Martin Boháč, Anežka Zezulová, Michaela Krejčí Kotlánová, Dana Kubátová, Theodor Staněk, Zdeněk Krejza, Dalibor Všianský, Radek Novotný, Jakub Palovčík, Karel Dvořák
{"title":"C4 AF 与硅灰的早期水化及其对卡托石成分的影响。","authors":"Martin Boháč, Anežka Zezulová, Michaela Krejčí Kotlánová, Dana Kubátová, Theodor Staněk, Zdeněk Krejza, Dalibor Všianský, Radek Novotný, Jakub Palovčík, Karel Dvořák","doi":"10.1111/jmi.13280","DOIUrl":null,"url":null,"abstract":"<p>C<sub>4</sub>AF is considered the least reactive main clinker phase, but its reactivity may be affected by adding supplementary cementitious materials (SCMs). Pure C<sub>4</sub>AF was synthesised in a laboratory furnace, and the role of silica fume without gypsum on its early hydration properties was monitored. Burning was carried out in four stages to achieve 99% purity of C<sub>4</sub>AF. Heat flow development was monitored by isothermal calorimetry over 7 days of hydration at 20°C and 40°C. The role of silica fume on hydrogarnet phase katoite (Ca<sub>3</sub>Al<sub>2</sub>(SiO<sub>4</sub>)<sub>3 –</sub> <i><sub>x</sub></i>(OH)<sub>4</sub><i><sub>x</sub> x</i> = 1.5–3) formation during early hydration was studied. Rapid dissolution of C<sub>4</sub>AF, formation of metastable C-(A,F)-H and its conversion to C<sub>3</sub>(A, F)H<sub>6</sub> was evidenced by isothermal calorimetry as a large exotherm. Changes in microstructure during early hydration were documented by SE micrographs, EDS point analyses, X-ray mapping and line scans by SEM-EDS. The phase composition was characterised by DTA-TGA and QXRD after 7 days of hydration. The katoite diffraction pattern is similar for the reference sample and sample with silica fume, but substitution in its structure can be revealed by X-ray microanalyses. The composition of katoite is variable due to the various extent of substitution of 4OH<sup>−</sup> by SiO<sub>4</sub><sup>4−</sup> due to silica fume.</p>","PeriodicalId":1,"journal":{"name":"Accounts of Chemical Research","volume":null,"pages":null},"PeriodicalIF":16.4000,"publicationDate":"2024-02-28","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":"{\"title\":\"Early hydration of C4AF with silica fume and its role on katoite composition\",\"authors\":\"Martin Boháč, Anežka Zezulová, Michaela Krejčí Kotlánová, Dana Kubátová, Theodor Staněk, Zdeněk Krejza, Dalibor Všianský, Radek Novotný, Jakub Palovčík, Karel Dvořák\",\"doi\":\"10.1111/jmi.13280\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"<p>C<sub>4</sub>AF is considered the least reactive main clinker phase, but its reactivity may be affected by adding supplementary cementitious materials (SCMs). Pure C<sub>4</sub>AF was synthesised in a laboratory furnace, and the role of silica fume without gypsum on its early hydration properties was monitored. Burning was carried out in four stages to achieve 99% purity of C<sub>4</sub>AF. Heat flow development was monitored by isothermal calorimetry over 7 days of hydration at 20°C and 40°C. The role of silica fume on hydrogarnet phase katoite (Ca<sub>3</sub>Al<sub>2</sub>(SiO<sub>4</sub>)<sub>3 –</sub> <i><sub>x</sub></i>(OH)<sub>4</sub><i><sub>x</sub> x</i> = 1.5–3) formation during early hydration was studied. Rapid dissolution of C<sub>4</sub>AF, formation of metastable C-(A,F)-H and its conversion to C<sub>3</sub>(A, F)H<sub>6</sub> was evidenced by isothermal calorimetry as a large exotherm. Changes in microstructure during early hydration were documented by SE micrographs, EDS point analyses, X-ray mapping and line scans by SEM-EDS. The phase composition was characterised by DTA-TGA and QXRD after 7 days of hydration. The katoite diffraction pattern is similar for the reference sample and sample with silica fume, but substitution in its structure can be revealed by X-ray microanalyses. The composition of katoite is variable due to the various extent of substitution of 4OH<sup>−</sup> by SiO<sub>4</sub><sup>4−</sup> due to silica fume.</p>\",\"PeriodicalId\":1,\"journal\":{\"name\":\"Accounts of Chemical Research\",\"volume\":null,\"pages\":null},\"PeriodicalIF\":16.4000,\"publicationDate\":\"2024-02-28\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"0\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Accounts of Chemical Research\",\"FirstCategoryId\":\"5\",\"ListUrlMain\":\"https://onlinelibrary.wiley.com/doi/10.1111/jmi.13280\",\"RegionNum\":1,\"RegionCategory\":\"化学\",\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"Q1\",\"JCRName\":\"CHEMISTRY, MULTIDISCIPLINARY\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Accounts of Chemical Research","FirstCategoryId":"5","ListUrlMain":"https://onlinelibrary.wiley.com/doi/10.1111/jmi.13280","RegionNum":1,"RegionCategory":"化学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q1","JCRName":"CHEMISTRY, MULTIDISCIPLINARY","Score":null,"Total":0}
引用次数: 0
摘要
C4 AF 被认为是反应性最低的熟料主相,但其反应性可能会受到添加胶凝辅料(SCM)的影响。在实验室熔炉中合成了纯 C4 AF,并监测了不含石膏的硅灰对其早期水化特性的影响。燃烧分四个阶段进行,使 C4 AF 的纯度达到 99%。在 20°C 和 40°C 水化的 7 天时间里,通过等温量热法对热流发展进行了监测。研究了早期水化过程中硅灰对水榴石相卡托石(Ca3 Al2 (SiO4 )3 - x (OH)4 x x x = 1.5-3)形成的作用。等温量热法显示,C4 AF 快速溶解,形成可转移的 C-(A,F)-H,并转化为 C3 (A,F)H6,产生大量放热。通过 SE 显微照片、EDS 点分析、X 射线制图和 SEM-EDS 线扫描,记录了早期水化过程中微观结构的变化。水化 7 天后,通过 DTA-TGA 和 QXRD 对相组成进行了表征。参考样品和含有硅灰的样品的卡托石衍射图样相似,但通过 X 射线显微分析可以发现其结构中的替代物。由于硅灰对 4OH- 的取代程度不同,卡托石的成分也不同。
Early hydration of C4AF with silica fume and its role on katoite composition
C4AF is considered the least reactive main clinker phase, but its reactivity may be affected by adding supplementary cementitious materials (SCMs). Pure C4AF was synthesised in a laboratory furnace, and the role of silica fume without gypsum on its early hydration properties was monitored. Burning was carried out in four stages to achieve 99% purity of C4AF. Heat flow development was monitored by isothermal calorimetry over 7 days of hydration at 20°C and 40°C. The role of silica fume on hydrogarnet phase katoite (Ca3Al2(SiO4)3 –x(OH)4x x = 1.5–3) formation during early hydration was studied. Rapid dissolution of C4AF, formation of metastable C-(A,F)-H and its conversion to C3(A, F)H6 was evidenced by isothermal calorimetry as a large exotherm. Changes in microstructure during early hydration were documented by SE micrographs, EDS point analyses, X-ray mapping and line scans by SEM-EDS. The phase composition was characterised by DTA-TGA and QXRD after 7 days of hydration. The katoite diffraction pattern is similar for the reference sample and sample with silica fume, but substitution in its structure can be revealed by X-ray microanalyses. The composition of katoite is variable due to the various extent of substitution of 4OH− by SiO44− due to silica fume.
期刊介绍:
Accounts of Chemical Research presents short, concise and critical articles offering easy-to-read overviews of basic research and applications in all areas of chemistry and biochemistry. These short reviews focus on research from the author’s own laboratory and are designed to teach the reader about a research project. In addition, Accounts of Chemical Research publishes commentaries that give an informed opinion on a current research problem. Special Issues online are devoted to a single topic of unusual activity and significance.
Accounts of Chemical Research replaces the traditional article abstract with an article "Conspectus." These entries synopsize the research affording the reader a closer look at the content and significance of an article. Through this provision of a more detailed description of the article contents, the Conspectus enhances the article's discoverability by search engines and the exposure for the research.