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Geochemical changes during Egyptian copper smelting? An experimental approach to the Ayn Soukhna process and broader implications for archaeometallurgy

机译:埃及铜冶炼过程中的地球化学变化? Ayn Soukhna工艺的实验方法以及对Archaeomethurgy的更广泛影响

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This paper presents the results of comprehensive geochemical analysis of experimental copper smelting products. An iterative, long-term experimental programme has been incorporated in the ongoing excavation of Middle Kingdom metallurgy remains at Ayn Soukhna (Egypt) in order to better understand the copper production chain at the site. The integration of archaeometry into this research methodology has enabled a detailed understanding of the geochemical changes which may occur during copper smelting in furnaces of this type. These include significant elemental fractionation, as well as important shifts in lead isotope ratios between ores and end products (slag and copper). This research presents an interpretative framework not only for understanding production waste from Ayn Soukhna itself, but more broadly the provenance and technology of copper alloys circulating in ancient Egypt. The significant shifts in lead isotope ratios observed for an experimental low-lead copper smelting system are highly relevant here, given the similar composition of many Sinai and Eastern Desert ores exploited throughout Pharaonic history. However, the implications of this research may be extrapolated beyond Egypt to low-lead copper provenance research across the ancient world and thus provide an important new methodological perspective for archaeometallurgy more generally. Furthermore, limitations to using iron in copper artefacts as a guide for their production technology are pointed out. Similar iron contents are observed for woodand charcoal-based smelting systems, inviting a reappraisal of fuel use at ancient metal production contexts in Egypt and elsewhere. A research approach integrating excavation, experimentation and analysis is essential when confronting the complexity of production chains underlying Egyptian copper artefacts. While daunting, this generates more nuanced interpretative frameworks for studying copper provenance and technology.
机译:本文介绍了实验铜冶炼产品综合地球化学分析的结果。迭代的长期实验计划一直纳入了中王冶金仍然在Ayn Soukhna(埃及)的挖掘中,以便更好地了解现场的铜生产链。 Archaeometry进入该研究方法的整合使得对这种类型的熔炉中的铜冶炼期间可能发生的地球化学变化进行了详细了解。这些包括显着的元素分级,以及在矿石和最终产品(炉渣和铜)之间的铅同位素比中的重要变化。该研究介绍了一种不仅用于了解Ayn Soukhna本身的生产浪费,而且更广泛地介绍了古埃及循环的铜合金的出处和技术。考虑到许多西奈和东部沙漠矿石在整个法致历史上阐述的许多西奈和东部沙漠矿石的相似性,观察到的实验性低引导铜冶炼系统的铅同位素比的显着变化。然而,这项研究的含义可能会在埃及之外推断到古代世界的低引导铜源研究,从而为大规模算法提供了一个重要的新方法看法。此外,指出了用铜伪成面用铁作为其生产技术指导的限制。对于木制炭的冶炼系统,观察到类似的铁内容物,邀请在埃及和其他地方的古代金属生产背景下重新评估燃料使用。一体化挖掘,实验和分析的研究方法是必要的,当埃及铜人工制品的生产链复杂时是必不可少的。虽然令人生畏,但这会产生更加肠化的解释性框架,用于研究铜处源和技术。

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