Book contents
- Frontmatter
- Contents
- Preface
- 1 The ionosphere and magnetosphere
- 2 The basic equations
- 3 The constitutive relations
- 4 Magnetoionic theory 1. Polarisation and refractive index
- 5 Magnetoionic theory 2. Rays and group velocity
- 6 Stratified media. The Booker quartic
- 7 Slowly varying medium. The W.K.B. solutions
- 8 The Airy integral function and the Stokes phenomenon
- 9 Integration by steepest descents
- 10 Ray tracing in a loss-free stratified medium
- 11 Reflection and transmission coefficients
- 12 Ray theory results for isotropic ionosphere
- 13 Ray theory results for anisotropic plasmas
- 14 General ray tracing
- 15 Full wave solutions for isotropic ionosphere
- 16 Coupled wave equations
- 17 Coalescence of coupling points
- 18 Full wave methods for anisotropic stratified media
- 19 Applications of full wave methods
- Answers to problems
- Bibliography
- Index of definitions of the more important symbols
- Subject and name index
3 - The constitutive relations
Published online by Cambridge University Press: 06 December 2010
- Frontmatter
- Contents
- Preface
- 1 The ionosphere and magnetosphere
- 2 The basic equations
- 3 The constitutive relations
- 4 Magnetoionic theory 1. Polarisation and refractive index
- 5 Magnetoionic theory 2. Rays and group velocity
- 6 Stratified media. The Booker quartic
- 7 Slowly varying medium. The W.K.B. solutions
- 8 The Airy integral function and the Stokes phenomenon
- 9 Integration by steepest descents
- 10 Ray tracing in a loss-free stratified medium
- 11 Reflection and transmission coefficients
- 12 Ray theory results for isotropic ionosphere
- 13 Ray theory results for anisotropic plasmas
- 14 General ray tracing
- 15 Full wave solutions for isotropic ionosphere
- 16 Coupled wave equations
- 17 Coalescence of coupling points
- 18 Full wave methods for anisotropic stratified media
- 19 Applications of full wave methods
- Answers to problems
- Bibliography
- Index of definitions of the more important symbols
- Subject and name index
Summary
Introduction
Before (2.45) can be applied to the theory of wave propagation in a plasma, it is necessary to express the electric displacement D, and therefore the electric polarisation P, in terms of the electric intensity E. The resulting expressions are called the constitutive relations of the plasma and are derived in this chapter. The subject of wave propagation is resumed in ch. 4.
From now on, except in § 3.8, all fields are assumed to vary harmonically in time, and are designated by capital letters representing complex vectors, as explained in § 2.5. Time derivatives of some of the fields appear in the constitutive relations, and since ∂/∂t ≡ iω, it follows that the angular frequency ω appears in the expression for the electric permittivity. When this happens the medium is said to be time dispersive.
In this and the following chapter the plasma is assumed to be homogeneous. In later chapters the results are applied to an inhomogeneous plasma. This is justified provided that the plasma is sufficiently slowly varying. The meaning of ‘slowly varying’ is discussed in § 7.10. It is further assumed, in the present chapter, that the spatial variation of the fields can be ignored. This means that, over a distance large compared with N−⅓, the fields can be treated as uniform. Thus spatial derivatives of the fields do not appear in the expression for the permittivity.
- Type
- Chapter
- Information
- The Propagation of Radio WavesThe Theory of Radio Waves of Low Power in the Ionosphere and Magnetosphere, pp. 38 - 65Publisher: Cambridge University PressPrint publication year: 1985