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作 者:Njimbouombouo Mouliom Soualiou Etone Macka Alexandre Dodo Ondoua Abondo Ebengue Yannick Che Randy Nangah Njoya André Mouncherou Oumar Farouk Ndigui Billong Njimbouombouo Mouliom Soualiou;Etone Macka Alexandre Dodo;Ondoua Abondo Ebengue Yannick;Che Randy Nangah;Njoya André;Mouncherou Oumar Farouk;Ndigui Billong(University of Yaounde I, Yaounde, Cameroon)
机构地区:[1]University of Yaounde I, Yaounde, Cameroon
出 处:《Journal of Minerals and Materials Characterization and Engineering》2020年第5期353-363,共11页矿物质和材料特性和工程(英文)
摘 要:This study focuses on the mineralogical, geochemical and petrographic characterization of three granite rock samples (LTP, LTS and LTMB) from Foumban, West Region of Cameroon. Fusibility tests were carried out on the samples containing the highest amount of alkali to assess the potential of these materials as fluxing admixture for ceramics. The results show that the granite consists of alkaline feldspars, notably orthoclase and microcline of perthitic micro-texture, plagioclases (in particular albite) and also mafic minerals such as amphibole and pyroxene. The quantity of alkali in the samples is quite high (16.83% for LTS, 17.08% for LTMB and 18.87% for LTP) compared to standard data. Fusibility tests carried out on the samples having the highest alkali content (LTMB and LTP) showed that the vitreous phase appears between 1050°C and 1100°C in these samples when they were heated. The Fe<sub>2</sub>O<sub>3</sub> and TiO<sub>2</sub> content of LTMB (3.01% and 1.49% respectively) led to a brown colour of its fired product. Therefore, based on their composition, these materials can be used as feldspathic fluxes for the formulation of ceramic products.This study focuses on the mineralogical, geochemical and petrographic characterization of three granite rock samples (LTP, LTS and LTMB) from Foumban, West Region of Cameroon. Fusibility tests were carried out on the samples containing the highest amount of alkali to assess the potential of these materials as fluxing admixture for ceramics. The results show that the granite consists of alkaline feldspars, notably orthoclase and microcline of perthitic micro-texture, plagioclases (in particular albite) and also mafic minerals such as amphibole and pyroxene. The quantity of alkali in the samples is quite high (16.83% for LTS, 17.08% for LTMB and 18.87% for LTP) compared to standard data. Fusibility tests carried out on the samples having the highest alkali content (LTMB and LTP) showed that the vitreous phase appears between 1050°C and 1100°C in these samples when they were heated. The Fe<sub>2</sub>O<sub>3</sub> and TiO<sub>2</sub> content of LTMB (3.01% and 1.49% respectively) led to a brown colour of its fired product. Therefore, based on their composition, these materials can be used as feldspathic fluxes for the formulation of ceramic products.
关 键 词:FELDSPARS GRANITE Characterization Fusibility CERAMICS Foumban Cameroon
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