On uniqueness in the inverse conductivity problem with local data
نویسنده
چکیده
The inverse condictivity problem with many boundary measurements consists of recovery of conductivity coefficient a (principal part) of an elliptic equation in a domain Ω ⊂ R, n = 2, 3 from the Neumann data given for all Dirichlet data (Dirichlet-to-Neumann map). Calderon [5] proposed the idea of using complex exponential solutions to demonstrate uniqueness in the linearized inverse condictivity problem. Complex exponential solutions of elliptic equations have been introduced by Faddeev [7] for needs of inverse scattering theory. Sylvester and Uhlmann in their fundamental paper [19] attracted ideas from geometrical optics, constructed almost complex exponential solutions for the Schrödinger operator, and proved global uniqueness of a ( and of potential c in the Schrödinger equation) in the three-dimensional case. In the two-dimensional case the inverse conductivity problem is less overdetermined, and the Sylvester and Uhlmann method is not applicable, but one enjoys advantages of the methods of inverse scattering and of theory of complex variables. Using these methods Nachman [17] demonstrated uniqueness of a ∈ C(Ω̄) and Astala and Päivärinta [1] showed uniqueness of a ∈ L∞(Ω) which is a final result in the inverse conductivity problem in R with many measurements from the whole boundary. There is a known hypothesis (see for example, [11], Problem 5.3, [14], [20]) that the Dirichlet-to-Neumann map given at any (nonvoid open) part Γ of the boundary also uniquely determines conductivity coefficient or potential in the Schrödinger equation. This local boundary measurements model important
منابع مشابه
تخمین پارامترهای هیدرولیکی خاکهای دارای اشباعشدگی متغیر بهروش مدل سازی معکوس و بهرهگیری از دادههای توزیع مجدد رطوبت
Modeling of flow and transport processes in variably saturated porous media requires detailed knowledge of the soil hydraulic properties. The hydraulic properties to be determined by the inverse problem solution are the unsaturated hydraulic conductivity K(h) and the water retention curve θ(h). The inverse modeling approach assumes that both θ(h) and K(h) as well as transport parame...
متن کاملA Uniqueness Theorem of the Solution of an Inverse Spectral Problem
This paper is devoted to the proof of the unique solvability ofthe inverse problems for second-order differential operators withregular singularities. It is shown that the potential functioncan be determined from spectral data, also we prove a uniquenesstheorem in the inverse problem.
متن کاملThe uniqueness theorem for inverse nodal problems with a chemical potential
In this paper, an inverse nodal problem for a second-order differential equation having a chemical potential on a finite interval is investigated. First, we estimate the nodal points and nodal lengths of differential operator. Then, we show that the potential can be uniquely determined by a dense set of nodes of the eigenfunctions.
متن کاملOn inverse problem for singular Sturm-Liouville operator with discontinuity conditions
In this study, properties of spectral characteristic are investigated for singular Sturm-Liouville operators in the case where an eigen parameter not only appears in the differential equation but is also linearly contained in the jump conditions. Also Weyl function for considering operator has been defined and the theorems which related to uniqueness of solution of inverse proble...
متن کاملSolving Inverse Sturm-Liouville Problems with Transmission Conditions on Two Disjoint Intervals
In the present paper, some spectral properties of boundary value problems of Sturm-Liouville type on two disjoint bounded intervals with transmission boundary conditions are investigated. Uniqueness theorems for the solution of the inverse problem are proved, then we study the reconstructing of the coefficients of the Sturm-Liouville problem by the spectrtal mappings method.
متن کامل