Waves in composites and metamaterials/Fading memory and waves in layered media

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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.

Viscoelastic Materials

In the previous lecture, we discussed viscoelastic materials and wondered why the Maxwell model works even though the effective Young's modulus Y(ω) for such materials is analytic in the entire complex plane (except for a few isolated points).

Recall that the Maxwell model (see Figure 1) predicts that the frequency dependent Young's modulus of the system is given by

Y(ω)=Ye+jHj1+iωτj.
File:GenMaxwell.jpg
Figure 1. A generalized Maxwell model for viscoelasticity.

This implies that the function Y(ω) is analytic in the entire imaginary ω plane except for poles at ω=i/τj. On the other hand, for the frequency dependent metamaterials that we have discussed earlier, the effective modulus is generally analytic only in the upper half ω plane (see Figure~2). Also, for such materials, Y*(ω)=Y(ω*), where (.)* indicates the complex conjugate. Note that we do not consider the mass when we derive the modulus of the Maxwell model. The relation between viscoelastic models of the Maxwell type and general frequency dependent materials continues to be an open question.

File:AnalyticPoles.jpg
Figure 2. Poles for a general frequency-dependent material vs. poles for a generalized Maxwell model.

A justification of the Maxwell model can be provided by considering the behavior of viscoelastic materials (Christ03). Consider an experiment where a bar of viscoelastic material of length l is deformed by a fixed amount. We want to see how the stress changes with time. Recall, that if the bar is extended by an amount u(x) where x=0 at one end of the bar, then the one-dimensional strain is defined as

ϵ=dudx.

Therefore, the displacement in the bar can be expressed in terms of the strain as

u(x)=ϵxϵ=u(l)l=Δll.

Also, if F is the applied force on the bar and A is its cross-sectional area, then the stress is given by

σ=FA.

Let us now apply a strain to the bar at time t=0 and hold the strain fixed. Due to the initial application of the strain, the stress reaches a value K0 and then relaxes at time increase (due to the relaxation of polymer chains for instance). Figure 3 shows a schematic of this situation.

File:StressRelax.jpg
Figure 3. One-dimensional stress relaxation of a viscoelastic material.

If the strain is applied by the superposition of a two step strains as shown in the figure, we have

dϵdt=aδ(tt1)+bδ(tt2).

The stress is then given by

σ=aK(tt1)+bK(tt2).

If the strain is applied by a series of infinitesimal steps, then we get a more general form for the stress:

(1)σ(t)=tK(tt)dϵ(t)dtdt

where the integral should be interpreted in the distributional sense. Integrating by parts (and assuming that ϵ=0 at t=), we get

σ(t)=K0ϵ(t)+tK(tt)ϵ(t)dt.

Now, σ(t) clearly depends on past values of dϵ/dt. We expect σ(t) should have a stronger dependence on dϵ/dt in the recent past than in the distant past. More precisely, the dependence should decrease monotonically as τ=tt increases. This implies that K(τ) should decrease at τ increases, i.e.,

dK(τ)dτ<0τ>0andK(τ)>0.

This is the assumption of fading memmory.

From equation (1) the rate of change of σ is given by

dσ(t)dt=tdK(τ)dτ|τ=ttdϵ(t)dtdt.

Again, we expect dσ/dt to have a stronger dependence on dϵ(t)/dt in the recent past than in the far past, i.e,.

|dK(τ)dτ|should decrease asτincreases.

Now,

dK(τ)dτ<0d2K(τ)dτ2>0d3K(τ)dτ3<0d4K(τ)dτ4>0τ>0.

Such functions are said to be completely monotonic. An example is

K(τ)=eτ/τdK(τ)dτ<0,d2K(τ)dτ2>0etc.

More generally,

K(τ)=K+0H(τ)eτ/τdτ

is completely monotonic if H(τ)0 for all τ and K0. The function H(τ) is called the {\bf relaxation spectrum.}

Conversely, any completely monotonic function can be written in this form (Bernstein28).

Specifically, if

ϵ(t)=Re(ϵ^eiωt)

then

dϵ(t)dt=Re(iωϵ^eiωt).

Therefore,

σ(t)=Re(iωϵ^tK(tt)eiωtdt).

Let τtt. Then

σ(t)=Re(iωϵ^eiωt0K(τ)eiωτdτ).

Define

(2)Y(ω):=iω0K(τ)eiωτdτ.

Then we have

σ(t)=Re(Y(ω)ϵ^eiωt).

If we define

σ^:=Y(ω)ϵ^

we get

σ(t)=Re(σ^eiωt).

Now, let K(τ) be a completely monotonic function of the form

K(τ)=K+0H(τ)eτ/τdτ.

Then from equation (2) we get

Y(ω)=iω0Keiωτdτiω0dτH(τ)0dτeτ(iω1/τ).

Assume that ω has a very small poistive imaginary part (which implies that ϵ(t) increases very slowly as t goes to ). Then

Y(ω)=iω(Kiω)iω0dτH(τ)(1iω1/τ)

or,

Y(ω)=K+0H(τ)1+iωτdτ.

This is the generalized Maxwell model.

This brings up the question: Is the assumption of fading memory always correct?

Recall the model of the Helmholtz resonator shown in Figure~4.

File:HelmholtzModel.jpg
Figure 4. A model of the Helmholtz resonator.
[hb]

If we apply a strain in the form of a step function to this model, the resulting stress response is not a monotonically decreasing function of time. Rather if oscillates around a certain value and may damp out over time. A similar oscillatory behavior is expected in other spring-mass systems and K(τ) will, in general, not be monotonic.

A short interlude: Maxwell's equations in Elasticity Form

In this section, we discuss how Maxwell's equation can be reduced to the form of the elasticity equations. Recall that, at a fixed ω, Maxwell's equation take the form

×๐„=iωμ(๐ฑ)๐‡(๐ฑ);×๐‡=iωϵ(๐ฑ)๐„(๐ฑ).

Therefore,

ω2ϵ๐„=iω×๐‡=×[μ1(×๐„)].

Recall that, in index notation and using the summation convention, we have

[×๐š]i=โ„ฐijkakxj

where โ„ฐijk is the permutation tensor defined as

โ„ฐijk={1for even permutations, i.e., 123, 231, 312 1for odd permutations, i.e., 132, 321, 213 0otherwise.

Therefore,

[ω2ϵ๐„]j=โ„ฐjimxi[μ1(×๐„)]m=โ„ฐjimxi[(μ1)mn(×๐„)n]=โ„ฐjimxi[(μ1)mnโ„ฐnklElxk]=xi[CijklElxk]whereCijkl:=โ„ฐjimโ„ฐnkl[μ1]mn

or,

ω2ϵ๐„=(๐–ข:๐„).

This is very similar to the elasticity equation

ω2ρ๐ฎ=(๐–ข:๐ฎ).

The permittivity is similar to a negative density and the electric field is similar to the displacement. The equations also hint at a tensorial density. However, continuity conditions are different for the two equations, i.e., at an interface, ๐ฎ is continuous while only the tangential component of ๐„ is continuous. Also, the tensor ๐–ข has different symmetries for the two situations. Interestingly, for Maxwell's equations

Cijkl=Cjikl=Cijlk=Cklij.

Waves in Layered Media

A detail exposition of waves in layer media can be found in Chew95. In this section we examine a few features of electromagnetic waves in layered media.

Assume that the permittivity and permeability are scalars and are locally isotropic though not globally so. Then we may write

ϵ=ϵ(x3)1andμ=μ(x3)1.

The TE (transverse electric field) equations are given by

(3)(1μE1)+ω2ϵE1=0

where represents the two-dimensional gradient operator.

Multiplying (3) by μ(x3), we have

(4)[x22+μ(x3)x3(1μ(x3)x3)+ω2ϵ(x3)μ(x3)]E1=0.

Equation (4) admits solutions of the form

E1(x2,x3)=E~1(x3)e±ik2x2

and equation (4) then becomes an ODE:

(5)[μ(x3)ddx3(1μ(x3)ddx3)+ω2ϵ(x3)μ(x3)k22]E~1=0.

The quantity

k32:=ω2ϵ(x3)μ(x3)k22

can be less than zero, implying that k3 may be complex. Also, at the boundary, both E~1 and 1/μE~1/x3 must be continuous.

Similarly, for TM (transverse magnetic) waves, we have

H1(x2,x3)=H~1(x3)e±ik2x2

and the ODE is

(6)[ϵ(x3)ddx3(1ϵ(x3)ddx3)+ω2ϵ(x3)μ(x3)k22]H~1=0.

References

  • S. Bernstein. Sur les fonctions absolument monotones. Acta Mathematica, 52:1--66, 1928.
  • W. C. Chew. Waves and field in inhomogeneous media. IEEE Press, New York, 1995.
  • R. M. Christensen. Theory of viscoelasticity: 2nd Edition. Courier Dover Publications, London, 2003.