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Raman and infrared spectroscopic study of the basic copper chloride minerals: implications for the study of the copper and brass corrosion and 'bronze disease'

机译:基本的氯化铜矿物的拉曼光谱和红外光谱研究:对铜和黄铜腐蚀和“青铜病”的研究意义

摘要

The vibrational spectra of both synthetic and natural atacamite and clinoatacamite are compared with natural paratacamite, have been obtained at 298 using a combination of FTIR and Raman microscopy. The vibrational spectra of the minerals are different, in line with differences in crystal structure and composition. The vibrational spectra of paratacamite are different from that of both atacamite and clinoatacamite. Paratacamite is not polymorphic with atacamite but rather is a separate phase. Some similarity in the Raman spectra of the polymorphs exists, particularly in the OH stretching region, but characteristic differences in the OH deformation regions are observed. These differences may be used to characterize the minerals. Differences are also observed in the chloride stretching and deformation regions. The implication from the study of these minerals is that copper, brass and bronze objects of archaeological, antiquarian and medieval significance can be studied by the use of Raman spectroscopy. Indeed the restoration of these types of articles can be aided by the application of Raman spectroscopy to the study of the degradation products from paintings of antiquity.
机译:将合成的和天然的钽铁矿和斜铁锰铁矿的振动光谱与天然的寄生金铁矿的振动光谱进行了比较,这是通过FTIR和拉曼显微镜的结合在298获得的。矿物的振动光谱是不同的,这与晶体结构和组成的差异一致。顺滑石的振动光谱不同于顺滑石和斜铁石的振动光谱。滑石粉与滑石粉不是多晶型的,而是一个独立的相。多晶型物的拉曼光谱中存在一些相似性,特别是在OH拉伸区域中,但是在OH变形区域中观察到了特性差异。这些差异可用于表征矿物。在氯化物拉伸和变形区域也观察到差异。对这些矿物的研究表明,可以通过拉曼光谱法研究具有考古,文物和中世纪意义的铜,黄铜和青铜器。确实,这些类型的物品的修复可以通过拉曼光谱技术应用于研究古代绘画的降解产物而得到帮助。

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