The rate at which chloride ions diffuse from archaeological iron into a tre
atment solution depends on how the chloride ions are initially distributed
int he corrosion layer. This paper compares solutions of the diffusion equa
tion for two limiting cases; (1) where the chloride ions are initially spre
ad uniformly through the corrosion layer; and (2) where the chloride ions a
re initially concentrated at the interface between the iron and the corrosi
on layer. Although the first model has been used int he past to describe ch
loride ions diffusing from marine iron, the second is more appropriate in c
ases where corrosion has drawn chloride ions toward the iron surface. Becau
se diffusion processes in archaeological iron are complicated, the limitati
ons of both these models are discussed.