Invisible Random Media And Diffraction Gratings That Don't Diffract
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1 Invisible Random Media And Diffraction Gratings That Don't Diffract 29/08/2017 Christopher King, Simon Horsley and Tom Philbin, University of Exeter, United Kingdom, webpage:
2 Outline Aims, Motivation. Mathematically modelling wave propagation in inhomogeneous media. 1d reflectionless media: Perfectly absorbing layers. Perfectly transmitting disordered media. 2d non-scattering media Periodic media suppressing diffraction. Conclusions. 2
3 Aims and Motivation Reduce scattering from objects- invisibility. Possible using Transformation Optics [1,2] [3] [1]: J. B. Pendry, D. Schurig, D. R. Smith, Science , (2006). [2]: U. Leonhardt, Science , (2006). [3]: I. D. Rukhlenko, Plasmonics (2014). 3
4 Incident Reflected y 1d Graded index medium ε x x Helmholtz equation Transmitted TE polarized, monochromatic light of frequency ω. Isotropic, planar dielectric. μ = 1. d 2 dx 2 + k 0 2 ε x E x = 0 k 0 = ω/c Spatial Kramers-Kronig media are one-way reflectionless. [4] [4]: S. A. R. Horsley, C. G. King, T. G. Philbin, J. Opt , (2016). 4
5 Perfectly absorbing media (Complex-valued) ε x = 1 ln k 0x + 2i k 0 x + 2i E x, y E x, y y [5] x [5]: C. G. King, S. A. R. Horsley and T. G. Philbin, J. Opt , (2017). 5
6 An Experimental Realisation [9]: W. Jiang et. al., Laser Phot. Rev., , (2017). 6
7 Condition for real-valued ε(x) d 2 dx 2 + k 0 2 ε x E x = 0 k 0 = ω/c Ansatz: Modify a plane wave: E x = Ae ik 0x A(x)e iκs(x) amplitude A(x) phase S(x) both real ε is real if d dx ds A2 = 0 dx Solution E x = 1 x p( p(x) 1/4 eiκ x)d x [6] [6]: M. V. Berry, C. J. Howls, J. Phys. A 23 6, (1990). 7
8 Real-valued single frequency reflectionless media Corresponding permittivity ε x, κ = p x p(x)1/4 κ 2 d 2 dx 2 1 p(x) 1/4. [7,8] [7]: C. G. King, S. A. R. Horsley and T. G. Philbin, Phys. Rev. Let , (2017). [8]: K. G. Makris et. al., Light: Sci. Apps. 6, e17035, (2017). 8
9 y Incident plane wave x 2d Graded index medium Scattered waves ε x, y TE polarized, monochromatic light of frequency ω. Isotropic, planar dielectric. μ = 1. 2 x y 2 + k 0 2 ε x, y E x, y = 0 k 0 = ω/c 9
10 10 Condition for real-valued ε(x) Ansatz: Modify a plane wave: E x, y = Ae ik 0x A(x, y)e ik 0S(x,y) amplitude A(x, y) phase S(x, y) both real ε is real if. A 2 S = 0 Energy conservation: A 2 S is proportional to the time averaged Poynting vector (energy flux density).
11 The characteristic method. A 2 S = 0 (PDE) Choose S x, y. Find the exact rays. dλ x λ, y λ Solve for A along rays subject to boundary condition. Solve for ε. 11
12 y x k 0 = 5 k 0 = Non-diffracting periodic gratings ε x, y E x, y k 0 =
13 13 Ongoing: Diffraction into a pair of modes A x, y y x
14 14 Conclusions 1d reflectionless perfectly absorbing media. 1d reflectionless perfectly transmitting disordered permittivity profiles. 2d Periodic non-diffracting media. Acknowledgements PhD supervisors: Dr Simon Horsley Dr Thomas Philbin EPSRC Centre for Doctoral Training in Electromagnetic Metamaterials EP/L015331/1.
15 15
16 16 Beamshifter Exact solution to. A 2 S = 0 ε x, y E x, y y x
17 17 Translationally Invariant rays. A 2 S = A A d2 S + 2 da ds + A d2 S + 2 da ds =0 dx 2 dx dx dy 2 dy dy 0 0 S x, y = s y + c x A x, y = 1 s y+c x c x ε x, y, k 0 = c x s y + c x k 0 2 g x, y
18 18 Translationally Invariant rays Phasefront ray slopes are independent ofy dy dx = 1 c x E.g. c x = sinh αx α
19 Model: Graded index medium Incident Reflected ε x Transmitted y TE polarised, monochromatic light of frequency ω. Isotropic, planar dielectric. x μ = 1. lim x ± ε x = 1. d 2 dx 2 + k 0 2 ε x k y 2 E x = 0 k 0 = (k x, k y, 0) k 0 = ω/c Assume k y = 0 from now on. 19
20 A condition for no reflection (all angles, oneway incidence) Complex position: x z = x 1 + ix 2 (c.f. transformation optics). Kramers-Kronig media [1,2]: ε(z) analytic in the upper half position plane. lim ε z = 1 (Im z > 0). z x 2 x 2 αe k 0x 2 + βe ik 0x 2 γe k 0x 2 + δe ik 0x 2 ε z = 1 ε z = 1 Inhomogeneity αe ik 0x 1 + βe ik 0x 1 γe ik 0x 1 + δe ik 0x 1 Inhomogeneity x 1 [1]: S. A. R. Horsley, M. Artoni, G. C. La Rocca, Non reflecting permittivity profiles and the spatial Kramers Kronig relations, Nature Phot (2015). [2]: S. A. R. Horsley, C. G. King, T. G. Philbin, Wave propagation in complex coordinates, J. Opt (2016). 20
21 21 Transmission coefficient for Kramers-Kronig media Transmission t 2 = e 2k Im( 0 ε(z)dz) ε z = 1 + N k=1 a k z z k + N k=1 b k (z z k ) 2 +
22 22 Complex-valued Kramers-Kronig broadband reflectionless media Choose real-valued function with compact support Χ R x and ΧR x dx = 0. Spatial Hilbert transform Χ I x = 1 P Χ R x π x x satisfies ΧI x dx = 0. dx also ε x = 1 + Χ R x + iχ I x has transmission 1 for all incident frequencies and angles.
23 Hurst exponent, H: Measuring Randomness H > 0.5 implies long term positive correlations. H < 0.5 implies long term negative correlations. Χ x Χ Two-point correlation function g s = (x+s)dx. μ(g(s)) 0 as N. Χ x 2 dx Berry-Howls correlation Fourier series correlation H =0.18 H =0.53 (real part), 0.47 (imaginary part) 23
24 Incident Anderson (Strong) Localization N slabs of randomly chosen homogeneous lossless media: ε 1 ε 2 ε 3 ε 4 ε 5 Transmitted Reflected Logarithmic average of transmission coefficient t eff 2 = exp N 2 i=1 1 t i [4] [4]: M. V. Berry, S. Klein, Transparent mirrors: rays, waves and localization, Eur. J. Phys , (1996). 24
25 Measuring Randomness: Correlation function Two-point correlation function g s = Χ x Χ (x+s)dx where Χ x = ε x 1. Χ x 2 dx g(s) 1 Fourier series correlation Berry-Howls correlation 0.5 5λ 10λ 15λ μ(g(s)) 0 as N. 25
26 Phase as a harmonic function. A 2 S = A A 2 S + 2 A. S = S=0 implies S = Re h(z) where z = x + iy A. S = 0 implies A = A Im h y x ε z = dh dz 2 1 A Im h k 0 2 A Im h ε(h) 26
27 ε z = dh dz Take ε h = 1: Transformation Optics 2 ε z = dh dz ε(h) 2 z space Vacuum solutions in h space Reflectionless solutions in z space [4] e.g. h = z + a2 z [4]: U. Leonhardt, Optical Conformal Mapping, Science , (2006). h space 27
28 Transverse reflectionless profiles A Im h ε h = 1 k 2 0 A Im h Profiles homogeneous along direction of propagation. e.g. ε h = 1 + ε Im h 2 k 0 2 cosh 2 Im h Re E Im h Re h Im h 28
29 29 Condition for real-valued ε(x) d 2 dx 2 + k 0 2 ε x E x = 0 k 0 = ω/c Plane wave Ae ik 0x solves Helmholtz for ε x = 1. Ansatz: Modify a plane wave: E x = Ae ik 0x A(x)e iκs(x) amplitude A(x) phase S(x) both real
30 Condition for real-valued ε(x) ε x, κ = 1 d 2 A + ds κ 2 A dx 2 dx 2 + i 1 κa 2 d dx ds A2 dx real part imaginary part ε is real if d dx ds A2 = 0 dx Solution E x = 1 x p( p(x) 1/4 eiκ x)d x [3] p(x) real function with lim x ± p x = 1. [3]: M. V. Berry, C. J. Howls, Fake Airy functions and the asymptotics of reflectionlessness, J. Phys. A 23 6, (1990). 30
31 31 y Transmitted modes x period θ i
32 y x θ i = 0 Non-diffracting periodic gratings- vary angle ε x, y E x, y θ i = π θ i = 2π
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