Waves in composites and metamaterials/Continuum limit and propagator matrix

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The content of these notes is based on the lectures by Prof. Graeme W. Milton (University of Utah) given in a course on metamaterials in Spring 2007.

Previous Lecture

Recall from the previous lecture that we have been dealing with the TE equation [1]

[μ(z)ddz(μ(z)1ddz)+ω2ϵ(z)μ(z)kx2]E~y=0

where

Ey(x,z)=E~y(z)e±ikxx.

For a a multilayered medium with N layers, we found that in the j-th layer

(1)E~yj(z)=Aj[exp(ikzjz)+R~j,j+1exp(ikzjz+2ikzjdj)]

where R~j,j+1 is a generalized reflection coefficient. This coefficient can be obtained from a recursion relation of the form

(2)R~j,j+1=Rj,j+1+R~j+1,j+2exp[2ikz,j+1(dj+1dj)]1+Rj,j+1R~j+1,j+2exp[2ikz,j+1(dj+1dj)]

where

(3)Rj,j+1=μj+1kz,jμjkz,j+1μj+1kz,j+μjkz,j+1

is the Fresnel reflection coefficient for TE waves. Equation (3) may also be written as

(4)Rj,j+1=kz,jμjkz,j+1μj+1kz,jμj+kz,j+1μj+1.

We will now proceed to determine the generalized reflection coefficient in the continuum limit.

Continuum Limit

Consider a medium where the layer thickness if Δ. Denote the reflection coefficient and the generalized reflection coefficient at the interface z=dj as R(z) and R~(z), respectively. Also denote the phase velocity kz,j+1 just below the interface as kz(zΔ/2) and the permeability μj+1 as μ(zΔ/2). \footnote {This implies that we are measuring the phase velocity and the permeability at the center of the layer. However, this is not strictly necessary and we could alternatively measure these quantities at zΔ.}

Then, equation (2) can be written as

(5)R~(z)=R(z)+R~(zΔ)exp[2ikz(zΔ/2)Δ]1+R(z)R~(zΔ)exp[2ikz(zΔ/2)Δ]

where

R(z)=kz(z+Δ/2)μ(z+Δ/2)kz(zΔ/2)μ(zΔ/2)kz(z+Δ/2)μ(z+Δ/2)+kz(zΔ/2)μ(zΔ/2)=k~(z+Δ/2)k~(zΔ/2)k~(z+Δ/2)+k~(zΔ/2)

with

k~:=kzμ.

Expanding in Taylor series about z and ignoring higher order terms, we get

(6)R(z)k~(z)+Δ/2k~'(z)k~(z)+Δ/2k~'(z)k~(z)+Δ/2k~'(z)+k~(z)Δ/2k~'(z)=Δk~'(z)2k~(z).

Similarly, igoring powers Δ2 and higher, we get

(7)exp[2ikz(zΔ/2)Δ]1+2Δikz(z)

and

(8)R~(zΔ)R~(z)ΔR~'(z).

Plugging the expansions (7) and (8) into (5) gives

(9)R~(z)R(z)+[R~(z)ΔR~'(z)][1+2Δikz(z)]1+R(z)[R~(z)ΔR~'(z)][1+2Δikz(z)].

Substituting (6) into (9) and dropping terms containing Δ2 and higher gives

(10)R~(z)Δk~'(z)2k~(z)+R~(z)ΔR~'(z)+2Δikz(z)R~(z)1+Δk~'(z)2k~(z)R~(z).

If we assume that Δk~' is small such that the denominator can be expanded in a series, we get

(11)R~(z)[Δk~'(z)2k~(z)+R~(z)ΔR~'(z)+2Δikz(z)R~(z)][1Δk~'(z)2k~(z)R~(z)+O(Δ2)].

After expanding and ingoring terms containing Δ2, we get

(12)R~(z)Δk~'(z)2k~(z)+R~(z)ΔR~'(z)+2Δikz(z)R~(z)Δk~'(z)2k~(z)[R~(z)]2

or,

(13)R~'(z)=2ikz(z)R~(z)+k~'(z)2k~(z){1[R~(z)]2}.Ricotti equation

We thus get an equation that gives a continuous representation of the generalized reflection coefficient R~(z). Equation (13) can be solved numerically using the Runge-Kutta method.

For example, in the stuation shown in Figure 1, the generalized reflectivity coefficient at the point z1 is R~(z1) while that at point z0 is 0. If we wish to determine the value of R~(zi) at a point inside the smoothly varying layer, then one possibility is to assume that μ(z) and ϵ(z) is constant for z>zi and compute the value of R~ in the usual manner.

File:Lec12Fig1.jpg
Figure 1. Reflectivity in a smoothly graded layered material.

There can also be a situation where there are a few isolated strong discontinuities inside the graded layer as shown in Figure 2. If there is a discontinuity at zc, we can use the discrete solution with layer thickness 0 at the discontinuity.

File:Lec12Fig2.jpg
Figure 2. Reflectivity in a smoothly graded material with a strong discontinuity.

Then, from (2), at the discontinuity

(14)R~(zc+)=R(zc)+R~(zc)1+R(zc)R~(zc).

Also, from (4)

(15)R(zc)=kz+μ+kzμkz+μ++kzμ.

Hence we can find the generalized reflection coefficients at isolated discontinuities within the material.

Determining the coefficients Aj

Recall equation (1):

E~yj(z)=Aj[exp(ikzjz)+R~j,j+1exp(ikzjz+2ikzjdj)].

So far we have determine the value of R~ is this equation. But how do we determine the coefficients Aj in multilayered media?

Let us start with the coefficients for a single layer that we determined in the previous lecture. We had

(16)A2=T12A1exp[i(kz1kz2)d1]1R21R23exp[2ikz2(d2d1)]

where

T12=2μ2kz1μ2kz1+μ1kz2.

We can rewrite (16) as

(17)A2exp(ikz2d1)=T12A1exp(ikz1d1)1R21R23exp[2ikz2(d2d1)]

Using the same arguments as before, we can generalize (17) to a medium with N layers. Thus, for the j-th layer, we have

(18)Ajexp(ikz,jdj1)=Tj1,jAj1exp(ikz,j1dj1)1Rj,j1R~j,j+1exp[2ikz,j(djdj1)].

Define

Sj1,j:=Tj1,j1Rj,j1R~j,j+1exp[2ikz,j(djdj1)].

Then we can write (18) as

(19)Ajexp(ikz,jdj1)=Sj1,jAj1exp(ikz,j1dj1)=Sj1,jAj1exp(ikz,j1dj2)exp[ikz,j1(dj1dj2)].

The second of equations (19) gives us a recurrence relation that can be used to compute the other Aj s. Thus, we can write

(20)Ajexp(ikz,jdj1)=Aj1exp(ikz,j1dj2)Sj1,jexp[ikz,j1(dj1dj2)]=Aj2exp(ikz,j2dj3)Sj2,j1exp[ikz,j2(dj2dj3)]Sj1,jexp[ikz,j1(dj1dj2)]==A1exp(ikz1d1)m=1j1Sm,m+1exp[ikz,m(dmdm1)].

We can introduce a generalized transmission coefficient

T~1N:=m=1N1Sm,m+1exp[ikz,m(dmdm1)].

Then,

ANexp(ikz,NdN1)=T~1NA1exp(ikz1d1).

So the downgoing wave amplitude in region N at z=dn+1 is T~1N times the downgoing amplitude in region 1 (z=d1). Due to the products involved in the above relation, a continuum extension of this formula is not straightforward.

State equations and Propagator matrix

The propagator matrix relates the fields at two points in a multilayered medium. This matrix is also known as the transition matrix or the transfer matrix.

Let us examine the propagation matrix for a TM wave. Recall the governing equation for a TM wave:

(21)[ϵ(z)ddz(ϵ(z)1ddz)+ω2ϵ(z)μ(z)kx2]H~y=0

where

Hy(x,z)=H~y(z)e±ikxx.

Define φ:=H~y. Also,

kz2=ω2ϵ(z)μ(z)kx2.

Therefore, (21) can be written as

(22)[ϵ(z)ddz(ϵ(z)1ddz)+kz2]φ=0.

To reduce (22) to a first order differential equation, introduce the quantity

(23)ψ:=1iωϵdφdzdφdz=iωϵψ.

Clearly, ψ has to be continuous across the interface for the differential equation (22) to be satisfied.

Plugging (23) into (22) gives

(24)dψdz=ikz2ϵωφ.

Therefore, (23)2 and (24) for a system of differential equations which can be written as

(25)ddz[φψ]=[0iωϵikz2ϵω0][φψ].

Define

𝐯:=[φψ];𝐇:=[0iωϵikz2ϵω0].

Then, equations (25) can be written as

(26)d𝐯dz=𝐇𝐯.

If 𝐇 is constant, particular solutions to (26) can be sought of the form

(27)𝐯=𝐯0eλz.

Plugging (27) into (25) leads to the eigenvalue problem

(𝐇λ𝟏)𝐯0=𝟎.

Solutions exist only if

det(𝐇λ𝟏)=0λ2=kz2λ=±ikz.

Therefore, the general solution of (26) is

(28)𝐯(z)=A+eikzz𝐧++Aeikzz𝐧

where 𝐧+ and 𝐧 are the eigenvectors corresponding to the eigenvalues ikz and ikz, respectively.

Equation (28) can be written more compactly in the form

(29)𝐯(z)=[𝐧+𝐧][eikzz00eikzz][A+A]

or,

(30)𝐯(z)=𝐧~𝐊(z)𝐚~

where

𝐧~:=[𝐧+𝐧];𝐊(z):=[eikzz00eikzz];𝐚~:=[A+A].

Note that, for a point z that is different from z,

𝐊(zz)=[eikz(zz)00eikz(zz)]=[eikzz00eikzz][eikzz00eikzz]=𝐊(z)𝐊(z).

Also,

𝐊(zz)𝐊(z)=[eikz(zz)00eikz(zz)][eikzz00eikzz]=𝐊(z).

Therefore we can write (30) in the form

𝐯(z)=𝐧~𝐊(zz)𝐊(z)𝐚~=𝐧~𝐊(zz)𝐧~1𝐧~𝐊(z)𝐚~

or,

(31)𝐯(z)=𝐏(z,z)𝐯(z)

where

𝐏(z,z):=𝐧~𝐊(zz)𝐧~1.

The matrix 𝐏 is called the propagator matrix or the transition matrix that related the fields at z and z.

In a multilayered system (see Figure~3), since the vector 𝐯 is discontinuous, we can show that

𝐏(d2,0)=𝐏(d2,d1)𝐏(d1,0)

where 𝐏(d2,d1) depends on ϵ3,μ3 and 𝐏(d1,0) depends on ϵ2,μ2.

File:Lec12Fig3.jpg
Figure 3. Multilayered medium.

Footnotes

  1. ↑ This lecture closely follows the work of Chew~Chew95. Please refer to that text for further details.

References

W. C. Chew. Waves and fields in inhomogeneous media. IEEE Press, New York, 1995.