摩洛哥建筑琉璃瓦的光谱特性分析

Mohamed EL AMRAOUI
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摘要

摘要 本作品涉及对摩洛哥建筑中用于保护天花板、墙壁和屋顶免受雨水侵蚀的由绿色单色釉陶组成的琉璃瓦的特征进行多重分析。这些瓦片来自五个遗址,可追溯到不同的历史时期:梅克内斯的 Bou-Inania Madrasa(14 世纪)、梅克内斯的 Qara 监狱(18 世纪)、梅克内斯的 Dar El-Beida 宫殿(18 世纪)和埃拉奇迪亚的 Mdaghra Al-Hibous 墓地(19 世纪)。为了追溯古代采用的技术工艺(材料、着色颜料、烧制温度等),使用了不同的分析技术。光学吸收光谱法在绿釉中发现了两种不同类型的致色离子,在 Dar El-Beida 宫殿和卡拉监狱的瓦片中发现了铬 Cr3+,在 Bou-Inania Madrasa 和 Al-Hibous 墓地的瓦片中发现了铜 Cu2+。拉曼显微光谱分析确定了两种绿色釉料的不同着色相,卡拉监狱釉料的着色相为escolaite(Cr2O3),Dar El-Beida 宫殿釉料的着色相为铜酞菁混合铬基颜料。不过,梅克内斯 Bou-Inania Medersa 和 Errachidia Al-Hibous 墓地的釉料中绿色的来源可能是由于铜在玻璃釉料中的溶解。X 射线衍射和拉曼微光谱分析揭示了陶土砖瓦的矿物成分。石英和方解石是主要物相,赤铁矿和 "高温 "物相(阳起石、透辉石和透辉石)则是次要物相。通过这些已确定的相,可以推算出瓦片在氧化气氛中的烧制温度约为 950 ℃。所有釉料的色度坐标都用实验室 CIE 色彩空间表示,因此可以客观地分辨出所有绿色。通过对不同历史遗址的釉料进行调查,可以探索着色材料,揭示所采用的工艺规程之间的差异,还可以建立一个颜色参考数据库,以跟踪釉料的退化情况,并在更换缺失或退化的瓦片时提供帮助。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Spectrometric Characterization of Moroccan Architectural Glazed Tiles
Abstract The present work relates to a multi-analytic characterization of glazed tiles consisting of green monochrome glazed ceramics used in Moroccan architecture to protect ceilings, walls and roofs from rainwater. These tiles originate from five sites and date back to different historical periods: Bou-Inania Madrasa in Meknes (14th century), Prison of Qara in Meknes (18th century), Dar El-Beida Palace in Meknes (18th century) and Al-Hibous Cemetery of Mdaghra in Errachidia (19th century). Different analysis techniques were used in view to go back to the ancient technological processes adopted (materials, coloring pigments, firing temperatures, etc..). Optical absorption spectrometry revealed two different types of chromogenic ions in green glazes, chromium Cr3+ in the case of the tiles from Dar El-Beida Palace and Prison of Qara, and copper Cu2+ in the case of the tiles from Bou-Inania Madrasa and Al-Hibous Cemetery. Raman microspectroscopy identified different coloring phases with two types of green glazes, escolaite (Cr2O3) in the case of the glazes of the Prison of Qara and copper phthalocyanine mixed with a chromium-based pigment in the case of the glazes of the Dar El-Beida Palace. However, the origin of the green color in the glazes from Bou-Inania Medersa in Meknes and Al-Hibous cemetery of Errachidia may be due to the dissolution of copper in the vitreous glazes. X-ray diffraction, supported by Raman microspectrometry, revealed the mineralogical compositions of the terracotta tiles. Quartz and calcite are the main phases, while hematite and "high temperature" phases (anorthite, gehlenite and diopside) appear as minority ones. These identified phases permit to estimate the firing temperature of the tiles at around 950 °C in an oxidizing atmosphere. The chromatic coordinates of all glazes, represented in the Lab CIE color space, made it possible to discriminate objectively all green colors. The present investigation of glazes from different historical sites allowed the exploration of the coloring materials, revealed differences in the adopted technological protocols and permitted the establishment of a color reference database to follow glazes degradation and to help while replacing missing or degraded tile pieces.
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