Crystallization and Quantification of Crystalline and Non-Crystalline Phases in Kaolin-Based Cordierites
The result's identifiers
Result code in IS VaVaI
<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F61989100%3A27360%2F19%3A10242534" target="_blank" >RIV/61989100:27360/19:10242534 - isvavai.cz</a>
Alternative codes found
RIV/61989100:27710/19:10242534
Result on the web
<a href="https://www.mdpi.com/1996-1944/12/19/3104" target="_blank" >https://www.mdpi.com/1996-1944/12/19/3104</a>
DOI - Digital Object Identifier
<a href="http://dx.doi.org/10.3390/ma12193104" target="_blank" >10.3390/ma12193104</a>
Alternative languages
Result language
angličtina
Original language name
Crystallization and Quantification of Crystalline and Non-Crystalline Phases in Kaolin-Based Cordierites
Original language description
Kaolin is most often used as traditional raw material in ceramic industry. The purpose of the study was to obtain understanding of the structural and chemical variability of cordierite ceramics influenced by chemical and mineralogical properties of six raw kaolins taken from dierent localities when they are applied in ceramics mixtures with vermiculite and sintered up to 1300 C. The X-ray diraction and simultaneous thermogravimetric and dierential thermal analysis were used to identify and characterize crystalline mineral phases and the course of reactions during the heating. The percentages of the crystalline and non-crystalline phases were newly determined by recalculation of the bulk chemical analyses of kaolins and cordierite ceramics using Chemical Quantitative Mineral Analysis (CQMA) method. Varying amounts of minerals in kaolins: kaolinite from 73.3 to 85.0, muscovite from 4.2 to 9.9, and quartz from 6.0 to 19.5 (mass %) aected amount of cordierite/indialite from 75.2 to 85.1, enstatite from 5.8 to 8.9 (when are calculated as their maximal possible percentages), and non-crystalline phases from 8.8 to 15.1 (mass %) in cordierite ceramics. Regression analysis predicted high relationship between quantity of: (a) kaolinite in kaolins and crystalline cordierite and (b) quartz in kaolins and non-crystalline phases in the ceramics. The migration of potassium from muscovite into the cordierite structure, melting point and crystallization of cordierite/indialite phases and pore size variability in relation to impurity of kaolins are documented and discussed.
Czech name
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Czech description
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Classification
Type
J<sub>imp</sub> - Article in a specialist periodical, which is included in the Web of Science database
CEP classification
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OECD FORD branch
10406 - Analytical chemistry
Result continuities
Project
Result was created during the realization of more than one project. More information in the Projects tab.
Continuities
P - Projekt vyzkumu a vyvoje financovany z verejnych zdroju (s odkazem do CEP)<br>S - Specificky vyzkum na vysokych skolach
Others
Publication year
2019
Confidentiality
S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů
Data specific for result type
Name of the periodical
Materials
ISSN
1996-1944
e-ISSN
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Volume of the periodical
12
Issue of the periodical within the volume
19
Country of publishing house
CH - SWITZERLAND
Number of pages
13
Pages from-to
1-13
UT code for WoS article
000493308500053
EID of the result in the Scopus database
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