direct and inverse elastic scattering problems for
play

Direct and Inverse Elastic Scattering Problems for Diffraction - PowerPoint PPT Presentation

Weierstrass Institute for Applied Analysis and Stochastics Direct and Inverse Elastic Scattering Problems for Diffraction Gratings Johannes Elschner & Guanghui Hu Mohrenstrasse 39 10117 Berlin Germany Tel. +49 30 20372 0


  1. Weierstrass Institute for Applied Analysis and Stochastics Direct and Inverse Elastic Scattering Problems for Diffraction Gratings Johannes Elschner & Guanghui Hu Mohrenstrasse 39 · 10117 Berlin · Germany · Tel. +49 30 20372 0 · www.wias-berlin.de · PICOF’12, April 4, 2012

  2. Content Direct and inverse elastic scattering problems in periodic structures 1 Direct scattering problem: uniqueness and existence 2 3 Inverse scattering problem: uniqueness for polygonal gratings 4 Inverse scattering problem: a two-step algorithm Direct and Inverse Elastic Scattering Problems for Diffraction Gratings · PICOF’12, April 4, 2012 · Page 2 (27)

  3. Elastic scattering by diffraction gratings Direct and Inverse Elastic Scattering Problems for Diffraction Gratings · PICOF’12, April 4, 2012 · Page 3 (27)

  4. Elastic scattering by periodic structures: application in geophysics Characterize fractures using elastic waves in search for gas and liquids Direct and Inverse Elastic Scattering Problems for Diffraction Gratings · PICOF’12, April 4, 2012 · Page 4 (27)

  5. Applications � Geophysics -search for oil, gas and ore bodies � Seismology -investigate earthquakes Direct and Inverse Elastic Scattering Problems for Diffraction Gratings · PICOF’12, April 4, 2012 · Page 5 (27)

  6. Applications � Geophysics -search for oil, gas and ore bodies � Seismology -investigate earthquakes � Nondestructive Testings (NDT) - detect cracks and flaws in concrete structures, such as bridges, buildings, dams, highways, etc. Direct and Inverse Elastic Scattering Problems for Diffraction Gratings · PICOF’12, April 4, 2012 · Page 5 (27)

  7. Applications � Geophysics -search for oil, gas and ore bodies � Seismology -investigate earthquakes � Nondestructive Testings (NDT) - detect cracks and flaws in concrete structures, such as bridges, buildings, dams, highways, etc. Problems: � Understand the reflection and transmission of elastic waves through an interface � Design efficient inversion algorithms using elastic waves Direct and Inverse Elastic Scattering Problems for Diffraction Gratings · PICOF’12, April 4, 2012 · Page 5 (27)

  8. Basic assumptions � The periodic surface Λ is invariant in one direction and 2 π -periodic in another direction, φ = 0 . � The elastic medium above Λ is homogeneous, isotropic with the Lamé constants λ , µ . The mass density ρ = 1 . � The elastic displacement-field is time-harmonic, U ( t , x ) = u ( x ) e − i ω t . Direct and Inverse Elastic Scattering Problems for Diffraction Gratings · PICOF’12, April 4, 2012 · Page 6 (27)

  9. Direct problems � Navier equation in 2D (case φ = 0 ): ( ∆ ∗ + ω 2 ) u = 0 ∆ ∗ : = µ ∆ +( λ + µ ) grad div , Ω Λ , in u = u in + u sc Ω Λ . in Angular frequency: ω > 0 Lamé constants: µ > 0 , λ + µ > 0 � Compressional wave number: k p : = ω / 2 µ + λ Shear wave number: k s : = ω / √ µ Direct and Inverse Elastic Scattering Problems for Diffraction Gratings · PICOF’12, April 4, 2012 · Page 7 (27)

  10. Direct problems � Navier equation in 2D (case φ = 0 ): ( ∆ ∗ + ω 2 ) u = 0 ∆ ∗ : = µ ∆ +( λ + µ ) grad div , Ω Λ , in u = u in + u sc Ω Λ . in Angular frequency: ω > 0 Lamé constants: µ > 0 , λ + µ > 0 � Compressional wave number: k p : = ω / 2 µ + λ Shear wave number: k s : = ω / √ µ Incident angle: θ ∈ ( − π / 2 , π / 2 ) Incident plane pressure wave: u in p ( x ) = ˆ θ exp ( ik p x · ˆ ˆ θ ) , θ : = ( sin θ , − cos θ ) , x = ( x 1 , x 2 ) Direct and Inverse Elastic Scattering Problems for Diffraction Gratings · PICOF’12, April 4, 2012 · Page 7 (27)

  11. Direct problems � Navier equation in 2D (case φ = 0 ): ( ∆ ∗ + ω 2 ) u = 0 ∆ ∗ : = µ ∆ +( λ + µ ) grad div , Ω Λ , in u = u in + u sc Ω Λ . in Direct and Inverse Elastic Scattering Problems for Diffraction Gratings · PICOF’12, April 4, 2012 · Page 8 (27)

  12. Direct problems � Navier equation in 2D (case φ = 0 ): ( ∆ ∗ + ω 2 ) u = 0 ∆ ∗ : = µ ∆ +( λ + µ ) grad div , Ω Λ , in u = u in + u sc Ω Λ . in � Quasi-periodicity: u ( x 1 + 2 π , x 2 ) = exp ( 2 i απ ) u ( x 1 , x 2 ) , α : = k p sin θ . Direct and Inverse Elastic Scattering Problems for Diffraction Gratings · PICOF’12, April 4, 2012 · Page 8 (27)

  13. Direct problems � Navier equation in 2D (case φ = 0 ): ( ∆ ∗ + ω 2 ) u = 0 ∆ ∗ : = µ ∆ +( λ + µ ) grad div , Ω Λ , in u = u in + u sc Ω Λ . in � Quasi-periodicity: u ( x 1 + 2 π , x 2 ) = exp ( 2 i απ ) u ( x 1 , x 2 ) , α : = k p sin θ . � Dirichlet boundary condition on the grating profile: u = 0 Λ . on Direct and Inverse Elastic Scattering Problems for Diffraction Gratings · PICOF’12, April 4, 2012 · Page 8 (27)

  14. Direct problems � Navier equation in 2D (case φ = 0 ): ( ∆ ∗ + ω 2 ) u = 0 ∆ ∗ : = µ ∆ +( λ + µ ) grad div , Ω Λ , in u = u in + u sc Ω Λ . in � Quasi-periodicity: u ( x 1 + 2 π , x 2 ) = exp ( 2 i απ ) u ( x 1 , x 2 ) , α : = k p sin θ . � Dirichlet boundary condition on the grating profile: u = 0 Λ . on � An appropriate radiation condition imposed on u sc as x 2 → ∞ . Direct and Inverse Elastic Scattering Problems for Diffraction Gratings · PICOF’12, April 4, 2012 · Page 8 (27)

  15. Rayleigh Expansion Radiation Condition (RERC) u sc = ∇ u p + − − → ( ∆ + k 2 ( ∆ + k 2 curl u s , p ) u p = 0 , s ) u s = 0 Direct and Inverse Elastic Scattering Problems for Diffraction Gratings · PICOF’12, April 4, 2012 · Page 9 (27)

  16. Rayleigh Expansion Radiation Condition (RERC) u sc = ∇ u p + − − → ( ∆ + k 2 ( ∆ + k 2 curl u s , p ) u p = 0 , s ) u s = 0 � Radiation condition � � α n u sc ( x ) ∑ = exp ( i α n x 1 + i β n x 2 ) A p , n β n n ∈ Z � � γ n + ∑ exp ( i α n x 1 + i γ n x 2 ) A s , n − α n n ∈ Z for x 2 > Λ + : = max ( x 1 , x 2 ) ∈ Λ x 2 . Here,  � k 2 p − α 2 | α n | ≤ k p if  n α n : = α + n , β n = β n ( θ ) : = � α 2 n − k 2 if | α n | > k p , i  p � � k 2 s − α 2 if | α n | ≤ k s n γ n = γ n ( θ ) : = � α 2 n − k 2 i if | α n | > k s . s The constants A p , n , A s , n ∈ C are called the Rayleigh coefficients. Direct and Inverse Elastic Scattering Problems for Diffraction Gratings · PICOF’12, April 4, 2012 · Page 9 (27)

  17. Direct and inverse scattering problems Direct Problem (DP) Given Λ ⊂ R 2 and u in , find u = u in + u sc ∈ H 1 loc ( Ω Λ ) 2 under the boundary, quasi-periodicity and radiation conditions. Direct and Inverse Elastic Scattering Problems for Diffraction Gratings · PICOF’12, April 4, 2012 · Page 10 (27)

  18. Direct and inverse scattering problems Direct Problem (DP) Given Λ ⊂ R 2 and u in , find u = u in + u sc ∈ H 1 loc ( Ω Λ ) 2 under the boundary, quasi-periodicity and radiation conditions. � Uniqueness and existence of solutions � Numerical solutions Direct and Inverse Elastic Scattering Problems for Diffraction Gratings · PICOF’12, April 4, 2012 · Page 10 (27)

  19. Direct and inverse scattering problems Direct Problem (DP) Given Λ ⊂ R 2 and u in , find u = u in + u sc ∈ H 1 loc ( Ω Λ ) 2 under the boundary, quasi-periodicity and radiation conditions. � Uniqueness and existence of solutions � Numerical solutions Inverse Problem (IP) Given incident field u in ( x ; θ ) and the near-field data u ( x 1 , b ; θ ) , determine the unknown scattering surface Λ . Direct and Inverse Elastic Scattering Problems for Diffraction Gratings · PICOF’12, April 4, 2012 · Page 10 (27)

  20. Direct and inverse scattering problems Direct Problem (DP) Given Λ ⊂ R 2 and u in , find u = u in + u sc ∈ H 1 loc ( Ω Λ ) 2 under the boundary, quasi-periodicity and radiation conditions. � Uniqueness and existence of solutions � Numerical solutions Inverse Problem (IP) Given incident field u in ( x ; θ ) and the near-field data u ( x 1 , b ; θ ) , determine the unknown scattering surface Λ . � Can we identify Λ uniquely ? � How to recover Λ numerically ? Direct and Inverse Elastic Scattering Problems for Diffraction Gratings · PICOF’12, April 4, 2012 · Page 10 (27)

  21. Solvability results on the direct scattering problem Theorem � If the grating profile Λ is a Lipschitz curve , then there always exists a solution of (DP). Direct and Inverse Elastic Scattering Problems for Diffraction Gratings · PICOF’12, April 4, 2012 · Page 11 (27)

  22. Solvability results on the direct scattering problem Theorem � If the grating profile Λ is a Lipschitz curve , then there always exists a solution of (DP). � Uniqueness holds for small frequencies, or for all frequencies excluding a discrete set with the only accumulation point at infinity. Direct and Inverse Elastic Scattering Problems for Diffraction Gratings · PICOF’12, April 4, 2012 · Page 11 (27)

  23. Solvability results on the direct scattering problem Theorem � If the grating profile Λ is a Lipschitz curve , then there always exists a solution of (DP). � Uniqueness holds for small frequencies, or for all frequencies excluding a discrete set with the only accumulation point at infinity. � If Λ is the graph of a Lipschitz function, then for any frequency ω > 0 , there exists a unique solution of (DP). Direct and Inverse Elastic Scattering Problems for Diffraction Gratings · PICOF’12, April 4, 2012 · Page 11 (27)

Download Presentation
Download Policy: The content available on the website is offered to you 'AS IS' for your personal information and use only. It cannot be commercialized, licensed, or distributed on other websites without prior consent from the author. To download a presentation, simply click this link. If you encounter any difficulties during the download process, it's possible that the publisher has removed the file from their server.

Recommend


More recommend