Fig. 6From: Silicate solution, cation properties, and mass transfer by aqueous fluid in the Earth’s interiorSilicate solubility in the SiO2–H2O, SiO2–NaOH–H2O, and SiO2–CaO–H2O systems as a function of fugacity of pure H2O (see text for details of calculations and source of fH2O calculation)Back to article page