Molecular dynamics simulations uncover cation-specific dissolution pathways in metakaolin using mixed alkalis, indicating enhanced reactivity.
The initial dissolution of metakaolin (MK) governs the supply and stoichiometry of dissolved aluminosilicate species for subsequent geopolymerization, yet the ion-specific roles of mixed alkalis at chemically heterogeneous MK basal surfaces remain poorly understood. In this work, ReaxFF reactive molecular dynamics simulations were performed at 350 K for 2.0 ns to investigate the dissolution of Al-rich and Si-rich MK (001) basal surfaces in 5 M NaOH, 5 M KOH, and a 5 M 1:1 NaOH/KOH mixed solution, using the ReaxFF parameter sets of Aryanpour et al. and Fedkin et al. The results reveal distinct cation-specific pathways: K + more effectively facilitates Al–O bond cleavage and promotes the formation of Al-bearing oligomers, whereas Na + more strongly perturbs the silicate network and sustains Si release. Most importantly, the 5 M 1:1 NaOH/KOH mixed solution exhibits a synergistic effect arising from the spatiotemporal complementarity of Na + and K + adsorption, which suppresses premature local passivation and yields a balanced dissolved Si/Al ratio of approximately 0.9. This mixed solution also gives the lowest residual fraction of CN = 4 Al species (14.6%), indicating enhanced framework destabilization and sustained early-stage bond-breaking reactivity; the associated framework response should be understood as structural relaxation rather than true diffusion of the solid phase. These findings provide atomistic insight into cation-regulated MK dissolution and offer a mechanistic basis for designing mixed-alkali activators for alkali-activated aluminosilicate materials.
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Zhang et al. (2026) studied this question.
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