J 2024

Early hydration of C4AF with silica fume and its role on katoite composition

BOHÁČ, Martin; Anežka ZEZULOVÁ; Michaela KREJČÍ KOTLÁNOVÁ; Dana KUBÁTOVÁ; Theodor STANĚK et. al.

Základní údaje

Originální název

Early hydration of C4AF with silica fume and its role on katoite composition

Autoři

BOHÁČ, Martin; Anežka ZEZULOVÁ; Michaela KREJČÍ KOTLÁNOVÁ; Dana KUBÁTOVÁ; Theodor STANĚK; Zdeněk KREJZA; Dalibor VŠIANSKÝ; Radek NOVOTNÝ; Jakub PALOVČÍK a Karel DVOŘÁK

Vydání

Journal of Microscopy, Wiley, 2024, 0022-2720

Další údaje

Jazyk

angličtina

Typ výsledku

Článek v odborném periodiku

Obor

20101 Civil engineering

Stát vydavatele

Spojené státy

Utajení

není předmětem státního či obchodního tajemství

Odkazy

Impakt faktor

Impact factor: 1.900

Kód RIV

RIV/00216224:14310/24:00138666

Organizační jednotka

Přírodovědecká fakulta

UT WoS

001177648400001

EID Scopus

2-s2.0-85186620066

Klíčová slova anglicky

C(4)AF; hydration; katoite; microstructure; silica fume

Štítky

Příznaky

Mezinárodní význam, Recenzováno
Změněno: 28. 1. 2025 09:59, Mgr. Marie Novosadová Šípková, DiS.

Anotace

V originále

4AF 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.