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Characterization, thermal behaviour and firing properties of clay materials from Cap Bon Basin, north-east Tunisia, for ceramic applications

机译:来自东北突尼斯帽盆地,东南突尼斯岩石盆地,陶瓷应用的特征,热行为和烧制性能

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摘要

This study focuses on the characterization, thermal behaviour and firing properties of clays from Cap Bon Basin, Tunisia. Chemical (inductively coupled plasma atomic emission spectroscopy) and mineralogical (X-ray diffraction (XRD), Fourier-transform infrared (FTIR) spectroscopy) characterization of the clays was carried out. Physical properties were identified using particle-size distribution and Atterberg limits tests. Differential thermal analysis/thermogravimetry, dilatometry, XRD and FTIR analyses were conducted to assess the thermal behaviour, transformations and crystalline phase development during firing. The clays studied show large proportions of silt and clay fractions. They are rich in SiO2, Al2O3 and Fe2O3 and mostly consist of illite, kaolinite, smectite and minor mixed-layer illite-smectite. Associated minerals are mainly quartz, calcite and feldspar. To monitor the firing properties, three clay mixtures referred to as M1, M2 and M3 were prepared according to the physicochemical and mineralogical characteristics of the raw clays. These were sintered at 900 degrees C, 1000 degrees C and 1100 degrees C and tested for firing shrinkage, flexural strength and water absorption. As a result, various mineralogical transformations occurred at 900-1100 degrees C associated with the crystallization of new phases. The main transformations identified at 1000 degrees C resulted in the formation of anorthite and mullite, causing significant densification of the fired ceramic materials. Sintering at 1100 degrees C increased the densification and thus improved the flexural strength. At this temperature, the sintered ceramic tiles exhibited excellent properties, namely water absorption of 2-3% and flexural strength of 30-41 MPa, indicating that these studied clays might be used as raw materials for the production of stoneware tile ceramics.
机译:本研究侧重于突尼斯帽池盆地粘土的表征,热行为和烧制特性。进行化学(电感耦合等离子体原子发射光谱)和矿物学(X射线衍射(XRD),傅里叶变换红外(FTIR)光谱)进行粘土表征。使用粒度分布和Atterberg限制测试来识别物理性质。进行差分热分析/热重量,膨胀测定,XRD和FTIR分析,以评估烧制期间的热行为,转化和结晶相发显性。研究的粘土显示出大量的淤泥和粘土馏分。它们含有富含SiO2,Al2O3和Fe2O3,主要包括伊利石,高岭石,蒙脱石和次次混合层硅灰石 - 蒙脱石。相关矿物主要是石英,方解石和长石。为了监测烧制性质,根据原始粘土的物理化学和矿物学特征制备三种称为M1,M2和M3的粘土混合物。这些烧结在900℃,1000摄氏度和1100摄氏度,并测试用于烧制收缩,弯曲强度和吸水。结果,与新相结晶相关的900-1100摄氏度发生了各种矿物学转化。 &gt的主要变换; 1000℃导致形成卤素和莫来石,导致燃烧陶瓷材料的显着致密化。在1100℃下烧结增加了致密化,从而提高了弯曲强度。在该温度下,烧结陶瓷砖表现出优异的性能,即吸水率为2-3%,弯曲强度为30-41MPa,表明这些研究的粘土可用作制造石器瓷砖陶瓷的原料。

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