A general dissolution model valid for solid oxides has been developed.
This kinetic model consists of reactions for the cleavage and formati
on of element-oxygen bonds as the rate-limiting steps and protolysis r
eactions for the surface groups of the oxide and the monomer in equili
brium. The experimental data for silica show that the dissolution rate
in the strong acid region can be compared with that in an alkaline me
dium. Therefore all possible reactions must be taken into consideratio
n so that a realistic description in a wide pH range can be achieved i
n terms of kinetic and thermodynamic parameters of the dissolution beh
avior. The dissolution kinetics of a porefree, spherical silica depend
ent on pH at 0.1, 0.01 and 0.001 mol/L background electrolyte concentr
ation (NaCl) at 40 degrees C is looked into to confirm the model. The
protolysis reactions are described in three different ways: first with
out formation of a double layer, second with the formation of a diffus
e double layer, and third with the additional formation of a gel layer
. The results of the three approaches are then compared. The character
istic parameters such as the pristine point of zero charge, the protol
ysis constants of the surface groups, the saturation concentration, an
d the partial rate constants are found in acceptable orders of magnitu
de. A further result is a detailed expression for the pH dependence of
the overall rate constant of dissolution determined by three partial
rate constants and the pH-dependent charge state of the surface.