https://doi.org/10.1088/1468-6996/9/1/013007
“In the case of several cationic zeolites, the chemical adsorption of CO2 is accompanied by the formation of carbonates including very stable monodentate or unidentate carbonates and bidentate carbonates, at their surface, due to the interaction of CO2 with the oxygen bridging aluminum and silicon atoms [24, 35, 58–62]. Gallei and Stumpf [58] have described the formation of monodentate carbonate at the surface of zeolite CaY by a reaction involving three steps. In the first step, the CO2 is polarized following its interaction with the neighboring Ca2 + ions. After this, the atom of carbon of CO2 attacks the oxygen bridging aluminum and silicon atoms, and this results in the rupture of aluminum oxygen bond, and the formation a stable monodentate carbonate species at the surface of zeolite (figure 4) [58, 59]. The presence of these carbonates might decrease the accessibility of CO2 at a great part of the surface of zeolites and thereby contribute to limit its adsorption. This is notably the case of the unidentate surface carbonate species formed during the CO2 adsorption on zeolite CaY that makes inaccessible approximately 20% of the surface cations [59].”