Plane Interface

Suppose a plane wave is incident upon a plane surface that is an interface between two materials, one with and the other with .

In order to derive an algebraic relationship between the intensities of the incoming wave, the reflected wave, and the refracted wave, we must begin by defining the algebraic form of each of these waves in terms of the wave numbers. The reflected wave and incident wave do not leave the first medium and hence retain speed , , and . The refracted wave changes to speed , , .

Note that the *frequency* of the waves is the same in both media as
a *kinematic constraint*! Why is that?

This yields the following forms for the various waves:

**Incident Wave**

(11.49) | |||

(11.50) |

**Refracted Wave**

(11.51) | |||

(11.52) |

**Reflected Wave**

(11.53) | |||

(11.54) |

Our goal is to *completely understand* how to compute the reflected
and refracted wave from the incident wave. This is done by matching the
wave across the boundary interface. There are two aspects of this
matching - a *static* or kinematic matching of the waveform itself
and a *dynamic* matching associated with the (changing) polarization
in the medium. These two kinds of matching lead to two distinct and
well-known results.