The present overview on salt induced deterioration of inorganic porous mate
rials focuses on those topics considered the most relevant for understandin
g this phenomenon. these are movement of both water/moisture and salts with
in the pore system; influence of the presence of salts in moisture absorpti
on; effect of the simultaneous presence of more than one salt; salt distrib
ution in masonry; deterioration mechanisms; and weathering patterns. Of the
latter, the most ubiquitous are powdering and scaling, and they have been
found to occur on most stone types. However, the mechanism that induces the
same outward appearance on different stones can vary significantly dependi
ng on the synergism that develops among porous material, salt, and moisture
.