STUDIES ON NEPHRITE AND JADEITE JADES BY FOURIER TRANSFORM INFRARED (FTIR) AND RAMAN SPECTROSCOPIC TECHNIQUES

T. L. Tan, L. Ng, L. C. Lim
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引用次数: 9

Abstract

The mineralogical properties of black nephrite jade from Western Australia are studied by Fourier transform infrared (FTIR) spectroscopy using both transmission and specular reflectance techniques in the 4000–400 cm-1 wavenumber region. The infrared absorption peaks in the 3700–3600 cm-1 region which are due to the O–H stretching mode provides a quantitative analysis of the Fe/(Fe+Mg) ratio in the mineral composition of jade samples. The Fe/(Fe+Mg) percentage in black nephrite is found to be higher than that in green nephrite, but comparable to that of actinolite (iron-rich nephrite). This implies that the mineralogy of black nephrite is closer to actinolite than tremolite. The jade is also characterized using Raman spectroscopy in the 1200–200 cm-1 region. Results from FTIR and Raman spectroscopic data of black nephrite jade are compared with those of green nephrite jade from New Zealand and jadeite jade from Myanmar. Black nephrite appears to have a slightly different chemical composition from green nephrite. Spectra from FTIR and Raman spectroscopic techniques were found to be useful in differentiating black nephrite, green nephrite, and green jadeite jades. Furthermore, data on refractive index, specific gravity, and hardness of black nephrite jade are measured and compared with those of green nephrite and of jadeite jade.
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傅里叶变换红外(ftir)和拉曼光谱技术对软玉和硬玉的研究
利用傅里叶变换红外光谱(FTIR)技术,在4000 ~ 400 cm-1波数范围内研究了西澳大利亚黑软玉的矿物学性质。在3700 ~ 3600 cm-1区域由于O-H拉伸模式产生的红外吸收峰可以定量分析玉石样品矿物组成中的Fe/(Fe+Mg)比值。黑色软玉的Fe/(Fe+Mg)比值高于绿色软玉,但与放线石(富铁软玉)相当。这表明黑软玉的矿物学特征更接近于放线石而不是透闪石。利用拉曼光谱在1200-200 cm-1区域对玉石进行了表征。对黑软玉的红外光谱和拉曼光谱数据与新西兰绿软玉和缅甸玉进行了比较。黑色软玉的化学成分似乎与绿色软玉略有不同。FTIR光谱和拉曼光谱技术可用于区分黑软玉、绿软玉和绿翡翠。测定了黑软玉的折射率、比重和硬度,并与绿软玉和硬玉进行了比较。
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