Other Environmental Evolutions in the Crevice Gap
In the case of stainless steels, Lott and Alkire [47] consider that the dissolution of
sulfide inclusions (MnS) inside a crevice is the main environment change before
passivity breakdown. They showed by direct analysis of the local environment in an
artificial crevice that manganese sulfides were oxidized to thiosulfates, which are
known to promote pitting in aerated chloride environments [48–50] and, more
generally, to inhibit film repair on stainless alloys. More recent work of Brossia and
Kelly [51,52] showed that the dissolution of manganese sulfides actually produced
sulfide rather than thiosulfate ions. Whatever the nature of the reactive sulfur species
produced by the degradation of MnS inclusions, they can be deleterious for the
passive layer, particularly because they may form on the bare metal surfaces an
adsorbed layer of sulfur that enhances the anodic dissolution and inhibits (or retards)
the formation of the passive film [53]. Indeed Crolet et al. [54] showed that in acidic
environments representing crevice solutions an increase in the sulfur content of the
stainless steels favored the onset of active dissolution.
In the case of dissimilar crevices where one of the crevice walls is made of
a nonmetallic material, such as a gasket, the possibility of dissolution of foreign
elements must also be considered.
Breakdown of Passivity inside the Crevice
The detailed mechanism of passivity breakdown inside a crevice is not clearly
established and different possibilities are still discussed. Indeed, it is quite possible
that different mechanisms may be involved depending on the material, bulk
environment, crevice geometry, and, possibly, surface condition of the metal.
“Classical” Mechanism”: General Breakdown of Passivity in Low
pH, High Chloride Solutions
The more “classical” mechanism involves general film breakdown in a critical
environment characterized by a low pH and a high chloride content. Low pH and high
chloride concentrations are known to be deleterious for the passivity of most alloys.
Thus, the progressive evolution of the crevice environment causes a degradation of
the passive film that may result in the following successive situations (Fig. 21a):
1. An increase of the passive current
2. The onset of an active dissolution domain with a peak current that increases with
decreasing pH and increasing chloride content (and, thus, increasing with time)
3. A complete inhibition of passivity
Passivity breakdown is thought to occur either when the corrosion potential of the
crevice surfaces is located in the active peak due to ohmic drop (Fig. 21b) or when
there is no more active-passive transition on the anodic curve.
This mechanism of initiation gave rise to the notion of critical pH for film
breakdow [55], which was extensively used as a criterion to rank the resistance of
stainless alloys to crevice corrosion. For Crolet et al. [55] the critical pH is the pH
corresponding to the onset of an active peak in the polarization curves, while Ogawa
[42] considered the pH of spontaneous film breakdown under free corrosion
conditions. These differences changed somewhat the critical pH values but usually not
Crevice Corrosion of Metallic Materials 367
Copyright © 2002 Marcel Dekker, Inc.