一种合成粉色蛋白石的谱学特征及颜色成因探讨

Spectral Characteristic and Colour Genesis of A Kind of Pink Synthetic Opal

  • 摘要: 采用超景深显微镜、傅里叶变换红外光谱(FTIR)、激光拉曼光谱(Raman)、紫外-可见吸收光谱(UV-Vis)、激光诱导击穿光谱(LIBS)和X射线荧光光谱(EDXRF)等测试技术,对一种合成粉色蛋白石样品的宝石学特征、谱学特征及颜色成因予以探讨。结果表明,该类合成蛋白石的外观呈粉色,玻璃光泽,透明,无变彩,折射率1.41~1.42,密度2.16~2.20 g/cm3,放大观察内部可见不同红色调的球状、椭球状的微纳米级固相包裹体。根据红外光谱和拉曼光谱特征,该类合成粉色蛋白石的类型应介于Opal-A型与Opal-CT型之间,且与Opal-A型蛋白石较为接近;红外透射光谱显示7 224、4 523、3 674、2 662、2 266 cm-1附近的一组特征红外吸收谱峰,与俄罗斯人工蛋白石较为吻合。该类样品的SiO2含量达97.581%~98.352%,此外分别含有0.287%~0.497%的Na2O,0.112%~0.326%的MgO,0.895%~1.507%的Al2O3,0.011%~0.026%的K2O,0.003%~0.015%的CaO以及0.079%~0.244%的Cu2O,其颜色是由铜的氧化物(主要为Cu2O)等矿物颗粒细微分散所致,并在可见光范围内产生570 nm附近的特征吸收峰。

     

    Abstract: In this paper, the gemmological characteristics, spectroscopic characteristics and colour genesis of a kind of pink synthetic opal were investigated applying ultra-depth microscope, Fourier transform infrared spectroscopy (FTIR), microscopic laser Raman spectroscopy (Raman), ultraviolet-visible absorption spectroscopy (UV-Vis), laser induced breakdown spectroscopy(LIBS), and X-ray fluorescence energy spectroscopy (EDXRF). The pink synthetic opal samples are transparent, show vitreous luster and have no play-of-colour phenomenon. The basic gemmological characteristics were tested with the refractive index of 1.41-1.42 and the density of 2.16-2.20 g/cm3. The spherical and ellipsoidal micro-nano scale solid inclusions with different shades of red were observed under microscopic inspection. The synthetic pink opal samples showed both opal-A and opal-CT characteristics and were closer to opal-A opal by FTIR and Raman. Besides, the FTIR transmission spectra showed a series of peaks at 7 224, 4 523, 3 674, 2 662 cm-1 and 2 266 cm-1, consistent with those of the Russian synthetic opal. The content of SiO2 of the samples is in the range of 97.581%-98.352%; in addition, 0.287%-0.497% of Na2O, 0.112%-0.326% of MgO, 0.895%-1.507% of Al2O3, 0.011%-0.026% of K2O, 0.003%-0.015% of CaO, and 0.079%-0.244% of Cu2O were tested. The colour is due to the fine dispersion of mineral particles such as copper oxides (mainly Cu2O) and the characteristic absorption peak near 570 nm is shown in the UV-Vis spectrum.

     

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