates in a neighborhood of .
We can then fix , , . Let , . We define the function and let approximate the cylindrical Dirac delta distribution, that is
[TABLE]
It is well known (see for instance [13, Lemma 2.1]) that
[TABLE]
In addition, we fix
[TABLE]
We use (5.14) to deduce that
[TABLE]
In particular, is a positive constant depending only on , and , and independent of . In order to deal with the left hand side above, we need the following Lemma:
Lemma 3**.**
Let be , and let . Then for any we have that
[TABLE]
Proof.
[TABLE]
∎
Since is bounded, , then we must have when . Thus, Lemma (3) together with (5.15) tells us that
[TABLE]
For \gamma\leq\min\big{(}(\frac{T}{4})^{6n+69},1\big{)} we can choose , , to deduce that
[TABLE]
with independent of . We now choose small enough so the right hand side is near [math] when . But this implies that remains close to integer multiples of whenever . Recall that is extended to by zero. Thus, for choices of corresponding to short geodesics remaining close to the boundary of , we have . Then, the continuity of in , together with the previous argument implies is close to zero when . But implies , and in turn .
Then interpolation gives
[TABLE]
Thus, for we conclude that the smallness assumption holds. Therefore, we can rerun the argument of the previous section with replaced by , and reach the same conclusion without the need to assume smallness a priori. On the other hand, if , we proceed as in (5.13). With this, the proof of Theorem 2 is now complete.
6. Stable Recovery of the Electric Potential
This section is devoted to proving the stability estimate in the recovery of the electric potential stated in Theorem 3. Henceforth, for we assume that with (so that ), and that conditions (1.7) and (1.8) are fulfilled. Additionally, we continue to assume that condition (1.5) holds true for the magnetic potential. In light of (3.15)-(3.20), we can use (4.3)-(4.4) to deduce that
[TABLE]
where again denotes . Using the fact that
[TABLE]
together with (6.1) and (3.15)-(3.20), we obtain
[TABLE]
Then, by the definition of together with Stokes’ theorem, we deduce
[TABLE]
whence we have
[TABLE]
Since it holds that
[TABLE]
we deduce
[TABLE]
Applying the mean value theorem to the second term on the right, we find that
[TABLE]
and, by combining the above with (6.3), we deduce that
[TABLE]
By the Sobolev interpolation theorem, we can choose such that , and by interpolation together with condition (1.5) we deduce that
[TABLE]
By combining this estimate with the result Theorem 2, we conclude that
[TABLE]
Thus, we can rewrite (6.4) as
[TABLE]
Proof of Theorem 3.
In order to prove (1.9) we will use the estimate (6.5) together with a suitable choice of . First, note that according to condition (1.7) we have with when . Recall, according to [16, Section 7], that with the adjoint of (see for instance [2, Subsection 2.2] for details) is an elliptic pseudodifferential operator of order for . Therefore, for all , we have and condition (1.8) implies
[TABLE]
Moreover, according to [14, Theorem 4.2.1], for all , the operator is bounded. Thus, we can choose . Integrating the left hand side of (6.5) with respect to and applying Fubini’s theorem yields
[TABLE]
Combining this with (6.5) and (6.6), and using the fact that is compact, we get
[TABLE]
with depending only on , and . Further, by the same argument as in (5.8), the estimate (6.7) can be rewritten as
[TABLE]
Note that for all we have . Thus, according to [16, Theorem 3], we have
[TABLE]
Integrating with respect to yields
[TABLE]
Then, by interpolation we obtain
[TABLE]
where depends on , and . Combining this with estimate (6.8), we find that
[TABLE]
and (1.9) follows from (6.9) by a similar argument to the one used to prove Theorem 2 from (5.9). ∎
Acknowledgments
The work of YK was partially supported by the Agence Nationale de la Recherche under grant ANR-17-CE40-0029. AT was supported by EPSRC DTP studentship EP/N509577/1.
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