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5.2.3 Dispersion Diagrams of Refracted Waves in Isotropic and Uniaxial Anisotropic Media
ОглавлениеThe dispersion diagrams of the EM-waves in the isotropic and also uniaxial anisotropic medium displaying Snell's law, given in equation (5.2.7), are represented on the (kz − ky)‐plane. Snell's law was obtained from the phase matching of the incident and refracted waves across the boundary of two media. The dispersion diagrams in the isotropic and uniaxial anisotropic media are obtained by continuing the process discussed in subsections (4.7.4) and (4.7.5) of chapter 4.
Figure (5.4a) shows the geometrical process of constructing the dispersion diagram showing the refraction of the wave at the interface of the air and dielectric media. The incident wavevector in the air medium (εr = 1) subtends an angle of incidence θi. The refracted wavevector , in the isotropic dielectric medium with relative permittivity εr, subtends an angle of refraction θr with respect to the kz, normal to the interface. Only half of the dispersion circle of each medium is shown. The normal RS intersects the dispersion circle of the isotopic dielectric medium at S. At the interface, the line segments show the phase‐matching across the interface. It is seen that the directions of the phase velocity vp and group velocity vg of the refracted wave are the same.
Likewise, Fig (5.4b) shows the geometrical construction of double refraction in the uniaxial anisotropic medium. In this case, the line segments PQ(k0 sin θi) = QR(kro sin θo = kre sin θe) provide the phase‐matching across the interface. The wavenumbers kro and kre belong to the refracted ordinary and extraordinary waves. The normal drawn from the location R on the dispersion circle to the interface of air-dielectric medium intersects the dispersion circle of the uniaxial anisotropic medium at S1 for the ordinary waves. It also intersects at the dispersion ellipse at S2 for the extraordinary waves. The wavevectors OS1 and OS2 for the ordinary and extraordinary waves subtend the angle of refraction θo and θe respectively with kz‐axis. The first refraction is for the ordinary waves with phase velocity vpo and group velocity vgo in the same direction. The second refraction, for the extraordinary waves, has phase velocity vpe and group velocity vge in different directions. The angles of refraction are different in both cases. The phase and group velocities for both kinds of waves are identical only along the optic axis OO', where the dispersion circle and dispersion ellipse touch each other.
Figure 5.4 Dispersion diagrams of refracted waves.