Organosilicon functionality modification mechanisms in geopolymers and the improvement of carbonation resistance
Abstract
This study explores a route for improving carbonation resistance of geopolymers by CO2–H2O–gel interface modification using organosilicon functionality. In this study, three organosilicon modifiers with distinct non-hydrolysable groups, including PMS, S823, and KH570, were added into geopolymers. The carbonation behavior of the geopolymers was comparatively evaluated under different drying conditions. Fresh-state properties, wettability, carbonation depth, and compressive strength were evaluated. To clarify the modification mechanism, gel structure evolution, carbonation products, and water-state changes were characterized by XRD, FTIR, TGA, LF 1H NMR, and MIP. The results showed that the carbonation resistance of the modified geopolymers was strongly dependent on organosilicon functionality. The water contact angle increased markedly from 36.52° for G0 to 117.87° for GS5. After 7 d of carbonation without pre-drying, the carbonation depth decreased from 30.25 mm for G0 to 15.31 mm for GS5, which was a 50% reduction. The residual compressive strengths of carbonated G0 and GS5 were 37.6 MPa and 36.7 MPa, respectively. Mechanistically, the long hydrophobic alkyl group of S823 promoted the formation of a low-surface-energy interfacial environment and disrupted the effective CO2–H2O–gel reaction interface, thereby most effectively suppressing carbonation. By contrast, KH570 mainly influenced local crystallization and carbonate phase evolution through its polar methacrylate functionality. PMS, containing only a small methyl group, showed limited improvement because it primarily participated in aluminosilicate network reorganization rather than establishing a strongly hydrophobic interfacial environment. This work provides a basis for the functionality-guided design of organosilicon-modified geopolymers with enhanced carbonation resistance, and contributes to their practical development for durable applications in CO2-rich environments.

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