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Eyges - The Classical Electromagnetic Field.

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Eyges The Classical Electromagnetic Field.
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Title Page; Dedication; Copyright Page; PREFACE; Table of Contents; PREFATORY NOTES; 1 - CONCEPTS OF A FIELD THEORY; REFERENCES; 2 - THE ELECTROSTATIC FIELD; 2.1 THE DISTRIBUTION OF CHARGE; 2.2 COULOMBS LAW AND SUPERPOSITION; 2.3 THE ELECTRIC FIELD; 2.4 THE POTENTIAL; PROBLEMS; REFERENCES; 3 - THE SUMMATION PROBLEM FOR CHARGES; 3.1 POINT CHARGE ON z-AXIS; 3.2 AXIAL MULTIPOLE EXPANSION; 3.3 GENERAL MULTIPOLE EXPANSION; 3.4 TWO-DIMENSIONAL DISTRIBUTIONS; 3.5 ONE-DIMENSIONAL DISTRIBUTIONS; 3.6 SURFACE CHARGES AND DOUBLE LAYERS; 3.7 DIPOLE DISTRIBUTIONS-EXTERIOR FIELDS.

3.8 DIPOLE DISTRIBUTIONS-INTERIOR FIELDSPROBLEMS; REFERENCES; 4 - BOUNDARY VALUE PROBLEMS WITH CONDUCTORS; 4.1 THE PHYSICS OF CONDUCTORS IN FIELDS; 4.2 HOMOGENEOUS AND INHOMOGENEOUS PROBLEMS; 4.3 A UNIQUENESS THEOREM; 4.4 METHOD OF IMAGES; 4.5 LAPLACES EQUATION AND SUPERPOSITION OF ELEMENTARY SOLUTIONS; 4.6 COMPOSITE PROBLEMS; 4.7 INTEGRAL EQUATIONS; PROBLEMS; REFERENCES; 5 - GENERAL BOUNDARY VALUE PROBLEMS; 5.1 DIRICHLET AND NEUMANN PROBLEMS; 5.2 SUPERPOSITION OF ELEMENTARY SOLUTIONS; 5.3 GREENS THEOREM AND AN INTEGRAL IDENTITY FOR THE POTENTIAL.

5.4 A GENERALIZED INTEGRAL IDENTITY AND GREEN FUNCTIONS5.5 APPLICATION OF GREEN FUNCTIONS; 5.6 GENERAL PROPERTIES OF GREEN FUNCTIONS; PROBLEMS; REFERENCES; 6 - DIELECTRICS; 6.1 INTRODUCTION; 6.2 POLARIZATION CHARGE AND THE AVERAGE INTERNAL FIELD; 6.3 THE RELATION OF POLARIZATION TO THE APPLIED FIELD; 6.4 CAPACITORS AND THE DIELECTRIC CONSTANT; 6.5 BOUNDARY VALUE PROBLEMS WITH DIELECTRICS; 6.6 MACROSCOPIC AND MICROSCOPIC PROPERTIES; PROBLEMS; REFERENCES; 7 - THE MAGNETOSTATIC FIELD; 7.1 CURRENT AND RELATED CONCEPTS; 7.2 FORCES BETWEEN CONDUCTORS AND THE MAGNETOSTATIC FIELD B.

7.3 DIFFERENTIAL AND INTEGRAL PROPERTIES OF B7.4 THE MAGNETIC SCALAR POTENTIAL; 7.5 THE VECTOR POTENTIAL; PROBLEMS; REFERENCE; 8 - THE SUMMATION PROBLEM FOR STATIONARY CURRENTS; 8.1 INTRODUCTION; 8.2 INTEGRAL MAGNETIC SCALAR POTENTIAL; 8.3 DIFFERENTIAL MAGNETIC SCALAR POTENTIAL; 8.4 THE VECTOR POTENTIAL AND A MULTIPOLE EXPANSION; 8.5 EXTERNAL FIELD OF DIPOLAR MAGNETIC MATTER; PROBLEMS; REFERENCES; 9 - MAGNETIC MATERIALS AND BOUNDARY VALUE PROBLEMS; 9.1 INTRODUCTION; 9.2 AN AVERAGE INTERNAL FIELD; 9.3 A POSTULATE RELATING MEAN MAGNETIZATION AND THE APPLIED FIELD.

9.4 THEORY OF PERMEABLE MATTER IN AN APPLIED FIELD9.5 THE VECTOR H; 9.6 A BOUNDARY VALUE PROBLEM; PROBLEMS; REFERENCES; 10 - FORCE AND ENERGY IN STATIC FIELDS; 10.1 ENERGY OF ASSEMBLAGE OF CHARGE DISTRIBUTION; 10.2 ENERGY OF FORMATION OF CURRENT DISTRIBUTION; 10.3 RIGID CHARGE DISTRIBUTION IN APPLIED ELECTRIC FIELD; 10.4 RIGID CURRENT DISTRIBUTION IN APPLIED MAGNETIC FIELD; 10.5 FORCE ON CONDUCTORS; 10.6 DIELECTRIC MATTER IN APPLIED ELECTRIC FIELD; 10.7 PERMEABLE MATTER IN APPLIED MAGNETIC FIELD; PROBLEMS; REFERENCES; 11 - TIME-VARYING FIELDS; 11.1 INTRODUCTION.

11.2 FARADAYS LAW OF INDUCTION.

This excellent text covers a years course in advanced theoretical electromagnetism, first introducing theory, then its application. Topics include vectors D and H inside matter, conservation laws for energy, momentum, invariance, form invariance, covariance in special relativity, and more. Read more...

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Table of Contents APPENDIXES APPENDIX A CONVERSION TABLE FOR GAUSSIAN - photo 1
Table of Contents

APPENDIXES
APPENDIX A CONVERSION TABLE FOR GAUSSIAN Picture 2 MKS UNITS

The following table gives the relations between the units of common quantities in the rationalized MKS system and in the Gaussian (CGS) system used in this book.

Read equals, with the numerical factor of column three, between the second and fourth columns. For example, one newton equals 105 dynes.

APPENDIX B DELTA FUNCTIONS The first point to grasp about -functions is that - photo 3
APPENDIX B DELTA FUNCTIONS The first point to grasp about -functions is that - photo 4
APPENDIX B DELTA FUNCTIONS

The first point to grasp about -functions is that they are not functions. They can be considered on occasion as a notational shorthand, or as the limit of a sequence of functions, or as a mnemonic for certain integration formulas, but they are not functions in the sense that sin x or e x are functions.

Their first guise in electromagnetic theory is perhaps this: We can write a general expression for the potential of any charge distribution by using the potential for a charge element and the principle of superposition. If the charge distribution is partially continuous with density p(r), and partially discrete with charges q at r i , then the expression for the potential at r consists of an integral and a sum:

B1 Now the integral and the sum are more closely akin than they may look - photo 5

(B.1)

Now the integral and the sum are more closely akin than they may look: the same physics, Coulombs law and superposition, is in both of them. It is then convenient to avoid the redundancy of writing both of them by generalizing the distribution p ( r ) so that it includes sharply localized integrals, i.e., point charges as a special case. We can then write the expression (B.1) in terms of the integral only, and this makes a very convenient shorthand.

To elaborate on this, consider one-dimensional charge distributions that are functions, say, of the x -coordinate. Suppose that we have such a distribution that is partially continuous and partially discrete. We can think of the discrete part, the one-dimensional point charges, as consisting of thin charge slabs at x 1, x 2,... , x n. The continuous part is described by a density distribution which is some function of x. How can we describe the point charges as well in terms of a density distribution ? Clearly the density distribution that describes a unit point source at, say, the origin must be a highly singular function. It must be nonvanishing essentially only at the origin, and moreover its integral must be unity. As a function of x, it is not an ordinary function, but if we call such a kind of function (x) it must have the properties

B2 Moreover since it is such a sharp function if it appears in an - photo 6

(B.2)

Moreover, since it is such a sharp function, if it appears in an integrand with any other function f ( x ) which is regular at the origin, then the contribution to the integral will come only from x = 0. Then we can evaluate f ( x ) in the integrand at the origin and get the basic defining equation of the -function,

B3 With this definition a source of strength q at x a is represented by - photo 7

(B.3)

With this definition, a source of strength q at x = a is represented by q (x a ), where the generalized defining equation is

B4 The extension to three dimensions is then straightforward If there is a - photo 8

(B.4)

The extension to three dimensions is then straightforward. If there is a point charge q at r = r1, i.e., at x = x 1, y = y , z = z , we can represent it by

p ( x, y, z ) = q(x x 1)(y y )(z z1)

or, as we shall write more succinctly,

p(r) = q(r r1).

A sum of charges with charge q i at r i is then represented by

B5 Given this last expression we can write the general expression for the - photo 9

(B.5)

Given this last expression, we can write the general expression for the potential of a charge distribution of any kind as

B6 for it is easy to verify that this formula combined with the - photo 10

(B.6)

for it is easy to verify that this formula, combined with the representation of point charges given by Eq. (B.5), just leads back to Eq. (B.1).

From the above point of view, the -function is defined by its integral properties, and the only real requirement on it is that the representation of a point charge by a -function must, when substituted in (B.6), lead back to a known correct formula. We see immediately, then, how to represent -functions in coordinates other than Cartesian. For example, in spherical coordinates r, , , ( r r 1) is represented by

The factor 1 r 2 sin is of course inserted here because in spherical - photo 11

The factor 1 /r 2 sin is, of course, inserted here because in spherical coordinates the volume element is r sin d d dr.

As we have presented it up to now, the -function is a notational shorthand, and the integral properties of the function essentially define it But as happens so often in mathematics, once the concept has been defined, it invites generalization. For example, in the expression (B.6) we may want to integrate by parts, or change variables, or expand in some series. The question then arises as to how to treat the -function part of the distribution function in these processes. Can we generalize the concept of the -function to make it close enough to the ordinary concept of a function so that at least some of the processes of analysis are defined for it? The answer is a limited yes. Although we cannot represent the -function as an ordinary function, we can represent it as the limit of a sequence of ordinary functions.

To elaborate on this, we shall go from the specific to the general. Consider for example the function

The Classical Electromagnetic Field - image 12

This is a function which has the value / at the origin, which integrates to unity independently of the value of , and, which as a function of x , becomes sharper as increases. In the limit when tends to infinity, it is then infinite at the origin, of zero width and with unit integral. In this limit, we can consider it to be a representation of the -function, and so can write

The Classical Electromagnetic Field - image 13

This specific example is only one of an infinite number of similar representations. Start with any function g(x) that has an absolute maximum at the origin, that drops off at least as 1/| x | for x large, and whose integral from to is unity,

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