210 3 Physics of Electron Scattering
enables the integral in Eq. (3.164) to be split into components. The first of these,
arising from the unity term in Eq. (3.164a), is zero because ψ
i
and ψ
f
are orthogo-
nal wavefunctions. The second integral containing (q·r)iszeroif ψ
i
and ψ
f
have the
same symmetry about the center of the excited atom (r = 0) such that their product
is even; q · r itselfisanodd function and the two halves of the integral then can-
cel. But if ψ
i
is an s-state (even symmetry) and ψ
f
is a p-state (odd symmetry), the
integral is nonzero and transitions are observed. This is the basis of the dipole selec-
tion rule, according to which the observed N(E) is a symmetry-projected density of
states.
For the dipole rule to hold, the higher order terms in Eq. (3.163)mustbe
negligible; if not, a third integral (representing dipole-forbidden transitions) will
modify the energy dependence of the fine structure. From the above argument, the
dipole condition is defined by the requirement q · r 1 for all r, equivalent to
q q
d
= 1/r
c
, where r
c
is the radius of the core state (defining the spatial region
in which most of the transitions occur). The hydrogenic model gives r
d
≈ a
0
/Z
∗
,
where Z
∗
is the effective nuclear charge.
For K-shells, Z
∗
≈ Z − 0.3 (see Section 3.6.1); for carbon K-shell excitation
by 100-keV electrons, dipole conditions should therefore prevail for θ θ
d
=
Z
∗
a
0
k
0
= 67 mrad, a condition fulfilled for most of the transitions since the median
angle of scattering is around 10 mrad (Fig. 3.41). In agreement with this esti-
mate, atomic calculations indicate that nondipole contributions are less than 10%
of the total for q < 45 nm
−1
, equivalent to θ < 23 mrad for 100-keV electrons
(Fig. 3.52a,b). A small spectrometer collection aperture (centered about the optic
axis) can therefore ensure that nondipole effects are minimized. Saldin and Yao
(1990) argue that dipole conditions hold only over an energy range ε
max
above the
excitation threshold, with ε
max
≈ 33 eV for Z = 3, increasing to 270 eV for Z =
8. Dipole conditions should therefore apply to the ELNES of elements heavier than
Li and to the EXELFS region for oxygen and heavier elements, for the incident
energies used in transmission spectroscopy.
For L
23
edges, atomic calculations (Saldin and Ueda, 1992)giveq
d
a
0
≈ Z
∗
/9
with Z
∗
= Z − 4.5, so for silicon and 100-keV incident electrons θ
d
≈ 11 mrad.
Solid-state calculations for Si (Ma et al., 1990) have suggested that nondipole effects
are indeed small (within 5 eV of the threshold) for 12.5-mrad collection semi-angle
(Fig. 3.52c) but are substantial for a large collection aperture, where monopole
2p → 3p transitions make a substantial contribution (Fig. 3.53d). Monopole tran-
sitions have been observed at the Si–L
23
edge of certain minerals and have been
attributed to the low crystal symmetry that induces mixing of p- and d-orbitals
(Brydson et al., 1992a).
A high density of dipole-forbidden states just above the Fermi level may lead
to observable monopole peaks, but mainly in spectra recorded with a displaced
collection aperture where the momentum transfer is large (Auerhammer and Rez,
1989). The dipole approximation appears justified for all M-edges, at incident ener-
gies above 10 keV and with an axial collection aperture (Ueda and Saldin, 1992).
A further discussion of nondipole effects is given by Hébert (2007) and (for the
low-loss region) by Gloter et al. (2009).