80 2. INTERFERENCE
where v is the phase velocity of light in the medium with refractive index n,
related to the speed of light c in vacuum as v c/n. The scalar wave equation
follows from Maxwell’s theory. It may also be written in spherical coordinates
∇
2
u + k
2
u 0, (2.2)
where ∇ is the differential operator in spherical coordinates, k 2π/λ, and λ
is the wavelength of the light. A simple solution of this equation is a spherical
wave of the type (e
ikr
)/r, where r is the distance from the origin to the ob-
servation point. The spherical wave propagates from its origin in all directions
and its intensity is attenuated by 1/r
2
. We consider such spherical waves only
conceptually and approximate them at a large distance by plane waves.
The differential equation of the scalar wave equation is linear and superposi-
tion of solutions of the differential equation will again result in a solution. This
is part of the superposition principle. In this chapter we only need the superpo-
sition of a number of monochromatic waves, each of frequency ν, to result in a
monochromatic wave having the same frequency ν.
For our model description we use some results from Maxwell’s theory for
quantitative expressions of the reflection and transmission coefficients of mate-
rials contained in Fresnel’s formulas. In particular, we use the results that waves
pick up a phase jump of π, when reflected at an optically denser medium, and
that they travel in the optically denser medium with wavelength λ/n, where n is
the index of refraction. The intensity is calculated either as the time average of
the square of the amplitude or the square of the absolute value of the complex
representation and may be normalized with an arbitrary constant.
2.2 HARMONIC WAVES
The solution of the scalar wave equation, (Eq. (2.1)), is a function, depending on
the space coordinates x, y, z and the time t . In addition, there may be an arbitrary
phase factor. We consider harmonic waves in vacuum and in an isotropic and
nonconducting medium of index n. However, in most cases, we only need waves
depending on one space coordinate and time. We describe the transverse waves
by vibrating in the u direction and moving in the x direction, having wavelength
λ and time period T .
u A cos[2π(x/λ − t/T +φ)]. (2.3)
The amplitude u of the wave varies in the x direction, A is the magnitude of
the wave, and φ is a phase constant. The first graph of FileFig 2.1 shows the
amplitude u, depending on the space coordinate x for three time instances t and
three phase constants. The second graph shows the dependence on time for three
points in space and three phase constants. The magnitudes A
1
to A
3
and B
1
to