光致发光光谱在蓝色尖晶石鉴定中的应用研究

Application of Photoluminescence Spectroscopy in the Identification of Blue Spinel

  • 摘要: 蓝色系镁铝尖晶石是珠宝市场上的热门品种,本研究选取6颗Co致色和5颗Fe致色蓝色系镁铝尖晶石进行X射线荧光光谱、紫外-可见光谱和光致发光光谱测试,结果表明,常见蓝色系尖晶石的颜色主要与Fe2+的自旋禁阻跃迁5E3E5E3T15E3T2和Fe3+的自旋禁阻跃迁6A1g4A1g有关;钴尖晶石的颜色主要由Co2+4A24T1跃迁所致,同时受到Fe2+和Fe3+的影响。405 nm激发光源在室温下光致发光测试结果显示,11颗蓝色镁铝尖晶石的光致发光光谱均具有明显位于675、685、697、707 nm和717 nm等5处发光峰组合,为Cr3+2Eg4A2g跃迁所致,且以685 nm零声子线及其振动子边带为主发光峰;532 nm激发光源在室温下光致发光测试结果发现,钴尖晶石样品在645 nm处存在发光宽带,由Co2+4T1(P)→4A2(F)产生。光致发光光谱有助于检测较低含量Co和Cr元素的存在,为蓝色系镁铝尖晶石的微量元素分析和品种判定提供重要依据。

     

    Abstract: Blue magnesium aluminum spinel is a popular variety in the jewelry market. In this study, 6 cobalt-coloured spinels and 5 iron-coloured blue spinels were selected for X-ray fluorescence spectroscopy and UV-Vis spectroscopy, and photoluminescence spectroscopy tests. The results showed that the colour of common blue spinels is mainly related to the spin forbidden transition of Fe2+ from 5E3E, 5E3T1, 5E3T2 and the spin forbidden transition of Fe3+ from 6A1g4A1g. The colour of natural cobalt spinels are mainly caused by the transition of Co2+ from 4A24T1, and also affected by Fe2+ and Fe3+.The photoluminescence spectra of 11 blue magnesium-aluminum spinels by 405 nm excitation light source at room temperature showed obvious 5 fluorescence peak combinations, including 675, 685, 697, 707 nm and 717 nm, which are caused by 2Eg4A2g transition of Cr3+. The strong zero phonon line near 685 nm and the vibron sideband of the line are the main luminescent peaks. The photoluminescence spectra tested by 532 nm excitation light source at room temperature showed that the cobalt spinel samples have a wide luminescence peak at 645 nm, which are generated by Co2+ from 4T1(P)→4A2(F). Therefore, photoluminescence spectroscopy is helpful to detect the presence of lower content of Co and Cr elements, and provides an important basis for the analysis of trace elements and variety determination of blue magnesium aluminum spinel species.

     

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