scattered multi static array imaging and eigenvalue
play

Scattered multi-static array imaging and eigenvalue problems - PDF document

Scattered multi-static array imaging and eigenvalue problems Wagner B. Muniz Department of Mathematics Federal University of Santa Catarina (UFSC) w.b.muniz@ufsc.br Brazilian Mathematics Colloquium 2013 Inverse scattering (acoustics, EM) u


  1. Scattered multi-static array imaging and eigenvalue problems Wagner B. Muniz Department of Mathematics Federal University of Santa Catarina (UFSC) w.b.muniz@ufsc.br Brazilian Mathematics Colloquium 2013

  2. Inverse scattering (acoustics, EM) u s u i D u i ( x ) = known incident wave u s ( x ) = measured scattered wave incident u i + scattered u s = total field u Time-harmonic assumption: ω = frequency { u ( x ) e − i ωt } acoustics: p ( x, t ) = ℜ e , { ( E , H )( x ) e − i ωt } EM: ( E , H )( x, t ) = ℜ e 1

  3. Inverse scattering (acoustics, EM) u s i u D u i ( x ) = known incident wave u s ( x ) = measured scattered wave Direct problem: Given D (and its physical properties) describe the scattered field u s Inverse ill-posed problem : Determine the support (shape) of D from the knowledge of u s far away from the scatterer (far field region) 2

  4. Outline 1 . Approaches for inverse scattering: − Traditional methods − Qualitative sampling methods 2 . Forward scattering − Radiating (outgoing) solutions − Rellich’s lemma 3 . The inverse scattering problem − Far field operator − Herglotz wave function 4 . Sampling formulation − Fundamental solution − Linear sampling method − Factorization method 5 . Failure (?) at eigenfrequencies − Modified Jones/Ursell far-field operator − Object classification at eigenfrequencies 6 . Applications 3

  5. 1. Approaches for inverse scattering Qualitative/sampling schemes Goal: try to • recover shape as opposed to physical properties • recover shape and possibly some extra info Fixed frequency of incidence ω : u s i u D Sampling: Collect the far field data u ∞ (or the near field data u s ) and solve an ill-posed linear integral equation for each sample point z 4

  6. Inverse Scattering Methods Nonlinear optimization methods Kleinmann, Angell, Kress, Rundell, Hettlich, Dorn, Weng Chew, Ho- hage, Lesselier ... • need some a priori information − parametrization, # scatterers, etc • flexibility w.r.t. data • need forward solver (major concern) • full wave model • inverse crimes not uncommon! Asymptotic approximations (Born, iterated- Born, geometrical optics, time-reversal/mi- gration, ...) Bret Borden, Cheney, Papanicolaou, ... • need a priori information so linearizations be applicable (not for resonance region) • (mostly) linear inversion schemes • radar imaging with incorrect model? Qualitative methods (sampling, Factoriza- tion, Point-source, Ikehata’s, MUSIC?...) Colton, Monk, Kirsch, Hanke-Bourgeois, Cakoni, Pot- thast, Devaney, Hanke, Ikehata, Ammari, Haddar, ... • no forward solver • no a priori info on the scatterer • no linearization/asymptotic approx.: – full nonlinear multiple scattering model • need more data • do not determine EM properties ( σ, ϵ r ) 5

  7. 2. Forward wave propagation 101 Wave equation (pressure p = p ( x, t ), velocity c ) ∂ 2 ∂t 2 p − c 2 △ p = 0 Time-harmonic dependency: ω = frequency { u ( x ) e − i ωt } p ( x, t ) = ℜ e Helmholtz (reduced wave) equation: ( − i ω ) 2 u − c 2 △ u = 0 −△ u − k 2 u = 0 ⇒ where k = ω/c is the wavenumber. Plane wave incidence ’Plane wave’ in the direction d , | d | = 1, { e i kx · d e − i ωt } p ( x, t ) = cos { k ( x · d − c 0 t ) } = ℜ e Plane wave u i ( x ) = e i kx · d satisfies −△ u i − k 2 u i = 0 em R 3 , where k = ω/c 0 6

  8. Forward scattering Incident field (say plane wave or point source) −△ u i − k 2 u i = f in R 3 , where k = ω/c 0 Helmholtz equation for the total field −△ u − k 2 u = 0 in R 3 \ D, B u = 0 on ∂D, Total field u = u i + u s , u s perturbation due to D Boundary condition (impenetrable) B u := ∂ ν u + i λu impedance (Neumann λ = 0) = u Dirichlet/PEC Analogous to Maxwell with ∇ × ∇ × E − k 2 E = F in R 3 \ D 7

  9. Sommerfeld/Silver-M¨ uller conditions Exterior boundary value problem for u s Uniqueness: u s travels away from the obstacle −△ u s − k 2 u s = 0 in R 3 \ D, B u s = f := −B u i on ∂D, 2 � � ∫ ∂ ∂ru s − i ku s � � lim ds ( x ) = 0 � � � � R →∞ r := | x | = R (Sommerfeld radiation condition) Here x = | x | ˆ x = r ˆ x , ˆ x ∈ Ω Notation: Ω unit sphere Sommerfeld: ”... energy does not propagate from infinity into the domain ...” 8

  10. Radiating solutions II Sommerfeld radiation condition on u s −△ u s − k 2 u s = 0 in R 3 \ D, B u s = f := −B u i on ∂D, 2 � � ∫ ∂ ∂ru s − i ku s � � lim ds ( x ) = 0 � � � � R →∞ r := | x | = R Asymptotic behavior of radiating solutions Def. u s is radiating if it satisifies – Helmholtz outside some ball and – Sommerfeld radiation condition If u s is radiating then Theor. ( ) e i k | x | 1 u s ( x ) = | x | u ∞ (ˆ x ) + O | x | 2 90 1.5 120 60 1 150 30 0.5 180 0 210 330 240 300 270 9

  11. Rellich’s lemma [1943] Key tool in scattering theory: Identical far field patterns ⇓ Identical scattered fields (in the domain of definition) Rellich’s lemma (fixed wave number k > 0) If v 1 x ) = v 2 ∞ (ˆ ∞ (ˆ x ) for infinitely many ˆ x ∈ Ω then 2 ( x ), x ∈ R 3 \ D . v s 1 ( x ) = v s That is, if v 1 ∞ (ˆ x ) = 0 for ˆ x ∈ Ω then 1 ( x ) = 0, x ∈ R 3 \ D . v s Remark : R >> 1, ∫ ∫ | x | = R | v s ( x ) | 2 ds ( x ) ≈ x ) | 2 ds (ˆ Ω | v ∞ (ˆ x ) 10

  12. 3. The Inverse Scattering Problem Inverse problem: ill-posed and nonlinear Given several incident plane waves with dir. d u i ( x, d ) = e i kx · d , measure the corresponding far-field pattern u ∞ (ˆ x, d ) , ˆ x ∈ Ω and determine the support of D Re Im 350 350 300 300 250 250 200 200 150 150 100 100 50 50 100 200 300 100 200 300 11

  13. Far field operator (data operator): F : L 2 (Ω) → L 2 (Ω) ∫ ( Fg )(ˆ x ) := Ω u ∞ (ˆ x, d ) g ( d ) ds ( d ) Remark 1: F is compact (smooth kernel u ∞ ) Remark 2: F is injective and has dense range whenever k 2 ̸ = interior eigenvalue Proof : Fg = 0 implies (Rellich) ∫ Ω u s ( x, d ) g ( d ) ds ( d ) = 0 , x ∈ R 3 \ D ∫ Ω u i ( x, d ) g ( d ) ds ( d ) = 0 , x ∈ ∂D −B that is, − B v g ( x ) = 0 , x ∈ ∂D where Herglotz wave function: ∫ Ω e ikx · d g ( d ) ds ( d ) , kernel g ∈ L 2 (Ω) v g ( x ) := so that v g satisfies the interior e-value problem −△ v g − k 2 v g = 0 in D, B v g = 0 on ∂D and v g = 0, g = 0, if k 2 ̸ = eigenvalue � 12

  14. Far field operator (data operator): (SKP) F : L 2 (Ω) → L 2 (Ω) ∫ ( Fg )(ˆ x ) := Ω u ∞ (ˆ x, d ) g ( d ) ds ( d ) Obs.: F normal in the Dirichlet, Neumann and non-absorbing medium cases 13

  15. Herglotz wave function Superposition with kernel g ∫ ∫ ∫ e ikx · d g ( d ) ds ( d ) u s ( x, d ) g ( d ) ds ( d ) u ∞ (ˆ x, d ) g ( d ) ds ( d ) ❀ ❀ Ω Ω Ω ∥ ∥ ∥ v s ( x ) v g ( x ) ( Fg )(ˆ x ) ❀ ❀ By superposition the incident Herglotz func- tion v g ( x ) induces the far field pattern ( Fg )(ˆ x ) ( R 3 ): The fundamental solution e i k | x − z | Φ( x, z ) := 4 π | x − z | , x ̸ = z, is radiating in R 3 \ { z } . Fixing the source z ∈ R 3 as a parameter, then Φ( · , z ) has far field pattern x, z ) = 1 4 πe − i k ˆ x · z Φ ∞ (ˆ 14

  16. 4. Linear Sampling Method (LSM) Let z ∈ R 3 . Consider Far field equation Fg z (ˆ x ) = Φ ∞ (ˆ x, z ) It is solvable only in special cases, if z = z 0 and D is a ball centered at z 0 . In general a solution doesn’t exist. Ex. 2D Neumann obstacle: ( k = 3 . 4, k = 4) k =3.4 k =4 −3 −3 60 60 −2 −2 50 50 −1 −1 40 40 0 0 30 30 1 1 20 20 2 2 10 10 3 3 −2 0 2 −2 0 2 z inside D , || g z || remains bounded z outside D , || g z || becomes unbounded Nevertheless the regularized algorithm is nu- merically robust and the following approxima- tion theorem holds 15

  17. LSM theorem (SKP) If − k 2 ̸ = Dirichlet eigenvalue for Theorem the Laplacian in D then (1) For any ϵ > 0 and z ∈ D , there exists a g z ∈ L 2 (Ω) such that - ∥ Fg z − Φ ∞ ( · , z ) ∥ L 2 (Ω) < ϵ, and - lim z → ∂D ∥ g z ∥ L 2 (Ω) = ∞ , lim z → ∂D ∥ v g z ∥ H 1 ( D ) = ∞ . (2) For any ϵ > 0, δ > 0 and z ∈ R 3 \ D , there exists a g z ∈ L 2 (Ω) such that - ∥ Fg z − Φ ∞ ( · , z ) ∥ L 2 (Ω) < ϵ + δ and - lim δ → 0 ∥ g z ∥ L 2 (Ω) = ∞ , lim δ → 0 ∥ v g z ∥ H 1 ( D ) = ∞ where v g z is the Herglotz function with kernel g z . 16

  18. LSM motivation (Dirichlet) • Assume u ∞ (ˆ x, d ) known for ˆ x, d ∈ Ω corresponding to u i ( x, d ) = e ikx · d • Let z ∈ D and g = g z ∈ L 2 (Ω) solve Fg = Φ ∞ ( · , z ): ∫ Ω u ∞ (ˆ x, d ) g ( d ) ds ( d ) = Φ ∞ (ˆ x, z ) • Rellich’s lemma: ∫ x ∈ R 3 \ D Ω u s ( x, d ) g ( d ) ds ( d ) = Φ( x, z ) , • Boundary condition u s ( x, d ) = − e i kx · d on ∂D implies: ∫ Ω e ikx · d g ( d ) ds ( d ) = Φ( x, z ) , − x ∈ ∂D, z ∈ D. If z ∈ D and z → x ∈ ∂D then || g || L 2 (Ω) → ∞ since | Φ( x, z ) | → ∞ Same analogy: Neumann, impedance, inho- mogeneous medium 17

  19. Factorization method (Dirichlet) f ∈ H 1 / 2 ( ∂D ) Generalized scattering problem: ∆ v + k 2 v = 0 in R 3 \ D, v = f on ∂D, v radiating Data to far-field operator: takes f into v ∞ G : H 1 / 2 ( ∂D ) → L 2 (Ω) , f ❀ Gf := v ∞ Theorem z ∈ D iff Φ ∞ ( · , z ) ∈ Range ( G ) Proof: Rellich + singularity of Φ( · , z ) at z . 18

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