In solid-state physics, the notion of Brillouin zones is used to describe
quantum mechanical properties of a crystal. In a crystal, the atoms are
arranged in a lattice; for example, in NaCl, the sodium and chorine atoms are
arranged along the points of the simple cubic lattice
.
If we pick a
specific atom and call it the origin, its first Brillouin zone consists
of the points in
which are closer to the origin than to any other
element of the lattice. This same zone can be constructed as follows:
for each element a in the lattice, let L0a be the perpendicular
bisecting plane of the line between 0 and a (this plane is called a Bragg
plane). The volume about the origin enclosed by these intersecting planes is
the first Brillouin zone, b1(0). This construction also allows us to define
the higher Brillouin zones as well: a point x is in bn if the line
connecting it to the origin crosses exactly n-1 planes L0a, counted
with multiplicity.
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This notion was introduced by Brillouin in the 1930s ([Br]), and plays an important role in solid-state theory (see, for example, [AM], or [Jo2], also [Ti]). The construction which gives rise to Brillouin zones is not limited to consideration of crystals, however. For example, in computational geometry, the notion of the Voronoi cell corresponds exactly to the first Brillouin zone described above (see [PS]). We shall also see below how, after suitable generalization, this construction coincides with the Dirichlet domain of Riemannian geometry, and in many cases, to the focal decomposition introduced in [Pe1] (see also [Pe3]).
With some slight hypotheses (see section 2), we
generalize the construction of Brillouin zones to any discrete set S in a
path-connected, proper metric space X. We generalize the Bragg planes
above as mediatrices, defined here.
Now choose a preferred point x0 in S, and consider the collection of
mediatrices
.
These partition X into Brillouin
zones as above: roughly, the n-th Brillouin zone Bn(x0) consists of
those points in X which are accessible from x0 by crossing exactly n-1mediatrices. (There is some difficulty accounting for multiple crossings--
see definition 2.7 for a precise statement.)
One basic property of the zones Bn is that they tile the space X:
We now discuss the relationship of Brillouin zones and focal decomposition
of Riemannian manifolds.
If x1(t) and x2(t) are two solutions of a second order differential
equation with
x1(0) = x2(0) and there is some
so that
x1(T) =
x2(T), then the trajectories x1 and x2 are said to focus at time
T. One can ask how the number of trajectories which focus varies with the
endpoint x(T)-- this gives rise to the
concept of a focal decomposition (originally called a sigma
decomposition). This concept was introduced in [Pe1] and
has important applications in physics, for example when computing the
semiclassical quantization using the Feynman path integral method (see
[Pe3]). There is also a connection with the arithmetic of positive
definite quadratic forms (see [Pe2], [KP], and [Pe3]).
Brillouin zones have a similar connection with arithmetic, as can be seen in
section 4.
More specifically, consider the two-point boundary problem
Later, in [KP], the idea of focal decomposition was approached in the
context of geodesics of a Riemannian manifold M (in addition to a
reformulation of the main theorem of [PT]). Here, one takes a basepoint
x0 in the manifold M: two geodesics
and
focus at some point
if
.
This
gives rise to a decomposition of the tangent space of M at x into regions
where the same number of geodesics focus.
In order to study focusing of geodesics on an orbifold (M,g) with metric
g via Brillouin zones, we do the following. Choose a base-point p0 in
M and construct the universal cover X, lifting p0 to a point x0 in
X. Let
be a smooth curve in M with initial point p0 and
endpoint p. Lift
to
in X with initial
point x0. Its endpoint will be some
.
The metric
g on M is lifted to a metric
on X by setting
.
Under the above conditions, the group G of deck transformations is
discontinuous and so
is a discrete set.
One can ask how many geodesics of length t there are which start at p0end in p, or translated
to
,
this becomes: How many mediatrices
Lx0,s intersect at x, as s ranges over
?
Notice that if the universal cover of M coincides with the tangent space
TMx, the focal decomposition of [KP] and that given by Brillouin zones
will be the same. If the universal cover and the tangent space are
homeomorphic (as is the case for a manifold of constant negative
curvature), the two decompositions are not identical, but there is a clear
correspondence. However, if the universal cover of the manifold is not
homeomorphic to the tangent space at the base point, the focal decomposition
and that given by constructing Brillouin zones in the universal cover are
completely different. For example, let M be
,
and let x be any
point in it. The focal decomposition with respect to x gives a collection
of nested n-1-spheres centered at x; on each of these infinitely many
geodesics focus (each sphere is mapped by the exponential to either x or
its antipodal point). Between the spheres are bands in which no focusing
occurs. (See [Pe3]). However, using the construction outlined in the
previous paragraph gives a very different result. Since
is simply
connected, it is its own universal cover. There is only one point in our
discrete set, and so the entire sphere Sn is in the first zone B1.
The organization of this paper is as follows. In section 2,
we set up the general machinery we need, and prove the main theorems in the
context of a discrete set S in a proper metric space.
Section 3 explores this in the context of manifolds of constant
curvature. The universal cover is
,
,
or
,
and the group
G of deck transformations is a discrete group of isometries (see
[doC]). The discrete set S is the orbit of a point not fixed by any
element of G under this discontinuous group. It is easy to see that the
mediatrices in this case are totally geodesic spaces. From the basic
property explained above, one can deduce that the n-th Brillouin zone is a
fundamental domain for the group G in X.
In section 4, we calculate exactly the number of geodesics of
length t that connect the origin to itself in two cases: the flat torus
and the Riemann surfaces
,
for
.
While these calculations could, of course, be done
independent of our construction, the Brillouin zones help visualize the
process.
In the final section, we give a nontrivial example in the case of a non-Riemannian metric, and mention a connection to the question of how many integer solutions there are to the equation ak + bk = n, for fixed k.
Acknowledgments: It is a pleasure to acknowledge useful
conversations with Federico Bonetto, Johann Dupont, Bernie Maskit, John
Milnor, Chi-Han Sah, and Duncan Sands.