
640 10. Scalar Diffraction Theory
0.0 .5 1.0 1.5 2.0 2.5 3.0 3.5 4.0
0.0
.2
.4
.6
.8
1.0
1.2
1.4
1.6
0
II
'wa
Figure 10.12: The diffraction intensity at a point on the beam axis as a
function of the radius of the aperture.
10.4 Diffraction of Plane Waves
in Anisotropic Media
In microwaves and optoelectronics, more and more crystal materials are used
to give rise to some particular functions which involve generation of mi-
crowave and light wave, propagation, transformation, and interaction with
other kinds of waves, etc. Most crystals are anisotropic, so it is valuable to
study the diffraction in anisotropic media.
In this section we will investigate the diffraction in uniaxial crystals. Since
the diffraction of ordinary wave is the same as that in isotropic media, we
discuss only the diffraction of the extraordinary wave.
10.4.1 Fraunhofer Diffraction at Square Apertures
In Fig. 10.13, a monochromatic plane wave with angular frequency ω is in-
cident normally on a square aperture of side 2a on the surface of a uniaxial
crystal from free space. The coordinate system is so chosen that its z axis
coincides with the optical axis of the crystal, the x axis and y axis are along
other principal dielectric axes. The angle between the incident direction and
the optical axis is α. In order to process more conveniently, the y axis is set
to be along a side of the aperture.
In crystals, if the coordinate axes are along the principal dielectric axes,
this coordinate system is called the principal coordinate system. The wave
equations for an extraordinary wave with angular frequency ω in the principal
coordinator system is given in (9.215) as:
1
n
2
e
∂
2
ψ
∂x
2
+
1
n
2
e
∂
2
ψ
∂y
2
+
1
n
2
o
∂
2
ψ
∂z
2
+ k
2
0
ψ = 0, (10.72)