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3

Electromagnetic

Potentials

Instead of expressing the laws of electrodynamics in terms of electric and magnetic fields, it turns out that it is often more convenient to express the theory in terms of potentials. In this Chapter we will introduce and study the properties of such potentials.

3.1 The electrostatic scalar potential

As we saw in Equation (1.6) on page 4, the electrostatic field Estat(x) is irrotational. Hence, it may be expressed in terms of the gradient of a scalar field. If we denote this scalar field by stat(x), we get

Estat(x) = r stat(x)

(3.1)

Taking the divergence of this and using Equation (1.7) on page 4, we obtain

Poissons' equation

r2 stat(x) = r Estat(x) =

(x)

(3.2)

"0

A comparison with the definition of Estat, namely Equation (1.5) on page 3, after the r has been moved out of the integral, shows that this equation has the solution

stat(x) =

1

 

(x0)

d3x0 +

(3.3)

 

 

 

4"0 V jx x0j

 

 

where the integration is taken over all source points x0 at which the charge density (x0) is non-zero and is an arbitrary quantity which has a vanishing gradient. An example of such a quantity is a scalar constant. The scalar function stat(x) in Equation (3.3) above is called the electrostatic scalar potential.

33

 

 

34

ELECTROMAGNETIC POTENTIALS

 

3.2 The magnetostatic vector potential

Consider the equations of magnetostatics (1.20) on page 8. From Equation (M.82) on page 175 we know that any 3D vector a has the property that r (r a) 0 and in the derivation of Equation (1.15) on page 7 in magnetostatics we found that r Bstat(x) = 0. We therefore realise that we can always write

Bstat(x) = r Astat(x)

(3.4)

where Astat(x) is called the magnetostatic vector potential.

We saw above that the electrostatic potential (as any scalar potential) is not unique: we may, without changing the physics, add to it a quantity whose spatial gradient vanishes. A similar arbitrariness is true also for the magnetostatic vector potential.

In the magnetostatic case, we may start from Biot-Savart's law as expressed by Equation (1.13) on page 6 and “move the r out of the integral:”

Bstat(x) =

0

 

 

 

 

 

 

x

 

x0

 

 

d3x0

 

 

 

 

j(x0)

 

 

 

 

 

3

 

 

4

 

 

 

 

 

 

 

 

0

 

V

 

 

jx x0j

 

1

 

 

 

d3x0

 

=

 

j(x0) r

 

 

 

 

 

(3.5)

 

 

 

 

 

 

 

4

x

 

x

0j

 

 

 

 

 

V

 

j(x0)

 

j

 

 

 

 

= r

 

0

 

 

d3x0

 

 

 

 

 

4 V

j

x

 

x

0j

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

An identification of terms allows us to define the static vector potential as

Astat(x) =

0

 

j(x0)

d3x0 +a(x)

(3.6)

4 V jx x0j

 

 

 

where a(x) is an arbitrary vector field whose curl vanishes. From Equation (M.78) on page 175 we know that such a vector can always be written as the gradient of a scalar field.

3.3 The electromagnetic scalar and vector potentials

Let us now generalise the static analysis above to the electrodynamic case, i.e., the case with temporal and spatial dependent sources (t;x) and j(t;x), and corresponding fields E(t;x) and B(t;x), as described by Maxwell's equations (1.43) on page 14. In other words, let us study the electromagnetic potentials(t;x) and A(t;x).

From Equation (1.43c) on page 14 we note that also in electrodynamics the homogeneous equation r B(t;x) = 0 remains valid. Because of this

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3.3 THE ELECTROMAGNETIC SCALAR AND VECTOR POTENTIALS

35

 

divergence-free nature of the timeand space-dependent magnetic field, we can express it as the curl of an electromagnetic vector potential:

B(t;x) = r A(t;x)

(3.7)

Inserting this expression into the other homogeneous Maxwell equation, Equation (1.30) on page 11, we obtain

r E(t;x) =

@

 

[r A(t;x)] = r

@

A(t;x)

(3.8)

 

 

 

 

@t

@t

or, rearranging the terms,

 

 

 

r E(t;x) +

@

A(t;x) = 0

 

 

(3.9)

 

 

 

@t

 

 

As before we utilise the vanishing curl of a vector expression to write this vector expression as the gradient of a scalar function. If, in analogy with the electrostatic case, we introduce the electromagnetic scalar potential function(t;x), Equation (3.9) becomes equivalent to

 

@

 

E(t;x) +

@t A(t;x) = r (t;x)

(3.10)

This means that in electrodynamics, E(t;x) can be calculated from the formula

E(t;x) = r (t;x)

@

 

@t A(t;x)

(3.11)

and B(t;x) from Equation (3.7) above. Hence, it is a matter of taste whether we want to express the laws of electrodynamics in terms of the potentials (t;x) and A(t;x), or in terms of the fields E(t;x) and B(t;x). However, there exists an important difference between the two approaches: in classical electrodynamics the only directly observable quantities are the fields themselves (and quantities derived from them) and not the potentials. On the other hand, the treatment becomes significantly simpler if we use the potentials in our calculations and then, at the final stage, use Equation (3.7) and Equation (3.11) above to calculate the fields or physical quantities expressed in the fields.

Inserting (3.11) and (3.7) into Maxwell's equations (1.43) on page 14 we obtain, after some simple algebra and the use of Equation (1.9) on page 5, the general inhomogeneous wave equations

1

@2

r2 =

(t;x)

@

1 @

 

 

 

 

 

 

 

+

 

r A +

 

 

 

 

 

 

 

(3.12a)

 

c2

@t2

"0

@t

c2

@t

1

@2

 

 

 

 

1 @

 

 

 

 

 

A r2A = 0j(t;x) r r A +

 

 

 

 

(3.12b)

 

c2

@t2

c2

@t

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36

ELECTROMAGNETIC POTENTIALS

 

These two second order, coupled, partial differential equations, representing in all four scalar equations (one for and one each for the three components A1, A2, and A3 of A) are completely equivalent to the formulation of electrodynamics in terms of Maxwell's equations, which represent eight scalar first-order, coupled, partial differential equations.

3.3.1 Electromagnetic gauges

Lorentz equations for the electromagnetic potentials

As they stand, Equations (3.12) look complicated and may seem to be of limited use. However, if we write Equation (3.7) on the preceding page in the form r A(t;x) = B(t;x) we can consider this as a specification of r A. But we know from Helmholtz' theorem that in order to determine the (spatial behaviour) of A completely, we must also specify r A. Since this divergence does not enter the derivation above, we are free to choose r A in whatever way we like and still obtain the same physical results! This is somewhat analogous to the freedom of adding an arbitrary scalar constant (whose grad vanishes) to the potential energy in classical mechanics and still get the same force.

With a judicious choice of r A, the calculations can be simplified considerably. Lorentz introduced

1 @

 

 

r A + c2 @t

= 0

(3.13)

which is called the Lorentz gauge condition, because this choice simplifies the system of coupled equations (3.12) on the previous page into the following set of uncoupled partial differential equations which we call the Lorentz inhomogeneous wave equations:

$2

def

1

@2

r2 =

(t;x)

(3.14a)

 

 

 

 

 

 

 

 

c2

@t2

"0

 

 

def

1

@2

 

 

 

 

$2A

 

 

 

A r2A = 0j(t;x)

(3.14b)

 

c2

@t2

where $2 is the d'Alembert operator discussed in Example M.5 on page 171. We shall call (3.14) the Lorentz equations for the electromagnetic potentials.

Gauge transformations

We saw in Section 3.1 on page 33 and in Section 3.2 on page 34 that in electrostatics and magnetostatics we have a certain mathematical degree of freedom,

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3.3 THE ELECTROMAGNETIC SCALAR AND VECTOR POTENTIALS

37

 

up to terms of vanishing gradients and curls, to pick suitable forms for the potentials and still get the same physical result. In fact, the way the electromagnetic scalar potential (t;x) and the vector potential A(t;x) are related to the physically observables gives leeway for similar “manipulation” of them also in electrodynamics. If we transform (t;x) and A(t;x) simultaneously into new ones 0(t;x) and A0(t;x) according to the mapping scheme

(t;x) 0

(t;x) = (t;x) +

@

(t;x)

(3.15a)

 

7!

(t;x) = A(t;x)

 

@t

(3.15b)

A(t;x) A0

 

r (t;x)

7!

 

 

 

 

where (t;x) is an arbitrary, differentiable scalar function called the gauge function, and insert the transformed potentials into Equation (3.11) on page 35 for the electric field and into Equation (3.7) on page 35 for the magnetic field, we obtain the transformed fields

E0

= r 0

@

A0

= r

@

r

@

A +

@

r= r

@

A (3.16a)

 

 

 

 

 

@t

@t

@t

@t

@t

B0

= r A0 = r A r r= r A

 

 

 

(3.16b)

where, once again Equation (M.78) on page 175 was used. Comparing these expressions with (3.11) and (3.7) we see that the fields are unaffected by the gauge transformation (3.15). A transformation of the potentials and A which leaves the fields, and hence Maxwell's equations, invariant is called a gauge transformation. A physical law which does not change under a gauge transformation is said to be gauge invariant. By definition, the fields themselves are, of course, gauge invariant.

The potentials (t;x) and A(t;x) calculated from (3.12) on page 35, with an arbitrary choice of r A, can be further gauge transformed according to (3.15) above. If, in particular, we choose r A according to the Lorentz condition, Equation (3.13) on the facing page, and apply the gauge transformation (3.15) on the resulting Lorentz equations (3.14) on the preceding page, these equations will be transformed into

1

@2

r2 +

@ 1 @2

 

r2 =

(t;x)

(3.17a)

 

c2

 

@t2

@t

 

c2

 

 

@t2

 

"0

 

1

@2

 

1 @2

 

 

 

 

 

 

 

 

A r2A r

 

 

 

 

r2 = 0j(t;x)

(3.17b)

 

c2

@t2

c2

@t2

 

We notice that if we require that the gauge function (t;x) itself be restricted to fulfil the wave equation

1 @2

 

c2 @t2 r2= 0

(3.18)

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38

ELECTROMAGNETIC POTENTIALS

 

these transformed Lorentz equations will keep their original form. The set of potentials which have been gauge transformed according to Equation (3.15) on the preceding page with a gauge function (t;x) which is restricted to fulfil Equation (3.18) on the previous page, i.e., those gauge transformed potentials for which the Lorentz equations (3.14) are invariant, comprises the Lorentz gauge.

Other useful gauges are

The radiation gauge, also known as the transverse gauge, defined by r A = 0.

The Coulomb gauge, defined by = 0, r A = 0.

The temporal gauge, also known as the Hamilton gauge, defined by= 0.

The axial gauge, defined by A3 = 0.

The process of choosing a particular gauge condition is referred to as gauge fixing.

3.3.2Solution of the Lorentz equations for the electromagnetic potentials

As we see, the Lorentz equations (3.14) on page 36 for (t;x) and A(t;x) represent a set of uncoupled equations involving four scalar equations (one equation for and one equation for each of the three components of A). Each of these four scalar equations is an inhomogeneous wave equation of the following generic form:

$2 (t;x) = f (t;x)

(3.19)

where is a shorthand for either or one of the vector components of A, and f is the pertinent generic source component.

We assume that our sources are well-behaved enough in time t so that the Fourier transform pair for the generic source function

F 1

def

 

 

1

 

 

(3.20a)

[ f!(x)] f (t;x) =

f!(x)e i!td!

 

 

1

1

 

 

 

 

def

 

1

i!t

 

 

F[ f (t;x)] f!(x) =

 

1 f (t;x) e

 

dt

(3.20b)

2

 

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3.3 THE ELECTROMAGNETIC SCALAR AND VECTOR POTENTIALS

39

 

exists, and that the same is true for the generic potential component:

 

1

!(x) e i!td!

 

(t;x) =

(3.21a)

 

1

 

 

 

!(x) =

1

 

1

(t;x) ei!tdt

(3.21b)

2 1

 

 

 

Inserting the Fourier representations (3.20a) and (3.21a) into Equation (3.19) on the preceding page, and using the vacuum dispersion relation for electromagnetic waves

! = ck

(3.22)

the generic 3D inhomogeneous wave equation Equation (3.19) on the facing page turns into

r2 !(x) +k2 !(x) = f!(x)

(3.23)

which is a 3D inhomogeneous time-independent wave equation, often called the 3D inhomogeneous Helmholtz equation.

As postulated by Huygen's principle, each point on a wave front acts as a point source for spherical waves which form a new wave from a superposition of the individual waves from each of the point sources on the old wave front. The solution of (3.23) can therefore be expressed as a superposition of solutions of an equation where the source term has been replaced by a point source:

r2G(x;x0) +k2G(x;x0) = (x x0)

(3.24)

and the solution of Equation (3.23) above which corresponds to the frequency ! is given by the superposition

! = f!(x0)G(x;x0)d3x0

(3.25)

The function G(x;x0) is called the Green's function or the propagator.

In Equation (3.24), the Dirac generalised function (x x0), which represents the point source, depends only on x x0 and there is no angular dependence in the equation. Hence, the solution can only be dependent on r = jx x0j. If we interpret r as the radial coordinate in a spherically polar coordinate system, the “spherically symmetric” G(r) is given by the solution of

d2

 

dr2 (rG) +k2(rG) = r (r)

(3.26)

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40

ELECTROMAGNETIC POTENTIALS

 

Away from r = jx x0j

= 0, i.e., away from the source point x0, this equation

takes the form

 

 

 

 

 

 

 

 

d2

(rG) +k2(rG) = 0

 

 

 

 

 

(3.27)

 

dr2

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

with the well-known general solution

 

 

 

 

 

 

+eikr

e ikr

 

+eikjx x0j

 

e ikjx x0j

 

G =C

 

 

+C

 

C

 

 

+C

 

(3.28)

 

r

r

 

jx x0j

jx x0j

where C are constants.

In order to evaluate the constants C , we insert the general solution, Equation (3.28) above, into Equation (3.24) on the preceding page and integrate

over a small volume around r = jx x0j = 0. Since

 

1

1

 

 

G( x x0 ) C+

 

+C

 

; x x0 ! 0

(3.29)

jx x0j

jx x0j

Equation (3.24) on the previous page can under this assumption be approximated by

 

#

r2

1

d3x0 +k2

"

# 1

d3x0

 

"C+ +C

 

 

 

C+ +C

 

 

 

 

 

jx x0j

 

jx x0j

(3.30)

0 3 0

= ( x x )d x

In virtue of the fact that the volume element d3x0 in spherical polar coordinates is proportional to jx x0j2, the second integral vanishes when jx x0j !0. Furthermore, from Equation (M.73) on page 174, we find that the integrand in the first integral can be written as 4 (jx x0j) and, hence, that

C+ +C =

 

1

 

 

 

 

 

(3.31)

4

 

 

 

Insertion of the general solution Equation (3.28) into Equation (3.25) on

the previous page gives

 

 

 

 

!(x) =C

+ f!(x0)

eikjx x0j

d3x0 +C f!(x0)

e ikjx x0j

d3x0

(3.32)

jx x0j

 

 

 

 

 

 

jx x0j

 

The Fourier transform to ordinary t domain of this is obtained by inserting the above expression for !(x) into Equation (3.21a) on the preceding page:

 

 

 

exp & i! t

 

kjx x0j

 

 

 

3

 

+ %

 

 

!

('

(t;x) =C

 

f!(x0)

 

 

 

 

 

d!d x0

 

 

jx x0j

 

 

 

 

 

 

 

 

(3.33)

 

 

 

exp & i! t + kjx x0j

3

 

 

%

 

 

 

!

)'

+C

f!(x0)

 

 

 

 

 

d!d x0

jx x0j

 

 

 

 

 

 

 

 

 

 

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3.3 BIBLIOGRAPHY

41

 

If we introduce the retarded time tret0 and the advanced time tadv0 in the following way [using the fact that in vacuum k=!=1=c, according to Equation (3.22) on page 39]:

 

 

 

 

 

 

 

 

 

 

k

x

 

x0

 

 

 

 

x

 

x0

 

 

 

t0

= t0

(t; x

 

x0

) = t

 

j

 

 

 

j

= t

j

 

 

 

 

j

 

(3.34a)

ret

 

ret

 

 

 

 

 

 

!

 

 

 

 

 

 

 

 

 

c

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

k

x

 

x0

 

 

 

 

 

x

 

x0

 

 

t0

 

= t0

 

(t; x

 

x0 ) = t +

 

j

 

 

 

j

= t +

j

 

 

 

j

(3.34b)

adv

adv

 

 

 

 

 

 

 

!

 

 

 

 

 

 

 

 

 

c

 

 

 

 

and use Equation (3.20a) on page 38, we obtain

 

+

f (t0

;x0)

 

 

f (t0

;x0)

 

(t;x) =C

 

ret

 

d3x0

+C

 

adv

 

d3x0

(3.35)

 

 

 

 

 

 

 

 

jx x0j

 

 

jx x0j

 

This is a solution to the generic inhomogeneous wave equation for the potential components Equation (3.19) on page 38. We note that the solution at time t at the field point x is dependent on the behaviour at other times t0 of the source at x0 and that both retarded and advanced t0 are mathematically acceptable solutions. However, if we assume that causality requires that the potential at

(t;x) is set up by the source at an earlier time, i.e., at (tret0 ;x0), we must in Equation (3.35) set C = 0 and therefore, according to Equation (3.31) on the

preceding page, C+ = 1=(4 ).

The retarded potentials

From the above discussion on the solution of the inhomogeneous wave equation we conclude that under the assumption of causality the electromagnetic potentials in vacuum can be written

1

 

 

(t0

;x0)

 

(t;x) =

 

 

 

 

ret

 

 

d3x0

(3.36a)

 

 

 

 

 

 

 

4 "0 jx x0j

 

 

0

j(t0 ;x0)

 

A(t;x) =

 

 

 

ret

 

d3x0

(3.36b)

4

 

 

 

 

jx x0j

 

Since these retarded potentials were obtained as solutions to the Lorentz equations (3.14) on page 36 they are valid in the Lorentz gauge but may be gauge transformed according to the scheme described in Subsection 3.3.1 on page 36. As they stand, we shall use them frequently in the following.

Bibliography

[1]L. D. FADEEV, AND A. A. SLAVNOV, Gauge Fields: Introduction to Quantum Theory, No. 50 in Frontiers in Physics: A Lecture Note and Reprint Series. Ben-

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42

ELECTROMAGNETIC POTENTIALS

 

jamin/Cummings Publishing Company, Inc., Reading, MA . . . , 1980, ISBN 0- 8053-9016-2.

[2]M. GUIDRY, Gauge Field Theories: An Introduction with Applications, Wiley & Sons, Inc., New York, NY . . . , 1991, ISBN 0-471-63117-5.

[3]J. D. JACKSON, Classical Electrodynamics, third ed., Wiley & Sons, Inc., New York, NY . . . , 1999, ISBN 0-471-30932-X.

[4]W. K. H. PANOFSKY, AND M. PHILLIPS, Classical Electricity and Magnetism, second ed., Addison-Wesley Publishing Company, Inc., Reading, MA . . . , 1962, ISBN 0-201-05702-6.

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