The dissolution kinetics of silicate glasses in aqueous environments i
n systems which included a variety of natural crystalline solids in ad
dition to the glass itself and the aqueous phase are reported. The res
ults demonstrate the possibility of a dramatic decrease in the rate of
dissolution of silicate glass in the presence of certain varieties of
olivine-based materials. This decrease in dissolution rate was shown
to be due to the fact that these additives consist mostly of Mg-based
material but also contain minor amounts of Al and Ca. The combined pre
sence of Mg with these minor species affected the corrosion rate of th
e glass as a whole, including its most soluble components such as boro
n. This study has potentially important implications to the durability
of glasses exposed to natural environments. The results may be releva
nt to the use of active backfill materials in burial sites for nuclear
waste glasses, as well as to better understanding of the environmenta
l degradation of natural and ancient glasses.