Abstract:We consider the inverse problem, in two and three dimensions, of identifying elastic cracks embedded in an inhomogeneous anisotropic elastic medium using point sources. The observable data is given by the near-field measurements of the outgoing Green's function for the related stationary system. We give a reconstruction algorithm for this inverse problem.
“…The following key lemma verifies that the Dirichlet-to-Neumann map can be constructed by G(x, y) on |x| = |y| = R. Lemma 2 (Nakamura et al [13,Lemma 5.3]) − e is injective and ( − e ) = I .…”
Section: Determination Of Coefficientsmentioning
confidence: 91%
“…The problem is the same as Inverse Problem 2 on p. 209 of Reference [8] and Section 5.2 on p. 608 of Reference [13]. We will not repeat the proof again and refer the readers to the above articles.…”
Section: Determination Of Coefficientsmentioning
confidence: 92%
“…However, the approaches developed in References EXPANSION THEOREM FOR 2D ELASTIC WAVES 1859 [7,8] essentially rely on an Atkinson-Wilcox-type expansion for three-dimensional Helmholtz equation. Having an Atkinson-Wilcox-type expansion for two-dimensional elastic wave at hand, the same arguments in References [7,8,12,13] can be applied to the two-dimensional inverse elastic wave scattering.…”
mentioning
confidence: 97%
“…Step 2: As the same arguments in Reference [13] where the inhomogeneous anisotropic elasticity system is considered, we show that the Dirichlet-to-Neumann map on *B R can be constructed by the measurements G(x, y) on |x| = |y| = R. For the reader's convenience, the similar notations in Reference [13] will be used. Define the Dirichlet-to-Neumann map : g(x) = −…”
SUMMARYWe prove an Atkinson-Wilcox-type expansion for two-dimensional elastic waves in this paper. The approach developed on the two-dimensional Helmholtz equation will be applied in the proof. When the elastic fields are involved, the situation becomes much harder due to two wave solutions propagating at different phase velocities. In the last section, we give an application about the reconstruction of an obstacle from the scattering amplitude.
“…The following key lemma verifies that the Dirichlet-to-Neumann map can be constructed by G(x, y) on |x| = |y| = R. Lemma 2 (Nakamura et al [13,Lemma 5.3]) − e is injective and ( − e ) = I .…”
Section: Determination Of Coefficientsmentioning
confidence: 91%
“…The problem is the same as Inverse Problem 2 on p. 209 of Reference [8] and Section 5.2 on p. 608 of Reference [13]. We will not repeat the proof again and refer the readers to the above articles.…”
Section: Determination Of Coefficientsmentioning
confidence: 92%
“…However, the approaches developed in References EXPANSION THEOREM FOR 2D ELASTIC WAVES 1859 [7,8] essentially rely on an Atkinson-Wilcox-type expansion for three-dimensional Helmholtz equation. Having an Atkinson-Wilcox-type expansion for two-dimensional elastic wave at hand, the same arguments in References [7,8,12,13] can be applied to the two-dimensional inverse elastic wave scattering.…”
mentioning
confidence: 97%
“…Step 2: As the same arguments in Reference [13] where the inhomogeneous anisotropic elasticity system is considered, we show that the Dirichlet-to-Neumann map on *B R can be constructed by the measurements G(x, y) on |x| = |y| = R. For the reader's convenience, the similar notations in Reference [13] will be used. Define the Dirichlet-to-Neumann map : g(x) = −…”
SUMMARYWe prove an Atkinson-Wilcox-type expansion for two-dimensional elastic waves in this paper. The approach developed on the two-dimensional Helmholtz equation will be applied in the proof. When the elastic fields are involved, the situation becomes much harder due to two wave solutions propagating at different phase velocities. In the last section, we give an application about the reconstruction of an obstacle from the scattering amplitude.
“…The domain D stands for the region of the inclusion or cavity embedded in Ω. In the degenerate case where the domain D represents the crack, the inverse problem of identifying D by near-field measurements was consider in [16] and [17]. To simply our presentation, we will not discuss this matter here.…”
Section: Applications To Inverse Problemsmentioning
Abstract. Under some generic assumptions we prove the unique continuation property for the two-dimensional inhomogeneous anisotropic elasticity system. Having established the unique continuation property, we then investigate the inverse problem of reconstructing the inclusion or cavity embedded in a plane elastic body with inhomogeneous anisotropic medium by infinitely many localized boundary measurements.
Let μ m Ω,b be the higher order commutator generated by Marcinkiewicz integral μ Ω and a BMO(R n ) function b(x). In this paper, we will study the continuity of μ Ω and μ m Ω,b on homogeneous Morrey-Herz spaces.
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