STABILITY ESTIMATES FOR THE INVERSE FRACTIONAL CONDUCTIVITY PROBLEM GIOVANNI COVI JESSE RAILO TEEMU TYNI AND PHILIPP ZIMMERMANN

2025-05-03 0 0 611.76KB 34 页 10玖币
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STABILITY ESTIMATES FOR THE INVERSE
FRACTIONAL CONDUCTIVITY PROBLEM
GIOVANNI COVI, JESSE RAILO, TEEMU TYNI, AND PHILIPP ZIMMERMANN
Abstract. We study the stability of an inverse problem for the frac-
tional conductivity equation on bounded smooth domains. We obtain
a logarithmic stability estimate for the inverse problem under suitable
a priori bounds on the globally defined conductivities. The argument
has three main ingredients: 1. the logarithmic stability of the related
inverse problem for the fractional Schr¨odinger equation by R¨uland and
Salo; 2. the Lipschitz stability of the exterior determination problem;
3. utilizing and identifying nonlocal analogies of Alessandrini’s work on
the stability of the classical Calder´on problem. The main contribution
of the article is the resolution of the technical difficulties related to the
last mentioned step. Furthermore, we show the optimality of the loga-
rithmic stability estimates, following the earlier works by Mandache on
the instability of the inverse conductivity problem, and by R¨uland and
Salo on the analogous problem for the fractional Schr¨odinger equation.
1. Introduction
Stability estimates for inverse problems give important information on
theoretical limitations of different imaging techniques appearing in various
medical, engineering, and scientific applications. They are also useful for
development of numerical methods. A common feature of many inverse
problems is that they are ill-posed, which means that small measurement
errors may lead to large errors in the reconstructed images. One of the most
popular model problems is the inverse conductivity problem, known as the
Calder´on problem [Cal80], where one aims to recover the conductivity γfrom
the voltage/current measurements on the boundary Ω of an object Ω. In
mathematical terms, one defines the data as a Dirichlet-to-Neumann (DN)
map Λγ:f7→ γνuf|, where νis the outer boundary normal derivative,
the electric potential ufis the unique solution of the boundary value problem
div(γu) = 0 in ,
u=fon ,
and the voltage fis the given Dirichlet boundary condition. The Calder´on
problem asks to recover γfrom the knowledge of Λγ, which corresponds
to knowing the outer normal fluxes (i.e. boundary currents) generated by
imposing different boundary voltages f.
Date: October 6, 2022.
2020 Mathematics Subject Classification. Primary 35R30; secondary 26A33, 42B37,
46F12.
Key words and phrases. Fractional Laplacian, fractional gradient, Calder´on problem,
conductivity equation.
1
arXiv:2210.01875v1 [math.AP] 4 Oct 2022
INVERSE FRACTIONAL CONDUCTIVITY PROBLEM 2
The Calder´on problem serves both as a mathematical model for electri-
cal impedance tomography [Uhl14], and more generally as a prototypical
model for inverse problems. In fact, methods and techniques originally
developed for the classical Calder´on problem have applications in a wide
range of other inverse problems, among which the anisotropic Calder´on prob-
lem [APL05, DSFKSU09], hyperbolic problems [RS88, Sun90] and inverse
problems related to the theory of elasticity [NU94]. The work of Sylvester
and Uhlmann proved a fundamental uniqueness theorem for the classical
Calder´on problem in dimension n3, using a reduction to an analogous
problem for the Schr¨odinger equation and constructing the so called complex
geometrical optics (or CGO) solutions [SU87]. Nachman established a re-
construction method [Nac88], and Astala–P¨aiv¨arinta showed a fundamental
uniqueness result when n= 2 using methods from complex analysis and a
reduction to the Beltrami equation [AP06]. We recall the stability theorem
of Alessandrini [Ale88], which is an important motivation for our present
work:
Theorem 1.1 (Alessandrini [Ale88, Theorem 1]).Let be a bounded do-
main in Rn,n3, with Cboundary . Given sand E,s > n/2,E > 0,
let γ1, γ2be any two functions in Hs+2(Ω) satisfying the following conditions
E1γ`(x),for every xin , ` = 1,2.
kγ`kHs+2(Ω) E, ` = 1,2.
The following estimate holds 1
kγ1γ2kL(Ω) CEω(kΛγ1Λγ2kH1/2(Ω)H1/2(Ω)),
where the function ωis such that
ω(t)≤ |log t|δ,for every t, 0<t<1/e,
and δ,0< δ < 1, depends only on nand s.
Mandache showed that the logarithmic stability estimates are optimal
up to the constants C, δ [Man01]. The works of Alessandrini and Man-
dache therefore show that the classical Calder´on problem is ill-posed and
furthermore accurately characterize this phenomenon. Mandache’s work
was recently systematically studied and extended by Koch, R¨uland and Salo
[KRS21] to many different settings. For the other recent works on the sta-
bility of the classical Calder´on problem, we point to the following works
[CDR16, CS14], where stability under partial data is obtained, and stability
for recovery of anisotropic conductivies is considered. Under certain a priori
assumptions, such as piecewise constant conductivities, the stronger result
of Lipschitz stability holds [AV05]. Lipschitz stability is also possible with a
finite number of measurements [AS22]. In a different direction, we mention
[AN19] for an application of stability to the statistical Calder´on problem.
In the present work, we study the stability properties of an inverse prob-
lem for a nonlocal analogue of the classical Calder´on problem. There has
been growing interest towards establishing the theory of inverse problems for
elliptic nonlocal variable coefficient operators. Other recent studies include
1Given a bounded linear mapping A:XYbetween two Banach spaces, we denote
its operator norm by kAkXY.
INVERSE FRACTIONAL CONDUCTIVITY PROBLEM 3
inverse problems for the fractional powers of elliptic second order operators
[GU21] and inverse problems for source-to-solutions maps related to frac-
tional geometric operators on manifolds [FGKU21, QU22]. We note that
the exterior value inverse problems considered in [GU21] for the operators
(div(γ))s, 0 <s<1, generated by the heat semigroups, give another
possibility to define a nonlocal conductivity equation which is presumably
different from the equation we study here.
Let s(0,1) and consider the exterior value problem for the fractional
conductivity equation
divsγsu) = 0 in ,
u=fin Ωe,
(1)
where Ωe:=Rn\Ω is the exterior of the domain Ω and Θγ:R2nRn×nis
the matrix defined as Θγ(x, y):=γ1/2(x)γ1/2(y)1n×n. We say uHs(Rn)
is a (weak) solution of (1) if ufe
Hs(Ω) and
Bγ(u, φ) := Cn,s
2ˆR2n
γ1/2(x)γ1/2(y)
|xy|n+2s(u(x)u(y))(φ(x)φ(y)) dxdy = 0
holds for all φC
c(Ω). For all fX:=Hs(Rn)/e
Hs(Ω) in the abstract
trace space there is a unique weak solutions ufHs(Rn) of the fractional
conductivity equation (1). The fractional conductivity operator converges in
the sense of distributions to the classical conductivity operator when applied
to sufficiently regular functions when s1 [Cov20, Lemma 4.2].
The exterior DN map Λγ:XXis defined by
hΛγf, gi:=Bγ(uf, g).
The inverse problem for the fractional conductivity equation asks to recover
the conductivity γfrom Λγ, which maps as Λγ:Hs(Ωe)Hs
e(Rn) in
the case of Lipschitz domains. We define mγ:=γ1/21 and call it the
background deviation of γ. Let Ω Rnbe bounded in one direction and
n1. (We suppose additionally that 0 < s < 1/2 when n= 1.) The
uniqueness properties of this inverse problem are studied extensively in the
recent literature and the following list summarizes these advances:
Global uniqueness. If Weis an open nonempty set such that
γi|Ware continuous a.e., and miH2s, n
2s(Rn)Hs(Rn), j= 1,2,
then γ1=γ2if and only if Λγ1f|W= Λγ2f|Wfor all fC
c(W)
[CRZ22]. This result generalizes and expands the scope of the earlier
works [Cov20, RZ22b], which solved the inverse problem in certain
special cases by means of the fractional Liouville transformation.
This is a technique used to reduce the fractional conductivity equa-
tion to the fractional Schr¨odinger equation introduced in [GSU20],
which is in turn better understood.
Low regularity uniqueness. If Weis an open nonempty set such
that γi|Ware continuous a.e., and miHs,n/s(Rn), then γ1=γ2
if and only if Λγ1f|W= Λγ2f|Wfor all fC
c(W) [RZ22c]. This
uses a general UCP result for the fractional Laplacians in [KRZ22].
Counterexamples for disjoint measurement sets. For any nonempty
open disjoint sets W1, W2ewith dist(W1W2,Ω) >0 there
INVERSE FRACTIONAL CONDUCTIVITY PROBLEM 4
exist two different conductivities γ1, γ2L(Rn)C(Rn) such
that γ1(x), γ2(x)γ0>0, m1, m2Hs,n/s(Rn)Hs(Rn), and
Λγ1f|W2= Λγ2f|W2for all fC
c(W1) [RZ22c]. See the original
work on the construction of counterexamples with H2s, n
2s(Rn) regu-
larity assumptions in [RZ22a], with some limitations in the cases of
unbounded domains when n= 2,3.
In this article, we obtain a quantitative stability estimate for the global
inverse fractional conductivity problem on bounded smooth domains with
full data. This is based on one of the possible global uniqueness proofs
presented in [CRZ22, RZ22c]. There remain some nontrivial challenges in
order to obtain a quantitative version of the partial data uniqueness re-
sults in [CRZ22, RZ22c], as well as to remove the regularity/boundedness
assumptions of the domain even for the full data case.
We will next recall two earlier stability results related to the fractional
Calder´on problems. The first one considers the stable recovery of γin the
exterior, based on [CRZ22, Proposition 1.4]. The second one considers the
stability of the analogous inverse problem for the fractional Schr¨odinger
equation (∆)s+qdue to R¨uland and Salo [RS20, Theorem 1.2]. The
uniqueness properties of the Calder´on problem for large classes of fractional
Schr¨odinger type equations have been extensively studied starting from the
seminal work of [GSU20]. These include perturbations to the fractional pow-
ers of elliptic operators [GLX17], first order perturbations [CLR20], nonlin-
ear perturbations [LL22], higher order equations with local perturbations
[CMR21, CMRU22], quasilocal perturbations [Cov21], and general theory
for nonlocal elliptic equations [RS20, RZ22b].
In particular, the following results are needed in our proofs:
Theorem 1.2 ([RZ22c, Remark 3.3]).Let Rnbe a domain bounded
in one direction and 0<s<1. Assume that γ1, γ2L(Rn)satisfy
γ1(x), γ2(x)γ0>0, and are continuous a.e. in e. There exists a
constant C > 0depending only on ssuch that 2
kγ1γ2kL(Ωe)CkΛγ1Λγ2k.
Given a Sobolev multiplier qM(HsHs) (cf. [RS20, CMRU22]), we
define the following bilinear form
Bq(u, v):=ˆRn
(∆)s/2u(∆)s/2v dx +hqu, vi, u, v Hs(Rn),
related to the fractional Schr¨odinger operator (∆)s+q.
Theorem 1.3 ([RS20, Theorem 1.2]).Let Rnbe a bounded smooth
domain, 0< s < 1, and W1, W2be nonemtpy open sets. Assume that
for some δ, M > 0the potentials q1, q2Hδ, n
2s(Rn)have the bounds
kqjkHδ, n
2s(Ω) M, j = 1,2.
Suppose also that zero is not a Dirichlet eigenvalue for the exterior value
problem
(2) (∆)su+qju= 0,in
2Here and in the rest of paper we use the notation kAk:= kAkHs(Ωe)(Hs(Ωe)).
INVERSE FRACTIONAL CONDUCTIVITY PROBLEM 5
with u|e= 0, for j= 1,2. Then one has 3
kq1q2kLn
2s(Ω) ω(kΛq1Λq2ke
Hs(W1)(
e
Hs(W2))),
where Λqj:XXwith Λqjf, g:= Bqj(uf, g)is the DN map related to
the exterior value problem for equation (2), and ωis a modulus of continuity
satisfying
ω(x)C|log x|σ,0< x 1
for some Cand σdepending only on ,n,s,W1,W2,δand M.
Lemma 1.4 (Liouville reduction, [RZ22c, Lemma 3.9]).Let 0< s <
min(1, n/2). Assume that γL(Rn)with conductivity matrix Θγand
background deviation msatisfies γ(x)γ0>0and mHs,n/s(Rn). Let
qγ:= (∆)sm
γ1/2. Then there holds
hΘγsu, sφiL2(R2n)=h(∆)s/2(γ1/2u),(∆)s/2(γ1/2φ))iL2(Rn)
+hqγ(γ1/2u),(γ1/2φ)i
for all u, φ Hs(Rn).
In the sequel, we will call qγabove a potential.
1.1. Main results. We next state our main result, whose proof is based on
a reduction to Theorems 1.2 and 1.3.
Theorem 1.5. Let 0< s < min(1, n/2), > 0and assume that Rn
is a smooth bounded domain. Suppose that the the conductivities γ1, γ2
L(Rn)with background deviations m1, m2fulfill the following conditions:
(i) γ0γ1(x), γ2(x)γ1
0for some 0< γ0<1,
(ii) m1, m2H4s+2, n
2s(Rn)and there exists C1>0such that
(3) kmikH4s+2, n
2s(Rn)C1
for i= 1,2,
(iii) m1m2Hs(Rn)and there exists C2>0
(4) k(∆)smikL1(Ωe)C2
for i= 1,2.
If θ0(max(1/2,2s/n),1) and there holds kΛγ1Λγ2k31for some
0< δ < 1θ0
2, then we have
kγ1/2
1γ1/2
2kLq(Ω) ω(kΛγ1Λγ2k)
for all 1q2n
n2s, where ω(x)is a logarithmic modulus of continuity
satisfying
ω(x)C|log x|σ,for 0< x 1,
for some constants σ, C > 0depending only on s, , n, , C1, C2, θ0and γ0.
Remark 1.6. We make several comments about Theorem 1.5 and its as-
sumptions to clarify some interesting points:
3Note kAke
Hs(W1)(
e
Hs(W2))= sup{ |hAu1, u2i| ;kujkHs(Rn)= 1, ujC
c(Wj)}.
摘要:

STABILITYESTIMATESFORTHEINVERSEFRACTIONALCONDUCTIVITYPROBLEMGIOVANNICOVI,JESSERAILO,TEEMUTYNI,ANDPHILIPPZIMMERMANNAbstract.Westudythestabilityofaninverseproblemforthefrac-tionalconductivityequationonboundedsmoothdomains.Weobtainalogarithmicstabilityestimatefortheinverseproblemundersuitableaprioribou...

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