7.4 Periodic Systems 413
For lossless uniform systems, γ = jβ, and
E (x, y, z) = F (x, y) e
−jβz
. (7.43)
Therefore, we conclude that the field of a guided mode in a uniform system
is a single spatial harmonic wave, i.e., a sinusoidal wave that satisfies the
uniform boundary condition.
(2) Periodic System
In a periodic transmission system, the shape, size, and constitutive material
vary periodically along its z axis, see Fig. 7.6(b). The basis for the study of
periodic systems is a theorem ascribed to the French mathematician Floquet,
which may be stated as follows.
In a periodic system, for a given mode of propagation at a given steady-
state frequency, the fields at one cross section differ from those one period
(or an integer multiple of periods) away by only a complex constant.
This theorem is true whether or not the structure has losses so long as it
is p eriodic. The proof of the theorem lies in the fact that when a periodic
system having infinite length is displaced along its axis by one period or an
integer multiple of periods, it cannot be distinguishable from its original self.
Suppose that the spatial period of the system is p, and the distance be-
tween the two cross sections is mp, m is an integer, then the complex constant
can be written as
e
−γ(z
2
−z
1
)
= e
−γ
0
mp
, where z
2
− z
1
= ∆z = mp, γ
0
= α
0
+ jβ
0
.
The relation between the complex amplitudes of the fields on the two cross
sections at z
1
and z
2
= z
1
+ mp are given by
E (x, y, z + mp) = E (x, y, z) e
−γ
0
mp
. (7.44)
This is the mathematical formulation of Floquet’s theorem.
In a periodic system, the distribution function of the field on the trans-
verse cross section is dependent on z, so the time-harmonic field at a given
steady-state frequency on an arbitrary cross section at z must be
E (x, y, z, t) = F (x, y, z) e
−γ
0
z
e
jωt
, (7.45)
and the complex amplitude of the field at z is
E (x, y, z) = F (x, y, z) e
−γ
0
z
. (7.46)
We can readily prove that if the function F (x, y, z) is a periodic function of
z with period p, then the Floquet’s theorem (7.44) is followed.
The complex amplitudes of the fields on the cross sections at z + mp is
E (x, y, z + mp) = F (x, y, z + mp) e
−γ
0
(z+mp)
. (7.47)