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Table of Contents

1.1 Maxwell Equations
1.2 Material Equations
1.3 Wave Equation with Refractive Index
1.4 TEM Wave and Impedance
1.5 Polarisation
1.6 Energy Density, Poynting Vector, and Intensity
1.7 Dispersion
1.8 Sellmeier Equation in the Visible and Near-Infrared


1 Plane Wave Propagation in Dispersive Media

We will now begin with the description of the simplest type of electromagnetic field: the plane wave, and we will consider its propagation in a dispersive medium. For this, we require Maxwell's equations. Note however, that we will not derive them here, as it is assumed the reader is already somewhat familiar with them. The following two sections on the Maxwell equations and the material equations are also treated in a similar way in my quantum electronics notes.

1.1 Maxwell Equations

In this chapter, Maxwell's equations will be discussed in SI units. This formulation is important because it incorporates the influence of bound charges and bound currents into the displacement field D and the magnetising field H. Then, the source terms in the equations only depend on the free charge density ρf, and the free current density jf. Free charges/currents could, for instance, be electrons in the conduction band of a metal or a semiconductor, in contrast to the core or bonding electrons which are considered bound. The macroscopic Maxwell's Equations in matter are then:

D=ρf,B=0,×H=jf+tD,×E=tB.

1.2 Material Equations

The material equations describe how bound charges within a material respond to an electromagnetic (EM) wave, driven by the Coulomb or Lorentz force. As long as the applied fields are not excessively large, the response of each atom or molecule can often be modelled as a harmonic oscillator, where a negatively charged electron cloud oscillates with respect to the positively charged core. Under the influence of an electromagnetic wave, the electrons are set into forced oscillations induced by the incident EM wave. In the linear regime, these oscillating electrons then emit secondary radiation at the same frequency as the incident wave, but generally with a frequency-dependent phase difference. Therefore, the field propagating in the medium is a superposition of the incident wave and the phase-shifted waves emitted by the electrons. In the visible and near-infrared spectrum for transparent media, this superposition of waves typically propagates more slowly than the original incident wave would in vacuum.

We will treat the medium as a continuum, which is a good approximation as long as the wavelength under consideration is long compared to atomic dimensions. The interaction of a material containing bound electrons with an electric field is described by the material equation for the electric displacement D:

D=ε0E+P,

where P is the induced electric polarisation of the material (electric dipole moment per unit volume), caused by the displacement of bound charges relative to their equilibrium positions. The polarisation is related to the bound charge density ρb via:

P=ρb.

Using this and Gauss's law for D (D=ρf), we can also write Gauss's law for E as:

E=ρtotalε0withρtotal=ρf+ρb.

For small electric fields, as in linear optics, the instantaneous polarisation is often directly proportional to the applied electric field in non-dispersive media:

P(t)=ε0χeE(t),

where χe is the electric susceptibility (a scalar for isotropic media). If χe is frequency dependent (i.e., the medium is dispersive), this simple proportionality is valid in the frequency domain:

P(ω)=ε0χe(ω)E(ω).

In this case, the polarisation P(ω) and the electric field E(ω) are generally not in phase, meaning that χe(ω) is a complex quantity.

The material equation for the magnetic field H is:

H=1μ0BM,

with M being the induced magnetisation field of the material (magnetic dipole moment per unit volume). The total current density jtotal=jf+jb is related to the microscopic Ampère-Maxwell law ×B=μ0(jtotal+ε0tE). The bound current density jb can be expressed in terms of P and M as jb=P/t+×M.
For small fields in linear magnetic media, the magnetisation is proportional to the magnetic field H:

M=χmH,

where χm is the magnetic susceptibility. In linear optics, it is useful to introduce the relative permittivity εr (dielectric constant) and the relative magnetic permeability μr. These are defined by the constitutive relations:

D=ε0εrE=εabsE,B=μ0μrH=μabsH.

Here εabs and μabs are the absolute permittivity and permeability of the medium. This implies:

χe=εr1,χm=μr1(when M=χmH).

We additionally define the refractive index n as:

nεrμr.

For the remainder of these notes, we will primarily consider dielectric materials, that is, materials that can be polarised by an applied electric field but are generally non-magnetic at optical frequencies. Thus, we may neglect magnetic interactions by setting μr1 (so χm0 and M0).


1.3 Wave Equation with Refractive Index

The wave equation in a material with bound electrons is a direct consequence of Maxwell's equations. We assume no free charges (ρf=0) and no free currents (jf=0), so D=0. The effect of the bound electrons is incorporated through the polarisation P (and thus through D=ε0E+P). For a homogeneous, isotropic, linear, non-magnetic medium, the wave equation for the electric field E can be written as:

2E1c22t2E=μ02t2P,

where c is the speed of light in vacuum, given by:

c=1ε0μ03×108m s1.

This is the relevant wave equation for dielectric dispersive materials, for which the induced polarisation P(ω)=ε0χe(ω)E(ω) depends on frequency, and the electric susceptibility χe(ω) is complex. Without polarisation (P=0), the equation reduces to the wave equation in vacuum, whose solutions are electromagnetic waves propagating at speed c.
If the material is further assumed to be non-dispersive (so χe(ω)=χe is a constant, real value, and P(t)=ε0χeE(t)), we may simplify the wave equation. Using D=ε0(1+χe)E=ε0εrE, and for non-magnetic media B=μ0H, the wave equation becomes:

2Eεrc22t2E=0,or2E1vp22t2E=0.

The solutions of this wave equation in such a linear, homogeneous, isotropic, non-dispersive dielectric medium are electromagnetic waves travelling with the phase velocity:

vp=cεr=cn.

Here, n=εr is the refractive index (since μr=1). The macroscopic change in the phase velocity of a plane EM wave in a material is thus given by its refractive index n, which is determined by the material’s atomic structure and its response to the EM field.

Nonlinear optical processes, such as frequency doubling, may also be included as source terms in the wave equation. For high field intensities, the material response becomes nonlinear, primarily because the atomic binding potential is anharmonic. The nonlinear polarisation PNL in the perturbative regime is usually expanded in a Taylor series as a function of the field components Ej,Ek,:

Pi,NL=ε0jkχijk(2)EjEk+ε0jklχijkl(3)EjEkEl+,

through which the wave equation generalises to:

2E1c22t2E=μ02t2(PL+PNL),

where PL=ε0χe(1)E contains only the linear part of the polarisation. Similar wave equations may be obtained for the magnetic field; however, they often take an analogous form. It is important to remember that both electric and magnetic fields are essential for the propagation of an electromagnetic wave. Nonlinear effects with more focus on magnetism are discussed more extensively in my notes on crystal optics, with a greater theoretical focus on their description.

1.3.1 Solutions to the Wave Equation: The Plane Wave

The monochromatic plane wave is an important special solution of the linear wave equation. We will see that any wave solution can be expressed as a superposition (integral) of such plane waves. Consider the real form of a plane wave travelling in the positive z-direction:

E(z,t)=|E0+|cos(ωtkz+φ),

where E0+=|E0+|eiφ is the complex amplitude vector (phasor) of the wave propagating in the +z direction. In the following, we will often omit the superscript + or for the amplitude if the direction is clear from context. The period T is defined through:

T=2πω=1f.

The next figure shows a plane wave for a constant position as a function of time (left), and for a constant time as a function of position (right):

Attachments/UltraFastLasers_Keller.webp|700

The period in the time domain is T. The wavelength in vacuum is λ0=cT. The optical frequency f (or ω) does not change when light enters a linear medium from vacuum. This is a direct consequence of the boundary conditions at the interface. Since the phase velocity changes in a dispersive medium from c to vp=c/n, the wavelength also changes:

λn=vpT=cnT=λ0n.

This is schematically shown in the next figure:

Attachments/UltraFastLasers_Keller 1.webp|700

It is often much easier to work with the complex notation for the plane wave:

E(z,t)=E~0+ei(ωtkz),

where E~0+ is the complex amplitude vector, including any initial phase. The physical field is understood to be the real part of this complex expression. This is permissible because the wave equation is linear, and therefore any superposition of solutions (including real and imaginary parts of a complex solution) is also a solution.

Next, there is a summary of relevant quantities and their behaviour in vacuum and in a dielectric medium (with refractive index n, assuming μr=1):

Quantity Vacuum Dispersive medium (n(ω))
Frequency f f
Period T=1/f,ω=2πf T=1/f,ω=2πf
Phase Velocity vp=c vp(ω)=c/n(ω)cn(ω)
Wave number k0=ω/c k(ω)=n(ω)ω/c=n(ω)k0
Wave number k0=2π/λ0 k(ω)=2π/λn(ω)=n(ω)2π/λ0
Wavelength λ0 λn(ω)=λ0/n(ω)

1.4 TEM Wave and Impedance

Very importantly, for plane waves in isotropic media, Maxwell's equations imply that the field vectors and the wavevector are mutually orthogonal:

EH,kE,kH.

Such a wave is called a transverse electromagnetic (TEM) wave because both the electric and magnetic fields are transverse (perpendicular) to the direction of wave propagation k. For a plane harmonic wave in a lossless medium, the fields E and H are in phase:

Attachments/UltraFastLasers_Keller 2.webp|700

Further, their amplitudes are related by the wave impedance Z of the medium. For a plane wave E(r,t)=E0ei(krωt), the magnetic field is H(r,t)=1Z(k^×E(r,t)), where k^=k/|k|. This means |H0|=|E0|/Z. The impedance Z is defined by:


1.5 Polarisation

So far, the electromagnetic wave discussed was implicitly linearly polarised, meaning that the electric field vector oscillates along one fixed direction in the plane perpendicular to k. The direction in which the electric field oscillates is called the polarisation direction. Mathematically, a linearly polarised plane wave propagating along z (figure a), polarised along the x-direction, has the form:

E(z,t)=x^E0ei(ωtknz).

The superposition of two linearly polarised waves with a phase difference Δφ and orthogonal polarisation directions generally results in an elliptically polarised plane wave (figure b). For instance, if one component is along x^ and the other along y^:

E(z,t)=(x^E1+y^E2eiΔφ)ei(ωtknz).

A special case is when Δφ=0 or Δφ=π; in this case, the wave remains linearly polarised, with its polarisation direction generally tilted in the xy-plane. Another special case occurs when E1=E2 and the phase difference is Δφ=±π/2. In that case, the wave is called circularly polarised (figure c), where the tip of the electric field vector traces out a circle in the xy-plane at frequency ω.

Attachments/UltraFastLasers_Keller 3.webp|700

1.6 Energy Density, Poynting Vector, and Intensity

For optically isotropic materials, both the Poynting vector (direction of energy flow) and the wave vector k (direction of phase propagation) are parallel and perpendicular to the wavefronts for plane waves. The following energy-related quantities are important:

For the special case of a monochromatic plane wave E(r,t)=Re[E~0ei(krωt)]:


1.7 Dispersion

The fact that the refractive index n(ω) is frequency dependent implies that the wave number k(ω)=n(ω)ω/c is no longer directly proportional to the frequency ω, as it is in vacuum (where k0=ω/c). This frequency dependence of n(ω) (and thus of k(ω) and vp(ω)) is called dispersion. For more details, see here. It is very important to know n(ω) to describe pulse propagation, as can be seen in examples of how different materials affect light:

Attachments/UltraFastLasers_Keller 4.webp|700


1.8 Sellmeier Equation in the Visible and Near-Infrared

In many cases, we will discuss transparent dielectric materials, meaning materials with negligible absorption in the spectral region of interest. Glass, for instance, is transparent in the visible spectrum but absorbs strongly in the ultraviolet (UV) and parts of the infrared (IR) spectral regions. The range in which a material is transparent is called its spectral window. Usually, within this window and away from absorption bands, materials exhibit normal dispersion, where the refractive index n(ω)=Re[n(ω)] increases with frequency (dndω>0), or equivalently, decreases with wavelength (dndλ0<0).

Attachments/UltraFastLasers_Keller 5.webp|700

Far away from absorption resonances, the dispersion of the real part of the refractive index can often be accurately described by the Sellmeier equation. This equation can be derived from a classical oscillator model (like the Lorentz model) by considering the contributions of multiple absorption resonances at frequencies ωj. If these resonances are narrow, their contribution to the real part of the susceptibility χr(ω) (and thus to n2(ω)=1+χr(ω) for non-magnetic media) can be approximated. The Kramers-Kronig relations connect the real part χr(ω) and imaginary part χi(ω) of the susceptibility:

χr(ω)=1πPχi(ω)ωωdω=2πP0ωχi(ω)ω2ω2dω,χi(ω)=1πPχr(ω)ωωdω=2ωπP0χr(ω)ω2ω2dω.

Here, P denotes the Cauchy Principal Value. Assuming sharp absorption lines (delta functions for χi(ω) at resonance frequencies ωj or wavelengths λj), the Sellmeier equation for n2(λ0) takes the form:

n2(λ0)=1+jAjλ02λ02λj2,

where λ0 is the vacuum wavelength, Aj are constants related to the strength and density of the j-th oscillator, and λj are the resonance wavelengths. For fused silica, a common form is:

n2(λ0)=1+B1λ02λ02C1+B2λ02λ02C2+B3λ02λ02C3,

where Bj and Cj(=λj2) are empirically determined Sellmeier coefficients.