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Technological Characterization and Industrial Application of Tunisian Clays from Makthar Area (Central Tunisia) in the Ceramic Industry

机译:突尼斯中部马克塔尔地区突尼斯粘土的技术表征和工业应用

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This study focused on the geochemical, mineralogical and technological characterization of clays in Makthar area (Central of Tunisia) of Cretaceous-Paleogene. Its aims are to identify and promote use in the field of ceramics industry. The result of the mineralogical analysis of clays showed a dominance of illite with a percentage higher than 65%, of kaolinite and smectite with percentages of 15%. Geochemical analysis of the major elements of clay showed a SiO2 content exceeding 29% and a percentage of Al2O3 higher than 7.5%. The Fe2O3 percentage was ranging from 3% to 8%. The percentage of CaO was between 22.5% and 28% while that of K2O is 4%. The percentages of SO4, MgO and NaO2 were in very small fractions. Granulometric and microgranulometric analysis showed that the clay fraction (2/g to 178 m2/g reflecting illite dominance. Drying behavior indicated that clay mixture had a drying shrinkage less than 7%, while the firing shrinkage didn’t exceed 2% giving the possibility of clay using in the ceramics field.
机译:这项研究的重点是白垩纪-古近纪马克塔尔地区(突尼斯中部)的粘土的地球化学,矿物学和技术特征。其目的是确定并促进在陶瓷工业领域的使用。粘土的矿物学分析结果显示,伊利石占65%以上,占主导地位的是高岭石和蒙脱石占15%的占主导地位。对粘土主要元素的地球化学分析显示,SiO2含量超过29%,Al2O3含量高于7.5%。 Fe 2 O 3的百分比为3%至8%。 CaO的百分比在22.5%至28%之间,而K2O的百分比为4%。 SO4,MgO和NaO2的百分比非常小。粒度分析和微观粒度分析表明,粘土分数(2 / g至178 m2 / g反映了伊利石优势。干燥行为表明粘土混合物的干燥收缩率小于7%,而烧成收缩率不超过2%,这有可能在陶瓷领域中使用的粘土。

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