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This work focuses on the isolated and combined influence of gypsum and KOH on the hydration of pure triclinic C 3 S. The addition of gypsum shows a prolonged induction period and increased maximum reaction rates during C 3 S hydration. These effects are further enhanced when KOH is added. Pore solution composition from ICP-OES measurements of suspension experiments show pore solutions dominated by an equilibrium with gypsum. Resulting changes in C-S-H interfacial precipitation rates are qualitatively correlated with either a prolonged or shortened induction period. A comparison of C 3 S reaction rates calculated based on C-S-H interfacial precipitation rate model and C 3 S reaction rates observed by XRD and TGA show an accurate quantitative description of the C 3 S hydration in the presence of gypsum and KOH. In the combined presence of KOH and gypsum, higher C-S-H surface areas quantitatively explain the increase in C 3 S reaction rates regarding the decreased interfacial precipitation rates. • Decreased C-S-H interfacial precipitation rate by gypsum addition prolongs C 3 S induction period. • Increased C-S-H surface area by gypsum addition leads to increased C 3 S maximum reaction rates. • Additional KOH enhances both effects in the presence of gypsum.
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Becker et al. (2025) studied this question.
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