2025
The effect of wollastonite on sintering of anorthite ceramic body based on illite-smectite clay and kaolin
SOKOLAR, Radomir; Martin NGUYEN; Dalibor VŠIANSKÝ; Oldrich PAVELKA; Anton TRNIK et. al.Základní údaje
Originální název
The effect of wollastonite on sintering of anorthite ceramic body based on illite-smectite clay and kaolin
Autoři
SOKOLAR, Radomir; Martin NGUYEN; Dalibor VŠIANSKÝ (203 Česká republika, domácí); Oldrich PAVELKA a Anton TRNIK
Vydání
Applied Clay Science, Elsevier Ltd, 2025, 0169-1317
Další údaje
Jazyk
angličtina
Typ výsledku
Článek v odborném periodiku
Obor
20504 Ceramics
Stát vydavatele
Nizozemské království
Utajení
není předmětem státního či obchodního tajemství
Odkazy
Impakt faktor
Impact factor: 5.800 v roce 2024
Organizační jednotka
Přírodovědecká fakulta
UT WoS
001441880100001
EID Scopus
2-s2.0-85219217946
Klíčová slova anglicky
Wollastonite; Anorthite ceramics; Mineralogical composition; Firing; Sintering temperature
Štítky
Příznaky
Mezinárodní význam, Recenzováno
Změněno: 15. 4. 2025 10:37, Mgr. Marie Novosadová Šípková, DiS.
Anotace
V originále
The effect of different character of plastic raw materials based on different clay minerals (kaolin vs. I/S clay based on interstratified illite/smectite clay minerals) and different source of wollastonite (bludovite rock vs. natural wollastonite) on the sintering process of anorthite porcelain body is studied. The sintering temperature according to vacuum water absorption is defined for samples containing 40 % of wollastonite raw material in the range of firing temperatures from 850°C to 1200°C. The mineralogical composition of fired samples was observed from the firing temperature of 850 °C up to the sintering temperature. The sintering temperature of all studied samples is lower than 1200 °C. The lowest value is obtained by the combination of illite/smectite clay and natural wollastonite (1115 °C). The type of used plastic raw material also significantly affected the mechanism of anorthite formation during firing. The highest content of anorthite (over 90 %) in the crystalline phase of the sintered body is observed in kaolin-based samples. Primary mullite is identified in small amounts and transiently only in kaolin-based samples after a firing at 950°C and 1050°C, and then participates in the formation of anorthite. Diopside was detected in sintered samples based on bludovite rock as a rest from wollastonite raw material.