Available
data on speciation of silica in aqueous solutions show
that the main forms of silica are the monomer Si(OH)4 and
the dimer Si2O(OH)6, with shares of higher polymers
growing with an increase of temperature and the total concentration
of silica in solution. Thermodynamic properties of the monomer and
dimer in the ideal gas state are determined from the quantum-chemical
calculations. The fugacity coefficients of these species in water
up to water densities of 1200 kg m–3 and temperatures
of up to 1350 K are estimated from an empirical correlation based
on the stoichiometry of hydroxide species. The fine-tuning of the
model is made by comparing calculations with the experimental solubility
and speciation data. It was found that to match the speciation results
reported as the share of the monomer, it is necessary to consider
polymerization of silica beyond the dimer, which can be achieved without
increasing the number of fitting parameters. The resulting model reproduces
well the experimental results on the solubility of quartz in water,
on the distribution of silica between the vapor and liquid phases
of water at subcritical temperatures, and on the speciation of silica
in water in equilibrium with quartz.