American Journal of Physics, Vol. 70, No. 11,
pp. 1129–1135, November 2002
©2002 American Association of Physics Teachers.
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Electromagnetic conic sections
Tevian Draya)
Department of Mathematics, Oregon State University, Corvallis,
Oregon 97331
Corinne A. Manogueb)
Department of Physics, Oregon State University, Corvallis, Oregon
97331
Received: 29 May 2001; accepted: 14 June 2002
Certain orthogonal coordinate
systems naturally correspond to basis vectors which are both
curl-free and divergence-free, and hence solve Maxwell's equations. After
first comparing several different traditional approaches to computing
div, grad, and curl in curvilinear coordinates, we present a new
approach, based on these "electromagnetic" basis vectors, which
combines geometry and physics. Not only is our approach tied to a
physical interpretation in terms of the electromagnetic field, it is
also a useful way to remember the formulas themselves. We give
several important examples of coordinate systems in which this
approach is valid, in each case discussing the electromagnetic
interpretation of the basis. We also give a general condition for
when an electromagnetic interpretation is possible. © 2002
American Association of Physics Teachers.
Contents
I. INTRODUCTION
What are the divergence and
curl of a vector field? Students in mathematics courses often learn
algebraic formulas for these derivatives, without learning the
geometry behind them. Those students who go on to take physics or
engineering courses which use these concepts often have trouble
"bridging the gap" between the way vector calculus is taught by
mathematicians and the way it is used in applications.1,2 One indication of the extent of this
problem is the fact that few mathematicians have seen the notation
{
,
,
} for
the unit vectors for spherical coordinates, yet most physicists
assume that their students learn this in vector calculus.3 This problem is exacerbated by the different
conventions for spherical coordinates used by physicists and
mathematicians.
We emphasize that the use of
nonrectangular coordinate bases is just one small step; the gap must
be bridged at a more fundamental level.4 And a few simple examples, such as
spherical coordinates, are sufficient for, say undergraduate physics.
The goal of this paper is rather to consider several more
sophisticated examples, showing explicitly how they relate to
electromagnetism.
Why are the formulas for
divergence and curl so much harder in curvilinear coordinates than in
rectangular coordinates? Because the basis vectors are not constant.
However, if the basis vectors were both curl-free and
divergence-free, they would pull through the computation of the curl
and divergence as though they were constant, dramatically simplifying
things. This is the basic idea we will develop here.
Furthermore, a (time-independent) vector field which is both curl-free
and divergence-free solves Maxwell's equations; such vector fields
correspond to an electromagnetic field in vacuum.
We begin by reviewing several
traditional ways of computing div, grad, and curl in curvilinear
coordinates, and in particular contrasting the approaches used by
mathematicians and physicists. We then consider several important
examples which naturally correspond to an "electromagnetic basis," in
each case discussing the electromagnetic interpretation. Most of the
examples we give are special cases of ellipsoidal coordinates; we
call them electromagnetic conic sections. We then give a
necessary and sufficient condition for a given vector field to be
electromagnetic, that is, to admit a rescaling which is both
curl-free and divergence-free. Finally, we show how to use these
basis vectors to simplify the computation of div, grad, and curl.
II. CALCULATING DIV, GRAD, AND CURL
A. Mathematics
In introductory mathematics courses,
one typically works in Cartesian coordinates, using the basis
{î,
,
}.
Given any vector field
the divergence and curl of
are defined by the formulas
and
respectively. It is an instructive exercise to try to use these
formulas to verify that
(the charge density for a point charge, away from the source) and
that
(the current density of a line charge, away from the source).
These are perhaps the two most important elementary physical examples
of divergence and curl.
B. Product rules
An important simplification occurs by
using basis vectors adapted to the symmetry of the problem.
Introducing the spherical basis vectors
it is straightforward but messy to use (2)
and (3)
to calculate, for instance, that
either using the chain rule, or by rewriting (r,
,
) in terms
of (x,y,z). If one now recalls that vector
differentiation satisfies the product rules
then it is an easy matter to use (9)
and (10)
to show that
for instance by using r2 = x2 +
y2 + z2 and r sin
=
. But these are precisely (4)
and (5);
the hard work here is in deriving the initial formulas (9)
and (10).
This approach is closely related to the concept of covariant
differentiation in differential geometry.
C. Physics
After defining the divergence and
curl in terms of a Cartesian basis, an introductory mathematics
course typically goes on to prove the divergence theorem and
Stokes' theorem. If there is time—there often is not—a geometric
interpretation is then provided through the formulas
which relate divergence and curl to flux and circulation,
respectively.
Physicists often turn this
around, and use these formulas to define the divergence and
curl, thus turning the divergence theorem and Stokes' theorem into
tautologies. These formulas are then used to compute the
formulas for the divergence and curl in various coordinate systems.
In spherical coordinates, for instance, this leads to formulas such
as
from which (13)
and (14)
follow immediately. For a good, informal description of this
approach, see Schey.5
D. Orthogonal coordinates
The preceding approach generalizes
naturally to any orthogonal coordinate system, that is, one in which
the three coordinate directions are everywhere orthogonal. Typical
examples are rectangular, cylindrical, and spherical coordinates, but
there are many more.
A general orthogonal coordinate
system (u,v,w) will have a line element of the
form
If we denote the unit vector fields in the coordinate
directions by {û,
,
}, then
we can expand any vector field
as
It is then a fairly simple computation6 to derive the general formulas
using the formulas (15)
and (16).
These formulas can hardly be
called obvious. The corresponding formula for the gradient is much
more natural. Starting from the chain rule, in the form
the all-important directional derivative, in the form
together with the "square root" of the line element (in the sense
d
·d
=
ds2), given by
we obtain
Examining (21)
and (22),
we see that there are special vector fields which are divergence or
curl free, since
and similarly for
and
. These formulas can also be derived from the
identities
when one realizes that in orthogonal coordinates one has
III. ELECTROMAGNETIC CONIC SECTIONS
A. More product rules
As discussed in Boas,7 the existence of a natural
divergence-free basis along the lines of (27)
can be used to reduce the computation of the divergence to the
much simpler computation of the gradient. Similarly, the existence of
a natural curl-free basis along the lines of (28)
can be used to simplify the computation of the curl. In each
case, this is accomplished using the appropriate product rule, (11)
or (12),
respectively. However, it is noteworthy that these two natural bases
only agree in rectangular coordinates.
What if one could find a basis
which was both divergence- and curl-free? In that case, one
would never need to remember the formulas for the divergence and
curl; all computations would reduce to the much simpler formula for
the gradient.
Such a basis would also be of
physical interest. A vector field which is both divergence- and
curl-free solves Maxwell's vacuum equations, and can hence be
interpreted as an electric or magnetic field. We are thus led to ask
whether we can find a basis of electromagnetic fields.
We begin by considering
several examples.
B. Plane
First of all, the rectangular basis
{î,
,
}
is constant, and therefore, of course, both divergence- and
curl-free. Each basis vector field must therefore describe an
electromagnetic field. Which one? Consider an infinite parallel-plate
capacitor,8 with infinite separation between the
plates. If the plates have equal but opposite (uniform) charge
densities, then there is a constant electric field orthogonal to the
plates. If, instead, the plates have equal but opposite (uniform)
current densities, then there is a constant magnetic field parallel
to the plates (but orthogonal to the currents).
C. Cylinder
Consider now the cylindrical coordinate
system, defined by9
Horizontal (z = constant) and vertical (tan
= constant) slices
through this coordinate system are shown in Fig. 1. Denoting the orthonormal basis for cylindrical
coordinates as usual by {
,
,
}, we
have 
![[equivalent]](ConicSections_files/equiv.gif)
,
and thus this basis vector field is both divergence- and
curl-free. But what about the other basis vectors?
Figure 1.
The simplest cylindrical
electromagnetic fields correspond to an infinite straight wire carrying
either a uniform charge density or a uniform current density. It
is straightforward to work out the corresponding fields: Up to
scale factors, the electric field of the (positively) charged
z axis is
and the magnetic field of the (upward) current-carrying z
axis is
Thus, an "electromagnetic" basis in this case is given by {
,
,
}.
All of our remaining examples will
be axially symmetric, and will thus have
as a
coordinate,
as a
basis vector field, and
as an electromagnetic basis vector field (although s =
will need to be expressed in
terms of the given coordinates). We will omit further discussion of
this case in (most of) the subsequent examples, and we will have no
further use for horizontal slices analogous to (a) in Fig. 1.
D. Sphere
What about the other standard
coordinate system, namely spherical coordinates, defined implicitly
by
(with
as before), and shown in Fig. 2. The orthonormal basis for spherical coordinates is
{
,
,
},
and we already know that
is both divergence- and curl-free.
Figure 2.
The only obvious spherical
electromagnetic field is the electric field of a point charge, which
is, up to a scale factor
This solves part of the problem. But what electromagnetic field,
if any, looks like
?
Somewhat surprisingly, it turns out there is one, namely the electric
field of two half-infinite uniform line charges, with equal but
opposite charge densities, as shown in Fig. 3. Up to a scale factor, the resulting
divergence-free and curl-free basis vector field is
and an electromagnetic basis is given by {
,
,
}.
Figure 3.
E. Spheroid and hyperboloid
What about other, less common,
orthogonal coordinate systems? Consider first prolate spheroidal10 coordinates, defined by
as shown in Fig. 4. The relevant orthonormal basis vectors are
û and
; our goal is to find multiples of
these which are both divergence- and curl-free, if possible.
Figure 4.
With the wisdom of hindsight, that
is, after having first computed the answer by brute force, it
is clear that such vector fields do indeed exist. Consider the
spherical model above, in which a multiple of
was produced by two half-infinite line charges which
were joined at the origin. Separate the two instead by a
finite distance, as shown in Fig. 5. The resulting electric field is just
(proportional to)
and is therefore spheroidal. Similarly, the electric field of the
"missing" finite line segment is just (proportional to)
which is hyperboloidal, as shown in Fig. 6.11 An electromagnetic basis in this case is
therefore given by {
,
,
}.
Figure 5.
Figure 6.
F. Paraboloid
Moving right along, now consider
parabolic coordinates, defined by
and shown in Fig. 7. Do there exist multiples of û and
which are both divergence- and curl-free?
Figure 7.
Again, with the wisdom of hindsight the
answer is clearly yes. The electric field of a half-infinite, uniform
line charge is shown in Fig. 8, corresponding to
respectively.
Figure 8.
G. Another hyperboloid
Buoyed by our success, let us finally
consider hyperboloidal (inverse paraboloidal) coordinates, defined by
and shown in Fig. 9. We have
and we seek multiples of û and
which are both divergence- and curl-free.
Figure 9.
There are none.
H. General case
So when does it work?
Given a vector field
, we ask whether there exists a function
such
that 
is both divergence- and curl-free, that is,
such that
Using the product rules (11)
and (12),
we can rewrite these conditions as
On the other hand, the identity
leads to
Rearranging terms and using (56)
and (57)
then yields
Dividing (60)
by
and taking the curl of both sides yields
since the left-hand side is the curl of
ln
. The necessary
and sufficient condition that a suitable
exist is
therefore (61);
if
exists, then (61)
is satisfied due to the identity (30),
whereas if (61)
is satisfied, then there exists a (local) potential function, which
is ln
.
IV. DISCUSSION
We have demonstrated a
possible alternative way to compute the divergence and curl in
certain standard cases. For instance, in spherical coordinates, one
really need only remember that {
,
,
}
is an electromagnetic basis—ideally by recalling the corresponding
electromagnetic fields. The divergence and curl are then easily
computed from formulas like
Yes, this requires knowing how to compute the gradient in
spherical coordinates, but this can easily be rederived as needed
from the geometrically obvious formula
We have given several examples of
orthogonal coordinates which admit an "electromagnetic basis." All of
these examples are separable coordinates in the sense of Morse
and Feschbach,12 that is, Laplace's equation is
separable in these coordinates. It is straightforward to check that
all 11 of the separable coordinate systems in Morse and Feschbach,12
all of which are special cases of ellipsoidal coordinates, admit an
electromagnetic basis.
One might suspect that
separable coordinates are the only ones which admit an
electromagnetic basis. However, there are also nonseparable coordinates
which admit an electromagnetic basis, an example being
"logcoshcylindrical" coordinates, defined by
Turning to the general case, the
condition (61)
not only characterizes the vector fields
which can be rescaled so as to be both divergence- and curl-free, it
also provides an explicit algorithm for determining
. There is
another, simpler characterization, but without this property.
Requiring
to
be curl-free means that (locally)
In particular, since we are assuming
=

, this forces the original vector
field
to be orthogonal to the surfaces
{f = constant}. Thus, a necessary condition on
is that it be hypersurface orthogonal. This
condition is always satisfied for the examples considered here,
constructed from a coordinate system.
The condition that
be divergence-free imposes the further
condition that
so that
must be the gradient of a
harmonic function. Thus, the question of which coordinate
systems admit basis vectors which can (all) be rescaled so as
to be divergence- and curl-free is equivalent to the question of
which coordinate systems can themselves be rescaled so as to be
harmonic coordinates.
We conclude by noting that
harmonic functions in two dimensions are closely related to analytic
functions. A vector field
=
Pî + Q
is divergence- and curl-free if, and
only if, P–iQ is analytic, since13
ACKNOWLEDGMENTS
It is a pleasure to thank Reed
College for a colloquium invitation which got this project started.
This material is based upon work supported by the National
Science Foundation under Grants Nos. DUE-9653250 (Paradigms Project) and
DUE-0088901 (Vector Calculus Bridging Project). This work has also
been supported by the Oregon Collaborative for Excellence in the
Preparation of Teachers (OCEPT) and by an L L Stewart Faculty
Development Award from Oregon State University.
REFERENCES
Citation links
[e.g., Phys. Rev. D 40, 2172 (1989)] go to online
journal abstracts. Other links (see Reference Information)
are available with your current login. Navigation of links may be more efficient
using a second browser
window.
- Jason W. Dunn and Julius Barbane, "One model for an integrated
math/physics course focusing on electricity and magnetism and related calculus
topics," Am. J. Phys.
68, 749–757 (2000). first
citation in article
- Tevian Dray and Corinne A. Manogue, "The vector calculus gap:
mathematics
physics," PRIMUS 9, 21–28 (1999). first
citation in article
- For the record, while a traditional course in multivariable or
vector calculus will certainly discuss polar, cylindrical, and spherical
coordinates, vectors will most likely be expressed exclusively in terms
of their rectangular components. first
citation in article
- Tevian Dray and Corinne A. Manogue, "Using differentials to
bridge the vector calculus gap," College Math. J. (to appear). first
citation in article
- H. M. Schey, div, grad, curl, and all that, 3rd ed.
(Norton, New York, 1997). first
citation in article
- David J. Griffiths, Introduction to Electrodynamics, 3rd
ed. (Prentice-Hall, New York, 1999). first
citation in article
- Mary L. Boas, Mathematical Methods in the Physical
Sciences, 2nd ed. (Wiley, New York, 1983). first
citation in article
- One plate is in fact sufficient. The advantage of two plates is
that the field vanishes outside the capacitor. first
citation in article
- We use
rather than
for compatibility
with our later examples, and srather than r to avoid confusion
with spherical coordinates. first
citation in article
- A spheroid is an ellipsoid with two axes of the same length.
first
citation in article
- It is instructive to consider this latter example as a
"stretched out" point charge. first
citation in article
- Philip M. Morse and Herman Feshbach, Methods of Theoretical
Physics (McGraw-Hill, New York, 1953), Chap. 5. first
citation in article
- A similar statement can be made in three dimensions, using
quaternions in place of the complex numbers. first
citation in article
FIGURES
Full figure (11 kB)
Fig. 1. (a) A horizontal slice of cylindrical coordinates,
resulting in the usual polar coordinate grid. (b) A vertical slice of
cylindrical coordinates, through the z axis (shown as a heavy
line). First
citation in article
Full figure (8 kB)
Fig. 2. A vertical slice of spherical coordinates, showing the
r
coordinate grid. First
citation in article
Full figure (5 kB)
Fig. 3. A spherical electric field. If the positive z axis
is given a uniform positive charge density, and the negative z
axis is given an equal and opposite charge density, the resulting
field lines are spherical, that is, in the
direction. First
citation in article
Full figure (10 kB)
Fig. 4. A vertical slice of prolate spheroidal coordinates. The
curves orthogonal to the ellipses are hyperbolas. First
citation in article
Full figure (7 kB)
Fig. 5. A spheroidal electric field. If the oppositely charged half-lines
in the spherical example are separated by a finite gap, the
resulting field lines are spheroidal. First
citation in article
Full figure (3 kB)
Fig. 6. A hyperboloidal electric field, the electric field of a
uniformly charged line segment. First
citation in article
Full figure (5 kB)
Fig. 7. A vertical slice of parabolic coordinates. Both families
of orthogonal curves are parabolas. First
citation in article
Full figure (8 kB)
Fig. 8. Two paraboloidal electrical fields, namely the electric
field of a half-infinite uniform line charge, along (a) the negative
z axis and (b) the positive z axis. First
citation in article
Full figure (7 kB)
Fig. 9. A vertical slice of hyperboloidal coordinates. Both
families of orthogonal curves are hyperbolas. First
citation in article
FOOTNOTES
aElectronic mail: tevian@math.orst.edu
bElectronic mail: corinne@physics.orst.edu
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