Evolution of silicate coordination in architected amorphous and crystalline magnesium silicates during carbon mineralization.

Advancing durable solutions for carbon storage and removal at the gigaton scale to produce solid carbonates carbon mineralization requires harnessing earth abundant magnesium silicate resources. Calibrated insights linking the structural and morphological features of earth abundant amorphous and crystalline magnesium silicate phases to their reactivity are essential for scalable deployment but remain underdeveloped. To resolve the influence of silica coordination and mass transfer on carbon mineralization behavior, magnesium silicates bearing amorphous and crystalline phases (AC Mg-silicate) are synthesized. The structural and morphological transitions starting from colloidal precursors to their final synthesized form on heating are delineated using ultra small/small/wide angle X-ray scattering (USAXS/SAXS/WAXS) measurements. The evolution of the silicate phases on carbon mineralization of AC Mg-silicate is contrasted with that of highly crystalline Mg-silicate (HC Mg-silicate) when reacted at 200 °C and a CO partial pressure of 20 atm in water and 1 M NaHCO solution in stirred and unstirred environments. These experimental conditions are analogous to those of the water-gas-shift reaction for sustainable recovery of H with inherent carbon mineralization. Enhancement in the extent of carbon mineralization by 13.3-19.5% noted in the presence of NaHCO compared to water in AC and HC Mg-silicate with and without stirring, is attributed to the buffering effect which aids simultaneous silicate dissolution and carbon mineralization. Enhanced extents of carbon mineralization in the presence of NaHCO correspond to the formation of MgSiO and SiO phases from the starting MgSiO precursors in AC and HC Mg-silicate. Unlocking these silicate transformations during carbon mineralization by harnessing architected Mg-silicate precursors reveals the feasibility of integrating these chemical pathways with sustainable H conversion pathways with inherent carbon mineralization.