5 Diffusion in Oxides 217
Cation Self- and Impurity Diffusion in Spinels A
3−δ
O
4
The best-known oxide where the transition from a vacancy to an intersti-
tial regime was found experimentally is magnetite, Fe
3−δ
O
4
[10]. It crystal-
lizes in the spinel structure where the oxygen ions form a cubic close pack-
ing while the cations occupy well defined octahedral and tetrahedral sites.
The observed exponents of the iron diffusion coefficients are 2/3 at high
p
O
2
and −2/3 at low p
O
2
, as expected for dominating cation vacancies and
cation interstitials, respectively (see Sect. 5.2.1). This typical behaviour of
the cation diffusion coefficients remains the same if the spinel consists of
several cations, e.g. (Co,Fe,Mn)
3
O
4
[11, 12]. Another example is manganese-
zinc-ferrite, Mn
1−x
Zn
x
Fe
2
O
4
, where part of the Fe-ions in magnetite has
been replaced by Mn- and Zn-ions. Cation tracer diffusion coefficients have
been measured with radioactive isotopes in the thin-film geometry, using both
the sectioning method (described already in Sect. 1.4.1 in Chap. 1) and the
residual activity method [13]. In the sectioning method a thin layer of the
sample is ground off and its activity, A
sect
, is counted, while in the residual
activity method the residual activity, A
res
, of the sample after grinding off
a thin layer is counted. In the first case the activity profile is a Gaussian
curve, A
sect
∝ exp(−x
2
/4D
∗
t), while in the second case an error function is
obtained, A
res
∝ (1 −erf(x/
√
4D
∗
t)). Typical profiles from both methods are
shown in Fig. 5.5 for diffusion of the radioisotope
54
Mn in manganese-ferrite.
The diffusion coefficients obtained from both methods agree well. Figure 5.6
shows in a double-logarithmic plot results for the tracer diffusion coefficients
of Mn, Fe and Zn and the impurity diffusion coefficient of Co as a function of
the oxygen partial pressure [13]. All diffusion coefficients show a minimum as
a function of p
O
2
. The slopes +2/3 and −2/3 at high and low p
O
2
indicate that
diffusion proceeds via cation vacancies and cation interstitials, respectively.
While all diffusion coefficients are nearly the same in the vacancy regime,
the diffusion coefficient of zinc is higher in the interstitial regime, resulting in
a minimum of the Zn-diffusion coefficient which is shifted to higher oxygen
partial pressures compared to the other cations. A more detailed analysis,
considering that the cation sublattice in the spinel structure consists of two
sublattices with octahedral and tetrahedral sites and that iron, manganese
and cobalt cations exist in two charge states, +2 and +3, can be found in [13].
Cation Self- and Impurity Diffusion in Monoxides A
1−δ
O
In most transition metal monoxides, such as Co
1−δ
O, Ni
1−δ
OorMn
1−δ
O,
the oxide is reduced to the metal before the stoichiometric point, δ =0,is
reached. Thus, only a vacancy regime for cation diffusion is observed [14–16].
However, as mentioned before, the typical exponent in the p
O
2
-dependence
of the cation diffusion coefficient quite often differs from the value 1/6 that is
expected if cation vacancies V
A
would dominate. Subsequently, two examples
will be discussed, pure cobalt oxide and gallium-doped cobalt oxide.