20 1 EPR (Electron Paramagnetic Resonance) Spectroscopy of Polycrystalline Oxide Systems
features in the spectrum from g and A strain to distorted and broadened line
shape. Various approaches can be adopted to unravel these complexities, and some
of them will be mentioned later. However, before presenting these methods for
interpreting the spectra of polycrystalline systems, it is fi rst necessary to briefl y
illustrate how the g values of a paramagnet can be extracted from a randomly ori-
ented solid. This analysis of the g tensor is generic, since the same angular depen-
dencies also exist for the A and D tensors.
The powder spectrum of a paramagnetic species dominated by g anisotropy is
given by the contributions of all molecules in their specifi c orientations with
respect to the external fi eld. The orientation of the external fi eld with respect to
the g principal axes was shown in Figure 1.7 . All orientations will have the same
probability in a polycrystalline environment, and this leads to the following equa-
tion for computing the line shape of a powder pattern:
I ω ω θθφ
ππ
()
⋅= ⋅⋅
0−∞
∞
∫∫∫
dddsin
2
0
(1.41)
According to this equation the total intensity of the EPR spectrum (I) is given
by the sum of the contributions of each single molecular orientation in a sphere
(dependent on θ and φ ). Powder patterns are therefore usually computed numeri-
cally using a simulation program by systematic variation of the angles θ and φ
between 0 and π and 0 and 2 π respectively and weighting the spectral contributions
with sin θ .
While the effective g value is expressed in terms of three principal values directed
along three axes or directions in a single crystal, only the principal values of g can
be extracted from the powder spectrum rather than the principal directions of the
tensor with respect to the molecular axes. (Therefore it is more correct to label
the observed g values as g
1
, g
2
, g
3
rather than g
xx
, g
yy
, g
zz
in a powder sample.) In
the simplest case, an isotropic g tensor can be observed, such that all three princi-
pal axes of the paramagnetic center are identical ( x = y = z and therefore g
1
= g
2
=
g
3
). In this case, only a single EPR line would be observed (in the absence of any
hyperfi ne interaction). With the exception of certain point defects in oxides and
the presence of signals from conduction electrons, such high symmetry cases are
rarely encountered in studies of oxides and surfaces.
More commonly the symmetry of the paramagnetic centers studied in metal
oxides will be lower than isotropic, such as axial ( g
xx
= g
yy
≠ g
zz
and A
xx
= A
yy
≠ A
zz
)
rhombic ( g
xx
≠ g
yy
≠ g
zz
and A
xx
≠ A
yy
≠ A
zz
), monoclinic or triclinic symmetry. For
example, consider a simple paramagnetic species ( S = 1/2) with uniaxial symmetry
and no hyperfi ne interaction. This system can be characterized by two principal
axis g values called g
⊥
and g
||
. As shown earlier in Equation 1.31 for the general
case where x = y = z , the variation in the g value will depend solely on the angle
θ between B and the x, y or z axis. For uniaxial symmetry where x = y ≠ z , then
Equation 1.31 simplifi es to:
B
h
gg
B
θ
ν
µ
θθ
()
=+
(
)
⊥
−
22 2
1
cos sin
2
(1.42)