Fig. 7
From: Silicate solution, cation properties, and mass transfer by aqueous fluid in the Earth’s interior

Silicate species abundance ratio, XQ1/XQ0 (X = mol fraction) as a function of SiO2 solubility (kg/mol)
From: Silicate solution, cation properties, and mass transfer by aqueous fluid in the Earth’s interior
Silicate species abundance ratio, XQ1/XQ0 (X = mol fraction) as a function of SiO2 solubility (kg/mol)