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Early hydration of C4AF with silica fume and its role on katoite composition.
Bohác, Martin; Zezulová, Anezka; Krejcí Kotlánová, Michaela; Kubátová, Dana; Stanek, Theodor; Krejza, Zdenek; Vsianský, Dalibor; Novotný, Radek; Palovcík, Jakub; Dvorák, Karel.
Afiliação
  • Bohác M; Research Institute for Building Materials, Brno, Czech Republic.
  • Zezulová A; Research Institute for Building Materials, Brno, Czech Republic.
  • Krejcí Kotlánová M; Research Institute for Building Materials, Brno, Czech Republic.
  • Kubátová D; Research Institute for Building Materials, Brno, Czech Republic.
  • Stanek T; Research Institute for Building Materials, Brno, Czech Republic.
  • Krejza Z; Research Institute for Building Materials, Brno, Czech Republic.
  • Vsianský D; Faculty of Science, Department of Geological Sciences, Masaryk University, Brno, Czech Republic.
  • Novotný R; Faculty of Chemistry, Brno University of Technology, Brno, Czech Republic.
  • Palovcík J; Faculty of Chemistry, Brno University of Technology, Brno, Czech Republic.
  • Dvorák K; Faculty of Civil Engineering, Institute of Technology of Building Materials and Components, Brno University of Technology, Brno, Czech Republic.
J Microsc ; 294(2): 168-176, 2024 May.
Article em En | MEDLINE | ID: mdl-38418930
ABSTRACT
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)4 x 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 SiO4 4- due to silica fume.
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Texto completo: 1 Base de dados: MEDLINE Idioma: En Ano de publicação: 2024 Tipo de documento: Article

Texto completo: 1 Base de dados: MEDLINE Idioma: En Ano de publicação: 2024 Tipo de documento: Article