Abstract
Evidence from laboratory experiments and field observations on near-neutral pH SCC of pipeline steel is reviewed. Emphasis is placed on the effects of environmental parameters, such as potential, pH and concentration, on the SCC mechanism. The results are interpreted in terms of either a dissolution-based or hydrogen-based mechanism.
The weight of evidence supports a hydrogen-based mechanism for near-neutral pH SCC. Dissolution may play a role in SCC initiation. Enhanced rates of hydrogen evolution and permeation appear possible under near-neutral pH SCC conditions, whilst the observed dissolution rates and the absence of an efficient mass-transport mechanism to support rapid crack-tip dissolution seem to rule out dissolution as an important contributor to crack growth.