Polynomial Chaos for Dispersive Electromagnetics Nathan L. Gibson - - PowerPoint PPT Presentation

polynomial chaos for dispersive electromagnetics
SMART_READER_LITE
LIVE PREVIEW

Polynomial Chaos for Dispersive Electromagnetics Nathan L. Gibson - - PowerPoint PPT Presentation

Polynomial Chaos for Dispersive Electromagnetics Nathan L. Gibson Associate Professor Department of Mathematics Computational Aspects of Time Dependent Electromagnetic Wave Problems in Complex Materials June 29, 2018 N. L. Gibson (Oregon


slide-1
SLIDE 1

Polynomial Chaos for Dispersive Electromagnetics

Nathan L. Gibson

Associate Professor Department of Mathematics

Computational Aspects of Time Dependent Electromagnetic Wave Problems in Complex Materials June 29, 2018

  • N. L. Gibson (Oregon State)

Maxwell-PC Dispersive ICERM 2018 1 / 72

slide-2
SLIDE 2

Outline

1

Maxwell System

  • N. L. Gibson (Oregon State)

Maxwell-PC Dispersive ICERM 2018 2 / 72

slide-3
SLIDE 3

Outline

1

Maxwell System

2

Maxwell-Random Debye System

  • N. L. Gibson (Oregon State)

Maxwell-PC Dispersive ICERM 2018 2 / 72

slide-4
SLIDE 4

Outline

1

Maxwell System

2

Maxwell-Random Debye System

3

Stability and Dispersion Analyses

  • N. L. Gibson (Oregon State)

Maxwell-PC Dispersive ICERM 2018 2 / 72

slide-5
SLIDE 5

Outline

1

Maxwell System

2

Maxwell-Random Debye System

3

Stability and Dispersion Analyses

4

Maxwell-Random Lorentz system

  • N. L. Gibson (Oregon State)

Maxwell-PC Dispersive ICERM 2018 2 / 72

slide-6
SLIDE 6

Acknowledgments Collaborators

  • H. T. Banks (NCSU)
  • V. A. Bokil (OSU)

Students Karen Barrese and Neel Chugh (REU 2008) Anne Marie Milne and Danielle Wedde (REU 2009) Erin Bela and Erik Hortsch (REU 2010) Megan Armentrout (MS 2011) Brian McKenzie (MS 2011) Jacky Alvarez and Andrew Fisher (REU 2017)

  • N. L. Gibson (Oregon State)

Maxwell-PC Dispersive ICERM 2018 3 / 72

slide-7
SLIDE 7

Maxwell System Maxwell’s Equations

Maxwell’s Equations ∂B ∂t + ∇ × E = 0, in (0, T) × D (Faraday) ∂D ∂t + J − ∇ × H = 0, in (0, T) × D (Ampere) ∇ · D = ∇ · B = 0, in (0, T) × D (Poisson/Gauss) E(0, x) = E0; H(0, x) = H0, in D (Initial) E × n = 0, on (0, T) × ∂D (Boundary) E = Electric field vector H = Magnetic field vector J = Current density D = Electric flux density B = Magnetic flux density n = Unit outward normal to ∂Ω

  • N. L. Gibson (Oregon State)

Maxwell-PC Dispersive ICERM 2018 4 / 72

slide-8
SLIDE 8

Maxwell System Maxwell’s Equations

Constitutive Laws Maxwell’s equations are completed by constitutive laws that describe the response of the medium to the electromagnetic field. D = ǫE + P B = µH + M J = σE + Js P = Polarization M = Magnetization Js = Source Current ǫ = Electric permittivity µ = Magnetic permeability σ = Electric Conductivity where ǫ = ǫ0ǫ∞ and µ = µ0µr.

  • N. L. Gibson (Oregon State)

Maxwell-PC Dispersive ICERM 2018 5 / 72

slide-9
SLIDE 9

Maxwell System Dispersive Media

Complex permittivity For linear materials we can define P in terms of a convolution with E P(t, x) = g ∗ E(t, x) = t g(t − s, x; q)E(s, x)ds, where g is the dielectric response function (DRF).

  • N. L. Gibson (Oregon State)

Maxwell-PC Dispersive ICERM 2018 6 / 72

slide-10
SLIDE 10

Maxwell System Dispersive Media

Complex permittivity For linear materials we can define P in terms of a convolution with E P(t, x) = g ∗ E(t, x) = t g(t − s, x; q)E(s, x)ds, where g is the dielectric response function (DRF). Allows for relaxation processes as well as resonance, and others.

  • N. L. Gibson (Oregon State)

Maxwell-PC Dispersive ICERM 2018 6 / 72

slide-11
SLIDE 11

Maxwell System Dispersive Media

Complex permittivity For linear materials we can define P in terms of a convolution with E P(t, x) = g ∗ E(t, x) = t g(t − s, x; q)E(s, x)ds, where g is the dielectric response function (DRF). Allows for relaxation processes as well as resonance, and others. In the frequency domain ˆ D = ǫˆ E + ˆ gˆ E = ǫ0ǫ(ω)ˆ E, where ǫ(ω) is called the complex permittivity.

  • N. L. Gibson (Oregon State)

Maxwell-PC Dispersive ICERM 2018 6 / 72

slide-12
SLIDE 12

Maxwell System Dispersive Media

Complex permittivity For linear materials we can define P in terms of a convolution with E P(t, x) = g ∗ E(t, x) = t g(t − s, x; q)E(s, x)ds, where g is the dielectric response function (DRF). Allows for relaxation processes as well as resonance, and others. In the frequency domain ˆ D = ǫˆ E + ˆ gˆ E = ǫ0ǫ(ω)ˆ E, where ǫ(ω) is called the complex permittivity. We are interested in ultra-wide bandwidth electromagnetic pulse interrogation of dispersive dielectrics, therefore we want an accurate representation of ǫ(ω) over a broad range of frequencies.

  • N. L. Gibson (Oregon State)

Maxwell-PC Dispersive ICERM 2018 6 / 72

slide-13
SLIDE 13

Maxwell System Dry skin data

10

2

10

4

10

6

10

8

10

10

10

1

10

2

10

3

f (Hz)

ε

True Data Debye Model Cole−Cole Model

Figure: Real part of ǫ(ω), ǫ, or the permittivity [GLG96].

  • N. L. Gibson (Oregon State)

Maxwell-PC Dispersive ICERM 2018 7 / 72

slide-14
SLIDE 14

Maxwell System Dry skin data

10

2

10

4

10

6

10

8

10

10

10

−4

10

−3

10

−2

10

−1

10 10

1

f (Hz)

σ

True Data Debye Model Cole−Cole Model

Figure: Imaginary part of ǫ(ω)/ω, σ, or the conductivity.

  • N. L. Gibson (Oregon State)

Maxwell-PC Dispersive ICERM 2018 8 / 72

slide-15
SLIDE 15

Maxwell System Dispersive Media

Dispersive Media

0.2 0.4 0.6 0.8 −1000 −500 500 1000 z E

Time=5.0ns

0.2 0.4 0.6 0.8 −80 −60 −40 −20 20 40

Time=10.0ns

E z

Figure: Debye model simulations [Banks2000].

  • N. L. Gibson (Oregon State)

Maxwell-PC Dispersive ICERM 2018 9 / 72

slide-16
SLIDE 16

Maxwell System Dispersive Media

Relaxation Polarization Models P(t, x) = g ∗ E(t, x) = t g(t − s, x; q)E(s, x)ds, Debye model [1913] q = [ǫ∞, ǫd, τ] g(t, x) = ǫ0ǫd/τ e−t/τ

  • r

τ ˙ P + P = ǫ0ǫdE

  • r

ǫ(ω) = ǫ∞ + ǫd 1 + iωτ with ǫd := ǫs − ǫ∞ and τ a relaxation time.

  • N. L. Gibson (Oregon State)

Maxwell-PC Dispersive ICERM 2018 10 / 72

slide-17
SLIDE 17

Maxwell System Dispersive Media

Relaxation Polarization Models P(t, x) = g ∗ E(t, x) = t g(t − s, x; q)E(s, x)ds, Debye model [1913] q = [ǫ∞, ǫd, τ] g(t, x) = ǫ0ǫd/τ e−t/τ

  • r

τ ˙ P + P = ǫ0ǫdE

  • r

ǫ(ω) = ǫ∞ + ǫd 1 + iωτ with ǫd := ǫs − ǫ∞ and τ a relaxation time. Cole-Cole model [1941] (heuristic generalization) q = [ǫ∞, ǫd, τ, α] ǫ(ω) = ǫ∞ + ǫd 1 + (iωτ)α

  • N. L. Gibson (Oregon State)

Maxwell-PC Dispersive ICERM 2018 10 / 72

slide-18
SLIDE 18

Maxwell System Dispersive Media

Polarization Models P(t, x) = g ∗ E(t, x) = t g(t − s, x; q)E(s, x)ds, Debye model [1913] q = [ǫ∞, ǫd, τ] ǫ(ω) = ǫ∞ + ǫd 1 + iωτ Cole-Cole model [1941] q = [ǫ∞, ǫd, τ, α] ǫ(ω) = ǫ∞ + ǫd 1 + (iωτ)α Havriliak-Negami model [1967] q = [ǫ∞, ǫd, τ, α, β] ǫ(ω) = ǫ∞ + ǫd (1 + (iωτ)α)β

  • N. L. Gibson (Oregon State)

Maxwell-PC Dispersive ICERM 2018 11 / 72

slide-19
SLIDE 19

Maxwell-Random Debye System Distributions of Relaxation Times

Distributions of Relaxation Times As early as 1897, experiments by Drude demonstrated that some materials exhibited “anomalous dispersion, i.e, the decrease in the dielectric constant with increasing frequency” [Debye 1929].

  • N. L. Gibson (Oregon State)

Maxwell-PC Dispersive ICERM 2018 12 / 72

slide-20
SLIDE 20

Maxwell-Random Debye System Distributions of Relaxation Times

Distributions of Relaxation Times As early as 1897, experiments by Drude demonstrated that some materials exhibited “anomalous dispersion, i.e, the decrease in the dielectric constant with increasing frequency” [Debye 1929]. In 1907, von Schweidler observed the need for multiple relaxation times.

  • N. L. Gibson (Oregon State)

Maxwell-PC Dispersive ICERM 2018 12 / 72

slide-21
SLIDE 21

Maxwell-Random Debye System Distributions of Relaxation Times

Distributions of Relaxation Times As early as 1897, experiments by Drude demonstrated that some materials exhibited “anomalous dispersion, i.e, the decrease in the dielectric constant with increasing frequency” [Debye 1929]. In 1907, von Schweidler observed the need for multiple relaxation times. Around the same time, Debye’s papers appeared (in German) defining and quantifying the relaxation time. Analogous to the Maxwell-Wiechert model of viscoelasticity from 1893.

  • N. L. Gibson (Oregon State)

Maxwell-PC Dispersive ICERM 2018 12 / 72

slide-22
SLIDE 22

Maxwell-Random Debye System Distributions of Relaxation Times

Distributions of Relaxation Times As early as 1897, experiments by Drude demonstrated that some materials exhibited “anomalous dispersion, i.e, the decrease in the dielectric constant with increasing frequency” [Debye 1929]. In 1907, von Schweidler observed the need for multiple relaxation times. Around the same time, Debye’s papers appeared (in German) defining and quantifying the relaxation time. Analogous to the Maxwell-Wiechert model of viscoelasticity from 1893. In 1913, Wagner proposed a continuous distribution of relaxation times.

  • N. L. Gibson (Oregon State)

Maxwell-PC Dispersive ICERM 2018 12 / 72

slide-23
SLIDE 23

Maxwell-Random Debye System Distributions of Relaxation Times

Distributions of Relaxation Times As early as 1897, experiments by Drude demonstrated that some materials exhibited “anomalous dispersion, i.e, the decrease in the dielectric constant with increasing frequency” [Debye 1929]. In 1907, von Schweidler observed the need for multiple relaxation times. Around the same time, Debye’s papers appeared (in German) defining and quantifying the relaxation time. Analogous to the Maxwell-Wiechert model of viscoelasticity from 1893. In 1913, Wagner proposed a continuous distribution of relaxation times. In 1927, Debye invited to US (and translated his works into English).

  • N. L. Gibson (Oregon State)

Maxwell-PC Dispersive ICERM 2018 12 / 72

slide-24
SLIDE 24

Maxwell-Random Debye System Distributions of Relaxation Times

Distributions of Relaxation Times As early as 1897, experiments by Drude demonstrated that some materials exhibited “anomalous dispersion, i.e, the decrease in the dielectric constant with increasing frequency” [Debye 1929]. In 1907, von Schweidler observed the need for multiple relaxation times. Around the same time, Debye’s papers appeared (in German) defining and quantifying the relaxation time. Analogous to the Maxwell-Wiechert model of viscoelasticity from 1893. In 1913, Wagner proposed a continuous distribution of relaxation times. In 1927, Debye invited to US (and translated his works into English). In 1927, K.S. Cole studied electrical properties of biological systems (during his postdoc at Harvard). Was invited to visit Debye in Germany in 1928.

  • N. L. Gibson (Oregon State)

Maxwell-PC Dispersive ICERM 2018 12 / 72

slide-25
SLIDE 25

Maxwell-Random Debye System Distributions of Relaxation Times

In 1940, R.H. Cole began PhD at Harvard and collaborated with brother on a graphical method to test the Debye model, as well as a heuristic fix.

  • N. L. Gibson (Oregon State)

Maxwell-PC Dispersive ICERM 2018 13 / 72

slide-26
SLIDE 26

Maxwell-Random Debye System Distributions of Relaxation Times

In 1940, R.H. Cole began PhD at Harvard and collaborated with brother on a graphical method to test the Debye model, as well as a heuristic fix. In 1950, D.W. Davidson and R.H. Cole discovered materials that are not well-represented by the Cole-Cole model, proposed a different heuristic.

  • N. L. Gibson (Oregon State)

Maxwell-PC Dispersive ICERM 2018 13 / 72

slide-27
SLIDE 27

Maxwell-Random Debye System Distributions of Relaxation Times

In 1940, R.H. Cole began PhD at Harvard and collaborated with brother on a graphical method to test the Debye model, as well as a heuristic fix. In 1950, D.W. Davidson and R.H. Cole discovered materials that are not well-represented by the Cole-Cole model, proposed a different heuristic. In 1967, Havriliak and Negami combined the two heuristics to form a generalized model.

  • N. L. Gibson (Oregon State)

Maxwell-PC Dispersive ICERM 2018 13 / 72

slide-28
SLIDE 28

Maxwell-Random Debye System Distributions of Relaxation Times

In 1940, R.H. Cole began PhD at Harvard and collaborated with brother on a graphical method to test the Debye model, as well as a heuristic fix. In 1950, D.W. Davidson and R.H. Cole discovered materials that are not well-represented by the Cole-Cole model, proposed a different heuristic. In 1967, Havriliak and Negami combined the two heuristics to form a generalized model. One can show that the Cole-Cole model (and extensions) corresponds to a continuous distribution of relaxation times “... it is possible to calculate the necessary distribution function by the method of Fuoss and Kirkwood.” [Cole-Cole1941].

  • N. L. Gibson (Oregon State)

Maxwell-PC Dispersive ICERM 2018 13 / 72

slide-29
SLIDE 29

Maxwell-Random Debye System Distributions of Relaxation Times

In 1940, R.H. Cole began PhD at Harvard and collaborated with brother on a graphical method to test the Debye model, as well as a heuristic fix. In 1950, D.W. Davidson and R.H. Cole discovered materials that are not well-represented by the Cole-Cole model, proposed a different heuristic. In 1967, Havriliak and Negami combined the two heuristics to form a generalized model. One can show that the Cole-Cole model (and extensions) corresponds to a continuous distribution of relaxation times “... it is possible to calculate the necessary distribution function by the method of Fuoss and Kirkwood.” [Cole-Cole1941].

  • N. L. Gibson (Oregon State)

Maxwell-PC Dispersive ICERM 2018 13 / 72

slide-30
SLIDE 30

Maxwell-Random Debye System Distributions of Relaxation Times

In 1940, R.H. Cole began PhD at Harvard and collaborated with brother on a graphical method to test the Debye model, as well as a heuristic fix. In 1950, D.W. Davidson and R.H. Cole discovered materials that are not well-represented by the Cole-Cole model, proposed a different heuristic. In 1967, Havriliak and Negami combined the two heuristics to form a generalized model. One can show that the Cole-Cole model (and extensions) corresponds to a continuous distribution of relaxation times “... it is possible to calculate the necessary distribution function by the method of Fuoss and Kirkwood.” [Cole-Cole1941]. F(y) = yαβ y2α + 2yα cos(πα) + 1

  • sin(βθ)/π − β/2,

where y = τ/τ0 and θ is defined implictly by (yα + cos(πα)) tan(θ) = sin(πα).

  • N. L. Gibson (Oregon State)

Maxwell-PC Dispersive ICERM 2018 13 / 72

slide-31
SLIDE 31

Maxwell-Random Debye System Distributions of Relaxation Times

[Garrappa2016]

  • N. L. Gibson (Oregon State)

Maxwell-PC Dispersive ICERM 2018 14 / 72

slide-32
SLIDE 32

Maxwell-Random Debye System Distributions of Relaxation Times

Figure: Relaxation Time Distribution for CC model [Garrappa2016].

  • N. L. Gibson (Oregon State)

Maxwell-PC Dispersive ICERM 2018 15 / 72

slide-33
SLIDE 33

Maxwell-Random Debye System Fit to dry skin data with uniform distribution

10

2

10

4

10

6

10

8

10

10

10

2

10

3

f (Hz)

ε

True Data Debye (27.79) Cole−Cole (10.4) Uniform (13.60)

Figure: Real part of ǫ(ω), ǫ, or the permittivity [REU2008].

  • N. L. Gibson (Oregon State)

Maxwell-PC Dispersive ICERM 2018 16 / 72

slide-34
SLIDE 34

Maxwell-Random Debye System Fit to dry skin data with uniform distribution

10

2

10

4

10

6

10

8

10

10

10

−3

10

−2

10

−1

10 10

1

f (Hz)

σ

True Data Debye (27.79) Cole−Cole (10.4) Uniform (13.60)

Figure: Imaginary part of ǫ(ω)/ω, σ, or the conductivity [REU2008].

  • N. L. Gibson (Oregon State)

Maxwell-PC Dispersive ICERM 2018 17 / 72

slide-35
SLIDE 35

Maxwell-Random Debye System Distribution of Relaxation Times

Distributions of Parameters To account for the effect of distributions of parameters q, consider the following polydispersive DRF h(t, x; F) =

  • Q

g(t, x; q)dF(q), where Q is some admissible set and F ∈ P(Q). Then the polarization becomes: P(t, x; F) = t h(t − s, x; F)E(s, x)ds. Alternatively we can define the random polarization P(t, x; q) to satisfy P(t, x; F) =

  • Q

P(t, x; q)dF(q).

  • N. L. Gibson (Oregon State)

Maxwell-PC Dispersive ICERM 2018 18 / 72

slide-36
SLIDE 36

Maxwell-Random Debye System Distribution of Relaxation Times

Random Polarization In the case of relaxation polarization, the random polarization P(t, x; τ) solves τ ˙ P + P = ǫ0ǫdE where τ is a random variable with PDF f (τ), for example, f (τ) = 1 τb − τa for a uniform distribution.

  • N. L. Gibson (Oregon State)

Maxwell-PC Dispersive ICERM 2018 19 / 72

slide-37
SLIDE 37

Maxwell-Random Debye System Distribution of Relaxation Times

Random Polarization In the case of relaxation polarization, the random polarization P(t, x; τ) solves τ ˙ P + P = ǫ0ǫdE where τ is a random variable with PDF f (τ), for example, f (τ) = 1 τb − τa for a uniform distribution. The electric field depends on the macroscopic polarization, which we take to be the expected value of the random polarization at each point (t, x) P(t, x; F) = τb

τa

P(t, x; τ)f (τ)dτ.

  • N. L. Gibson (Oregon State)

Maxwell-PC Dispersive ICERM 2018 19 / 72

slide-38
SLIDE 38

Maxwell-Random Debye System Polynomial Chaos

Polynomial Chaos Apply Polynomial Chaos (PC) method to approximate each spatial component of the random polarization τ ˙ P + P = ǫ0ǫdE, τ = τ(ξ) = τrξ + τm, ξ ∼ F (with ξ mean 0 and variance 1) resulting in (τrM + τmI) ˙

  • α +

α = ǫ0ǫdE ˆ e1

  • r

A ˙

  • α +

α = f .

  • N. L. Gibson (Oregon State)

Maxwell-PC Dispersive ICERM 2018 20 / 72

slide-39
SLIDE 39

Maxwell-Random Debye System Polynomial Chaos

Polynomial Chaos Apply Polynomial Chaos (PC) method to approximate each spatial component of the random polarization τ ˙ P + P = ǫ0ǫdE, τ = τ(ξ) = τrξ + τm, ξ ∼ F (with ξ mean 0 and variance 1) resulting in (τrM + τmI) ˙

  • α +

α = ǫ0ǫdE ˆ e1

  • r

A ˙

  • α +

α = f . The electric field depends on the macroscopic polarization, the expected value of the random polarization at each point (t, x), which is P(t, x; F) = E[P] ≈ α0(t, x). Note that A is positive definite if τr < τm since λ(M) ∈ (−1, 1).

  • N. L. Gibson (Oregon State)

Maxwell-PC Dispersive ICERM 2018 20 / 72

slide-40
SLIDE 40

Maxwell-Random Debye System Polynomial Chaos 1 2 3 4 5 6 7 8 9 10 10

−12

10

−10

10

−8

10

−6

10

−4

10

−2

10 10

2

Maximum Difference Calculated for different values of p and r p Maximum Error r = 1.00τ r = 0.75τ r = 0.50τ r = 0.25τ

  • N. L. Gibson (Oregon State)

Maxwell-PC Dispersive ICERM 2018 21 / 72

slide-41
SLIDE 41

Maxwell-Random Debye System Inverse Problem Numerical Results 10

−12

10

−11

10

−10

1 2 3 4 5 6 x 10

11

Distributions, noise = 0.1, refinement = 1, perturb = −0.8 Initial J=983.713 Optimal J=1.25869 Actual J=1.25879

Comparison of initial to final distribution [Armentrout-G., 2011].

  • N. L. Gibson (Oregon State)

Maxwell-PC Dispersive ICERM 2018 22 / 72

slide-42
SLIDE 42

Maxwell-Random Debye System Inverse Problem Numerical Results 0.2 0.4 0.6 0.8 1 1.2 1.4 1.6 x 10

−9

−80 −60 −40 −20 20 40 60 80 100 t E Comparison, noise = 0.1, refinement = 1, perturb = −0.8 Data Initial J=983.713 Optimal J=1.25869 Actual J=1.25879

Comparison of simulations to data [Armentrout-G., 2011].

  • N. L. Gibson (Oregon State)

Maxwell-PC Dispersive ICERM 2018 23 / 72

slide-43
SLIDE 43

Maxwell-Random Debye System Inverse Problem Numerical Results 0.2 0.4 0.6 0.8 1 1.2 ×10 -11 0.5 1 1.5 2 2.5 3 3.5 ×10 11 Distributions, noise = 0.1, refinement = 1,test = 5

Initial J=9.59699 Optimal J=3.02332 Actual J=3.02348

  • N. L. Gibson (Oregon State)

Maxwell-PC Dispersive ICERM 2018 24 / 72

slide-44
SLIDE 44

Stability and Dispersion Analyses Debye Dispersion Relation

(Deterministic) Maxwell-Debye System Combining Maxwell’s Equations, Constitutive Laws, and the Debye model, we have µ0 ∂H ∂t = −∇ × E, (1a) ǫ0ǫ∞ ∂E ∂t = ∇ × H − ǫ0ǫd τ E + 1 τ P − J, (1b) τ ∂P ∂t = ǫ0ǫdE − P. (1c)

  • N. L. Gibson (Oregon State)

Maxwell-PC Dispersive ICERM 2018 25 / 72

slide-45
SLIDE 45

Stability and Dispersion Analyses Debye Dispersion Relation

Assuming a solution to (1) of the form E = E0exp(i(ωt − k · x)), the following relation must hold. Debye Dispersion Relation The dispersion relation for the Maxwell-Debye system is given by ω2 c2 ǫ(ω) = k2 where the complex permittivity is given by ǫ(ω) = ǫ∞ + ǫd

  • 1

1 + iωτ

  • Here, k is the wave vector and c = 1/√µ0ǫ0 is the speed of light.
  • N. L. Gibson (Oregon State)

Maxwell-PC Dispersive ICERM 2018 26 / 72

slide-46
SLIDE 46

Stability and Dispersion Analyses Random Debye Dispersion Relation

Maxwell-Random Debye system In a polydispersive Debye material, we have µ0 ∂H ∂t = −∇ × E, (2a) ǫ0ǫ∞ ∂E ∂t = ∇ × H − ∂P ∂t − J (2b) τ ∂P ∂t + P = ǫ0ǫdE (2c) with P(t, x; F) = τb

τa

P(t, x; τ)dF(τ).

  • N. L. Gibson (Oregon State)

Maxwell-PC Dispersive ICERM 2018 27 / 72

slide-47
SLIDE 47

Stability and Dispersion Analyses Random Debye Dispersion Relation

Theorem (G., 2015) The dispersion relation for the system (14) is given by ω2 c2 ǫ(ω) = k2 where the expected complex permittivity is given by ǫ(ω) = ǫ∞ + ǫdE

  • 1

1 + iωτ

  • .

Where k is the wave vector and c = 1/√µ0ǫ0 is the speed of light.

  • N. L. Gibson (Oregon State)

Maxwell-PC Dispersive ICERM 2018 28 / 72

slide-48
SLIDE 48

Stability and Dispersion Analyses Random Debye Dispersion Relation

Theorem (G., 2015) The dispersion relation for the system (14) is given by ω2 c2 ǫ(ω) = k2 where the expected complex permittivity is given by ǫ(ω) = ǫ∞ + ǫdE

  • 1

1 + iωτ

  • .

Where k is the wave vector and c = 1/√µ0ǫ0 is the speed of light. Note: for a uniform distribution on [τa, τb], this has an analytic form since E

  • 1

1 + iωτ

  • =

1 ω(τb − τa)

  • arctan(ωτ) + i 1

2 ln

  • 1 + (ωτ)2τ=τa

τ=τb

. The exact dispersion relation can be compared with a discrete dispersion relation to determine the amount of dispersion error.

  • N. L. Gibson (Oregon State)

Maxwell-PC Dispersive ICERM 2018 28 / 72

slide-49
SLIDE 49

Stability and Dispersion Analyses Debye Stability

2D Maxwell-Debye Transverse Electric (TE) curl equations For simplicity in exposition and to facilitate analysis, we reduce the Maxwell-Debye model to two spatial dimensions (we make the assumption that fields do not exhibit variation in the z direction). µ0 ∂H ∂t = −curl E, (3a) ǫ0ǫ∞ ∂E ∂t = curl H − ǫ0ǫd τ E + 1 τ P − J, (3b) τ ∂P ∂t = ǫ0ǫdE − P, (3c) where E = (Ex, Ey)T, P = (Px, Py)T and Hz = H. Note curl U = ∂Uy

∂x − ∂Ux ∂y and curl V =

  • ∂V

∂y , − ∂V ∂x

T .

  • N. L. Gibson (Oregon State)

Maxwell-PC Dispersive ICERM 2018 29 / 72

slide-50
SLIDE 50

Stability and Dispersion Analyses Debye Stability

Stability Estimates for Maxwell-Debye System is well-posed since solutions satisfy the following stability estimate. Theorem (Li2010) Let D ⊂ R2, and let H, E, and P be the solutions to (the weak form of) the 2D Maxwell-Debye TE system with PEC boundary conditions. Then the system exhibits energy decay E(t) ≤ E(0), ∀t ≥ 0 where the energy is defined by E(t)2 = √µ0H(t)2

2 + √ǫ0ǫ∞E(t)2 2 +

  • 1

√ǫ0ǫd P(t)

  • 2

2

and · 2 is the L2(D) norm.

  • N. L. Gibson (Oregon State)

Maxwell-PC Dispersive ICERM 2018 30 / 72

slide-51
SLIDE 51

Stability and Dispersion Analyses Random Debye Stability

We introduce the random Hilbert space VF = (L2(Ω) ⊗ L2(D))2 equipped with an inner product and norm as follows (u, v)F = E[(u, v)2], u2

F = E[u2 2].

The weak formulation of the 2D Maxwell-Random Debye TE system is ∂H ∂t , v

  • 2

=

  • − 1

µ0 curl E, v

  • 2

, (4)

  • ǫ0ǫ∞

∂E ∂t , u

  • 2

= (H, curl u)2 − ∂P ∂t , u

  • 2

, (5) ∂P ∂t , w

  • F

= ǫ0ǫd τ E, w

  • F −

1 τ P, w

  • F

, (6) for v ∈ L2(D), u ∈ H0(curl, D)2, and w ∈ VF.

  • N. L. Gibson (Oregon State)

Maxwell-PC Dispersive ICERM 2018 31 / 72

slide-52
SLIDE 52

Stability and Dispersion Analyses Random Debye Stability

Stability Estimates for Maxwell-Random Debye System is well-posed since solutions satisfy the following stability estimate. Theorem (G., 2015) Let D ⊂ R2, and let H, E, and P be the solutions to the weak form of the 2D Maxwell-Random Debye TE system with PEC boundary conditions. Then the system exhibits energy decay E(t) ≤ E(0), ∀t ≥ 0 where the energy is defined by E(t)2 = √µ0H(t)2

2 + √ǫ0ǫ∞E(t)2 2 +

  • 1

√ǫ0ǫd P(t)

  • 2

F

.

  • N. L. Gibson (Oregon State)

Maxwell-PC Dispersive ICERM 2018 32 / 72

slide-53
SLIDE 53

Stability and Dispersion Analyses Random Debye Stability

Proof: (for 2D) By choosing v = H, u = E, and w = P in the weak form, and adding all three equations into the time derivative of the definition of E2, we obtain 1 2 dE2(t) dt = −

  • curl E, H
  • 2 +
  • H, curl E
  • 2 −

ǫ0ǫd τ E, E

  • F +

1 τ P, E

  • F

+ 1 τ E, P

  • F −
  • 1

ǫ0ǫdτ P, P

  • F

= − ǫ0ǫd 1 τ E, E

  • F + 2

1 τ P, E

  • F −

1 ǫ0ǫd 1 τ P, P

  • F

= −1 ǫ0ǫd

  • 1

τ (P − ǫ0ǫdE)

  • 2

F

. dE(t) dt = −1 ǫ0ǫdE(t)

  • 1

τ (P − ǫ0ǫdE)

  • 2

F

≤ 0.

  • N. L. Gibson (Oregon State)

Maxwell-PC Dispersive ICERM 2018 33 / 72

slide-54
SLIDE 54

Stability and Dispersion Analyses Maxwell-PC Debye Stability

Maxwell-PC Debye Replace the Debye model with the PC approximation. In two dimensions we have the 2D Maxwell-PC Debye TE scalar equations µ0 ∂H ∂t = ∂Ex ∂y − ∂Ey ∂x , (7a) ǫ0ǫ∞ ∂Ex ∂t = ∂H ∂y − ∂α0,x ∂t , (7b) ǫ0ǫ∞ ∂Ey ∂t = −∂H ∂x − ∂α0,y ∂t , (7c) A ˙

  • αx +

αx = fx, (7d) A ˙

  • αy +

αy = fy. (7e) where fx = ǫ0ǫdEx ˆ e1 and fy = ǫ0ǫdEy ˆ

  • e1. Denote

α = [ αx, αy]T.

  • N. L. Gibson (Oregon State)

Maxwell-PC Dispersive ICERM 2018 34 / 72

slide-55
SLIDE 55

Stability and Dispersion Analyses Maxwell-PC FDTD

Finite Difference Time Domain (FDTD) We now choose a discretization of the Maxwell-PC Debye model. Note that any scheme can be used independent of the spectral approach in random space employed here. The Yee Scheme (FDTD) This gives an explicit second order accurate scheme in time and space. It is conditionally stable with the CFL condition ν := c∆t h ≤ 1 √ d where ν is called the Courant number and c∞ = 1/√µ0ǫ0ǫ∞ is the fastest wave speed and d is the spatial dimension, and h is the (uniform) spatial step. The Yee scheme can exhibit numerical dispersion and dissipation.

  • N. L. Gibson (Oregon State)

Maxwell-PC Dispersive ICERM 2018 35 / 72

slide-56
SLIDE 56

Stability and Dispersion Analyses Maxwell-PC FDTD

Discrete Debye Dispersion Relation (Petropolous1994) showed that for the Yee scheme applied to the Maxwell-Debye, the discrete dispersion relation can be written ω2

c2 ǫ∆(ω) = K 2

where the discrete complex permittivity is given by ǫ∆(ω) = ǫ∞ + ǫd

  • 1

1 + iω∆τ∆

  • with discrete (mis-)representations of ω and τ given by

ω∆ = sin (ω∆t/2) ∆t/2 , τ∆ = sec(ω∆t/2)τ.

  • N. L. Gibson (Oregon State)

Maxwell-PC Dispersive ICERM 2018 36 / 72

slide-57
SLIDE 57

Stability and Dispersion Analyses Maxwell-PC FDTD

Discrete Debye Dispersion Relation (cont.) The quantity K∆ is given by K∆ = sin (k∆z/2) ∆z/2 in 1D and is related to the symbol of the discrete first order spatial difference operator by iK∆ = F(D1,∆z). In this way, we see that the left hand side of the discrete dispersion relation ω2

c2 ǫ∆(ω) = K 2

is unchanged when one moves to higher order spatial derivative approximations [Bokil-G,2012] or even higher spatial dimension [Bokil-G,2013].

  • N. L. Gibson (Oregon State)

Maxwell-PC Dispersive ICERM 2018 37 / 72

slide-58
SLIDE 58

Stability and Dispersion Analyses Maxwell-PC FDTD

Let τ Ex

h , τ Ey h , τ H h be the sets of spatial grid points on which the Ex, Ey,

and H fields, respectively, will be discretized. The discrete L2 grid norms are defined as V2

E = ∆x∆y L−1

  • ℓ=0

J−1

  • j=0
  • |Vxℓ+ 1

2 ,j|2 + |Vyℓ,j+ 1 2 |2

, (8) U2

H = ∆x∆y L−1

  • ℓ=0

J−1

  • j=0

|Uℓ+ 1

2 ,j+ 1 2 |2,

(9) with corresponding inner products. Each component αk is discretized on τ Ex

h

× τ Ey

h

with discrete L2 grid norm

  • α2

α = p

  • k=0

αk2

E,

with a corresponding inner product ( α, β)α =

p

  • k=0
  • αk, βk
  • E.
  • N. L. Gibson (Oregon State)

Maxwell-PC Dispersive ICERM 2018 38 / 72

slide-59
SLIDE 59

Stability and Dispersion Analyses PC-Debye FDTD Stability

Energy Decay and Stability Energy decay implies that the method is stable and hence convergent. Theorem (G., 2015) For n ≥ 0, let Un = [Hn− 1

2 , E n

x , E n y , αn 0,x, . . . , αn 0,y, . . .]T be the solutions of

the 2D Maxwell-PC Debye TE FDTD scheme with PEC boundary

  • conditions. If the usual CFL condition for Yee scheme is satisfied

c∞∆t ≤ h/ √ 2, then there exists the energy decay property En+1

h

≤ En

h

where the discrete energy is given by (En

h)2 =

  • √µ0H

n

  • 2

H + ||√ǫ0ǫ∞En||2 E +

  • 1

√ǫ0ǫd

  • αn
  • 2

α

.

  • N. L. Gibson (Oregon State)

Maxwell-PC Dispersive ICERM 2018 39 / 72

slide-60
SLIDE 60

Stability and Dispersion Analyses PC-Debye FDTD Stability

Energy Decay and Stability Energy decay implies that the method is stable and hence convergent. Theorem (G., 2015) For n ≥ 0, let Un = [Hn− 1

2 , E n

x , E n y , αn 0,x, . . . , αn 0,y, . . .]T be the solutions of

the 2D Maxwell-PC Debye TE FDTD scheme with PEC boundary

  • conditions. If the usual CFL condition for Yee scheme is satisfied

c∞∆t ≤ h/ √ 2, then there exists the energy decay property En+1

h

≤ En

h

where the discrete energy is given by (En

h)2 =

  • √µ0H

n

  • 2

H + ||√ǫ0ǫ∞En||2 E +

  • 1

√ǫ0ǫd

  • αn
  • 2

α

. Note: P2

F = E[P2 2] = E[P]2 + Var(P)2 2 ≈

α2

α.

  • N. L. Gibson (Oregon State)

Maxwell-PC Dispersive ICERM 2018 39 / 72

slide-61
SLIDE 61

Stability and Dispersion Analyses PC-Debye FDTD Stability

Energy Decay and Stability (cont.) Proof. First, showing that this is a discrete energy, i.e., a positive definite function of the solution, involves recognizing that (En

h)2 = µ0H n2 H + ǫ0ǫ∞(E n, AhE n)E +

1 ǫ0ǫd ( αn − E ˆ e1, A−1( αn − E ˆ e1))α with Ah positive definite when the CFL condition is satisfied, and A−1 is always positive definite (eigenvalues between τm − τr and τm + τr).

  • N. L. Gibson (Oregon State)

Maxwell-PC Dispersive ICERM 2018 40 / 72

slide-62
SLIDE 62

Stability and Dispersion Analyses PC-Debye FDTD Stability

Energy Decay and Stability (cont.) Proof. First, showing that this is a discrete energy, i.e., a positive definite function of the solution, involves recognizing that (En

h)2 = µ0H n2 H + ǫ0ǫ∞(E n, AhE n)E +

1 ǫ0ǫd ( αn − E ˆ e1, A−1( αn − E ˆ e1))α with Ah positive definite when the CFL condition is satisfied, and A−1 is always positive definite (eigenvalues between τm − τr and τm + τr). The rest follows the proof for the deterministic case [Bokil-G, 2014] to show En+1

h

− En

h

∆t = −

  • 2

En+1

h

+ En

h

  • 1

ǫ0ǫd

  • ǫ0ǫdE

n+ 1

e1 − α

n+ 1

2

  • 2

A−1 .

(10)

  • N. L. Gibson (Oregon State)

Maxwell-PC Dispersive ICERM 2018 40 / 72

slide-63
SLIDE 63

Stability and Dispersion Analyses PC-Debye FDTD Dispersion Relation

Theorem (G., 2015) The discrete dispersion relation for the Maxwell-PC Debye FDTD scheme is given by ω2

c2 ǫ∆(ω) = K 2

where the discrete expected complex permittivity is given by ǫ∆(ω) := ǫ∞ + ǫd ˆ eT

1 (I + iω∆A∆)−1 ˆ

e1 and the discrete PC matrix is given by A∆ := sec(ω∆t/2)A. The definitions of the parameters ω∆ and K∆ are the same as before. Recall the exact complex permittivity is given by ǫ(ω) = ǫ∞ + ǫdE

  • 1

1 + iωτ .

  • N. L. Gibson (Oregon State)

Maxwell-PC Dispersive ICERM 2018 41 / 72

slide-64
SLIDE 64

Stability and Dispersion Analyses PC-Debye FDTD Dispersion Analysis

Dispersion Error We define the phase error Φ for a scheme applied to a model to be Φ =

  • kEX − k∆

kEX

  • ,

(11) where the numerical wave number k∆ is implicitly determined by the corresponding dispersion relation and kEX is the exact wave number for the given model.

  • N. L. Gibson (Oregon State)

Maxwell-PC Dispersive ICERM 2018 42 / 72

slide-65
SLIDE 65

Stability and Dispersion Analyses PC-Debye FDTD Dispersion Analysis

Dispersion Error We define the phase error Φ for a scheme applied to a model to be Φ =

  • kEX − k∆

kEX

  • ,

(11) where the numerical wave number k∆ is implicitly determined by the corresponding dispersion relation and kEX is the exact wave number for the given model. We wish to examine the phase error as a function of ω∆t in the range [0, π]. ∆t is determined by hττm, while ∆x = ∆y determined by CFL condition. We note that ω∆t = 2π/Nppp, where Nppp is the number of points per period, and is related to the number of points per wavelength as, Nppw = √ǫ∞νNppp. We assume a uniform distribution and the following parameters which are appropriate constants for modeling aqueous Debye type materials: ǫ∞ = 1, ǫs = 78.2, τm = 8.1 × 10−12 sec, τr = 0.5τm.

  • N. L. Gibson (Oregon State)

Maxwell-PC Dispersive ICERM 2018 42 / 72

slide-66
SLIDE 66

Stability and Dispersion Analyses PC-Debye FDTD Dispersion Analysis

0.5 1 1.5 2 2.5 3 0.05 0.1 0.15 0.2 0.25 0.3 0.35 0.4 PC−Debye dispersion for FD with hτ=0.01, r=0.5τ, θ=0 ω ∆ t Φ M=0 M=1 M=2 M=3 0.5 1 1.5 2 2.5 3 0.05 0.1 0.15 0.2 0.25 0.3 0.35 0.4 PC−Debye dispersion for FD with hτ=0.01, r=0.9τ, θ=0 ω ∆ t Φ M=0 M=1 M=2 M=3 M=4 M=5 M=6

Figure: Plots of phase error at θ = 0 for (left column) τr = 0.5τm, (right column) τr = 0.9τm, using hτ = 0.01.

  • N. L. Gibson (Oregon State)

Maxwell-PC Dispersive ICERM 2018 43 / 72

slide-67
SLIDE 67

Stability and Dispersion Analyses PC-Debye FDTD Dispersion Analysis

0.5 1 1.5 2 2.5 3 0.05 0.1 0.15 0.2 0.25 0.3 0.35 0.4 0.45 0.5 PC−Debye dispersion for FD with hτ=0.001, r=0.5τ, θ=0 ω ∆ t Φ M=0 M=1 M=2 M=3 0.5 1 1.5 2 2.5 3 0.05 0.1 0.15 0.2 0.25 0.3 0.35 0.4 0.45 0.5 PC−Debye dispersion for FD with hτ=0.001, r=0.9τ, θ=0 ω ∆ t Φ M=0 M=1 M=2 M=3 M=4 M=5 M=6

Figure: Plots of phase error at θ = 0 for (left column) τr = 0.5τm, (right column) τr = 0.9τm, using hτ = 0.001.

  • N. L. Gibson (Oregon State)

Maxwell-PC Dispersive ICERM 2018 44 / 72

slide-68
SLIDE 68

Stability and Dispersion Analyses PC-Debye FDTD Dispersion Analysis

−5 −3 −1 23 210 60 240 90 270 120 300 150 330 180 PC−Debye dispersion for FD with hτ=0.01, r=0.5τ, ωτµ=1 M=0 M=1 M=2 M=3 −5 −3 −1 23 210 60 240 90 270 120 300 150 330 180 PC−Debye dispersion for FD with hτ=0.01, r=0.9τ, ωτµ=1 M=0 M=1 M=2 M=3 M=4 M=5 M=6

Figure: Log plots of phase error versus θ with fixed ω = 1/τm for (left column) τr = 0.5τm, (right column) τr = 0.9τm, using hτ = 0.01. Legend indicates degree M of the PC expansion.

  • N. L. Gibson (Oregon State)

Maxwell-PC Dispersive ICERM 2018 45 / 72

slide-69
SLIDE 69

Stability and Dispersion Analyses PC-Debye FDTD Dispersion Analysis

−5 −3 −1 23 210 60 240 90 270 120 300 150 330 180 PC−Debye dispersion for FD with hτ=0.001, r=0.5τ, ωτµ=1 M=0 M=1 M=2 M=3 −5 −3 −1 23 210 60 240 90 270 120 300 150 330 180 PC−Debye dispersion for FD with hτ=0.001, r=0.9τ, ωτµ=1 M=0 M=1 M=2 M=3 M=4 M=5 M=6

Figure: Log plots of phase error versus θ with fixed ω = 1/τm for (left column) τr = 0.5τm, (right column) τr = 0.9τm, using hτ = 0.001. Legend indicates degree M of the PC expansion.

  • N. L. Gibson (Oregon State)

Maxwell-PC Dispersive ICERM 2018 46 / 72

slide-70
SLIDE 70

Random Debye Summary

Summary We have presented a random ODE model for polydispersive Debye media

  • N. L. Gibson (Oregon State)

Maxwell-PC Dispersive ICERM 2018 47 / 72

slide-71
SLIDE 71

Random Debye Summary

Summary We have presented a random ODE model for polydispersive Debye media We described an efficient numerical method utilizing polynomial chaos (PC) and finite difference time domain (FDTD)

  • N. L. Gibson (Oregon State)

Maxwell-PC Dispersive ICERM 2018 47 / 72

slide-72
SLIDE 72

Random Debye Summary

Summary We have presented a random ODE model for polydispersive Debye media We described an efficient numerical method utilizing polynomial chaos (PC) and finite difference time domain (FDTD) Exponential convergence in the number of PC terms was demonstrated

  • N. L. Gibson (Oregon State)

Maxwell-PC Dispersive ICERM 2018 47 / 72

slide-73
SLIDE 73

Random Debye Summary

Summary We have presented a random ODE model for polydispersive Debye media We described an efficient numerical method utilizing polynomial chaos (PC) and finite difference time domain (FDTD) Exponential convergence in the number of PC terms was demonstrated We have proven (conditional) stability of the scheme via energy decay

  • N. L. Gibson (Oregon State)

Maxwell-PC Dispersive ICERM 2018 47 / 72

slide-74
SLIDE 74

Random Debye Summary

Summary We have presented a random ODE model for polydispersive Debye media We described an efficient numerical method utilizing polynomial chaos (PC) and finite difference time domain (FDTD) Exponential convergence in the number of PC terms was demonstrated We have proven (conditional) stability of the scheme via energy decay We have derived a discrete dispersion relation and computed phase errors

  • N. L. Gibson (Oregon State)

Maxwell-PC Dispersive ICERM 2018 47 / 72

slide-75
SLIDE 75

Maxwell-Random Lorentz system Lorentz Model

Lorentz Model We employ the physical assumption that electrons behave as damped harmonic oscillators, m¨ x + 2mν ˙ x + mω2

0x = Fdriving.

The polarization is then defined as electron dipole moment density: ¨ P + 2ν ˙ P + ω2

0P = ǫ0ω2 pE

where ω0 is the resonant frequency, ν is a damping coefficient, and ωp is referred to as a plasma frequency defined by ω2

p = (ǫs − ǫ∞)ω2 0.

  • N. L. Gibson (Oregon State)

Maxwell-PC Dispersive ICERM 2018 48 / 72

slide-76
SLIDE 76

Maxwell-Random Lorentz system Lorentz Model

Complex Permittivity Taking a Fourier transform of D = ǫE + P and inserting the convolution form of the polarization model in for P, we get ˆ D(ω) = ǫ0ǫ(ω) ˆ E(ω) where ǫ(ω) = ǫ∞ + ω2

p

ω2

0 − ω2 − i2νω.

For multiple Lorentz poles, the complex permittivity includes a (weighted) sum of mechanisms: ǫ(ω) = ǫ∞ +

Np

  • i=1

ω2

p,i

ω2

0,i − ω2 − i2νiω.

  • N. L. Gibson (Oregon State)

Maxwell-PC Dispersive ICERM 2018 49 / 72

slide-77
SLIDE 77

Maxwell-Random Lorentz system Maxwell-Random Lorentz

Random Polarization The multi-pole Lorentz model motivates a model with a continuum of Lorentz mechanisms, i.e., a distribution of dielectric parameters. We define a random polarization to be a function of a dielectric parameter treated as a random variable. The random Lorentz model is ¨ P + 2ν ˙ P + ω2

0P = ǫ0ω2 pE

with parameter ω2

0 treated as a random variable with probability

distribution F on the interval (a, b). The macroscopic polarization is taken to be the expected value of the random polarization, P(t, z) = b

a

P(t, z; ω2

0) dF(ω2 0).

  • N. L. Gibson (Oregon State)

Maxwell-PC Dispersive ICERM 2018 50 / 72

slide-78
SLIDE 78

Maxwell-Random Lorentz system Maxwell-Random Lorentz

Random Polarization

Figure: ω2

0 ∼ U(0.75ω2 0,1.25ω2 0)

  • N. L. Gibson (Oregon State)

Maxwell-PC Dispersive ICERM 2018 51 / 72

slide-79
SLIDE 79

Maxwell-Random Lorentz system Maxwell-Random Lorentz

Complex Permittivity with random ω2 Separate complex permittivity into real and imaginary parts (ǫ = ǫr + iǫi): ǫr = ǫ∞ + ω2

p(ω2 0 − ω2)

(ω2

0 − ω2)2 + 4ν2ω2

ǫi = 2ω2

pνω

(ω2

0 − ω2)2 + 4ν2ω2 .

Analytic integration is possible for uniform distribution:

E[ǫr] = 1 b − a b

a

ǫrdω2

0 = ǫ∞ +

ω2

p

2(b − a)

  • ln(ω2

0)2 − 2ω2 0ω2 + ω4 + 4ν2ω2

  • b

a

E[ǫi] = 1 b − a b

a

ǫidω2

0 =

ω2

p

(b − a)arctan ω2 − ω2 2νω

  • b

a

  • N. L. Gibson (Oregon State)

Maxwell-PC Dispersive ICERM 2018 52 / 72

slide-80
SLIDE 80

Maxwell-Random Lorentz system Maxwell-Random Lorentz

Saltwater Data

Figure: Fits for single-pole, saltwater data

  • N. L. Gibson (Oregon State)

Maxwell-PC Dispersive ICERM 2018 53 / 72

slide-81
SLIDE 81

Maxwell-Random Lorentz system Maxwell-Random Lorentz

Maxwell-Random Lorentz system

In a polydisperse Lorentz material, we have ǫ0ǫ∞ ∂E ∂t = ∇ × H − ∂P ∂t (14a) ∂H ∂t = − 1 µ0 ∇ × E (14b) ¨ P + 2ν ˙ P + ω2

0P = ǫ0ω2 pE

(14c) with P(t, x) = b

a

P(t, x; ω2

0)f (ω2 0)dω2 0.

  • N. L. Gibson (Oregon State)

Maxwell-PC Dispersive ICERM 2018 54 / 72

slide-82
SLIDE 82

Maxwell-Random Lorentz system Maxwell-Random Lorentz

Theorem (Stability of Maxwell-Random Lorentz) Let D ⊂ R2 and suppose that E ∈ C(0, T; H0(curl, D)) ∩ C 1(0, T; (L2(D))2), P ∈ C 1(0, T;

  • L2(Ω) ⊗ L2(D)

2), and H(t) ∈ C 1(0, T; L2(D)) are solutions of the weak formulation for the Maxwell-Random Lorentz system along with PEC boundary conditions. Then the system exhibits energy decay E(t) ≤ E(0) ∀t ≥ 0, where the energy E(t) is defined as E(t)2 =

  • √µ0 H(t)
  • 2

2 +

  • √ǫ0ǫ∞ E(t)
  • 2

2 +

  • ω0

ωp√ǫ0 P(t)

  • 2

F +

  • 1

ωp√ǫ0 J (t)

  • 2

F

(15) where u2

F = E[u2 2] and J := ∂P ∂t .

Proof involves showing that dE(t) dt = −1 E(t)

ǫ0ω2

p

J

  • 2

F ≤ 0.

  • N. L. Gibson (Oregon State)

Maxwell-PC Dispersive ICERM 2018 55 / 72

slide-83
SLIDE 83

Maxwell-Random Lorentz system Maxwell-PC Lorentz

Polynomial Chaos We wish to approximate the random polarization with orthogonal polynomials of the standard random variable ξ. Let ω2

0 = rξ + m and

ξ ∈ [−1, 1]. Suppressing the dimension of P and the spatial dependence, we have P(ξ, t) =

  • i=0

αi(t)φi(ξ) → ¨ P + 2ν ˙ P + ω2

0P = ǫ0ω2 pE.

Utilizing the Triple Recursion Relation for orthogonal polynomials: ξφn(ξ) = anφn+1(ξ) + bnφn(ξ) + cnφn−1(ξ). the differential equation becomes

  • i=0

[ ¨ αi(t) + 2ν ˙ αi(t) + mαi(t)] φi(ξ) + r

  • i=0

αi(t) [aiφi+1(ξ) + biφi(ξ) + ciφi−1(ξ)] = ǫ0ω2

pEφ0(ξ).

  • N. L. Gibson (Oregon State)

Maxwell-PC Dispersive ICERM 2018 56 / 72

slide-84
SLIDE 84

Maxwell-Random Lorentz system Maxwell-PC Lorentz

Galerkin Projection We apply a Galerkin Projection onto the space of polynomials of degree at most p: ¨

  • α + 2ν ˙
  • α + A

α = f A = rM + mI, M =          b0 c1 · · · a0 b1 c2 . . . ... ... ... . . . ap−2 bb−1 cp · · · ap−1 bp          . Or we can write as a first order system: ˙

  • α =

β ˙

  • β = −A

α − 2νI β + f , where f = ˆ e1ǫ0ω2

pE with ωp meaning expected value.

  • N. L. Gibson (Oregon State)

Maxwell-PC Dispersive ICERM 2018 57 / 72

slide-85
SLIDE 85

Maxwell-Random Lorentz system Maxwell-PC Lorentz

Maxwell-PC Lorentz The polynomial chaos system coupled with 1D Maxwell’s equations becomes ǫ∞ǫ0 ∂E ∂t = −∂H ∂z − β0 ∂H ∂t = − 1 µ0 ∂E ∂z ˙

  • α =

β ˙

  • β = −A

α − 2νI β + f Initial Conditions: E(0, z) = H(0, z) = α(0, z) = β(0, z) = 0 Boundary Conditions: E(t, 0) = EL(t) and E(t, zR) = 0

  • N. L. Gibson (Oregon State)

Maxwell-PC Dispersive ICERM 2018 58 / 72

slide-86
SLIDE 86

Maxwell-Random Lorentz system Maxwell-PC Lorentz-FDTD

We stagger three discrete meshes in the x and y directions and two discrete meshes in time: τ Ex

h

:=

  • xℓ+ 1

2, yj

  • |0 ≤ ℓ ≤ L − 1, 0 ≤ j ≤ J
  • τ Ey

h

:=

  • xℓ, yj+ 1

2

  • |0 ≤ ℓ ≤ L, 0 ≤ j ≤ J − 1
  • τ H

h :=

  • xℓ+ 1

2, yj+ 1 2

  • |0 ≤ ℓ ≤ L − 1, 0 ≤ j ≤ J − 1
  • τ E

t := {(tn) |0 ≤ n ≤ N}

τ H

t :=

  • tn+ 1

2

  • |0 ≤ n ≤ N − 1
  • .
  • N. L. Gibson (Oregon State)

Maxwell-PC Dispersive ICERM 2018 59 / 72

slide-87
SLIDE 87

Maxwell-Random Lorentz system Discrete Stability

Staggered L2 normed spaces

Next, we define the L2 normed spaces VE :=

  • F : τ Ex

h × τ Ey h

− → R2 | F = (Fxl+ 1

2 ,j, Fyl,j+ 1 2 )T, FE < ∞

  • (18)

VH :=

  • U : τ H

h −

→ R | U = (Ul+ 1

2 ,j+ 1 2 ), UH < ∞

  • (19)

with the following discrete norms and inner products F2

E = ∆x∆y L−1

  • ℓ=0

J−1

  • j=0
  • |Fxℓ+ 1

2 ,j|2 + |Fyℓ,j+ 1 2 |2

, ∀ F ∈ VE (20) (F, G)E = ∆x∆y

L−1

  • ℓ=0

J−1

  • j=0
  • Fxℓ+ 1

2 ,jGxℓ+ 1 2 ,j + Fyℓ,j+ 1 2 Gyℓ,j+ 1 2

  • , ∀ F, G ∈ VE

(21) U2

H = ∆x∆y L−1

  • ℓ=0

J−1

  • j=0

|Uℓ+ 1

2 ,j+ 1 2 |2, ∀ U ∈ VH

(22) (U, V )H = ∆x∆y

L−1

  • ℓ=0

J−1

  • j=0

Uℓ+ 1

2 ,j+ 1 2 Vℓ+ 1 2 ,j+ 1 2 , ∀ U, V ∈ VH.

(23)

  • N. L. Gibson (Oregon State)

Maxwell-PC Dispersive ICERM 2018 60 / 72

slide-88
SLIDE 88

Maxwell-Random Lorentz system Discrete Stability

We define a space and inner product for the random polarization in vector notation, since α and β are now 2 × p + 1 matrices: Vα :=

  • α : τ Ex

h × τ Ey h

− → R2 × Rp+1

  • α = [α0, . . . , αp], αk ∈ VE,

α where the discrete L2 grid norm and inner product are defined as

  • α2

α = p

  • k=0

αk2

E,

∀ α ∈ Vα ( α, β)α =

p

  • k=0
  • αk, βk
  • E,

∀ α, β ∈ Vα. We choose both spatial steps to be uniform and equal (∆x = ∆y = h), and require that the usual CFL condition for two dimensions holds: √ 2c∞∆t ≤ h. (24)

  • N. L. Gibson (Oregon State)

Maxwell-PC Dispersive ICERM 2018 61 / 72

slide-89
SLIDE 89

Maxwell-Random Lorentz system Discrete Stability

Theorem (Energy Decay for Maxwell-PC Lorentz-FDTD) If the stability condition (24) is satisfied, then the Yee scheme for the 2D TE mode Maxwell-PC Lorentz system satisfies the discrete identity δtE

n+ 1

2

h

= −1 E

n+ 1

2

h

ǫ0ω2

p

  • β

n+ 1

2

h

  • 2

A

(25) for all n where En

h =

 µ0(Hn+ 1

2 , Hn− 1 2 )H + √ǫ0ǫ∞ En2

E +

  • ω2

ǫ0ω2

p

  • αn
  • 2

α

+

  • 1

ǫ0ω2

p

  • βn
  • 2

α

 

1/2

(26) defines a discrete energy. In the above α2

A := (A

α, α)α given A positive definite, which is true iff r < m. Note that α2

α ≈ E[P]2 2 + StdDev(P)2 2 = E[P2 2] = P2 F so that this is a

natural extension of the Maxwell-Random Lorentz energy (15).

  • N. L. Gibson (Oregon State)

Maxwell-PC Dispersive ICERM 2018 62 / 72

slide-90
SLIDE 90

Maxwell-Random Lorentz system Random Lorentz Dispersion Relation

Theorem The dispersion relation for the Maxwell-Random Lorentz system is given by ω2 c2 ǫ(ω) = k2 where the expected complex permittivity is given by ǫ(ω) = ǫ∞ + (ǫs − ǫ∞)E

  • ω2

ω2

0 − ω2 − i2νω

  • .

Where k is the wave vector and c = 1/√µ0ǫ0 is the speed of light. The exact dispersion relation can be compared with a discrete dispersion relation to determine the amount of dispersion error.

  • N. L. Gibson (Oregon State)

Maxwell-PC Dispersive ICERM 2018 63 / 72

slide-91
SLIDE 91

Maxwell-Random Lorentz system PC-Lorentz FDTD Dispersion Analysis

Dispersion Error We define the phase error Φ for a scheme applied to a model to be Φ =

  • kEX − k∆

kEX

  • ,

(27) where the numerical wave number k∆ is implicitly determined by the corresponding discrete dispersion relation and kEX is the exact wave number for the given model.

  • N. L. Gibson (Oregon State)

Maxwell-PC Dispersive ICERM 2018 64 / 72

slide-92
SLIDE 92

Maxwell-Random Lorentz system PC-Lorentz FDTD Dispersion Analysis

Dispersion Error We define the phase error Φ for a scheme applied to a model to be Φ =

  • kEX − k∆

kEX

  • ,

(27) where the numerical wave number k∆ is implicitly determined by the corresponding discrete dispersion relation and kEX is the exact wave number for the given model. We wish to examine the phase error as a function of ω in the range around ω0. ∆t is determined by h := ω0∆t/(2π), while ∆x = ∆y are determined by the CFL condition. We assume a uniform distribution and the following parameters Lorentz material: ǫ∞ = 1, ǫs = 2.25, ν = 2.8×1015 1/sec, ω0 = 4×1016 rad/sec.

  • N. L. Gibson (Oregon State)

Maxwell-PC Dispersive ICERM 2018 64 / 72

slide-93
SLIDE 93

Maxwell-Random Lorentz system PC-Lorentz FDTD Dispersion Analysis

2 4 6 8 10 16 0.1 0.2 0.3 0.4 0.5 0.6 0.7 PC Lorentz Dispersion with h=0.1 and p=1

r=0.1

2

r=0.2

2

r=0.3

2

r=0.4

2

r=0.5

2

Figure: Plots of phase error at θ = 0.

  • N. L. Gibson (Oregon State)

Maxwell-PC Dispersive ICERM 2018 65 / 72

slide-94
SLIDE 94

Maxwell-Random Lorentz system PC-Lorentz FDTD Dispersion Analysis

2 4 6 8 10 16 0.1 0.2 0.3 0.4 0.5 0.6 0.7

h=0.1 and r=0.1 w0^2

P=1 P=2 P=3 P=4

Figure: Plots of phase error at θ = 0.

  • N. L. Gibson (Oregon State)

Maxwell-PC Dispersive ICERM 2018 66 / 72

slide-95
SLIDE 95

Maxwell-Random Lorentz system PC-Lorentz FDTD Dispersion Analysis

2 4 6 8 10 16 0.1 0.2 0.3 0.4 0.5 0.6 0.7

h=0.1 and r=0.5 w0^2

P=1 P=2 P=3 P=4

Figure: Plots of phase error at θ = 0.

  • N. L. Gibson (Oregon State)

Maxwell-PC Dispersive ICERM 2018 67 / 72

slide-96
SLIDE 96

Maxwell-Random Lorentz system PC-Lorentz FDTD Dispersion Analysis

2 4 6 8 10 16 0.01 0.02 0.03 0.04 0.05 0.06 0.07 0.08

h=0.01 and r=0.1 w0^2

P=1 P=2 P=3 P=4

Figure: Plots of phase error at θ = 0.

  • N. L. Gibson (Oregon State)

Maxwell-PC Dispersive ICERM 2018 68 / 72

slide-97
SLIDE 97

Maxwell-Random Lorentz system PC-Lorentz FDTD Dispersion Analysis

2 4 6 8 10 16 0.1 0.2 0.3 0.4 0.5 0.6 0.7

h=0.01 and r=0.5 w0^2

P=1 P=2 P=3 P=4 P=5 P=6

Figure: Plots of phase error at θ = 0.

  • N. L. Gibson (Oregon State)

Maxwell-PC Dispersive ICERM 2018 69 / 72

slide-98
SLIDE 98

Maxwell-Random Lorentz system PC-Lorentz FDTD Dispersion Analysis

2 4 6 8 10 16 1 2 3 4 5 6 7 8 10 -3

h=0.001 and r=0.1 w0^2

P=2 P=3 P=4

Figure: Plots of phase error at θ = 0.

  • N. L. Gibson (Oregon State)

Maxwell-PC Dispersive ICERM 2018 70 / 72

slide-99
SLIDE 99

Future Directions

Future Directions

Extend to

Drude meta-material models nonlinear polarization models viscoelastic system (partially done)

Inverse problems from (actual) time-domain data

  • N. L. Gibson (Oregon State)

Maxwell-PC Dispersive ICERM 2018 71 / 72

slide-100
SLIDE 100

References

Bokil, V. A. & Gibson, N. L. (2012), Analysis of Spatial High Order Finite Difference Methods for Maxwell’s equations in dispersive media, IMA

  • J. Numer. Anal. 32 (3): 926-956.

Bokil, V. A. & Gibson, N. L. (2013), Stability and Dispersion Analysis

  • f High Order FDTD Methods for Maxwell’s Equations in Dispersive Media,

Contemporary Mathematics, Vol. 586. Bokil, V. A. & Gibson, N. L. (2014), Convergence Analysis of Yee Schemes for Maxwell’s Equations in Debye and Lorentz Dispersive Media, IJNAM, 11(4), 657-687. Gibson, N. L. (2015), A Polynomial Chaos Method for Dispersive Electromagnetics, Comm. in Comp. Phys., vol. 18, issue 5, pp 1234-1263. Alvarez, Jacky & Fisher, Andrew (2017), Approximating Dispersive Materials With Parameter Distributions in the Lorentz Model, Oregon State University Math REU.

  • N. L. Gibson (Oregon State)

Maxwell-PC Dispersive ICERM 2018 72 / 72

slide-101
SLIDE 101
  • N. L. Gibson (Oregon State)

Maxwell-PC Dispersive ICERM 2018 73 / 72

slide-102
SLIDE 102

Appendix Polynomial Chaos

Polynomial Chaos: Simple example Consider the first order, constant coefficient, linear IVP ˙ y + ky = g, y(0) = y0 with k = k(ξ) = ξ, ξ ∼ N(0, 1), g(t) = 0. We can represent the solution y as a Polynomial Chaos (PC) expansion in terms of (normalized) orthogonal Hermite polynomials Hj: y(t, ξ) =

  • j=0

αj(t)φj(ξ), φj(ξ) = Hj(ξ). Substituting into the ODE we get

  • j=0

˙ αj(t)φj(ξ) +

  • j=0

αj(t)ξφj(ξ) = 0.

  • N. L. Gibson (Oregon State)

Maxwell-PC Dispersive ICERM 2018 74 / 72

slide-103
SLIDE 103

Appendix Polynomial Chaos

Triple recursion formula

  • j=0

˙ αj(t)φj(ξ) +

  • j=0

αj(t)ξφj(ξ) = 0. We can eliminate the explicit dependence on ξ by using the triple recursion formula for Hermite polynomials ξHj = jHj−1 + Hj+1. Thus

  • j=0

˙ αj(t)φj(ξ) +

  • j=0

αj(t)(jφj−1(ξ) + φj+1(ξ)) = 0.

  • N. L. Gibson (Oregon State)

Maxwell-PC Dispersive ICERM 2018 75 / 72

slide-104
SLIDE 104

Appendix Polynomial Chaos

Galerkin Projection onto span({φi}p

i=0)

In order to approximate y we wish to find a finite system for at least the first few αi. We take the weighted inner product with the ith basis, i = 0, . . . , p,

  • j=0

˙ αj(t)φj, φiW + αj(t)(jφj−1, φiW + φj+1, φiW ) = 0, where f (ξ), g(ξ)W :=

  • f (ξ)g(ξ)W (ξ)dξ.
  • N. L. Gibson (Oregon State)

Maxwell-PC Dispersive ICERM 2018 76 / 72

slide-105
SLIDE 105

Appendix Polynomial Chaos

Galerkin Projection onto span({φi}p

i=0)

In order to approximate y we wish to find a finite system for at least the first few αi. We take the weighted inner product with the ith basis, i = 0, . . . , p,

  • j=0

˙ αj(t)φj, φiW + αj(t)(jφj−1, φiW + φj+1, φiW ) = 0, where f (ξ), g(ξ)W :=

  • f (ξ)g(ξ)W (ξ)dξ.

By orthogonality, φj, φiW = φi, φiW δij, we have ˙ αiφi, φiW + (i + 1)αi+1φi, φiW + αi−1φi, φiW = 0, i = 0, . . . , p.

  • N. L. Gibson (Oregon State)

Maxwell-PC Dispersive ICERM 2018 76 / 72

slide-106
SLIDE 106

Appendix Polynomial Chaos

Deterministic ODE system Let α represent the vector containing α0(t), . . . , αp(t). Assuming α−1(t), αp+1(t), etc., are identically zero, the system of ODEs can be written ˙

  • α + M

α = 0, with M =         1 1 2 ... ... ... ... ... p 1         The degree p PC approximation is y(t, ξ) ≈ yp(t, ξ) = p

j=0 αj(t)φj(ξ).

The mean value E[y(t, ξ)] ≈ E[yp(t, ξ)] = α0(t). The variance Var(y(t, ξ)) ≈ p

j=1 αj(t)2.

  • N. L. Gibson (Oregon State)

Maxwell-PC Dispersive ICERM 2018 77 / 72

slide-107
SLIDE 107

Appendix Polynomial Chaos

Figure: Convergence of error with Gaussian random variable by Hermitian-chaos.

  • N. L. Gibson (Oregon State)

Maxwell-PC Dispersive ICERM 2018 78 / 72

slide-108
SLIDE 108

Appendix Polynomial Chaos

Generalizations Consider the non-homogeneous IVP ˙ y + ky = g(t), y(0) = y0 with k = k(ξ) = σξ + µ, ξ ∼ N(0, 1), then ˙ αi + σ [(i + 1)αi+1 + αi−1] + µαi = g(t)δ0i, i = 0, . . . , p,

  • r the deterministic ODE system is

˙

  • α + (σM + µI)

α = g(t) e1. Note that the initial condition for the PC system is α(0) = y0 e1.

  • N. L. Gibson (Oregon State)

Maxwell-PC Dispersive ICERM 2018 79 / 72

slide-109
SLIDE 109

Appendix Polynomial Chaos

Generalizations For any choice of family of orthogonal polynomials, there exists a triple recursion formula. Given the arbitrary relation ξφj = ajφj−1 + bjφj + cjφj+1 (with φ−1 = 0) then the matrix above becomes M =         b0 a1 c0 b1 a2 ... ... ... ... ... ap cp−1 bp        

  • N. L. Gibson (Oregon State)

Maxwell-PC Dispersive ICERM 2018 80 / 72

slide-110
SLIDE 110

Appendix Polynomial Chaos

Generalized Polynomial Chaos

Table: Popular distributions and corresponding orthogonal polynomials.

Distribution Polynomial Support Gaussian Hermite (−∞, ∞) gamma Laguerre [0, ∞) beta Jacobi [a, b] uniform Legendre [a, b] Note: lognormal random variables may be handled as a non-linear function (e.g., Taylor expansion) of a normal random variable.

  • N. L. Gibson (Oregon State)

Maxwell-PC Dispersive ICERM 2018 81 / 72