12.4 Applications 435
We have now established that
π
3
(S
2
) = Z. (12.69)
This result, implying that there are many maps from the 3-sphere to the 2-sphere that are
not smoothly deformable to a constant map, was a great surprise when Hopf discovered it.
One of the principal physics consequences of the existence of the Hopf index is that
“quantum lump” quasi-particles such as the skyrmion can be fermions, even though they
are described by commuting (and therefore bosonic) fields.
To understand how this can be, we first explain that the collection of homotopy classes
π
n
(M ) is not just a set. It has the additional structure of being a group: we can compose
two homotopy classes to get a third, the composition is associative, and each homotopy
class has an inverse. To define the group composition law, we think of S
n
as the interior
of an n-dimensional cube with the map f : S
n
→ M taking a fixed value m
0
∈ M at all
points on the boundary of the cube. The boundary can then be considered to be a single
point on S
n
. We then take one of the n dimensions as being “time” and place two cubes
and their maps f
1
, f
2
into contact, with f
1
being “earlier” and f
2
being “later”. We thus
get a continuous map from a bigger box into M. The homotopy class of this map, after
we relax the condition that the map takes the value m
0
on the common boundary, defines
the composition [f
2
]◦[f
1
] of the two homotopy classes corresponding to f
1
and f
2
. The
composition may be shown to be independent of the choice of representative functions
in the two classes. The inverse of a homotopy class [f ] is obtained by reversing the
direction of “time” for each of the maps in the class. This group structure appears to
depend on the fixed point m
0
. As long as M is arcwise connected, however, the groups
obtained from different m
0
’s are isomorphic, or equivalent. In the case of π
2
(S
2
) = Z
and π
3
(S
2
) = Z, the composition law is simply the addition of the integers N ∈ Z that
label the classes. A useful exposition of homotopy theory for physicists is to be found in
a review article by David Mermin.
3
When we quantize using Feynman’s “sum over histories” path integral, we have the
option of multiplying the contributions of histories f that are not deformable into one
another by distinct phase factors exp{iφ([f ])}. The choice of phases must, however,
be compatible with the composition of histories by concatenating one after the other
– the same operation as composing homotopy classes. This means that the product
exp{iφ([f
1
]))}exp{iφ([f
2
])} of the phase factors for two possible histories must be the
phase factor exp{iφ([f
2
]◦[f
1
])} assigned to the composition of their homotopy classes.
If our quantum system consists of spins n in two space and one time dimension we can
consistently assign a phase factor exp(iπ N
Hopf
) to a history. The rotation of a single
skyrmion twists the world-line cable through 2π and so makes N
Hopf
= 1. The rotation
therefore causes the wavefunction to change sign. We will show, in the next section,
that a history where two particles change places can be continuously deformed into a
history where they do not interchange, but instead one of them is twisted through 2π. The
3
N. D. Mermin, Rev. Mod. Phys., 51 (1979) 591.