Unravelling the role of iron and manganese oxides in colouring Late Antique glass by micro-XANES and micro-XRF spectroscopies

IF 4.6 Q1 OPTICS
Francesca Gherardi, Clément Hole, Ewan Campbell, Marine Cotte, Rachel Tyson, Sarah Paynter
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Abstract

This research aims to understand colouring technologies in 5th–7th centuries glass imported to Atlantic Britain by correlating the iron (Fe) and manganese (Mn) ratios and oxidation states with colour. Despite having a similar matrix chemical composition and concentrations of Fe and Mn oxides, these vessels display different colours (from green to yellow/amber, sometimes with purple streaks). Colour changes can be induced by controlling the reduction-oxidation reactions that occur during glass production, which are influenced by the raw materials, furnace and melt atmosphere, and recycling. To evaluate these parameters, reference glasses were prepared, following the composition of Late Antique archaeological glass recovered from Tintagel (UK) and Whithorn (UK). A corpus of archaeological and experimental glass samples was analysed using bulk Fe and Mn K-edge x-ray absorption near edge structure (XANES) spectroscopy, micro-XANES and micro x-ray fluorescence (μ-XRF) at beamline ID21, at the European Synchrotron Radiation Facility. Fe and Mn XANES spectra of the archaeological glass indicate that Fe and Mn are in a similar oxidation state in all the yellow samples, predominantly Fe3+ and Mn2+. No detectable difference in Mn and Fe oxidation state occurs in the purple streaks compared to the yellow glass bulk but μ-XRF maps of the distribution of Fe and Mn show that Mn is more concentrated in the purple streaks. This indicates that the purple colour of the streaks is mainly due to a higher Mn/Fe ratio and persistence of more oxidised manganese in the purple areas, even though it is difficult to detect. Many archaeological fragments appear pale green in transmitted light but amber in reflected light. XANES studies detected the presence of surface layers where manganese is more oxidised. This layer is believed to scatter transmitted and reflected light differently and might be responsible for the optical features of the archaeological glass.
通过显微 XANES 和显微 XRF 光谱揭示铁和锰氧化物在晚期古董玻璃着色中的作用
这项研究旨在通过将铁(Fe)和锰(Mn)的比率和氧化状态与颜色联系起来,了解 5-7 世纪进口到大西洋不列颠的玻璃的着色技术。尽管基质化学成分以及铁和锰氧化物的浓度相似,但这些器皿却呈现出不同的颜色(从绿色到黄色/琥珀色,有时还带有紫色条纹)。玻璃生产过程中发生的还原-氧化反应受原材料、熔炉和熔融气氛以及回收利用的影响,通过控制这些反应可以诱发颜色变化。为了评估这些参数,我们按照从廷塔吉尔(英国)和惠索恩(英国)出土的晚期古代考古玻璃的成分制备了参考玻璃。在欧洲同步辐射设施的 ID21 光束线,使用体铁和锰 K 边 X 射线吸收近缘结构 (XANES) 光谱、微 XANES 和微 X 射线荧光 (μ-XRF) 分析了大量考古和实验玻璃样品。考古玻璃的铁和锰 XANES 光谱表明,所有黄色样品中的铁和锰都处于相似的氧化态,主要是 Fe3+ 和 Mn2+。紫色条纹中的锰和铁的氧化态与黄色玻璃块体中的锰和铁的氧化态相比没有可检测到的差异,但是铁和锰的μ-XRF 分布图显示,锰在紫色条纹中更为集中。这表明,条纹的紫色主要是由于锰/铁比率较高,以及紫色区域持续存在较多氧化锰,尽管很难检测到。许多考古碎片在透射光下呈淡绿色,但在反射光下呈琥珀色。XANES 研究发现了锰氧化程度较高的表层。据信,这一层对透射光和反射光的散射不同,可能是造成考古玻璃光学特征的原因。
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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来源期刊
CiteScore
10.70
自引率
0.00%
发文量
27
审稿时长
12 weeks
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