Multidimensional inverse Problems and Completeness of the Products of Solutions to PDE
نویسنده
چکیده
A method is given for proving uniqueness theorems for some inverse problems. The method is based on a result on completeness of the products of solutions to PDE. As an example, the following uniqueness theorems are proved: (1) the scattering amplitude A(fY, 0, k) known for all W, BE Sz and a fixed k > 0 determines the compactly supported q(x)~ L*(D) uniquely; (2) the surface data u(x,y, k) known for all x, y E P := {x: x, = 0) and a tixed k > 0 determine the compactly supported u(x) E L’(D), D c RT := {x: xj < 0) uniquely. Here [V2 + k2 + k%(x)] u(x, y, k) = -6(x-y) in R’; (3) the surface data u(x, y, k) known for all x, ye P and ail 0~ k < k,, k,zO is arbitrarily small; determine a,(x), j= 1, 2, uniquely. Here V2u + k2u + k2a,(x) + V. (a2(x) VU) = -6(x-y) in R’, a, E L2(D), a, E H*(D); the same conclusion holds if the surface data are known at two distinct frequencies. (4) The surface data u(x, y, k) known for all x, yo P and all k > 0 determine v(x) and h(k) uniquely. Here [V’+ k2 + k%(x)] u = -6(x-y) h(k), V(X)E L’(D), h(k) is Fourier transform of a wavelet of compact support; (5) the conductivity U(X)E W2.2(D), U(X)> c>O, is uniquely determined by the measurements of u and uuN on dD. Here N is the outward normal to dD, D c R’ is a bounded domain with a smooth boundary dD, V. (a(x)Vu)=O in D. (6) Necessary and sufficient conditions are given for a function A(B’, 6, k), B’, 6 ES, k > 0 is fixed, to be the scattering amplitude corresponding to a local potential from a certain class.
منابع مشابه
Completeness of the products of solutions of PDE and inverse problems
A brief summary of the author’s results is given and some new results are presented.
متن کاملAn inverse problem for a heat equation with piecewise- constant thermal conductivity
The governing equation is ut= a x ux x, 0 x 1, t 0, u x ,0 =0, u 0, t =0, a 1 u 1, t = f t . The extra data are u 1, t =g t . It is assumed that a x is a piecewise-constant function and f 0. It is proved that the function a x is uniquely defined by the above data. No restrictions on the number of discontinuity points of a x and on their locations are made. The number of discontinuity points is ...
متن کامل2D inversion of gravity data in bedrock identification (case study: a part of Qotrum plain in Yazd province)
Introduction The gravity method measures the vertical component of the acceleration at the Earth’s surface. The earth’s gravity field is affected by the density of different rocks and structures. Therefore, this method can be used in mineral exploration or studying the subsurface cavities and structures such as bedrocks, channels, and dikes. Inverse modeling is useful in understanding the p...
متن کاملInverse Laplace transform method for multiple solutions of the fractional Sturm-Liouville problems
In this paper, inverse Laplace transform method is applied to analytical solution of the fractional Sturm-Liouville problems. The method introduces a powerful tool for solving the eigenvalues of the fractional Sturm-Liouville problems. The results how that the simplicity and efficiency of this method.
متن کاملA numerical Algorithm Based on Chebyshev Polynomials for Solving some Inverse Source Problems
In this paper, two inverse problems of determining an unknown source term in a parabolic equation are considered. First, the unknown source term is estimated in the form of a combination of Chebyshev functions. Then, a numerical algorithm based on Chebyshev polynomials is presented for obtaining the solution of the problem. For solving the problem, the operational matrices of int...
متن کامل