Brillouin zone. The alternative is considered below. Here, the push forward of the
embedding F is another homomorphism F
: H
2
ðFS; RÞ!H
2
ðT
3
p
; RÞ; which is
trivial, F
ðH
2
ðFS; RÞÞ ¼ 0; since FS is a boundary in T
3
p
: Therefore, for any closed
2-form x; dx ¼ 0,onT
3
p
the bilinear form
R
FS
x ¼h½x; ½FSi ¼
R
o
1
FS
dx ¼ 0
(cf. (5.40), o
1
FS is the domain in T
3
p
to which FS is the boundary), which implies
that the pull back F
: H
2
dR
ðT
3
p
Þ!H
2
dR
ðFSÞ is also trivial. Moreover, since Z
r
¼
F
ðp
1
ðFSÞÞ ¼ F
ðH
1
ðFS; ZÞÞ; there are r mutually non-homologous cycles cðFSÞ
(not combined into boundaries) on FS which remain non-homologous on T
3
p
: Again
exploiting the non-degeneracy of (5.40), there must be r linearly independent
cohomology classes ½r of closed 1-forms r on T
3
p
so that h½r; ½cðFSÞi 6¼ 0: Hence,
F
ðH
1
dR
ðT
3
p
; RÞÞ ¼ R
r
H
1
dR
ðFSÞ¼R
2g
: Now, in R
2g
a symplectic structure may
be introduced with the non-degenerate closed 2-form x ¼
P
g
i¼1
dq
i
^ dp
i
(cf. p. 113), where q
i
and p
i
may be, roughly speaking, local coordinates along the
cycles a
i
and b
i
of Fig. 5.8. Assume for some i that dq
i
and dp
i
are both pull-backs of
some closed 1-forms r
i
; s
i
on T
3
p
: Then, F
ð½r
i
^ s
i
Þ F
ðH
2
dR
ðT
3
p
ÞÞ ¼ 0 which
contradicts the non-degeneracy of x: Hence, at most one of each pair of 1-forms in
the symplectic form x can be a pull-back of a closed 1-form on T
3
p
; and consequently
2r 2g: (Accordingly, in Fig. 5.15 at least one of the cycles a
i
; b
i
for each pretzel
hole of the FS is contractible in the Brillouin zone T
3
p
:)
Note that in these considerations a central point was that the considered single
FS sheet is a boundary. The only alternative is a pair of corrugated planes ‘in
average’ parallel to each other which are not pathwise connected in T
3
p
but which
only together form a boundary. For that reason they must always appear in pairs,
since the total FS is necessarily a boundary as shown earlier. According to their
orientation, the two partners have homology classes opposite to each other. They
are heuristically seen to form two 2-tori ðg ¼ 2Þ with r ¼ 2 each, which also can
be proved formally.
On Fig. 5.16, the development of a real Fermi surface of YCo
5
under increasing
pressure is shown where sheets of all ranks except r ¼ 3 appear. In the third upper
panel there are small sheets with g ¼ r ¼ 0 centered at the top and bottom faces of
the Brillouin zone while in the lower panels the emergence under pressure of a
sheet with g ¼ r ¼ 0 around the center of the Brillouin zone is shown. In the
second upper panel there are small sheets (tori) with g ¼ 2; r ¼ 0 centered on the
edges of the hexagonal faces. The sheet of the left upper panel is a corrugated
cylinder with g ¼ r ¼ 1: The large sheet of the second panel has g ¼ 3; r ¼ 1: the
six holes around the vertical edges of the hexagonal Brillouin zone yield, after
closing the sides of the Brillouin zone as shown in Fig. 5.14 on p. 162, two holes
centered at the points AEC and DBF of Fig. 5.14 (each of the six holes belongs to
three zones). Cycles around these holes are, however, obviously contractible (into
the above mentioned points) in T
3
p
: Hence the only non-contractible class of
trajectories appears due to closing the top and bottom face of the Brillouin zone
168 5 Integration, Homology and Cohomology