composition of the oxide surface, if at all, and the pH of the solution but not with
the applied electrode potential, at least for stationary conditions. An overpotential η
2,3
for the potential drop E
2,3
is mainly expected for nonstationary conditions of the passive
layer that will directly influence the adsorption equilibrium of Cl
–
. The specific role of
chloride and other halides in breakdown of passivity is still not sufficiently understood
in light of this theory. Further refinements might improve this interesting view.
Surface analytical methods unfortunately do not always give a clear answer
about the penetration of aggressive anions. Some authors found chloride within the
film with XPS, Auger electron spectroscopy (AES) [15,16], and secondary ion mass
spectroscopy (SIMS) [17]; others could not find it within the film [18–22]. The
contradictory results may be explained in terms of sample preparation and the
sensitivity of the methods. Very careful XPS studies with Fe-Cr alloys show
incorporation within the outer hydroxide part of the duplex passivating film [23,24].
The inner oxide layer remains free of Cl
–
if prepared within chloride-free electrolytes
before exposure to the aggressive anions. Similarly, incorporation of Cl
–
within the
outer hydroxide layer was found for pure Ni [25]. It was found in the inner oxide part
only when the passive layer was formed in solutions already containing Cl
–
. If the
electrode potential was above the critical value for breakdown, Cl
–
penetrated
into the preexisting oxide with possible lateral fluctuations of its concentration,
leading finally to the formation of pits. According to these studies, the accumulation
within the hydroxide overlayer serves as an accumulation of a sufficiently large
amount to cause breakdown in the following step. Further discussions of the
surface analytical investigations of passive layers that have been exposed to
chloride-containing solutions may be found in the chapter on passivity in this book.
A detailed bilayer or even multilayer structure is observed for passive films on
many metals and alloys [26,27]. The outer part is usually a hydroxide, whereas the
main inner part is an oxide [23,25–27]. The hydroxide structure may well act as an
ion exchanger or at least absorb anions, as has been proved for some systems.
Although the access of aggressive anions leads to changes of the passive layer
detected by ellipsometry [28] and reflection spectroscopy [29], it is still unclear what
conclusion may be drawn from these observations. If the penetration of aggressive
anions leads to weak channels where intense dissolution may start, it is unclear why
the film does not re-form specifically at this site and why these defects do not
repassivate. The self-healing mechanism of the passive layer is essential for its
excellent protecting property. The specific role of the aggressive anions is missing
in this mechanism of breakdown. Any explanation should involve the characteristic
chemical properties of anions such as the halides.
Experiments with well-prepassivated specimens show that the formation of a
corrosion pit may be an extremely fast process, in the time range of <1 s or even
<1 ms [4,30]. Figure 3 depicts as an example the increase of the current density within
less than 1 ms as a consequence of growing pits for an Ni specimen prepassivated
for 1 s before a potential shift above the critical pitting potential. A simple
comparison of the small stationary passive current densities in the range of μA/cm
2
with these short times leads to contradictions with the penetration mechanism
[30,31]. If anions migrate inward as cations migrate outward during stationary
dissolution, these fast nucleation times cannot be understood. Furthermore, it seems
questionable that large anions such as SO
4
2–
and ClO
4
–
migrate sufficiently fast in the
250 Strehblow
Copyright © 2002 Marcel Dekker, Inc.