Читать книгу Introduction To Modern Planar Transmission Lines - Anand K. Verma - Страница 153

Inside the isotropic dielectric medium, the electric displacement vector and the electric field intensity are parallel to each other, i.e. the applied electric field views the same relative permittivity of a medium in all directions. Likewise, the magnetic displacement vector is parallel to the magnetic field intensity within the isotropic medium. These properties are expressed through constitutive relations (4.1.7a) and (4.1.7b). For the isotropic media, permittivity and permeability are scalar quantities.

However, there are dielectrics, such as quartz, sapphire, alumina, MgO, and so forth, where and are not parallel to each other, i.e. they are not in the same direction. Such dielectrics form the anisotropic medium. In such a medium, the relative permittivity viewed by the applied electric field is direction‐dependent. For instance, Fig. (4.3a) forms a composite anisotropic medium as the effective permittivity along the x‐axis is different from the effective permittivity along the z‐axis. Similarly, magnetic materials such as ferrite, garnet, and so forth are also anisotropic because and vectors are not in the same direction. Several authors have treated the properties of anisotropic medium and EM‐wave propagation through such media in detail [B.1–B.4, B.9, B.11, B.13–B.15, B.17–B.23]. This subsection reviews basic concepts related to anisotropic media.

The relative permittivity and relative permeability of these anisotropic media are not scalar quantities. They are tensor quantity, described by 3 × 3 matrices. The constitutive relations of such electric and magnetic media are written as follows:

(4.2.4)

In general, elements of permittivity and permeability matrices could be complex quantities and also frequency‐dependent, accounting for the losses and dispersion in the material medium. Equation (4.2.4a) shows that for the anisotropic dielectric medium, the electric flux density is not parallel to electric field intensity . Likewise, equation (4.2.4b) shows that the vector is not parallel to the vector . For instance, if the incident field on an anisotropic dielectric medium has only E_x component, i.e. x‐polarized incident E‐field, it generates all three components of electric flux density – D_x, D_y, and D_z. The same applies to the anisotropic magnetic medium.

The above equations can be written in a more compact form as

(4.2.5)

The above permittivity and permeability matrices could be either symmetric or anti‐symmetric. Thus, the anisotropic materials could be divided into two broad groups: (i) symmetric anisotropic materials and (ii) anti‐symmetric anisotropic materials. The symmetric anisotropic materials support linearly polarized EM‐waves propagating as the normal modes of the homogeneous unbounded medium. However, circularly polarized EM‐waves are the normal modes of the anti‐symmetric anisotropic medium. The normal modes of media travel without any change in polarization.