Carleman estimate and application to an inverse source problem for a viscoelasticity model in anisotropic case
Paola Loreti, Daniela Sforza, Masahiro Yamamoto

TL;DR
This paper develops a Carleman estimate for an anisotropic hyperbolic equation with memory, applies it to derive observability inequalities, and uses these results to solve an inverse source problem with stability in viscoelasticity models.
Contribution
It introduces a new Carleman estimate for anisotropic hyperbolic equations with memory and applies it to inverse problems and controllability in viscoelasticity.
Findings
Established a Carleman estimate with boundary data.
Derived an observability inequality for the initial state.
Proved Lipschitz stability for the inverse source problem.
Abstract
We consider an anisotropic hyperbolic equation with memory term: for and or , which is a model equation for viscoelasticity. First we establish a Carleman estimate for this equation with overdetermining boundary data on a suitable lateral subboundary . Second we apply the Carleman estimate to establish a both-sided estimate of by under the assumption that and is sufficiently large, satisfies some geometric condition. Such an estimate is a kind of observability inequality and related to the exact controllability. Finally we…
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Carleman estimate and application to an inverse source problem
for a viscoelasticity model in anisotropic case
Paola Loreti , Daniela Sforza , Masahiro Yamamoto
Dipartimento di Scienze di Base e Applicate per l’Ingegneria, Sapienza Università di Roma, Via Antonio Scarpa 16, 00161 Roma, Italy e-mail: [email protected] Dipartimento di Scienze di Base e Applicate per l’Ingegneria, Sapienza Università di Roma, Via Antonio Scarpa 16, 00161 Roma, Italy e-mail: [email protected] Department of Mathematical Sciences, The University of Tokyo, Komaba, Meguro, Tokyo 153, Japan e-mail: [email protected]. Partially supported by Grant-in-Aid for Scientific Research (S) 15H05740 of Japan Society for the Promotion of Science
Abstract
We consider an anisotropic hyperbolic equation with memory term:
[TABLE]
for and or , which is a model equation for viscoelasticity. First we establish a Carleman estimate for this equation with overdetermining boundary data on a suitable lateral subboundary . Second we apply the Carleman estimate to establish a both-sided estimate of by under the assumption that and is sufficiently large, satisfies some geometric condition. Such an estimate is a kind of observability inequality and related to the exact controllability. Finally we apply the Carleman estimate to an inverse source problem of determining a spatial varying factor in and we establish a both-sided Lipschitz stability estimate.
1 Introduction and main results
Let be a bounded domain with smooth boundary . We consider an integro-hyperbolic equation
[TABLE]
[TABLE]
We assume that
[TABLE]
Here and henceforth let be a multi-index and we set , , , , .
Throughout this paper, we assume
[TABLE]
if not specified. Let be the unit outward normal vector to at and let
[TABLE]
For concise description, we set
[TABLE]
The equation (1.1) is a model equation for the viscoelasticity.
We point out that for some materials, the effects of memory cannot be neglected without failing the analysis, as observed by Volterra [56]. He embraced Boltzmann model, according to which the stress has to depend linearly on strain history.
Our integro-differential equation (1.1) serves as a model for describing the viscoelastic properties of those materials whose properties are different along several directions. There is a huge number of papers treating viscoelastic models, as shown, e.g., in the book Renardy, Hrusa and Nohel [53]. With no pretension to be exhaustive, we cite the papers Dafermos [17] and Edelstein and Gurtin [19]. In particular, in a pioneering work [17], Dafermos studied an abstract formulation of our equation, giving as an application the case of an anisotropic viscoelastic equation.
In this paper, we first establish a Carleman estimate for (1.1). A Carleman estimate is a weighted -estimate for solutions to a partial differential equation which holds uniformly in large parameter , and was derived by Carleman [13] for proving the unique continuation property. Second we apply the Carleman estimate to prove an estimate of initial value by data on suitable lateral boundary data, which is called an observability inequality. Finally we discuss an inverse source problem. More precisely, the external force is assumed to cause the action, but in practice it is often that is not a priori known and so we have to identify by available data for the sake of accurate analysis of the system. We are concerned with the determination of a spatial component of with given . The form is special but in applications we model the external force in a more special form where is the time changing ratio and is the spatial distribution of the external force.
For the statement of the Carleman estimate, we need to introduce notations. We set and
[TABLE]
for all and . Given functions and , we define the Poisson bracket by
[TABLE]
We set
[TABLE]
with fixed . In addition to (1.2), throughout this paper, we assume that there exists a constant such that
[TABLE]
(e.g., Bellassoued and Yamamoto [9], [10]). For proving a Carleman estimate, it is known that we need some condition like (1.5), which ic called the pseudo-convexity (e.g., Hörmande [25]). We refer to Yao [58] which discusses anisotropic materials without intregral terms and shows a counterexample to the observability inequality without such condition for the principal part.
Next as subboundary where we take boundary data of the solution , we define
[TABLE]
Here and henceforth denotes the scalar product in .
Furthermore we set
[TABLE]
[TABLE]
and
[TABLE]
where is chosen sufficienly small for the constant in (1.5) and is a second large paramater and chosen later.
The conditions (1.5) and (1.6) pose extra conditions for and respectively and are a sufficient condition for the Carleman estimate below stated.
Now we introduce a cut-off function in . For fixed sufficiently small , let satisfy in and
[TABLE]
We further set
[TABLE]
Then for and .
Now we are ready to state our first main result.
**Theorem 1.1.
**Let
[TABLE]
We set
[TABLE]
(i) There exists a constant such that for , we can choose constants and such that
[TABLE]
[TABLE]
and
[TABLE]
[TABLE]
for all and satisfying for all and .
(ii) Moreover we assume
[TABLE]
Then
[TABLE]
[TABLE]
for all and satisfying for all and .
In (ii) of the theorem, we can rewrite (1.13) in terms of , but we omit.
Inequalities (1.12) and (1.13) hold for each solution to (1.1) and both are weighted with and uniform for sufficiently large in the sense that the constant is independent of all large . Such an inequality is called a Carleman estimate. The Carleman estimate is effectively applied to the unique continuation for partial differential equations, the observability inequality and inverse problems. In this paper, by Theorem 1.1 we establish the observability inequality (Theorem 1.2) and the Lipschitz stability in an inverse source problem (Theorem 1.3) for (1.1).
As for general treatments on Carleman estimates for partial differential equations without integral terms, we refer to Hörmander [25], Isakov [38]. There are many works concerning Carleman estimates for partial differential equations without integral terms. Since inverse problems are often concerned with the determination of the principal coefficients , we have to concretely realize the condition (1.5). As for such concrete Carleman estimates which give sufficient conditions for (1.5) and more directly applicable to inverse problems, see Amirov and Yamamoto [1]. We refer to Baudouin, de Buhan and Ervedaza [2], Imanuvilov [27], Khaĭdarov [42], Romanov [54] which establish Carleman estimates for hyperbolic equations. For Carleman estimates for parabolic equations, in addition to Isakov [38], [39], Isakov and Kim [40], see Fursikov and Imanuvilov [22], Imanuvilov [26], Imanuvilov, Puel and Yamamoto [30], Yamamoto [57]. For elliptic Carleman estimates where the right-hand side is estimated in -space, see Imanuvilov and Puel [29].
As for isotropic hyperbolic equations with integral terms, Cavaterra, Lorenzi and Yamamoto [14] established a Carleman estimate and applied it for proving a stability result for some inverse source problem. Here the isotropic hyperbolic equation means
[TABLE]
in (1.1). After [14], in the case where and are isotropic Lamé operators, the following works discuss Carleman estimates and inverse problems: de Buhan and Osses [18], Lorenzi, Messina and Romanov [51], Lorenzi and Romanov [52], Romanov and Yamamoto [55]. However, to the best knowledge of the authors, there are no publications on Carleman estimates for anisotropic hyperbolic equations with integral terms . For this anisotropic case, differently from the isotropic case, we need a lot of technicalities because and are not commutative modulo lower-order terms of derivatives.
Now we present two applications of the Carleman estimate (Theorem 1.1). First we derive a partial observability inequality of estimating one component of a pair of initial values.
Let satisfy with and
[TABLE]
Let and be given.
**Partial observability inequality.
**Estimate by .
Thanks to the integral term , our method requests that or in , and here we discuss only the case of .
The observability inequality is regarded as a dual problem to the exact controllability, and for a hyperbolic type of equations without integral terms, there have been enormous works. Here we refer only to Komornik [48], Lions [50], and Yao [58] which discusses anisotropic hyperbolic equations without integral terms. For proving observability inequalities, the multiplier method is commonly applied, but also a Carleman estimate is applicable for wider classes of partial differential equations (e.g., Kazemi and Klibanov [41], Klibanov and Malinsky [45]). As for the first application of Theorem 1.1, we show an observability inequality for (1.14).
**Theorem 1.2.
**We assume that satisfies (1.6), and
[TABLE]
Then there exists a constant such that
[TABLE]
for each solution to (1.14) with .
In this theorem, we can replace (1.3) by weaker condition
[TABLE]
By the finiteness of the propagation speed, we need to assume (1.15), and also a geometric condition (1.6) on the observation subboundary is assumed. This is the same for the inverse source problem stated below.
Finally we discuss an inverse source problem. That is, we consider
[TABLE]
Here we assume
[TABLE]
Let be given and be fixed. Then we discuss
**Inverse source problem.
**Determine , from .
As the stability for the inverse problem, we prove
**Theorem 1.3.
**We assume (1.6) and (1.15). Then there exists a constant such that
[TABLE]
for each .
The second inequality in (1.18) asserts the Lipschitz stability for our inverse problem. The first inequality means that our estimate is the best possible estimate for the inverse source problem.
Our argument for the inverse problem is based on Bukhgeim and Klibanov [12], which relies on a Carleman estimate. Klibanov [44] corresponds to the full version of [12]. Since Bukhgeim and Klibanov [12], their methodology has been developed for various equations and we can refer to many papers on inverse problems of determining spatially varying coefficients and components of source terms. As a partial list of references on inverse problems for hyperbolic and parabolic equations by Carleman estimates, we refer to Baudouin and Yamamoto [3], Bellassoued [5], [6], Bellassoued and Yamamoto [8], Benabdallah, Cristofol, Gaitan and Yamamoto [11], Cristofol, Gaitan and Ramoul [16], Imanuvilov and Yamamoto [31] - [34], Klibanov [43], [44], Klibanov and Yamamoto [47], Yamamoto [57], Yuan and Yamamoto [60].
As for similar inverse problems for the Navier-Stokes equations, see Bellassoued, Imanuvilov and Yamamoto [7], Choulli, Imanuvilov, Puel and Yamamoto [15], Fan, Di Cristo, Jiang and Nakamura [20], Fan, Jiang and Nakamura [21]. Gaitan and Ouzzane [23], and Gölgeleyen and Yamamoto [24] discuss inverse problems for transport equations by Carleman estimate, and Imanuvilov, Isakov and Yamamoto [28], Imanuvilov and Yamamoto [35] - [37] discuss Carleman estimates and inverse problems for non-stationary isotropic Lamé systems, which are related to our equation for the viscoelasticity. See Yuan and Yamamoto [59] about a Carleman estimate and inverse problems for a plate equation. As related books on Carleman estimates and inverse problems, see Beilina and Klibanov [4], Klibanov and Timonov [46], Lavrent’ev, Romanov and Shishatskiĭ[49].
This paper is composed of five sections. In section 2, we prove Theorem 1.1 and section 3 is devoted to providing fundamental energy estimates. In sectios 4 and 5, we prove Theorems 1.2 and 1.3 respectively.
2 Proof of Theorem 1.1
The proof is combination of hyperbolic and elliptic Carleman estimates (Lemmata 2.1 and 2.2) with another key lemma (Lemma 2.3) which can incorporate the integral term in (1.1). We divide the proof into five steps.
**First Step.
**Henceforth we set
[TABLE]
Under the assumption (1.7), a Carleman estimate for hyperbolic equations is known (e.g., Bellassoued and Yamamoto [9], [10]).
**Lemma 2.1.
**There exists a constant such that for , we can choose constants and such that
[TABLE]
[TABLE]
for all and satisfying .
Moreover we have a Carleman estimate for the elliptic operator without the extra conditions on .
**Lemma 2.2.
**Let be given. There exists a constant such that for , we can choose constants and such that
[TABLE]
[TABLE]
for all and .
In the case of , Lemma 2.2 is classical and we refer to Lemma 7.1 in Bellassoued and Yamamoto [10] for example. For completeness, we give the proof of Lemma 2.2 for arbitrary on the basis of the case of in Appendix.
Second Step.
For gaining compact supports in time for functions under consideration, we use the cut-off function. That is, we recall that we choose a cut-off function such that and
[TABLE]
In the succeeding arguments, we notice that all the terms with derivatives of can be regarded as of minor orders with respect to the large parameter .
For treating an integral, it is essential to introduce a new function
[TABLE]
Then
[TABLE]
We set
[TABLE]
Then we have
[TABLE]
and so
[TABLE]
[TABLE]
Then satisfies
[TABLE]
By (2.3), we note that only if . Moreover, since
[TABLE]
we obtain
[TABLE]
By and (2.5), we see that . Thus
[TABLE]
where
[TABLE]
and , .
Applying Lemma 2.1 to (2.8), we have
[TABLE]
[TABLE]
for .
**Third Step.
**For estimating the integral term in (1.1) with the weight , we need to prove
**Lemma 2.3.
**Let . Then
[TABLE]
This type of inequality is essential for applications of Carleman estimates to inverse problems (Bukhgeim and Klibanov [12], Klibanov [44]) and the inequality not involving the cut-off function , is proved in [44], [46].
**Proof.
**It suffices to prove for , because the proof for is similar. By the Cauchy-Schwarz inequality, we have
[TABLE]
[TABLE]
Noting that
[TABLE]
by integration by parts, we obtain
[TABLE]
[TABLE]
Here we used
[TABLE]
by (2.3).
Therefore we can shift the first term on the right-hand side into the left-hand side, we have
[TABLE]
Choosing and sufficiently large and noting that and in , we can obtain . Therefore
[TABLE]
Substituting this into (2.12), by (2.11) we can complete the proof of Lemma 2.3.
**Fourth Step.
**Henceforth generically denotes functions in such that
[TABLE]
Henceforth we denote , . We note that , , can be replaced by in the following estimation.
Applying Lemma 2.3 to the third term on the right-hand side of (2.10) and noting that , we have
[TABLE]
We set
[TABLE]
Then
[TABLE]
Therefore
[TABLE]
[TABLE]
for .
We will estimate the second and the third terms on the right-hand side of (2.13). By (2.4), we have
[TABLE]
in , and so we apply (2.2) with , we obtain
[TABLE]
Next we apply Lemma 2.3 with to the second term on the right-hand side and, similarly to (2.13), we obtain
[TABLE]
[TABLE]
Therefore
[TABLE]
Choosing sufficiently large, we can absorb the second term on the right-hand side into the left-hand side. Moreover we choose sufficiently larger such that , and by we obtain
[TABLE]
[TABLE]
for .
Now we estimate the third term on the right-hand side of (2.13). By (2.4) we have
[TABLE]
Apply (2.2) with , and we obtain
[TABLE]
By an argument similar to (2.14) for the third term on the right-hand side, we have
[TABLE]
Applying (2.15), we obtain
[TABLE]
[TABLE]
for .
Applying (2.15) and (2.16) to (2.13), we obtain
[TABLE]
Choosing sufficiently large, we can absorb the second term on the right-hand side into the left-hand side. Therefore
[TABLE]
[TABLE]
for . By the definition of , the estimate (2.17) proves (1.11).
Next we will prove (1.12). The addition of (2.15) and (2.16) yields
[TABLE]
[TABLE]
Applying (2.17) in (2.18), we obtain
[TABLE]
By (2.4) and , we have on . Consequently the estimate (1.12), and the proof of Theorem 1.1 (i) is completed.
**Fifth Step.
**We will prove Theorem 1.1 (ii). By (2.4), we have
[TABLE]
Henceforth generically denotes a function satisfying
[TABLE]
for . Applying Lemma 2.2 to (2.19) with , we obtain
[TABLE]
We estimate the second term on the right-hand side as follows. By , we have
[TABLE]
Lemma 2.3 with yields
[TABLE]
Consequently
[TABLE]
Thus we can absorb the second term on the right-hand side into the left-hand side, so that
[TABLE]
Fixing sufficiently large and applying Theorem 1.1 (i) to the second term on the right-hand side, we obtain
[TABLE]
[TABLE]
Next, setting , we differentiate the first equation in (2.8) in , and we have
[TABLE]
Since
[TABLE]
and
[TABLE]
in terms of (2.22) and (2.23), we apply Lemma 2.1 to (2.21) to obtain
[TABLE]
Applying (2.20) and Theorem 1.1 (i) to the third and the second terms on the right-hand side respectively, we see
[TABLE]
By (2.4), we have and
[TABLE]
on . Choosing and sufficiently large, we can absorb the fourth terms on the right-hand side into the left-hand side, we have
[TABLE]
[TABLE]
for .
Substituting (2.24) into (2.20), we obtain
[TABLE]
Thus the proof of Theoerem 1.1 (ii) is completed.
We close this section with the following lemma which is nothing but (2.24) where we fix sufficiently large. The lemma plays an essential role for the proof of Theorem 1.3.
**Lemma 2.4.
**Let satify (1.16) and let (1.17) hold. Under the same assumptions in Theorem 1.1 (ii), we have
[TABLE]
for . Here we set
[TABLE]
3 Energy estimates
For proving Theorems 1.2 and 1.3, we show energy estimates for hyperbolic equations with integral terms. Such an energy estimate is classical for hyperbolic equations without integral terms (e.g., Komornik [48], Lions [50]), but the presence of the integral terms makes extra estimation demanded.
**Lemma 3.1.
**We assume that
[TABLE]
and
[TABLE]
If satisfies
[TABLE]
and
[TABLE]
then there exists a constant , which is independent of choice of , such that
[TABLE]
Here and henceforth we set
[TABLE]
Proof of Lemma 3.1. We multiply (3.3) with and integrate over : By (3.1), (3.2) and (3.4) and integration by parts, we obtain
[TABLE]
and
[TABLE]
Next we calculate
[TABLE]
For , we set with . Noting
[TABLE]
we write
[TABLE]
Here
[TABLE]
Therefore
[TABLE]
where
[TABLE]
[TABLE]
For , we have
[TABLE]
[TABLE]
and for , we use the Poincaré inequality to obtain
[TABLE]
[TABLE]
Hence
[TABLE]
Thus we obtain
[TABLE]
We choose arbitrarily. Integrating both sides with respect to in , we reach
[TABLE]
Here we have
[TABLE]
Moreover, for any , we can choose a constant such that
[TABLE]
Moreover (3.9) and (3.10) yield
[TABLE]
and
[TABLE]
Thus we obtain
[TABLE]
Choosing sufficiently small such that , we have
[TABLE]
The Gronwall inequality implies
[TABLE]
Thus the proof of Lemma 3.1 is completed.
Next, on the basis of Lemma 3.1, we prove an energy estimate in Sobolev spaces of higher orders for the solution to (1.16). We assume that satisfies (1.16), and that (1.17) holds. Then we prove
**Lemma 3.2.
**There exists a constant such that
[TABLE]
for each .
Proof of Lemma 3.2. We set
[TABLE]
and
[TABLE]
We set
[TABLE]
Then
[TABLE]
[TABLE]
and
[TABLE]
Indeed we can verify (3.14) as follows. We differentiate (1.16) in to have
[TABLE]
Noting that by and changing the orders of integration, we obtain
[TABLE]
and
[TABLE]
[TABLE]
Therefore (3.14) is verified. The systems (3.15) and (3.16) can be verified similarly by noting that
[TABLE]
Applying Lemma 3.1 to (3.14) - (3.16), we have
[TABLE]
Next we have to estimate , . Since and by in , it suffices to estimate . By (3.17) we have
[TABLE]
Therefore (3.15) implies
[TABLE]
and so
[TABLE]
Since , we apply the a priori estimate for the elliptic boundary value problem, by (3.18) we obtain
[TABLE]
The Gronwall inequality yields
[TABLE]
Thus the proof of Lemma 3.2 is completed.
In this section we further show the following lemma for the hyperbolic equation without integral terms.
**Lemma 3.3.
**We assume (3.1). Let satisfy
[TABLE]
(i) There exists a constant such that
[TABLE]
(ii) There exists a constant such that
[TABLE]
Proof of Lemma 3.3. The estimate (3.20) is proved by the multiplier method (e.g., Komornik [48]). That is, we choose such that and which is the unit outward normal vector to . Then multiplyng (3.19) with and integrating over , we see (3.20). We omit the details and see e.g., [48] for the complete proof.
A usual energry estimate yields
[TABLE]
Since (3.19) is time-reversing, we can consider (3.19) by regarding as initial time and, applying (3.22), we obtain (3.21). Thus the proof of Lemma 3.3 is completed.
4 Proof of Theorem 1.2
Our proof is a modification of Kazemi and Klibanov [41] and Klibanov and Malinsky [45] which discuss hyperbolic equations without integral terms.
We make the even extension of to :
[TABLE]
Then, by , we can verify that
[TABLE]
[TABLE]
Hence
[TABLE]
Next we will estimate . By (4.1) and (4.2), it is sufficient to estimate for , that is, . Similarly to the proof of Lemma 3.2, we set
[TABLE]
[TABLE]
We recall that
[TABLE]
Noting that and and , in a way similar to (3.13) and (3.14), we can
[TABLE]
and
[TABLE]
Applying Lemma 3.1 to (4.4) and (4.5), we obtain
[TABLE]
By the first equation in (4.4), we have
[TABLE]
and
[TABLE]
Applying the a priori estimate for the elliptic boundary value problem, we reach
[TABLE]
¿From (4.6) and the Gronwall inequality it follows that
[TABLE]
Since , it follows from (4.7) that
[TABLE]
Thus
[TABLE]
Now we choose and in (1.10). The assumption (1.15) implies
[TABLE]
and
[TABLE]
by . Therefore there exist and such that
[TABLE]
By (4.10) we note that for , and so if we choose sufficiently small in (1.10). Then we can set with . Then
[TABLE]
We set
[TABLE]
Noting that in , we apply (1.11) in Theorem 1.1 to (1.14) where we fix large and applying (4.8) and so
[TABLE]
[TABLE]
for all large . On the other hand, similarly to (2.8), we see
[TABLE]
where
[TABLE]
for . Here, in terms of , and the first equation in (1.14), we calculated and .
Applying (3.21) in Lemma 3.3, we fix sufficiently small such that and
[TABLE]
Here we recall that . By (4.14) and (4.8), we obtain
[TABLE]
[TABLE]
At the last inequality, in view of the Poincaré inequality, and the a priori estimate for the boundary value problem for , we used
[TABLE]
[TABLE]
Hence, by (4.15), we have
[TABLE]
We further choose small such that and fix. Then for . Therefore
[TABLE]
for all large . Substituting this into the left-hand side of (4.12) and using (4.17), we obtain
[TABLE]
for all large . Hence
[TABLE]
for all large . Choosing sufficiently large such that , we complete the proof of the second inequality in the conclusion of Theorem 1.2.
Next we prove the first inequality of the conclusion. In place of , we set . Then, similarly to (2.8), we have
[TABLE]
where satisfies (4.14). Similarly to (4.16) and (4.17), we can verify
[TABLE]
Applying (3.20) in Lemma 3.3, we have
[TABLE]
[TABLE]
By on , we see
[TABLE]
and
[TABLE]
Therefore
[TABLE]
and
[TABLE]
With (4.19), we complete the proof of the first inequality. Thus the proof of Theorem 1.2 is completed.
5 Proof of Theorem 1.3
Once that the Carleman estimate Theorem 1.1 is established, we can prove Theorem 1.3 by an argument similar to Imanuvilov and Yamamoto [33]. See also Bellassoued and Yamamoto [10].
**First Step.
**We set and
[TABLE]
Similarly to (2.8) in , using on , by (2.4) we can verify
[TABLE]
and
[TABLE]
We make the even extension of to :
[TABLE]
Accordingly we make the even extensions of . Then, by for we can prove that
[TABLE]
[TABLE]
and
[TABLE]
We recall that . Hence, setting , we have
[TABLE]
Here we used that by and (2.7), (2.9).
We set
[TABLE]
We write (5.5) in terms of . First we have
[TABLE]
and
[TABLE]
Moreover
[TABLE]
and so
[TABLE]
Hence
[TABLE]
Using in the second term on the right-hand side, we obtain
[TABLE]
Thus (5.5) yields
[TABLE]
[TABLE]
[TABLE]
and
[TABLE]
We rewrite Lemma 2.4 in terms of . First and then , so that
[TABLE]
and we have similar estimates for . Hence
[TABLE]
and so
[TABLE]
for . Here we include into . Henceforth we set
[TABLE]
We estimate by Lemma 3.2, so that we obtain
[TABLE]
[TABLE]
for .
**Second Step.
**We will carry out the energy estimate. We multiply (5.6) with and integrate by parts over . Then
[TABLE]
Here by and , integrating by parts, we see
[TABLE]
Using in and noting that is independent of , we obtain
[TABLE]
Next, by the Cauchy-Schwarz inequality, we have
[TABLE]
[TABLE]
Here we extended the integral domain to . Moreover we note
[TABLE]
and
[TABLE]
By (2.22) and (1.13), we have
[TABLE]
and (2.23) yields
[TABLE]
Consequently substituting these inequalities and applying Lemma 2.4 and (5.9) to estimate
[TABLE]
from (5.11) we reach
[TABLE]
[TABLE]
for .
By (5.7), (5.10) and (5.12), using , we see
[TABLE]
for .
**Third Step.
**We complete the proof by an elliptic Carleman estimate. Since
[TABLE]
we estimate
[TABLE]
and
[TABLE]
and so
[TABLE]
By , we replace the second term on the right-hand side by the second term on the left-hand side, and we apply on by (1.17). Therefore
[TABLE]
[TABLE]
Since
[TABLE]
and for , the Lebesgue theorem yields
[TABLE]
as .
Therefore by choosing sufficiently large, the estimate (5.13) implies
[TABLE]
for . By for , we apply the Carleman estimate for the elliptic operator of the second order which is similar to Lemma 2.2 (here we fix ), we have
[TABLE]
for . Again choosing sufficienly large, we can absorb the first term on the right-hand side into the left-hand side, multiplying with and replacing by , we have
[TABLE]
for .
Hence
[TABLE]
that is,
[TABLE]
for all . We choose sufficiently large so that . Then . Noting that
[TABLE]
we complete the proof of the second inequality of (1.18).
Finally we have to prove the first inequality in (1.18). We set . Similarly to (2.8), we can obtain
[TABLE]
where and
[TABLE]
Therefore by (1.4) we see
[TABLE]
for and . We set
[TABLE]
Then we readily verify that . Applying (3.20) to (5.15) and noting (5.16), we obtain
[TABLE]
The second term on the right-hand side is estimated by Lemma 3.2, so that
[TABLE]
Finally, since
[TABLE]
by and , we have
[TABLE]
Consequently . Thus the proof of the first inequality, and so Theorem 1.3 is completed.
Acknowledgements. This work was completed when the third author was a guest professor at Sapienza Università di Roma in May - June 2016. The author thanks the university for that opportunity yielding the current joint work.
Appendix. Proof of Lemma 2.2 for general .
It is known that
[TABLE]
[TABLE]
for all and . See e.g., Bellassoued and Yamamoto [10] or we can prove (1) similarly to Yamamoto [57] where the parabolic Carleman estimate is proved. However here we omit the proof of (1). Now let , . We set
[TABLE]
and
[TABLE]
Then we directly verify
[TABLE]
and
[TABLE]
and
[TABLE]
[TABLE]
Therefore we have
[TABLE]
that is,
[TABLE]
By , we can write
[TABLE]
By (3), applying (1) to (6), we obtain
[TABLE]
Choosing sufficiently large, we can absorb the second term on the right-hand side into the left-hand side and using
[TABLE]
by , we have
[TABLE]
[TABLE]
Similarly to (4) and (5), we see
[TABLE]
and
[TABLE]
Therefore, since
[TABLE]
we obtain
[TABLE]
[TABLE]
Here we used (8) for the final term. Moreover by (8) and (9), we have
[TABLE]
[TABLE]
Substituting (8) - (10) in (7), we obtain
[TABLE]
[TABLE]
for all . Here in choosing , we further assume that to have
[TABLE]
with sufficiently large constant . Multiplying (11) with , we reach the conclusion and thus the proof of Lemma 2.2 with is completed.
The reference list from the paper itself. Each links out to its DOI / PubMed record.
- 1[1] A. Amirov and M. Yamamoto, A timelike Cauchy problem and an inverse problem for general hyperbolic equations, Applied Mathematics Letters 21 (2008), 885-891 (2008).
- 2[2] L. Baudouin, M. de Buhan and S. Ervedoza, Global Carleman estimates for waves and applications, Comm. Partial Differential Equations 38 (2013), 823-859.
- 3[3] L. Baudouin and M. Yamamoto, Inverse problem on a tree-shaped network: unified approach for uniqueness, Appl. Anal. 94 (2015), 2370-2395.
- 4[4] L. Beilina and M.V. Klibanov, Approximate Global Convergence and Adaptivity for Coefficient Inverse Problems, Springer-Verlag, Berlin, 2012.
- 5[5] M. Bellassoued, Uniqueness and stability in determining the speed of propagation of secondorder hyperbolic equation with variable coefficients, Appl. Anal. 83 (2004), 983-1014.
- 6[6] M.Bellassoued: Global logarithmic stability in inverse hyperbolic problem by arbitrary boundary observation, Inverse Problems 20 (2004), 1033-1052.
- 7[7] M. Bellassoued, O. Y. Imanuvilov and M. Yamamoto, Carleman estimate for the Navier-Stokes equations and an application to a lateral Cauchy problem, Inverse Problems 32 (2016), 025001, 23 pp.
- 8[8] M. Bellassoued and M. Yamamoto, Logarithmic stability in determination of a coefficient in an acoustic equation by arbitrary boundary observation, J. Math. Pures Appl. 85 (2006), 193-224.
