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Ageing of fired-clay ceramics: Comparative study of rehydroxylation processes in a kaolinitic raw material and moon-shaped ceramic idol from the Bronze Age

机译:陶土的老化:青铜时代高岭土原料和月形陶瓷偶像中再羟基化过程的比较研究

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摘要

Sources of raw materials and identification of the provenance of ancient ceramics as well as the estimation of the firing temperatures of ceramic findings are two principal problems archaeologists solve with material scientists. These two problems are closely interconnected. This paper is focused on the identification of clay mineral kaolinite in a ceramic body of archaeological ceramic idol in comparison with a reference kaolinitic raw material. Kaolinite identified in studied ceramic samples can be from a primary source or a product of rehydroxylation of metakaolinite of the ceramics. The rehydroxylation process is simulated here in laboratory conditions in an autoclave by modifications of standardized test methods. The rehydroxylation process was studied on a kaolinitic raw material and the acquired results were then applied to evaluate samples of a unique archaeological object from the Late Bronze Age a moon-shaped ceramic idol, which was found at an archaeological site near Prague in the Czech Republic. XRF, XRD, TG-DTA, TG-DSC and IR analyses were used to study this process. XRD and TA proved the presence of the clay mineral kaolinite in its end parts. A small amount of kaolinite was also detected in the central part, but only by TA. It was proved that kaolinite in the end parts originated from raw material and that its presence in the central part was caused by the rehydroxylation of the metakaolinite. It was probably due to the use of the moon-shaped ceramic idol as an andiron in an open fireplace. (C) 2015 Elsevier B.V. All rights reserved.
机译:考古学家与材料科学家共同解决的两个主要问题是原材料的来源,鉴定古代陶瓷的起源以及估计陶瓷发现的烧成温​​度。这两个问题是紧密联系在一起的。与参考高岭土原料相比,本文着重于鉴定考古陶瓷偶像陶瓷体中的粘土矿物高岭石。在研究的陶瓷样品中鉴定出的高岭石可以来自陶瓷的偏高岭石的主要来源或重新羟基化的产物。通过修改标准测试方法,在实验室条件下,在高压釜中模拟了重新羟基化过程。对高岭土原料进行了重新羟基化过程的研究,然后将获得的结果用于评估青铜时代晚期一个独特的考古对象的样品,该样品是在捷克共和国布拉格附近的考古现场发现的一个月形陶瓷偶像。 。 XRF,XRD,TG-DTA,TG-DSC和IR分析用于研究这一过程。 XRD和TA证明在其端部存在粘土矿物高岭石。在中部也检测到少量高岭石,但仅通过TA检出。事实证明,端部的高岭石起源于原材料,并且其中心部分的存在是由偏高岭石的再羟基化引起的。这可能是由于在开放式壁炉中使用了月亮形的陶瓷偶像作为熨斗。 (C)2015 Elsevier B.V.保留所有权利。

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