Polynomial Chaos Approach for Maxwell's Equations in...

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Polynomial Chaos Approach for Maxwell’s Equations in Dispersive Media Prof. Nathan L. Gibson Department of Mathematics Applied Mathematics and Computation Seminar March 15, 2013 Prof. Gibson (OSU) PC-FDTD AMCS 2013 1 / 41

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Polynomial Chaos Approach for Maxwell’sEquations in Dispersive Media

Prof. Nathan L. Gibson

Department of Mathematics

Applied Mathematics and Computation SeminarMarch 15, 2013

Prof. Gibson (OSU) PC-FDTD AMCS 2013 1 / 41

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Acknowledgements

Collaborators

H. T. Banks (NCSU)

V. A. Bokil (OSU)

W. P. Winfree (NASA)

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)

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Outline

1 Maxwell’s EquationsDispersive MediaPolarization ModelsDistribution of Parameters

2 Dispersion AnalysisDiscrete Dispersion

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Maxwell’s Equations

Maxwell’s Equations

∂D

∂t= ∇×H− J in Ω× (0,T]

∂B

∂t= −∇× E in Ω× (0,T]

∇ ·D = ∇ · B = 0 in Ω× (0,T]

E(0, x) = E0(x); H(0, x) = H0(x) in Ω

E× n = 0 on ∂Ω, t ∈ (0,T]

E = Electric field vector

H = Magnetic field vector

J = Current density

D = Electric flux density

B = Magnetic flux density

n = Unit outward normal to ∂ΩProf. Gibson (OSU) PC-FDTD AMCS 2013 4 / 41

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Maxwell’s Equations

Constitutive Laws

Maxwell’s equations are completed by constitutive laws that describe theresponse of the medium to the electromagnetic field.

D = εE + P

B = µH + M

J = σE + Js

P = Polarization

M = Magnetization

Js = Source Current

ε = Electric permittivity

µ = Magnetic permeability

σ = Electric Conductivity

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Maxwell’s Equations Dispersive Media

Complex permittivity

We can usually define P in terms of a convolution

P(t, x) = g ∗ E(t, x) =

∫ t

0g(t − s, x; q)E(s, x)ds,

where g is the dielectric response function (DRF).

In the frequency domain D = εE + gE = ε0ε(ω)E, where ε(ω) iscalled the complex permittivity.

ε(ω) described by the polarization model

We are interested in ultra-wide bandwidth electromagnetic pulseinterrogation of dispersive dielectrics, therefore we want an accuraterepresentation of ε(ω) over a broad range of frequencies.

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Maxwell’s Equations Dispersive Media

Dry skin data

102

104

106

108

1010

101

102

103

f (Hz)

ε

True DataDebye ModelCole−Cole Model

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

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Maxwell’s Equations Dispersive Media

Dry skin data

102

104

106

108

1010

10−4

10−3

10−2

10−1

100

101

f (Hz)

σ

True DataDebye ModelCole−Cole Model

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

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Maxwell’s Equations Polarization Models

P(t, x) = g ∗ E(t, x) =

∫ t

0g(t − s, x; q)E(s, x)ds,

Debye model [1929] q = [εd , τ ]

g(t, x) = ε0εd/τ e−t/τ

or τ P + P = ε0εdE

or ε(ω) = ε∞ +εd

1− ωτ

with εd := εs − ε∞ and τ a relaxation time.

Cole-Cole model [1936] (heuristic generalization)q = [εd , τ, α]

ε(ω) = ε∞ +εd

1 + (iωτ)1−α

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Maxwell’s Equations Polarization Models

Dispersive Dielectrics

Debye Material

Input is five cycles (periods) of a sine curve.

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Maxwell’s Equations Polarization Models

Dispersive Media

0 0.2 0.4 0.6 0.8−1000

−500

0

500

1000

z

E

Time=5.0ns

0 0.2 0.4 0.6 0.8−80

−60

−40

−20

0

20

40

Time=10.0ns

E

z

Figure: Debye model simulations.

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Maxwell’s Equations Polarization Models

Scalar Equations in Two Dimensions (cont)

Letting H = Hz , we have the 2D Maxwell-Debye TE scalar equations:

∂H

∂t=

1

µ0

(∂Ex

∂y− ∂Ey

∂x

),

ε0ε∞∂Ex

∂t=∂H

∂y− ∂Px

∂t,

ε0ε∞∂Ey

∂t= −∂H

∂x− ∂Py

∂t,

∂Px

∂t=ε0εdτ

Ex −1

τPx ,

∂Py

∂t=ε0εdτ

Ey −1

τPy .

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Maxwell’s Equations Polarization Models

Stability Estimates for Maxwell-Debye

Theorem (Li2010)

For Ω ∈ R2, let E, P, and H be the solutions to the 2D Maxwell-DebyeTE scalar equations with PEC boundary conditions. Then the Debyemodel satisfies the stability estimate

E(t) ≤ E(0)

where the energy is defined as

E(t) = ||√µ0H(t)||2L2 + ||√ε0ε∞E(t)||2L2 +

∣∣∣∣∣∣∣∣ 1√ε0εd

P(t)

∣∣∣∣∣∣∣∣2L2

.

and the L2(Ω) norm is defined as

‖U(t)‖22 =

∫Ω|U(z , t)|2dz .

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Maxwell’s Equations Distribution of Relaxation Times

Motivation for Distributions

The Cole-Cole model corresponds to a fractional order ODE in thetime-domain and is difficult to simulate

Debye is efficient to simulate, but does not represent permittivity well

Better fits to data are obtained by taking linear combinations ofDebye models (discrete distributions), idea comes from the knownexistence of multiple physical mechanisms: multi-pole debye (likestair-step approximation)

An alternative approach is to consider the Debye model but with a(continuous) distribution of relaxation times [von Schweidler1907]

Empirical measurements suggest a log-normal or Beta distribution[Wagner1913] (but uniform is easier)

Using Mellin transforms, can show Cole-Cole corresponds to acontinuous distribution

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Maxwell’s Equations Fit to dry skin data with uniform distribution

102

104

106

108

1010

102

103

f (Hz)

ε

True DataDebye (27.79)Cole−Cole (10.4)Uniform (13.60)

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

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Maxwell’s Equations Fit to dry skin data with uniform distribution

102

104

106

108

1010

10−3

10−2

10−1

100

101

f (Hz)

σ

True DataDebye (27.79)Cole−Cole (10.4)Uniform (13.60)

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

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Maxwell’s Equations Distribution of Parameters

Distributions of Parameters

To account for the effect of possible multiple parameter sets q, consider

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) =

∫ t

0h(t − s, x; F )E(s, x)ds.

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Maxwell’s Equations Distribution of Parameters

Random Polarization

Alternatively we can define the random polarization P(t, x; τ) to be thesolution to

τ P + P = ε0εdE

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 taketo be the expected value of the random polarization at each point (t, x)

P(t, x) =

∫ τb

τa

P(t, x; τ)f (τ)dτ.

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Dispersion Analysis

Maxwell-Random Debye system

In a polydisperse Debye material, we have

ε0ε∞∂E

∂t= ∇×H− P

∂t(1a)

∂H

∂t= − 1

µ0∇× E (1b)

τ∂P∂t

+ P = ε0εdE (1c)

with

P(t, x) =

∫ τb

τa

P(t, x; τ)f (τ)dτ.

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Dispersion Analysis Dispersion Relation

Theorem (Gibson2013)

The dispersion relation for the system (1) is given by

ω2

c2ε(ω) = |~k |2

where the complex permittivity is given by

ε(ω) = ε∞ + εdE[

1

1− iωτ

]Here, ~k is the wave number and c = 1/

√µ0ε0 is the speed of light in

freespace.Note: for a uniform distribution, this has an analytic form since

E[

1

1− iωτ

]=

1

2τrω

[arctan(ωτ)− i

1

2ln(1 + (ωτ)2

)]τ=τm+τr

τ=τm−τr

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Dispersion Analysis Dispersion Relation

Proof: (for 2D)

Letting H = Hz , we have the 2D Maxwell-Random Debye TE scalarequations:

∂H

∂t=

1

µ0

(∂Ex

∂y− ∂Ey

∂x

), (2a)

ε0ε∞∂Ex

∂t=∂H

∂y− ∂Px

∂t, (2b)

ε0ε∞∂Ey

∂t= −∂H

∂x− ∂Py

∂t, (2c)

τPx

∂t+ Px = ε0εdEx (2d)

τPy

∂t+ Py = ε0εdEy . (2e)

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Dispersion Analysis Dispersion Relation

Proof: (cont.)

Assume plane wave solutions of the form

V = V e(kxx+kyy−ωt)

and let ~x = (x , y)T and ~k = (kx , ky )T . Then (2) becomes

−iωH =1

µ0

(iky Ex − ikx Ey

), (3a)

−ε0ε∞iωEx = iky H − (−iωPx), (3b)

−ε0ε∞iωEy = −ikx H − (−iωPy ), (3c)

−iωτ Px + Px = ε0εd Ex (3d)

−iωτ Py + Py = ε0εd Ey . (3e)

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Dispersion Analysis Dispersion Relation

Proof: (cont.)

By (3d) we have

Px = E[Px ] = ε0εd ExE[

1

1− iωτ

](4)

Substituting into (3b) we have

−ε0ε∞iωEx = iky H +

(iωε0εd ExE

[1

1− iωτ

]),

−iωε0

(ε∞ + εdE

[1

1− iωτ

])Ex = iky H,

−iωε0ε(ω)Ex = iky H. (5)

Similarly for combining (3e) and (3c)

−iωε0ε(ω)Ey = −ikx H. (6)

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Dispersion Analysis Dispersion Relation

Proof: (cont.)

Substituting both (5) and (6) into (3a) yields

−iωH =1

µ0

((iky )2

−iωε0ε(ω)+

(ikx)2

−iωε0ε(ω)

)H,

−(iω)2µ0ε0ε(ω) = k2y + k2

x

ω2

c2ε(ω) = |~k |2

The proof is similar in 1 and 3 dimensions.

The exact dispersion relation will be compared with a discretedispersion relation to determine the amount of dispersion error.

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Dispersion Analysis Discrete Dispersion

Finite Difference Methods

The Yee Scheme

In 1966 Kane Yee originated a set of finite-difference equations for thetime dependent Maxwell’s curl equations.

The finite difference time domain (FDTD) or Yee algorithm solves forboth the electric and magnetic fields in time and space using thecoupled Maxwell’s curl equations rather than solving for the electricfield alone (or the magnetic field alone) with a wave equation.

Approximates first order derivatives very accurately by evaluating onstaggered grids.

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Dispersion Analysis Discrete Dispersion

Yee Scheme in One Space Dimension

Staggered Grids: The electric field/flux is evaluated on the primarygrid in both space and time and the magnetic field/flux is evaluatedon the dual grid in space and time.

The Yee scheme is

H|n+ 12

`+ 12

− H|n−12

`+ 12

∆t= − 1

µ

E |n`+1 − E |n`∆z

E |n+1` − E |n`

∆t= −1

ε

H|n+ 12

`+ 12

− H|n+ 12

`− 12

∆z

-h

tn+ 12

tn+1

v v v v v. . . z− 5

2

z−2 z− 32

z−1 z− 12

z0 z1z 12

z2z 32

z 52. . .

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Dispersion Analysis Discrete Dispersion

The FDTD or Yee grid in 1D

¡¡µ

¡¡µ

¡¡µ

¡¡µ

@@I

@@I

@@I

@@I

N N N Nf

f

¡¡µ

¡¡µ

¡¡µ

¡¡µ

@@I

@@I

@@I

@@I

H H H H

H H H H

f

f

¡¡¡µ

¡¡¡µ

¡¡¡µ

¡¡¡µ

@@@I

@@@I

@@@I

@@@I

¡¡¡µ

¡¡¡µ

¡¡¡µ

¡¡¡µ

@@@I

@@@I

@@@I

@@@I

N N N N6 6 6 6 6

¡¡µ

¡¡µ

¡¡µ

¡¡µ

@@I

@@I

@@I

@@I

6 6 6 6 6

6 6 6 6 6

f f f f f f f f f fn

n + 1

n + 2

k k+1 . . .

n +12

n +32

k+12 k+

32

?

( H)n+2k+ 1

2

?

(E )n+ 3

2k+2

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Dispersion Analysis Discrete Dispersion

This gives an explicit second order accurate scheme in both time andspace.

It is conditionally stable with the CFL condition

ν =c∆t

h≤ 1√

d

where ν is called the Courant number and c = 1/√εµ and d is the

spatial dimension.

The initial value problem is well-posed and the scheme is consistentand stable. The method is convergent by the Lax-RichtmyerEquivalence Theorem.

The Yee scheme can exhibit numerical dispersion.

Dispersion error can be reduced by decreasing the mesh size orresorting to higher order accurate finite difference approximations.

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Dispersion Analysis Discrete Dispersion

Extensions of the Yee Scheme to Dispersive Media

The ordinary differential equation for the polarization is discretizedusing an averaging of zero order terms.

The resulting scheme remains second-order accurate in both time andspace with the same CFL condition.

However, the Yee scheme for the Maxwell-Debye system is nowdissipative in addition to being dispersive.

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Dispersion Analysis Discretization

Yee Scheme for Maxwell-Debye System (in 1D)

ε0ε∞∂E

∂t= −∂H

∂z− ∂P

∂t

µ0∂H

∂t= −∂E

∂z

τ∂P

∂t= ε0εdE − P

become

ε0ε∞E

n+ 12

j − En− 1

2j

∆t= −

Hnj+ 1

2

− Hnj− 1

2

∆z−

Pn+ 1

2j − P

n− 12

j

∆t

µ0

Hn+1j+ 1

2

− Hnj+ 1

2

∆t= −

En+ 1

2j+1 − E

n+ 12

j

∆z

τP

n+ 12

j − Pn− 1

2j

∆t= ε0εd

En+ 1

2j + E

n− 12

j

2−

Pn+ 1

2j + P

n− 12

j

2.

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Dispersion Analysis Discretization

Discrete Debye Dispersion Relation

(Petropolous1994) showed that for the Yee scheme applied to the(deterministic) Maxwell-Debye, the discrete dispersion relation can bewritten

ω2∆

c2ε∆(ω) = K 2

where the discrete complex permittivity is given by

ε∆(ω) = ε∞ + εd

(1

1− iω∆τ∆

)with discrete representations of ω and τ given by

ω∆ =sin (ω∆t/2)

∆t/2, τ∆ = sec(ω∆t/2)τ

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Dispersion Analysis Discretization

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 spatialdifference operator by

iK∆ = F(D1,∆z).

In this way, we see that the left hand side of the discrete dispersion relation

ω2∆

c2ε∆(ω) = K 2

is unchanged when one moves to higher order spatial derivativeapproximations (Bokil-Gibson2011) or even higher spatial dimension.

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Dispersion Analysis Discretization

Polynomial Chaos

Apply Polynomial Chaos (PC) method to approximate the randompolarization

τ P + P = ε0εdE , τ = τ(ξ) = τrξ + τm

resulting in(τr M + τmI )~α + ~α = ε0εdE e1

orA~α + ~α = ~f .

The macroscopic polarization, the expected value of the randompolarization at each point (t, x), is simply

P(t, x ; F ) = E[P] ≈ α0(t, x).

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Dispersion Analysis Discretization

The discretization of the PC system

A~α + ~α = ~f

is performed similarly to the deterministic system in order to preservesecond order accuracy. Applying second order central differences to

~αn+ 1

2j = ~α(tn, zj):

A~α

n+ 12

j − ~αn− 12

j

∆t+~α

n+ 12

j + ~αn− 1

2j

2=~f

n+ 12

j + ~fn− 1

2j

2. (7)

Couple this with the equations from above:

ε0ε∞E

n+ 12

j − En− 1

2j

∆t= −

Hnj+ 1

2

− Hnj− 1

2

∆z−

αn+ 1

20,j − α

n− 12

0,j

∆t(8a)

µ0

Hn+1j+ 1

2

− Hnj+ 1

2

∆t= −

En+ 1

2j+1 − E

n+ 12

j

∆z. (8b)

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Dispersion Analysis Discretization

Energy Decay and Stability

Theorem (Gibson2013)

For n ≥ 0, let Un = [Hn,Enx ,E

ny , α

n0,x , . . . , α

n0,y , . . .]

T be the solutions ofthe 2D TE mode Maxwell-PC Debye FDTD scheme with PEC boundaryconditions. If the usual CFL condition for Yee scheme is satisfiedc∆t ≤ ∆z/

√2, then there exists the energy decay property

En+1h ≤ En

h

where

Enh =

∣∣∣∣∣∣√µ0Hn∣∣∣∣∣∣2

H+ ||√ε0ε∞En||2E +

∣∣∣∣∣∣∣∣ 1√ε0εd

~αn

∣∣∣∣∣∣∣∣2α

.

Note: E[‖P‖2] = ‖E[P]2 + Var(P)‖2 ≈ ‖~α‖2α

Energy decay implies that the method is (conditionally) stable and henceconvergenent.

Prof. Gibson (OSU) PC-FDTD AMCS 2013 35 / 41

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Dispersion Analysis Discretization

Energy Decay and Stability (cont.)

Proof.

Involves recognizing that

(Enh )2 = µ0‖H

n‖2H + ε0ε∞(En,AhEn)E +

1

ε0εd(~αn − E e1,A

−1(~αn − E e1))2α

with Ah positive definite when the CFL condition is satisfied, and A−1 isalways positive definite (eigenvalues between τm − τr and τm + τr ).

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Dispersion Analysis Discretization

Theorem (Gibson2013)

The discrete dispersion relation for the Maxwell-PC Debye FDTD schemein (8) and (7) is given by

ω2∆

c2ε∆(ω) = K 2

where the discrete complex permittivity is given by

ε∆(ω) := ε∞ + εd eT1 (I − iω∆A∆)−1 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

ε(ω) = ε∞ + εdE[

1

1− iωτ

]Prof. Gibson (OSU) PC-FDTD AMCS 2013 37 / 41

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Dispersion Analysis Discretization

Proof: (for 1D)

Assume plane wave solutions of the form

V nj = V ei(kj∆z−ωn∆t)

andαn`,j = α`ei(kj∆z−ωn∆t)

Substitute into (8b)

µ0Hei(k(j+ 12

)∆z−ω(n+ 12

)∆t)(e−iω∆t

2 − eiω∆t

2

)/∆t

= Eei(k(j+ 12

)∆z−ω(n+ 12

)∆t)(e

ik∆z2 − e

−ik∆z2

)/∆z

µ0H

(−2i

∆tsin(ω∆t/2)

)= −E

(2i

∆zsin(k∆z/2)

)(µ0∆z

∆t

)H sin(ω∆t/2) = E sin(k∆z/2) (9)

Prof. Gibson (OSU) PC-FDTD AMCS 2013 38 / 41

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Dispersion Analysis Discretization

Proof: (cont.)

Similarly (8a) yields(ε0ε∞

∆z

∆tE +

∆z

∆tα0

)sin(ω∆t/2) = H sin(k∆z/2) (10)

and (7) yields

(−2i

∆tsin(ω∆t/2)

)+ cos(ω∆t/2)α = ε0εd cos(ω∆t/2)E e1 (11)

which impliesα0 = eT

1 (I − iω∆A∆)−1 e1εoεd E . (12)

The rest of the proof follows as before.

Note that the same relation holds in 2 and 3D as well as with higher orderaccurate spatial difference operators.

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Dispersion Analysis Discretization

Dispersion Error

We define the phase error Φ for any method applied to a particular modelto be

Φ =

∣∣∣∣kEX − k∆

kEX

∣∣∣∣ , (13)

where the numerical wave number k∆ is implicitly determined by thecorresponding dispersion relation and kEX is the exact wave number forthe given model.

We wish to examine the phase error as a function of ω∆t in therange [0, π].

We note that ω∆t = 2π/Nppp, where Nppp is the number of pointsper period, and is related to the number of points per wavelength as,Nppw =

√ε∞νNppp.

We assume the following parameters which are appropriate constantsfor modeling water Debye type materials:

ε∞ = 1, εs = 78.2, τm = 8.1× 10−12 sec, τr = 0.5τm.

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Dispersion Analysis Discretization

0 0.5 1 1.5 2 2.5 3

0.1

0.2

0.3

0.4

0.5

0.6

0.7

Debye dispersion for FD with hτ=0.1

ω ∆ t

Φ

degree=0, r=0.5τdegree=1, r=0.5τdegree=2, r=0.5τ

0 0.1 0.2 0.3 0.4 0.5 0.6 0.7

0.05

0.1

0.15

0.2

0.25

Debye dispersion for FD with hτ=0.1

ω ∆ t

Φ

degree=0, r=0.5τdegree=1, r=0.5τdegree=2, r=0.5τ

0 0.5 1 1.5 2 2.5 3

0.02

0.04

0.06

0.08

0.1

0.12

0.14

Debye dispersion for FD with hτ=0.01

ω ∆ t

Φ

degree=0, r=0.5τdegree=1, r=0.5τdegree=2, r=0.5τ

0 0.1 0.2 0.3 0.4 0.5 0.6 0.7

0.005

0.01

0.015

0.02

0.025

0.03

0.035

0.04

0.045

0.05

Debye dispersion for FD with hτ=0.01

ω ∆ t

Φ

degree=0, r=0.5τdegree=1, r=0.5τdegree=2, r=0.5τ

Prof. Gibson (OSU) PC-FDTD AMCS 2013 41 / 41