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Characterization of the corrosion layer on iron archaeological artefacts from K_2 (825-1220 AD), an archaeological site in South Africa

机译:南非考古遗址K_2(825-1220 AD)的铁考古文物上腐蚀层的特征

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摘要

A study of the composition and phase distribution of the corrosion layers on three ferrous objects, excavated at K_2 (Bambandyanalo), an archaeological site in South Africa, was conducted. The objective of the study was to obtain information that can contribute to conservation procedures to be performed on the iron artefacts from this site. Examination of cross sections by means of energy-dispersive X-ray spectroscopy coupled to a scanning electron microscope (SEM-EDX), X-ray powder diffraction (XRD), and micro-Raman spectroscopy revealed the same corrosion composition and structure for all the objects under study, namely an internal layer adjacent to the metal surface with ghost inclusions and an external layer containing quartz grains. The study also revealed that the presence of magnetite (Fe_3O_4), maghemite (γFe_2O_3), and lepidocrocite (γ-FeOOH) within the internal layer is the only difference between the chemical compositions of iron corrosion products within the two layers. The results also made it possible to retrace the corrosion history during burial and long-term storage.
机译:研究了在南非的一个考古遗址K_2(Bambandyanalo)出土的三个铁质物体上腐蚀层的组成和相分布。该研究的目的是从该站点获得有助于铁制品保存程序的信息。通过与扫描电子显微镜(SEM-EDX)耦合的能量色散X射线光谱学,X射线粉末衍射(XRD)和显微拉曼光谱对横截面进行检查,发现所有材料的腐蚀成分和结构均相同。研究对象,即与金属表面相邻的带有重影夹杂物的内层和含有石英晶粒的外层。研究还表明,在内层内存在磁铁矿(Fe_3O_4),磁赤铁矿(γFe_2O_3)和纤铁矿(γ-FeOOH)是两层铁腐​​蚀产物化学成分之间的唯一区别。结果还使得可以追溯到埋葬和长期存储期间的腐蚀历史。

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