首页> 外文期刊>Journal of Raman Spectroscopy: An International Journal for Original Work in All Aspects of Raman Spectroscopy, Including Higher Order Processes, and Also Brillouin- and Rayleigh Scattering >Characterization of pottery from Republic of Macedonia. III. A study of comparative mineralogical detection efficiency using micro-Raman mapping and X-ray diffraction
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Characterization of pottery from Republic of Macedonia. III. A study of comparative mineralogical detection efficiency using micro-Raman mapping and X-ray diffraction

机译:马其顿共和国陶器的特征。三,显微拉曼谱图和X射线衍射法比较矿物学检测效率的研究

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摘要

Point-to-point micro-Raman and X-ray diffraction (XRD) techniques were employed for characterization of minerals present in the pottery body of 27 glazed Byzantine and Ottoman pottery shreds, excavated at two different archaeological sites in the Republic of Macedonia: in Skopje (Skopsko Kale) and in Prilep (Markovi Kuli and Sv. Atanas Church). The Raman spectra of 18 Byzantine samples (dating from 12th-14th century) and nine Ottoman samples (dating from 17th-19th century) revealed 26 different minerals. XRD measurements were further performed on the same powder samples to validate the mineralogical assessment obtained by point-to-point micro-Raman spectroscopy. Although only 13 different mineral phases were obtained by the XRD, the results obtained from the Raman and XRD spectra for the most abundant minerals in the investigated pottery bodies match quite well. However, the identification of the less abundant minerals in the clay matrixes from the XRD data was very difficult, if at all possible. The results emphasize the specifics of the applied techniques and their limits. Additionally, wavelength dispersive X-ray fluorescence spectroscopy was used for the elemental analysis.
机译:点对点微拉曼光谱和X射线衍射(XRD)技术用于表征存在于马其顿共和国两个不同考古现场的27块釉面拜占庭和奥斯曼陶器碎片中的矿物质。斯科普里(斯科普斯科羽衣甘蓝)和普里莱普(马尔科维·库利和阿塔那斯教堂)。 18个拜占庭样本(可追溯到12-14世纪)和9个奥斯曼样本(可追溯到17-19世纪)的拉曼光谱揭示了26种不同的矿物。对相同的粉末样品进一步进行XRD测量,以验证通过点对点显微拉曼光谱法获得的矿物学评估。尽管通过XRD只能获得13种不同的矿物相,但是从拉曼光谱和XRD光谱中获得的被研究陶体中最丰富的矿物的结果非常吻合。但是,如果可能的话,很难从XRD数据中识别出粘土基质中含量较低的矿物。结果强调了所应用技术的细节及其局限性。另外,将波长色散X射线荧光光谱法用于元素分析。

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