ABSTRACT

ABSTRACT The penetration of chloride ions into concrete is recognized to not be a homogeneous process. The aim of this study is to reveal the factors underlying the spatial variability of chloride ion penetration into concrete via the superstructure of an open-type wharf. The chloride ion contents of two slabs (Slab-L and Slab-S) obtained from an open-type wharf that was about 30 years old were measured. The surface chloride ion content (C0) in Slab-S varied widely and the average value of C0 in both slabs significantly differed. From the distribution of C0, it was found that C0 at the back side of each slab was relatively higher than that at the middle and front side of the slabs. In conclusion, it was found that the distribution of C0 was affected by factors including the location of the slab, the environmental conditions such as the sea level, and the other structural members surrounding the slab.