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• W3020678275 endingPage "106087" @default.
• W3020678275 startingPage "106087" @default.
• W3020678275 abstract "The first 24 h of hydration of tricalcium silicate (C3S) have been studied at varying water/solid (w/s) mass ratios ranging from 0.5 to 10. Gathered data comprise the reaction degree, pore solution concentrations and specific surface area evolution. Combined with interfacial C3S dissolution rates and C-S-H precipitation rates found in the literature, these data are used to calculate theoretical reaction rates from C-S-H precipitation and C3S dissolution. Compared with the measured reaction rates, theoretical rates calculated from C-S-H precipitation show a good match, indicating a correct kinetic description of C-S-H precipitation. Theoretical rates calculated from C3S dissolution are higher than expected during the first hours of hydration which could be explained by the buildup of a metastable hydrate phase barrier. Furthermore, a comparison of the reaction rates shows no effect of the w/s ratio. The Ca concentration evolution indicates a delay of the first portlandite precipitation with increasing w/s ratio." @default.
• W3020678275 created "2020-05-01" @default.
• W3020678275 creator A5041343652 @default.
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• W3020678275 creator A5077989766 @default.
• W3020678275 date "2020-08-01" @default.
• W3020678275 modified "2023-10-16" @default.
• W3020678275 title "Influence of w/s ratio on alite dissolution and C-S-H precipitation rates during hydration" @default.
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• W3020678275 doi "https://doi.org/10.1016/j.cemconres.2020.106087" @default.
• W3020678275 hasPublicationYear "2020" @default.
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