Molecular statics calculations on gas-phase and solvated clusters and
on gas-phase and solvated slabs representing aqueous species and surfa
ces were applied to investigate acid/base reactions on silica surfaces
. Our gas-phase approach, which was previously applied to goethite, pr
edicts a surface pK(a) of 8.5 for the reaction >SiOH-->>SiO- + H+ whic
h is in good agreement with estimates based on potentiometric titratio
n. However, the model gives an unrealistically large pK(a) for the rea
ction >SiOH2+ --> >SiOH + H+. The model dependence of this result was
checked by using two different types of interaction potentials, one ba
sed on quantum mechanical calculations on H4SiO4 clusters, and another
empirical model fitted to the structure and elastic properties of Lu-
quartz. Because these models gave similar results, we hypothesize that
the failure of the gas-phase models is due to intrinsic solvation eff
ects not accounted for by our previously developed correlations. We te
sted this idea by carrying out energy minimization calculations on gas
-phase clusters with one hydration shell as well as molecular dynamics
simulations on fully-solvated H5SiO4+ and a fully solvated (0001) sur
face of beta-quartz. Though we are unable to establish a quantitative
measure of the pK(a) of SiOH2 groups, the solvated systems do indicate
that SiOH groups do not protonate in any of our solvated models. (C)
1998 Academic Press.