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Influence of firing temperature on the ceramic properties of Triassic clays from Tunisia

机译:烧成温度对突尼斯三叠纪黏土陶瓷性能的影响

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摘要

This study deals with the mineralogical, physico-chemical, thermal analysis and technological of representative Triassic clay in the south-Eastem Tunisia, in order to use in the faience ceramic. That is why the study had recourse to several quantitative and qualitative techniques of analysis; chemical analysis, mineralogical study, thermal analyses and analyses of geotechnical traits. The data collected from these techniques show that illite and kaolinite are the major clay phases. The accessory minerals detected in powdered rock are quartz, dolomite and hematite. The samples were dry pressed and sintered at temperatures ranging from 850 to 1150 ℃. The samples were characterised before and after firing. The densification was measured by three parameters: firing shrinkage, water absorption, and resistance to the inflection. A series of phase transformations takes place during sintering is governed by different mechanisms according to the temperature, which play an important role on the densification. The neomineralization processes were investigated principally by X-ray diffraction. The development of resistance to the inflection and reduction in water absorption on samples products from this Triassic clay material was noticed at elevated temperatures due to enhanced vitrification. Given the mineralogy and physico-chemical characteristics of this clay deposits could be used for the manufacture of faience ceramic production.
机译:这项研究涉及突尼斯南部突尼斯地区典型的三叠纪粘土的矿物学,理化,热分析和技术,以便用于陶艺陶瓷。这就是为什么这项研究采用几种定量和定性分析技术的原因。化学分析,矿物学研究,热分析和岩土特征分析。从这些技术收集的数据表明,伊利石和高岭石是主要的粘土相。在粉状岩石中检测到的辅助矿物是石英,白云石和赤铁矿。将样品进行干压并在850至1150℃的温度范围内进行烧结。在焙烧之前和之后对样品进行表征。通过三个参数测量致密化:烧成收缩率,吸水率和抗弯曲性。烧结过程中会发生一系列相变,取决于温度的不同机制,这对致密化起着重要作用。主要通过X射线衍射研究新矿化过程。由于增强的玻璃化作用,在升高的温度下,人们注意到这种三叠纪粘土材料对样品产品的抗弯折性和吸水性的降低。鉴于这种粘土沉积物的矿物学和理化特性,可用于制造陶艺陶瓷产品。

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