High-Temperature Mineral Formation after Firing Clay Materials Associated with Mined Coal in Teruel (Spain)
Autor: | Francisco Pardo, S. Meseguer, M.A. Montero, Manuel Miguel Jordán |
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Přispěvatelé: | The authors would like to express their gratitude to Emilio Galán for his help in the discussion and comments, and dedicate this manuscript to the memory of T. Sanfeliu, for his hard work in the study of Spanish ceramic clays., UCH. Departamento de Ciencias de la Educación, Producción Científica UCH 2020 |
Rok vydání: | 2020 |
Předmět: |
Materials science
Hercynite Arcillas - Análisis - España - Aragón - Teruel (Provincia) XRD Dolomite 020101 civil engineering Mullite 02 engineering and technology engineering.material lcsh:Technology Clay - Analysis - Spain - Aragon - Teruel (County) vitreous phase 0201 civil engineering lcsh:Chemistry Ceramic materials - Analysis - Spain - Aragon - Teruel (County) clay spoils Kaolinite General Materials Science lcsh:QH301-705.5 Instrumentation Fluid Flow and Transfer Processes Mineral lcsh:T Process Chemistry and Technology Metallurgy General Engineering Mineralogy - Analysis firing transformations Hematite 021001 nanoscience & nanotechnology Cristobalite lcsh:QC1-999 Computer Science Applications phase generation lcsh:Biology (General) lcsh:QD1-999 FTIR lcsh:TA1-2040 visual_art Illite Materiales cerámicos - Análisis - España - Aragón - Teruel (Provincia) Teruel engineering visual_art.visual_art_medium Mineralogía - Análisis lcsh:Engineering (General). Civil engineering (General) 0210 nano-technology lcsh:Physics |
Zdroj: | Applied Sciences Volume 10 Issue 9 Repositori Universitat Jaume I Universitat Jaume I Applied Sciences, Vol 10, Iss 3114, p 3114 (2020) CEU Repositorio Institucional Fundación Universitaria San Pablo CEU (FUSPCEU) |
ISSN: | 2076-3417 |
Popis: | The production of porcelain stoneware has experienced a considerable increase. Therefore, it was necessary to undertake an investigation that would allow knowing the mineralogical evolution that porcelain stoneware undergoes during the firing process, as well as establishing the influence of the formation of mullite and other mineral or vitreous phases and their quantification. The firing transformations of mine spoils associated with mined coal in the Utrillas-Escucha-Estercuel and Ariñ o-Andorra areas are studied in this paper. The mineralogical composition of the bulk mine spoils is kaolinite, illite, chlorite, and smectites (in traces), with quartz and feldspar, and minor hematite, calcite, and dolomite. The main objective is to understand the generation of high-temperature mineral phases after firing, and their quantification. The formation of mullite and other high-temperature phases are studied from samples that include variable proportions of illite. Samples with a high content of illite generate mullite at 995 ° C. Cristobalite was not detected as a high-temperature phase. Mullite is the most abundant mineral. The hercynite content is higher at low temperatures (995 ° C), and hematite content is higher at 1150 ° C. The vitreous phase represents about 50% of fired bodies. Despite observing a porous microstructure, the non-porous areas are well sintered. |
Databáze: | OpenAIRE |
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