International
Tables for Crystallography Volume C Mathematical, physical and chemical tables Edited by E. Prince © International Union of Crystallography 2006 |
International Tables for Crystallography (2006). Vol. C. ch. 4.3, pp. 404-411
Section 4.3.4.4. Excitation spectrum of core electrons
C. Colliexa
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As for any core-electron spectroscopy, EELS spectroscopy at higher energy losses mostly deals with the excitation of well defined atomic electrons. When considering solid specimens, both initial and final states in the transition are actually eigenstates in the solid state. However, the initial wavefunction can be considered as purely atomic for core excitations. As a first consequence, one can classify these transitions as a function of the parameters of atomic physics: Z is the atomic number of the element; n, l, and j = l + s are the quantum numbers describing the subshells from which the electron has been excited. The spectroscopy notation used is shown in Fig. 4.3.4.21
. The list of major transitions is displayed as a function of Z and
in Fig. 4.3.4.22
.
![]() | Definition of electron shells and transitions involved in core-loss spectroscopy [from Ahn & Krivanek (1982 |
![]() | Chart of edges encountered in the 50 eV up to 3 keV energy-loss range with symbols identifying the types of shapes [see Ahn & Krivanek (1982 |
Core excitations appear as edges superimposed, from the threshold energy upwards, above a regularly decreasing background. As explained below, the basic matrix element governing the probability of transition is similar for optical absorption spectroscopy and for small-angle-scattering EELS spectroscopy. Consequently, selection rules for dipole transitions define the dominant transitions to be observed, i.e.
This major rule has important consequences for the edge shapes to be observed: approximate behaviours are also shown in Fig. 4.3.4.22
. A very useful library of core edges can be found in the EELS atlas (Ahn & Krivanek, 1982
), from which we have selected the family of edges gathered in Fig. 4.3.4.23
. They display the following typical profiles:
4.3.4.4.2. Bethe theory for inelastic scattering by an isolated atom (Bethe, 1930
; Inokuti, 1971
; Inokuti, Itikawa & Turner, 1978
, 1979
)
As a consequence of the atomic nature of the excited wavefunction in core-loss spectroscopy, the first step involves deriving a useful theoretical expression for inelastic scattering by an isolated atom. The differential cross section for an electron of wavevector k to be scattered into a final plane wave of vector k′, while promoting one atomic electron from to
, is given in a one-electron excitation description by
see, for instance, Landau & Lifchitz (1966
) and Mott & Massey (1952
). The potential V(r) corresponds to the Coulomb interaction with all charges (both in the nucleus and in the electron cloud) of the atom. The momentum change in the scattering event is
. The final-state wavefunction is normalized per unit energy range. The orthogonality between initial- and final-state wavefunctions restricts the inelastic scattering to the only interactions with atomic electrons:
The first part of the above expression has the form of Rutherford scattering. γ is introduced to deal, to a first approximation, with relativistic effects. The ratio k′/k is generally assumed to be equal to unity. This kinematic scattering factor is modified by the second term, or matrix element, which describes the response of the atomic electrons: where the sum extends over all atomic electrons at positions
. The dimensionless quantity is known as the inelastic form factor.
For a more direct comparison with photoabsorption measurements, one introduces the generalized oscillator strength (GOS) as for transitions towards final states
in the continuum [ΔE is then the energy difference between the core level and the final state of kinetic energy
above the Fermi level, scaled in energy to the Rydberg energy (R)]. Also,
for transition towards bound states. In this case,
is the energy difference between the two states involved.
The generalized oscillator strength is a function of both the energy ΔE and the momentum transferred to the atom. It is displayed as a three-dimensional surface known as the Bethe surface (Fig. 4.3.4.24
), which embodies all information concerning the inelastic scattering of charged particles by atoms. The angular dependence of the cross section is proportional to
at a given energy loss ΔE.
In the small-angle limit , where
is the average radius of the initial orbital), the GOS reduces to the optical oscillator strength
and
where u is the unit vector in the q direction. When one is concerned with a given orbital excitation, the sum over
reduces to a single term r for this electron. With some elementary calculations, the resulting cross section is
The major angular dependence is contained, as in the low-loss domain, in the Lorentzian factor , with the characteristic inelastic angle
being again equal to
. Over this reduced scattering-angle domain, known as the dipole region, the GOS is approximately constant and the inner-shell EELS spectrum is directly proportional to the photoabsorption cross section
, whose data can be used to test the results of single-atom calculations. For larger scattering angles, Fig. 4.3.4.24
exhibits two distinct behaviours for energy losses just above the edge (df/dΔE drops regularly to zero), and for energy losses much greater than the core-edge threshold. In the latter case, the oscillator strength is mostly concentrated in the Bethe ridge, the maximum of which occurs for:
This contribution at large scattering angles is equivalent to direct knock-on collisions of free electrons, i.e. to the curve lying in the middle of the valence-electron–hole excitations continuum (see Fig. 4.3.4.13
). The non-zero width of the Bethe ridge can be used as an electron Compton profile to analyse the momentum distribution of the atomic electrons [see also §4.3.4.4.4(c)
].
The energy dependence of the cross section, responsible for the various edge shapes discussed in §4.3.4.4.1, is governed by
i.e. it corresponds to sections through the Bethe surface at constant q. Within the general theory described above, various models have been developed for practical calculations of energy differential cross sections.
The hydrogenic model due to Egerton (1979) is an extension of the quantum-mechanical calculations for a hydrogen atom to inner-shell electron excitations in an atom Z by introduction of some useful parametrization (effective nuclear charge, effective threshold energy). It is applied in practice for K and
shells.
In the Hartree–Slater (or Dirac–Slater) description, one calculates the final continuum-state wavefunction in a self-consistent central field atomic potential (Leapman, Rez & Mayers, 1980; Rez, 1989
). The radial dependence of these wavefunctions is given by the solution of a Schrödinger equation with an effective potential:
where
is the centrifugal potential, which is important for explaining the occurrence of delayed maxima in spectra involving final states of higher
. This approach is now useful for any major
edge, as illustrated by Ahn & Rez (1985
) and more specifically in rare-earth elements by Manoubi, Rez & Colliex (1989
).
These differential cross sections can be integrated over the relevant angular and energy domains to provide data comparable with experimental measurements. In practice, one records the energy spectral distribution of electrons scattered into all angles up to the acceptance value β of the collection aperture. The integration has therefore to be made from for the zero scattering-angle limit, up to
. Fig. 4.3.4.25
shows how such calculated profiles can be used for fitting experimental data.
Setting β = π [or equal to an effective upper limit corresponding to the criterion
, the integral cross section is the total cross section for the excitation of a given core level. These ionization cross sections are required for quantification in all analytical techniques using core-level excitations and de-excitations, such as EELS, Auger electron spectroscopy, and X-ray microanalysis (see Powell, 1976
, 1984
). A convenient way of comparing total cross sections is to rewrite the Bethe asymptotic cross section as
when the result is given in cm2,
is the total cross section per atom or molecule or ionization of the nl subshell with edge energy
,
is the number of electrons on the nl level, and
is the overvoltage defined as
.
and
are two parameters representing phenomenologically the average number of electrons involved in the excitation and their average energy loss (one finds for the major K and
edges
0.6–0.9 and
0.5–0.7). These values are in practice estimated from plots of curves
as a function of
, known as Fano plots. From least-squares fits to linear regions, one can evaluate the values of
(slope of the curves) and of
(coordinate at the origin) for various elements and shells. However, it has been shown more recently (Powell, 1989
) that the interpretation of Fano plots is not always simple, since they typically display two linear regions. It is only in the linear region for the higher incident energies that the plots show the asymptotic Bethe dependence with the slope directly related to the optical data. At lower incident energies, another linear region is found with a slope typically 10–20% greater. Despite great progress over the last two decades, more cross-section data, either theoretical or experimental, are still required to improve to the 1% level the accuracy in all techniques using these signals.
The characteristic core edges recorded from solid specimens display complex structures different from those described in atomic terms. Moreover, their detailed spectral distributions depend on the type of compound in which the element is present (Leapman, Grunes & Fejes, 1982; Grunes, Leapman, Wilker, Hoffmann & Kunz, 1982
; Colliex, Manoubi, Gasgnier & Brown, 1985
). Modifications induced by the local solid-state environment concern (see Fig. 4.3.4.26
) the following:
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