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首页> 外文期刊>Archaeological and Anthropological Sciences >Combined Raman spectroscopic and Rietveld analyses as a useful and nondestructive approach to studying flint raw materials at prehistoric archaeological sites
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Combined Raman spectroscopic and Rietveld analyses as a useful and nondestructive approach to studying flint raw materials at prehistoric archaeological sites

机译:拉曼光谱和Rietveld分析相结合是一种有用的无损方法,用于研究史前考古现场的火石原料

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摘要

A set of six lithic tools, unearthed along 2011 in two karst sites of the Guadalteba County (Malaga, Spain), has been nondestructively investigated by Raman spectroscopy and laboratory x-ray diffraction. From a chemist's point of view, our goal is to develop a systematic screening protocol for a quick, easy, low cost and nondestructive characterization of archaeological flints based on Raman spectroscopy, x-ray diffraction and Rietveld refinement. In this paper, we firstly made use of Raman spectroscopy to determine, in a semiquantitative way, but with the generic advantage of a faster data acquisition than x-ray diffraction, the surface content of moganite of each lithic tool, from the ratio between the relative intensities of the two Raman-active symmetric stretching vibrations (A(1) modes) of alpha-quartz (465 cm(-1)) and moganite (501 cm(-1)). The precise bulk quartz/moganite weight content was then accurately quantified by means of high-quality x-ray diffraction, followed by Rietveld refinement. We found a general good correlation between Raman and x-ray data. Nonetheless, as recently reported in the scientific literature by other authors, the vibrational spectroscopic quantification of moganite in silica rocks like flint and chert have to be performed very cautiously, to avoid undesired interferences from other Raman features due to the eventual presence of silanol (SiOH) groups, which could finally lead to an overestimation of the surface moganite concentration. As reported in such a recent article, a useful treatment to reduce the interference from silanol-bands is to heat the samples prior to their Raman analysis at a minimum of 600 A(0)C (but better at 700 or 800 A(0)C) for silanol "dehydration". This, in our opinion, may be for sure a satisfactory procedure when studying flint or chert samples of a "geological origin". But not of practical use when studying lithic tools which were manufactured by men thousands and thousands of years ago.
机译:拉曼光谱法和实验室X射线衍射已对2011年在瓜达特巴县(西班牙马拉加)的两个喀斯特地貌出土的一套六种石器工具进行了非破坏性研究。从化学家的角度来看,我们的目标是开发一种系统的筛选方案,以基于拉曼光谱,X射线衍射和Rietveld精细化技术快速,轻松,低成本且无损地表征考古fl石。在本文中,我们首先使用拉曼光谱法以半定量的方式确定,但具有比X射线衍射更快的数据采集的通用优势,可以从每个岩性工具之间的比率来确定每个岩性工具的锰矿的表面含量。阿尔法石英(465 cm(-1))和蒙脱石(501 cm(-1))的两个拉曼主动对称拉伸振动(A(1)模式)的相对强度。然后,通过高质量的X射线衍射,然后进行Rietveld精炼,精确地定量出精确的石英/蒙脱石重量含量。我们发现拉曼光谱和X射线数据之间通常具有良好的相关性。但是,正如其他作者最近在科学文献中所报道的那样,必须非常谨慎地对硅石(如fl石和石)中的锰铁矿进行振动光谱定量分析,以避免由于最终存在的硅烷醇(SiOH)而不受其他拉曼特征的干扰)组,这可能最终导致表面锰矿浓度的高估。正如最近一篇文章中所报道的那样,减少硅烷醇带干扰的一种有效方法是在进行拉曼分析之前将样品加热到最低600 A(0)C(但最好在700或800 A(0)C的温度) C)用于硅烷醇的“脱水”。我们认为,在研究“地质起源”的fl石或石样品时,这肯定是令人满意的程序。但是,在研究数千年前的人类制造的石器工具时并没有实际用途。

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