Structural controls on the solubility of CO2 in silicate melts Part I: bulk solubility data

CO2 solubility data are presented for a wide range of melt compositions in the following systems: SiO2-Na2O-Al2O3 + CO, (SNA) at 2.0 GPa and 1600 degr eesC; SNA + CaO (SNAC) and SNA + MgO + CaO (MSNAC) at 1.5 Cpa and 1275-1400 degreesC; and-for several "natural" magma compositions (Mg- and Ca-rich me lilitites, andesite and phonolite) at 1.2-2.7 GPa and 1300-1600 degreesC. A t a given pressure and temperature, the solubility is found to be a strong function of the "non-bridging oxygen" (NBO) content of the melt, expressed as the NBO/T ratio, where 'T represents tetrahedral network-forming cations . The NBO/T ratio, calculated from the melt composition, thus provides a us eful parameter for expressing and predicting the CO2 solubility. In highly polymerised melts, other dissolution mechanisms involving bridging oxygens become important and NBO/T is no longer the exclusive control on solubility . In Fe-bearing systems, the best correlation between CO2 solubility and NB O/T is found when both Fe3+ and Fe2+ are assumed to be tetrahedral (T), ind icating that these cations should be considered in a polymerising role in t he melt, with respect to CO2 dissolution. There is also evidence that some fraction of the Mg2+ in the melt should be assigned to a polymerising role. (C) 2001 Elsevier Science B.V. All rights reserved.