Transfer-matrix method (optics)

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For the transfer-matrix method in geometric optics, see Ray transfer matrix analysis. For the transfer-matrix method in statistical physics, see Transfer-matrix method.
Propagation of a ray through a layer

The transfer-matrix method is a method used in optics and acoustics to analyze the propagation of electromagnetic or acoustic waves through a stratified (layered) medium.[1] This is for example relevant for the design of anti-reflective coatings and dielectric mirrors.

The reflection of light from a single interface between two media is described by the Fresnel equations. However, when there are multiple interfaces, such as in the figure, the reflections themselves are also partially transmitted and then partially reflected. Depending on the exact path length, these reflections can interfere destructively or constructively. The overall reflection of a layer structure is the sum of an infinite number of reflections, which is cumbersome to calculate.

The transfer-matrix method is based on the fact that, according to Maxwell's equations, there are simple continuity conditions for the electric field across boundaries from one medium to the next. If the field is known at the beginning of a layer, the field at the end of the layer can be derived from a simple matrix operation. A stack of layers can then be represented as a system matrix, which is the product of the individual layer matrices. The final step of the method involves converting the system matrix back into reflection and transmission coefficients.

Formalism for electromagnetic waves[edit]

Below is described how the transfer matrix is applied to electromagnetic waves (for example light) of a given frequency propagating through a stack of layers at normal incidence. It can be generalized to deal with incidence at an angle, absorbing media, and media with magnetic properties. We assume that the stack layers are normal to the z\, axis and that the field within one layer can be represented as the superposition of a left- and right-traveling wave with wave number k\,,

E(z) = E_r e^{ikz} + E_l e^{-ikz}\,.

Because it follows from Maxwell's equation that E\, and F=dE/dz\, must be continuous across a boundary, it is convenient to represent the field as the vector (E(z),F(z))\,, where

F(z) = ik E_r e^{ikz} - ik E_l e^{-ikz}\,.

Since there are two equations relating E\, and F\, to E_r\, and E_l\,, these two representations are equivalent. In the new representation, propagation over a distance L\, into the positive z\, direction is described by the matrix

M = \left( \begin{array}{cc} \cos kL & \frac{1}{k} \sin kL \\ -k \sin kL & \cos kL \end{array} \right),

and

\left(\begin{array}{c} E(z+L) \\ F(z+L) \end{array} \right) =
   M\cdot  \left(\begin{array}{c} E(z) \\ F(z) \end{array} \right)

Such a matrix can represent propagation through a layer if k\, is the wave number in the medium and L\, the thickness of the layer: For a system with N\, layers, each layer j\, has a transfer matrix M_j\,, where j\, increases towards higher z\, values. The system transfer matrix is then

M_s = M_N \cdot \ldots \cdot M_2 \cdot M_1.

Typically, one would like to know the reflectance and transmittance of the layer structure. If the layer stack starts at z=0\,, then for negative z\,, the field is described as

E_L(z) = E_0 e^{ik_Lz} + r E_0 e^{-ik_Lz}\,,

where E_0\, is the amplitude of the incoming wave, k_L\, the wave number in the left medium, and r\, is the amplitude (not intensity!) reflectance coefficient of the layer structure. On the other side of the layer structure, the field consists of a right-propagating transmitted field

E_R(z) = t E_0 e^{ik_R z}\,,

where t\, is the amplitude transmittance and k_R\, is the wave number in the rightmost medium. If F_L = dE_L/dz\, and F_R = dE_R/dz\,, then we can solve

\left(\begin{array}{c} E(z_R) \\ F(z_R) \end{array} \right) =
   M\cdot \left(\begin{array}{c} E(0) \\ F(0) \end{array} \right)

in terms of the matrix elements M_{mn}\, of the system matrix M_s\, and obtain

t = 2 i k_L e^{-i k_R L}\left[\frac{M_{11} M_{22} - M_{12} M_{21}}{-M_{21} + k_L k_R M_{12} + i(k_R M_{11} + k_L M_{22})}\right]

and

r = \left[\frac{ (M_{21} + k_L k_R M_{12}) + i(k_L M_{22} - k_R M_{11})}{(-M_{21} + k_L k_R M_{12}) + i(k_L M_{22} + k_R M_{11})}\right].

The transmittance and reflectance (i.e., the fractions of the incident intensity \left|E_0\right|^2 transmitted and reflected by the layer) are often of more practical use and are given by T=|t|^2\, and R=|r|^2\,, respectively (at normal incidence).

Example[edit]

As an illustration, consider a single layer of glass with a refractive index n and thickness d suspended in air at a wave number k (in air). In glass, the wave number is k'=nk\,. The transfer matrix is

M=\left(\begin{array}{cc}\cos k'd & \sin(k'd)/k' \\ -k' \sin k'd & \cos k'd \end{array}\right).

The amplitude reflection coefficient can be simplified to

r = \frac{(1/n - n) \sin k'd}{(n+1/n)\sin k'd  + 2 i \cos(k'd)}.

This configuration effectively describes a Fabry–Pérot interferometer or etalon: for k'd=0, \pi, 2\pi, \cdots\,, the reflection vanishes.

Acoustic waves[edit]

It is possible to apply the transfer-matrix method to sound waves. Instead of the electric field E and its derivative F, the displacement u and the stress \sigma=C du/dz, where C is the p-wave modulus, should be used.

Abeles matrix formalism[edit]

The Abeles matrix method is a computationally fast and easy way to calculate the specular reflectivity from a stratified interface, as a function of the perpendicular momentum transfer, Qz.

Q_z=\frac{4\pi}{\lambda}\sin\theta=2k_z


Reflection from a strafied interface

Where θ is the angle of incidence/reflection of the incident radiation and λ is the wavelength of the radiation. The measured reflectivity depends on the variation in the scattering length density (SLD) profile, (ρ(z)) perpendicular to the interface. Although the scattering length density profile is normally a continuously varying function, the interfacial structure can often be well approximated by a slab model in which layers of thickness (dn), scattering length density (ρn) and roughness (σn,n+1) are sandwiched between the super- and sub-phases. One then uses a refinement procedure to minimise the differences between the theoretical and measured reflectivity curves, by changing the parameters that describe each layer.

In this description the interface is split into n layers. Since the incident neutron beam is refracted by each of the layers the wavevector, k, in layer n, is given by:

k_n=\sqrt{{k_z}^2-4\pi({\rho}_n-{\rho}_0)}

The Fresnel reflection coefficient between layer n and n+1 is then given by:

 r_{n,n+1} = \frac{k_{n}-k_{n+1}}{k_{n}+k_{n+1}}


Since the interface between each layer is unlikely to be perfectly smooth the roughness/diffuseness of each interface modifies the Fresnel coefficient and is accounted for by an error function, as described by Nevot and Croce (1980).

r_{n,n+1} = \frac{k_{n}-k_{n+1}}{k_{n}+k_{n+1}}\exp(-2k_{n}k_{n+1}{\sigma_{n,n+1}}^2)


A phase factor, β is introduced, which accounts for the thickness of each layer.

\beta_{0} = 0
\beta_{n} = i k_{n}d_{n}


where i^2 = -1. A characteristic matrix, cn is then calculated for each layer.

c_{n}=\left[\begin{array}{cc}
\exp\left(\beta_{n}\right) & r_{n,n+1}\exp\left(\beta_{n}\right)\\
r_{n,n+1}\exp\left(-\beta_{n}\right) & \exp\left(-\beta_{n}\right)\end{array}\right]


The resultant matrix is defined as the product of these characteristic matrices

M=\prod_{n}c_{n}

from which the reflectivity is calculated

R=\left|\frac{M_{10}}{M_{00}}\right|^{2}

See also[edit]

References[edit]

  1. ^ Born, M.; Wolf, E., Principles of optics: electromagnetic theory of propagation, interference and diffraction of light. Oxford, Pergamon Press, 1964.

Abeles matrix formalism[edit]

  • O. S. Heavens. Optical Properties of Thin Films. Butterworth, London (1955).
  • L. Nevot, P. Croce, Revue de physique appliquée, 15, 761 (1980).
  • F. Abeles, Le Journal de Physique et le Radium, "La théorie générale des couches minces", 11, 307–310 (1950).

External links[edit]

Derivations and explanations[edit]

Computer programs[edit]

There are a number of computer programs that implement this calculation: