1. Introduction
Inverse source problems have been an active research topic in inverse scattering theory due to their significant applications in both science and engineering including antenna synthesis, seismic imaging and biomedical imaging [Reference Bao, Hu, Kian and Yin4, Reference Bao, Li and Zhao6, Reference Fokas, Kurylev and Marinakis13, Reference Isakov and Lu15, Reference Zhai and Zhao22]. Theoretically, it is known in general that there is no uniqueness for the inverse source problem at a fixed frequency due to the existence of non-radiating sources [Reference Acosta, Chow, Taylor and Villamizar1, Reference Albanese and Monk2, Reference Kow and Wang16]. From the computational point of view, a more challenging issue is the lack of stability. A small variation of the data might lead to a huge error in the reconstruction. Recently, it has been realised that the use of multi-frequency data is an effective approach to overcome the difficulties of non-uniqueness and instability which are encountered at a single frequency [Reference Bao, Li, Lin and Triki5]. The increasing stability estimates for the inverse source problems by multi-frequency measurements have been extensively studied in [Reference Bao, Li and Zhao6, Reference Cheng, Isakov and Lu8, Reference Dyatlov and Zworski11, Reference Isakov and Lu15, Reference Li and Yuan19, Reference Li, Zhai and Zhao20, Reference Zhao23]. We also mention some recent works [Reference Bai, Diao, Liu and Meng3, Reference Diao, Liu and Wang9, Reference Diao, Liu and Sun10] on inverse scattering problems of elastic wave equations. This paper is concerned with the stability for the inverse source problem of the elastic wave equation with attenuation from multi-frequency boundary measurements.
We consider the three-dimensional elastic wave equation
where the positive constant $\sigma \gt 0$ is a damping or attenuation coefficient, $\Delta ^* = \lambda \Delta + (\lambda + \mu )\nabla \nabla \cdot$ , $\omega \gt 0$ is the frequency. Here, $\lambda$ and $\mu$ are the Lamé parameters satisfying $\mu \gt 0$ and $3\lambda +2\mu \gt 0$ , the vector $\mathbf{u}$ denotes the outgoing elastic field and the source function $\mathbf{f}\in L^\infty \left(\mathbb R^3\right)^3$ is assumed to have a compact support contained in the ball $B_R$ . We are interested in the inverse problem of determining the source function $\mathbf{f}(x)$ by multi-frequency boundary measurements $\{\mathbf{u}(x, \omega )\vert _{\partial B_R}, \nabla \mathbf{u}(x, \omega )\vert _{\partial B_R}\}$ with $\omega$ given in a finite interval.
The main result in this paper is the derivation of the increasing stability estimate for the elastic wave modelled by the Navier equation with a damping coefficient. Motivated by [Reference Isakov and Lu15], by the Fourier transform the inverse source problem is reduced to the identification of the initial data for the initial value problem of the time-domain damped elastic wave equation by lateral Cauchy data. Then, we obtain an exact observability bound for the source function using the Carleman estimates, which connects the scattering data and the unknown source function by taking the inverse Fourier transform. The Fourier transform is justified by proving an appropriate rate of time decay for the time-domain damped elastic wave equation. Using the resolvent estimates for the elastic wave equation, we obtain a sectorial resonance-free region and resolvent estimates for the data with respect to the complex frequency in this region, which lead to the bound of the analytic continuation of the data from the given data to the higher frequency data. By tracing the dependence of the bound for analytic continuation and of the exact observability bound for the elastic wave equation on the attenuation coefficient, we show the exponential dependence of increasing stability on the damping constant. An important ingredient of the analysis is the application of the Helmholtz decomposition to the elastic wave. The stability estimate consists of the Lipschitz type of data discrepancy and the high wavenumber tail for the source function. The latter decreases as the wavenumber of the data increases, which implies that the inverse problem is more stable when the higher wavenumber data is used. However, the stability deteriorates as the damping constant becomes larger. We point out that the method in this work can be used to deal with the case of variable attenuation coefficient.
This paper is organised as follows. Section 2 is devoted to the well-posedness of the direct scattering problem. In Section 3, we prove an exact observability bound for elastic wave equations. By Carleman estimates for wave equations, we trace the dependence of the exact observability bound on the attenuation coefficient. Section 4 is devoted to the proof of the stability estimate. We employ scattering theory to obtain resolvent estimates for the elliptic operator which gives explicit bounds for analytic continuation. The Fourier transform in time is justified using the decay estimates of the damped elastic wave equation, which is obtained from the decay estimates for the acoustic wave equation and the Helmholtz decomposition. Section 5 is devoted to the decay estimates of the damped acoustic wave.
2. Direct source problem
Using the Helmholtz decomposition, the source function $\mathbf{f}\in L^2(B_R)^3$ can be decomposed as
where $\mathbf{f}_p, \mathbf{f}_s\in L^2(B_R)^3$ with $\nabla \times \mathbf{f}_p = 0$ and $\nabla \cdot \mathbf{f}_s = 0$ . Hence, the solution $\mathbf u$ to the equation (1.1) can be decomposed into the pressure wave $\mathbf u_p$ and shear wave $\mathbf u_s$
where $\nabla \times \mathbf{u}_p=0$ , $\nabla \cdot \mathbf{u}_s=0$ and
Here, $ k_p=\sqrt{\dfrac{\omega ^2 + \textrm{i}\omega \sigma }{\lambda +2\mu }}$ , $ k_s=\sqrt{\dfrac{\omega ^2 + \textrm{i}\omega \sigma }{\mu }}$ are the wavenumbers for the damped pressure and shear waves. Actually, one has
Motivated by the Helmholtz decomposition (2.1)–(2.2), to investigate the direct scattering problem of the elastic wave we first study the damped Helmholtz equation. Consider the following Helmholtz equation:
Here, we note that $u$ and $f$ are scalar-valued functions. The following theorem concerns its well-posedness.
Theorem 2.1. Given $f\in L^2\left(\mathbb R^3\right)$ with a compact support, there exists a unique exponentially decaying outgoing solution $u\in H^2\left(\mathbb R^3\right)$ to (2.4) for every $k\gt 0$ with the following estimate:
as $|x|\longrightarrow \infty$ . Here, $C(f)$ and $c(k, \sigma )$ are positive constants depending on $f$ and $k, \sigma$ , respectively.
Proof. We define
where
This definition is motivated by taking the Fourier transform of $u(x, k)$ formally with respect to the spatial variable $x$ . Then by the Plancherel’s theorem, for each $k\gt 0$ one has that $u^*(\cdot, k)\in H^2\left(\mathbb R^3\right)$ and satisfies equation (2.4).
Since
where $ \kappa = (k^2 + \textrm{i}k\sigma )^{\frac{1}{2}}$ with $\Im \kappa \gt 0$ , one can rewrite $u^*(x, k)$ as
Thus, since $f$ has a compact support by (2.5) one has that the solution $u^*(x, k)$ satisfies the estimate
where $C(f)$ and $c(k, \sigma )$ are positive constants depending on $f$ and $k, \sigma$ , respectively. Using direct calculations, one may show that $\nabla u^*$ and $\Delta u^*$ have similar exponential decay estimates.
Now we prove the uniqueness. Assume that $\tilde{u}^*(x, k)$ is another solution to (2.4). Then one has
and applying Fourier transform to the above equation gives
Since for $k\gt 0$ one has that $|\xi |^2 - k^2 - \textrm{i}k\sigma \neq 0$ for all $\xi \in \mathbb R^3$ , the inverse Fourier transform gives $u^* - \tilde{u}^* = 0$ , which proves the uniqueness.
The well-posedness of the direct scattering problem is a direct consequence of the Helmholtz decomposition (2.1)–(2.2) and Theorem 2.1 for the Helmholtz equation.
Theorem 2.2. Let $\mathbf{f}\in L^2\left(\mathbb R^3\right)^3$ with a compact support. Then there exists a unique outgoing solution $\mathbf{u}$ of Schwartz distribution to (1.1) for every $\omega \gt 0$ . Moreover, the solution satisfies
as $|x|\to \infty,$ where $C(\mathbf{f})$ and $c(\omega, b, \lambda, \mu )$ are positive constants depending on $\mathbf f$ , and $\omega, \sigma$ and Lamé parameters, respectively.
3. Exact observability bounds for elastic wave equations
In order to bound the unknown source $\mathbf{f}$ by boundary data of $\mathbf{u}$ (see Lemma 4.2), we will prove an observability bound for the initial data of the corresponding time-domain damped elastic wave equation by noting that the solution to the time-harmonic damped elastic wave equation can be connected with the time-domain damped elastic wave equation by Fourier transformation.
We will derive an exact observability bound for the initial data $\mathbf{f}$ of the following time-domain damped elastic wave equation
Using Helmholtz decomposition again to the vector-valued initial condition $\mathbf{f}\in L^2(B_R)^3$ , one has
where $\mathbf{f}_p, \mathbf{f}_s\in L^2(B_R)^3$ with $\nabla \times \mathbf{f}_p = 0$ and $\nabla \cdot \mathbf{f}_s = 0$ . As a consequence, we decompose the solution $\mathbf U$ to the equation (3.1) into a sum of pressure wave $\mathbf U_p$ and shear wave $\mathbf U_s$ (see, e.g., [Reference Bao, Hu, Kian and Yin4])
where $\mathbf{U}_p$ and $\mathbf{U}_s$ satisfy $\nabla \times \mathbf{U}_p=0$ , $\nabla \cdot \mathbf{U}_s=0$ and the following damped pressure and shear wave equations
and
Here, $c_p= \sqrt{\lambda +2\mu }$ and $c_s=\sqrt{\mu }$ are the wave speeds for pressure and shear waves, respectively.
The following Carleman estimate is useful in deriving the exact observability bound.
Lemma 3.1. Let $T\gt 2R+1$ , $\varphi (x, t) = |x - a|^2 - \theta ^2\left(t - \frac{T}{2}\right)^2$ where $a\notin \overline{B_R}$ , dist(a, $\partial B_R$ ) = 1 and $\theta = \frac{1}{2}$ . Let $\mathbf{U}$ be a solution to (3.1) with $\mathbf{f}\in H^1(B_R)^3$ , $\text{supp}\mathbf{f}\subset B_R$ . Then we have the following Carleman estimate:
where $\alpha =(\alpha _1, \alpha _2, \alpha _3, \alpha _4)\in \mathbb N^4$ and $\partial _\alpha = \partial _{t}^{\alpha _1}\,\partial _{x_1}^{\alpha _2}\,\partial _{x_2}^{\alpha _3}\,\partial _{x_3}^{\alpha _4}$ .
Proof. Let $v = \nabla \cdot \mathbf{U}$ and $\mathbf{w} = \nabla \times \mathbf{U}$ . Assume $\mathbf{U}$ is the solution to (3.1). By Carleman estimate in [Reference Isakov14] or [Reference Bellassoued and Yamamoto7] one has that
Since the Helmholtz decomposition (3.2) gives
by the elliptic regularity theory one has
and
Hence, from (3.5) we have
Since $\mathbf{f}$ has compact support contained in $B_R$ , one has
and
which completes the proof.
Using Lemma 3.1 and following the arguments in the proof of [[Reference Isakov and Lu15], Theorem 3.1], we obtain the exact observability bound.
Theorem 3.2. Assume that the observation time $T$ satisfies $4(2R + 1) \lt T \lt 5(2R + 1)$ . There exists a constant $C$ depending on the domain $B_R$ such that
for all $\mathbf{U}$ solving (3.1) with $\mathbf{f}\in H^1(B_R)^3$ , $ \text{supp} \mathbf{f}\subset B_R$ .
4. Inverse source problem
In this section, we study the inverse source problem for elastic waves. Denote the resolvent of the elliptic operator $-\Delta ^*$ by
The following results on analyticity and resolvent estimates of $\mathbf{R}_0(\zeta )$ with respect to complex frequency $\zeta \in \mathbb C$ are useful in the subsequent analysis of the stability estimate. The proof utilises the method for the classical Schrödinger operator in [Reference Dyatlov and Zworski11].
Proposition 4.1. Fix a smooth cut-off function $\rho \in C_0^\infty \left(\mathbb R^3\right)$ . The free resolvent defined by (4.4) is analytic in $\mathbb C$ with respect to $\zeta$ as a family of operators
with the following resolvent estimate:
Here, $\langle \zeta \rangle = \sqrt{1 + |\zeta |^2}$ , $\widetilde{k}_s=\zeta \sqrt{\frac{1}{\mu }}$ , $(\Im \widetilde{k}_s)_- = \max \{0, -\Im \widetilde{k}_s\}$ and $L$ satisfies $c_s L\gt \textrm{diamsupp}\rho$ with $\textrm{diamsupp}\, \rho = \textrm{sup}\{|x - y|\,:\, x, y \in \textrm{supp}\rho \}$ .
Proof. Recall the wavenumbers for compressional and shear waves given by
respectively. Denote the resolvents of the pressure and shear waves in the frequency domain respectively by
Fix a smooth cut-off function $\rho \in C_0^\infty \left(\mathbb R^3\right)$ and denote $\textrm{diamsupp}\, \rho = \textrm{sup}\{|x - y|\,:\, x, y \in \textrm{supp}\rho \}$ . As in [Reference Dyatlov and Zworski11], for $\zeta \in \mathbb C$ the resolvents of the wave speed for pressure and shear waves can be represented by
where $\mathbf W (t) = \frac{\sin t \sqrt{-\Delta }}{ \sqrt{-\Delta } }$ and $L$ satisfies $c_s L\gt \textrm{diamsupp}\rho$ . Consequently, by (3.2), (3.3) and (3.4) we obtain that
Moreover, since by [[Reference Dyatlov and Zworski11], Theorem 3.1]
and
where $(t)_-: = \max \{0, -t\}$ , we obtain from (4.4) and (4.3) that
Now we can derive the analyticity of the free resolvent $\rho \mathbf{R}_0(\zeta ) \rho$ from those of $\rho \mathbf{R}_{p}(\zeta ) \rho$ and $\rho \mathbf{R}_{s}(\zeta ) \rho$ . In what follows, we prove the resolvent estimates (4.2) by standard regularity theory of elliptic equations. The case for $j = 0$ is a consequence of (4.5). For $j = 2$ , taking $\tilde{\rho }\in C^\infty _0\left(\mathbb R^3\right)$ such that $\tilde{\rho } = 1$ near the support of $\rho$ , we have from [[Reference Stein21], $(7.13)$ ] that
where $C\gt 0$ is a constant. Let $\mathbf{u} = \mathbf{R}_0(\zeta )(\rho \mathbf{f})$ with $\mathbf{f}\in L^2\left(\mathbb R^3\right)^3$ . One has
Since
we get
Finally, the case of $j = 1$ can be obtained from the interpolation between $j=0$ and $j = 2$ , which completes the proof.
Define a vector-valued real function space
Due to the exact observability bound (3.6), we introduce the boundary measurement of the elastic wave
In the following lemma, we bound the unknown source by the boundary measurements (4.6).
Lemma 4.2. There holds
where $\mathbf{u}(x, \omega )$ is the solution to the direct scattering problem (1.1) with $\mathbf{f}\in \mathcal C_Q$ .
Remark 4.3. The proof of Lemma 4.2 depends on the exact observability inequality (3.6) and Fourier transform. Intuitively, by letting $\mathbf{U}(x,t)=0$ , $t\lt 0$ , we can see $\mathbf{u}(x,\omega )=\int _{-\infty }^{+\infty } \mathbf{U}(x,t)e^{\textrm{i}\omega t}dt=\int _{0}^{+\infty } \mathbf{U}(x,t)e^{\textrm{i}\omega t}dt$ . By Theorem 3.6 and Plancherel’s theorem, we have
Thus, we formally proved Lemma 4.2. To justify the Fourier transform rigorously, one can obtain the decay estimates of the solution $\mathbf{U}$ to the time-domain initial-valued elastic wave (3.1) by combining the Helmholtz decomposition (3.2) and the decay estimates for acoustic wave equations proved in Theorem 5.1 assuming that the source $\mathbf{f}$ has sufficient regularity ( $\mathbf{f}\in H^n, n\geq 5$ ). As the proof follows the arguments in [[Reference Li, Yao and Zhao17], Lemma 3.1] in a straightforward way, we omit it for brevity.
Define
where $:$ denotes the double dot product which is defined by $A\,:\,B=\sum \limits _{i,j=1}^3 a_{ij}b_{ij}$ for $A=(a_{ij})_{i,j=1}^3$ , $B=(b_{ij})_{i,j=1}^3$ . Since the integrands are entire analytic functions of $\omega$ , the integrals in $I_0(s)$ and $I_1(s)$ with respect to $\omega$ can be taken over any path joining points $0$ and $s$ of the complex plane. Consequently, $I_0(s)$ and $I_1(s)$ are entire analytic functions of $s=s_1+\textrm{i}s_2$ .
The following lemma gives estimates of $I_0(s)$ and $I_1(s)$ . The proof employs the resolvent estimates in Proposition 4.1.
Lemma 4.4. Denote $S=\{z=x+\textrm{i}y\in \mathbb{C}\,: -\frac{\pi }{4}\lt \textrm{arg} z\lt \frac{\pi }{4}\}$ . Let $s=s_1+\textrm{i}s_2\in S$ . The following estimates hold:
Proof. We first show that $ \kappa (\omega ) = \sqrt{\omega ^2 + \textrm{i}\omega \sigma }$ is analytic for $\omega \in S$ . When $\omega = \omega _1 + \textrm{i}\omega _2 \in S$ the image of $\omega ^2 + \textrm{i}\sigma \omega$ satisfies
In fact, assume that $\omega \in S$ . Since
if $\omega ^2 + \textrm{i}\sigma \omega \in \textrm{i}({-}\infty, 0]$ , then we have
which gives $\omega _2 \leq -\frac{\sigma }{2}$ . Then, we have
which is in contradiction with the assumption that $\omega \in S$ where $\omega _1\geq |\omega _2|$ . Therefore, by choosing the branch cut of $\sqrt{z}$ to be $z\in \mathbb C\backslash \textrm{i}({-}\infty, 0]$ we obtain that $ \kappa (\omega ) = \sqrt{\omega ^2 + \textrm{i}\omega b}$ is analytic for $\omega \in S$ .
Let $\kappa (\omega ) = \kappa _1(\omega ) + \textrm{i}\kappa _2(\omega )$ . A direct calculation gives $| \kappa _2(\omega )|^2 \leq (1 + \sqrt{2})\Big (\omega _1 + \frac{\sigma }{4}\Big )^2$ for $\omega \in S$ . Consequently, by the resolvent estimates in Proposition 4.1 we have that for $j = 0, 1, 2$
Then letting $\omega = s t, t\in [0, 1]$ , we obtain that
For $I_1(s)$ repeating the above arguments for $I_0(s)$ , we have that
The proof is completed.
The following lemma proved in [Reference Bao, Li and Zhao6] provides an estimate of the high frequency tail of $\|\mathbf{u}(x, \omega )\|^2_{\partial B_R}$ .
Lemma 4.5. Let $\mathbf{f}\in \mathcal C_Q$ . Then the following estimate holds:
The following lemma on analytic continuation is proved in [Reference Cheng, Isakov and Lu8] which will be useful in the subsequent analysis.
Lemma 4.6. Let $J(z)$ be analytic in $S=\{z=x+\textrm{i}y\in \mathbb{C}\,: -\frac{\pi }{4}\lt \textrm{arg} z\lt \frac{\pi }{4}\}$ and continuous in $\bar{S}$ satisfying
Then there exits a function $\beta (z)$ satisfying
such that
The following lemma is a direct consequence of Lemmas 4.4 and 4.6.
Lemma 4.7. Let $f\in \mathcal C_Q$ . Then there exists a function $\beta (s)$ satisfying
such that
where
Proof. It follows from Lemma 4.4 that there exists $C\gt 0$ such that
Moreover, we have
A direct application of Lemma 4.6 shows that there exists a function $\beta (s)$ satisfying (4.8) such that
which completes the proof.
In the following theorem, we present an increasing stability estimate for the inverse source problem following the arguments in [Reference Li and Yuan19].
Theorem 4.8. Let $\mathbf{u}(x, \omega )$ be the outgoing solution of the scattering problem (1.1) corresponding to the source $\mathbf{f} \in \mathcal{C}_Q$ . Then for $\epsilon$ sufficiently small the following estimate holds:
where
Proof. We can assume that $\epsilon \lt e^{-1}$ , otherwise the estimate is obvious. Let
If $2^{\frac{1}{4}}((C+3)\pi )^{\frac{1}{3}}K^{\frac{1}{3}} \lt |\ln \epsilon |^{\frac{1}{4}}$ , then we have from Lemma 4.7 that
Noting
we have
Using the elementary inequality
we get
If $|\ln \epsilon |^{\frac{1}{4}}\leq 2^{\frac{1}{4}}((C+3)\pi )^{\frac{1}{3}}K^{\frac{1}{3}}$ , then $s=K$ . We have that
Here, we have used the fact that
Hence, we obtain from Lemma 4.5 and (4.11) that
By Lemma 4.2, we have
Since $K^{\frac{2}{3}}|\ln \epsilon |^{\frac{1}{4}}\leq K^2 |\ln \epsilon |^{\frac{3}{2}}$ when $K\gt 1$ and $|\ln \epsilon |\gt 1$ , we finish the proof and obtain the stability estimate (4.9).
The stability estimate (4.9) consists of two parts: the first part is the Lipschitz type of data discrepancy and the second part is the high frequency tail of the source function. As the upper bound $K$ of the frequency increases, the stability estimate (4.9) tends to a Lipschitz-type stability which suggests that the inverse source problem becomes more stable when data of higher frequency are used. It also shows that the stability deteriorates if the attenuation $\sigma$ becomes larger.
5. Useful decay estimates for acoustic waves
To justify the Fourier transform in Remark 4.3, we need to prove some decay estimates for the solution $\mathbf{U}$ to the time-domain initial-valued elastic wave (3.1). As mentioned in Remark 4.3, in order to obtain the decay estimates of the solution to the time-domain initial-valued elastic wave (3.1), we just need to prove decay estimates for the dumped acoustic wave equation since we have the Helmholtz decomposition (3.2). In this section, we will prove some decay estimates which can guarantee that the Fourier transform for the solution of the dumped acoustic wave equation is well defined (see Remarks 5.2 and 5.3).
We consider the following initial-valued damped acoustic wave equation in $\mathbb R^3$
where $f(x)\in L^1\left(\mathbb R^3\right)\cap H^s\left(\mathbb R^3\right)$ . The regularity assumption $H^s\left(\mathbb R^3\right)$ for $f(x)$ will be specified later. Since the equation in (5.1) has constant coefficients, the decay estimates of the solution $U(x, t)$ can be derived by the standard Fourier transform.
Applying the Fourier transform to the solution $U(x, t)$ to (5.1) with respect to the spatial variable $x$ , we obtain that
where $\mathcal{F}^{-1}$ denotes the inverse Fourier transform, the multiplies $m_\sigma (t, \xi )$ takes the form
and $\hat{f}(\xi )$ is the Fourier transform of $f$ defined as follows:
Assume that $\sqrt{\sigma ^2 - 4|\xi |^2} = \textrm{i} \sqrt{4|\xi |^2 - \sigma ^2}$ when $|\xi |^2\gt \frac{\sigma ^2}{4}$ . Then (5.2) becomes
Notice from the representation of the multiplies $m_\sigma (t, \xi )$ above that the solution $U(x, t)$ behaves as a “parabolic type” of $e^{-t\Delta } f$ in the low frequency, while for the high frequency part it behaves like a “dispersive type” of $e^{\textrm{i}t\Delta } f$ .
Theorem 5.1. Let $U(x, t)$ be the solution of (5.1). Then $U(x, t)$ satisfies the decay estimate
where $j\in \mathbb N$ , $\alpha$ is a multi-index vector in $\mathbb N^3$ such that $\partial _x^\alpha = \partial _{x_1}^{\alpha _1}\,\partial _{x_2}^{\alpha _2}\,\partial _{x_3}^{\alpha _3}$ , $s\gt j + |\alpha | + \frac{1}{2}$ and $c\gt 0$ is some positive constant. In particular, for $|\alpha | = j = 0$ , the following estimate holds:
Remark 5.2. The estimate (5.4) provides a time decay of the order $O((1 + t)^{-\frac{3}{2}})$ for $U(x, t)$ uniformly for all $x\in \mathbb R^3$ , which gives
Hence, letting $U(x, t) = 0$ when $t\lt 0$ then $U(x, t)$ has a Fourier transform $\hat{U}(x, k) \in L^2(\mathbb R)$ for each $x\in \mathbb R^3$ . Moreover, the following Plancherel equality holds:
Remark 5.3. To study the inverse source problem, it suffices to assume that $f\in H^s\left(\mathbb R^3\right), s\geq 5$ . In this case, it follows from the above theorem that both $\partial _t U(x, t)$ and $\partial _{tt}\nabla U(x, t)$ are continuous functions. Moreover, we have from (5.3) that the following estimate holds:
Proof. Without loss of generality, we may assume that $\sigma = 1$ , and then
First we prove (5.3) for $j = 0$ . Choose $\chi \in C_0^\infty \left(\mathbb R^3\right)$ such that $\textrm{supp}\chi \subset B(0, \frac{1}{4})$ and $\chi (\xi ) = 1$ for $|\xi |\leq \frac{1}{16}$ . Let
For $U_1(x, t)$ , since $\sqrt{1 - 4|\xi |^2}\leq 1 - 2|\xi |^2$ when $0\leq |\xi | \leq \frac{1}{4}$ , we have for $|\xi |\leq \frac{1}{4}$ that
For each $x\in \mathbb R^3$ , we have
which gives
Since
and $\|\hat{f}\|_{L^\infty \left(\mathbb R^3\right)} \lesssim \|f\|_{L^1\left(\mathbb R^3\right)}$ , we obtain
To estimate $U_2(x, t)$ , noting
we have from Plancherel’s theorem that
There exists a positive constant $c$ such that
Hence, when $|\xi |\geq \frac{1}{16}$ we have
It follows from (5.6) that
On the other hand, by Sobolev’s theorem, we have for $p\gt \frac{3}{2}$ that
More generally, for any $\alpha \in \mathbb N^3$ it holds that
which leads to
Here $s = p - 1 + |\alpha |\gt |\alpha | + \frac{1}{2}$ by choosing $p \gt \frac{3}{2}$ . Combining the estimate (5.5) with (5.7) yields (5.3) for $j = 0.$
Next we consider the general case with $j\neq 0$ . Noting
we obtain from direct calculations that
where $\left (\begin{array}{c} l\\ j \end{array}\right )=\frac{j!}{(j-l)!l!}$ . Hence, we can write $\partial _t^j U(x, t)$ as
For each $0\leq l \leq j, \, j\neq 0$ , using similar arguments for the case $j = 0$ we obtain
for $s\gt l + |\alpha | - \frac{1}{2}$ . Combining (5.8) and (5.9), we obtain the general estimate (5.3).
6. Conclusion
We have presented an increasing stability result for the inverse source problem of the elastic wave equation with attenuation. A key ingredient in the proof is the use of the scattering theory to analyse the resolvent of the elliptic operator. The advantage of this method is that it can be used to study the case of a variable attenuation coefficient. For instance, consider the following elastic wave equation:
where $V$ is a bounded potential function. Formally, one has from the classical resolvent identity that
where $\mathbf I$ is the identity operator. The operator $\mathbf{I} + (\textrm{i}\omega \sigma (x) + V)\mathbf{R}_0(\omega )$ is invertible if the attenuation coefficient $\sigma (x)$ is assumed to be small. Indeed, for small $\sigma (x)$ using the free resolvent estimate (4.2) one has for $\Im \omega \gt 0$ sufficiently large that
which gives by the Neumann series argument that the operator $\mathbf{I} + (\textrm{i}\omega \sigma (x) + V)\mathbf{R}_0(\omega )$ is invertible. As a consequence, using the standard perturbation argument in scattering theory one may prove a similar resolvent estimates as Proposition 4.1 for the resolvent $({-}\Delta ^* - \textrm{i}\omega \sigma (x) - \omega ^2)^{-1}$ with variable attenuation. An exact observability may also be derived using Carleman estimates for wave equation. A more challenging problem is to remove the smallness assumption. We hope to report the progress on this problem elsewhere.
Acknowledgements
The authors sincerely thank the anonymous referees for their thorough reading and invaluable comments.
The research of GY was supported in part by NSFC (No. 11,771,074) and National Key R&D Program of China (No. 2020YFA0714102). The research of YZ was supported in part by NSFC (No. 12,001,222).
Conflict of interest
None.