Plausible explanations for previously obtained kinetic data on the dissolut
ion of silicon dioxide aerogels in an aqueous 0.05 N NaOH solution in the t
emperature range 15-37 degrees C were considered. Because the coincidence o
f specific surface areas measured by the BET and small-angle X-ray scatteri
ng techniques suggests an absence of closed pores in the structure of inves
tigated aerogels, the heterogeneity of their surfaces was considered to be
the most probable reason for the variations in the shape of kinetic curves.
A model of dissolution was proposed. The model is based on the assumption
of two kinetically nonequivalent types of surface atoms (inactive and activ
e) and takes into account finite sizes of these atoms. The model is a modif
ication of the known Delmon model and uses a parameter E-s having a simple
physical meaning of the initial number of active sites of dissolution on a
primary aerogel particle. The activation energy of dissolution (80 +/- 6 kJ
/mol) and the interfacial energy (0.09 and 0.24 J/m(2) for coarsely and fin
ely dispersed samples, respectively) were obtained by approximating experim
ental data by calculated dissolution curves. It was shown that the number o
f active sites, E-s, increases linearly with the radius of primary particle
s.