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Influence of w/s ratio on alite dissolution and C-S-H precipitation rates during hydration
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 an...
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Published in: | Cement and concrete research 2020-08, Vol.134, p.106087, Article 106087 |
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description | 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. |
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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. 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The Ca concentration evolution indicates a delay of the first portlandite precipitation with increasing w/s ratio.</description><subject>Ca3SiO5 (D)</subject><subject>Calcium-silicate-hydrate (C-S-H) (B)</subject><subject>Chemical precipitation</subject><subject>Dissolution</subject><subject>Evolution</subject><subject>Hydration</subject><subject>Hydration (A)</subject><subject>Kinetics (A)</subject><subject>Mass ratios</subject><subject>Mathematical analysis</subject><subject>Pore solution (B)</subject><subject>Tricalcium silicate</subject><issn>0008-8846</issn><issn>1873-3948</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2020</creationdate><recordtype>article</recordtype><recordid>eNqFkEtPwzAQhC0EEqXwG7DEOa0fqeMcqwpopUocgAsXy_EDHKVxsBNQ_z1Og7hyWu1oZlb7AXCL0QIjzJb1QpmD8m0wcUEQGVWGeHEGZpgXNKNlzs_BDCHEM85zdgmuYqzTygjlM_C2a20zmFYZ6C38XkYYZO889C2UjesN1C5G3wxJS0qr4SZ7zrawC0a5zvXypKeIiVAPwbXv8OOoTxXtNbiwsonm5nfOwevD_ctmm-2fHneb9T5TNKd9xlaUVJwZXaEK89LagpaMM1tWVZVborWUBaoIoqUqmZWMsAITrBGxiLFVoegc3E29XfCfg4m9qP0Q2nRSkDynJSpKzpKrmFwq-BiDsaIL7iDDUWAkRpCiFn8gxQhSTCBTcj0lTXriy5kgonIjMe0ShV5o7_7t-AE2H4BQ</recordid><startdate>202008</startdate><enddate>202008</enddate><creator>Naber, C.</creator><creator>Bellmann, F.</creator><creator>Neubauer, J.</creator><general>Elsevier Ltd</general><general>Elsevier BV</general><scope>AAYXX</scope><scope>CITATION</scope><scope>7QQ</scope><scope>7SR</scope><scope>8BQ</scope><scope>8FD</scope><scope>FR3</scope><scope>JG9</scope><scope>KR7</scope></search><sort><creationdate>202008</creationdate><title>Influence of w/s ratio on alite dissolution and C-S-H precipitation rates during hydration</title><author>Naber, C. ; Bellmann, F. ; Neubauer, J.</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c343t-6532b86edb0b189ff739686f9bbb4f2ddaa70b2039c96fa6267121d02f06657c3</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2020</creationdate><topic>Ca3SiO5 (D)</topic><topic>Calcium-silicate-hydrate (C-S-H) (B)</topic><topic>Chemical precipitation</topic><topic>Dissolution</topic><topic>Evolution</topic><topic>Hydration</topic><topic>Hydration (A)</topic><topic>Kinetics (A)</topic><topic>Mass ratios</topic><topic>Mathematical analysis</topic><topic>Pore solution (B)</topic><topic>Tricalcium silicate</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Naber, C.</creatorcontrib><creatorcontrib>Bellmann, F.</creatorcontrib><creatorcontrib>Neubauer, J.</creatorcontrib><collection>CrossRef</collection><collection>Ceramic Abstracts</collection><collection>Engineered Materials Abstracts</collection><collection>METADEX</collection><collection>Technology Research Database</collection><collection>Engineering Research Database</collection><collection>Materials Research Database</collection><collection>Civil Engineering Abstracts</collection><jtitle>Cement and concrete research</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Naber, C.</au><au>Bellmann, F.</au><au>Neubauer, J.</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Influence of w/s ratio on alite dissolution and C-S-H precipitation rates during hydration</atitle><jtitle>Cement and concrete research</jtitle><date>2020-08</date><risdate>2020</risdate><volume>134</volume><spage>106087</spage><pages>106087-</pages><artnum>106087</artnum><issn>0008-8846</issn><eissn>1873-3948</eissn><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. 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subjects | Ca3SiO5 (D) Calcium-silicate-hydrate (C-S-H) (B) Chemical precipitation Dissolution Evolution Hydration Hydration (A) Kinetics (A) Mass ratios Mathematical analysis Pore solution (B) Tricalcium silicate |
title | Influence of w/s ratio on alite dissolution and C-S-H precipitation rates during hydration |
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