Characterization of ancient ceramic shreds: Insights into firing conditions and manufacturing technology

S. Mammadov, M. Gurbanov, A. Ahadova, A. Abishov
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Abstract

Four ancient ceramic shreds from the archaeological site Leletepe in the Fizuli region of the Republic of Azerbaijan and two local raw ceramic pastes were characterized by powder X-ray diffraction (PXRD) and thermal analysis (TG-DTG) techniques. XRD analysis of ceramic sherds reveals that all investigated samples contain similar minerals: quartz, feldspar, and clay. Three samples out of four contain calcite. Based on the traditional approach, it has been assumed that the firing process in these samples stopped before 700 °C. The mass loss ratios of samples of ancient ceramics also indicate that reversible dehydroxylation took place in all four samples, thus indicating the initial mild firing conditions. The summary of all the applied methods indicates that the ceramic samples were made using a similar manufacturing technology. According to XRD analysis, samples N1 and N4 contain diopside, and samples N2 and N3 contain maghemite, indicating the different origins of the ceramic shreds. Analysis of the raw ceramic mass also did not reveal the presence of these minerals, which may indicate a discrepancy between the origin of ancient ceramic sherds and modern ones.
古代陶瓷碎片的特征:对烧制条件和制造技术的见解
采用粉末x射线衍射(PXRD)和热分析(TG-DTG)技术对阿塞拜疆共和国菲祖利地区莱莱特佩考古遗址的4块古代陶瓷碎片和两种当地原料陶瓷糊进行了表征。对陶瓷碎片的XRD分析表明,所有被调查的样品都含有相似的矿物:石英、长石和粘土。四个样品中有三个含有方解石。基于传统的方法,假设这些样品的烧制过程在700°C之前停止。古陶瓷样品的质量损失比也表明,四种样品都发生了可逆的脱羟基作用,从而表明最初的温和烧成条件。对所有应用方法的总结表明,陶瓷样品是采用类似的制造技术制成的。通过XRD分析,样品N1和N4中含有透辉石,样品N2和N3中含有磁赤铁矿,说明陶瓷碎片的来源不同。对原始陶瓷块的分析也没有发现这些矿物质的存在,这可能表明古代陶瓷碎片和现代陶瓷碎片的来源存在差异。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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