School of Gemmology, China University of Geosciences (Beijing), Beijing, 100083, China.
National Gems & Jewelry Testing Co. Ltd, Beijing, 100013, China.
Sci Rep. 2023 Feb 10;13(1):2426. doi: 10.1038/s41598-023-29675-w.
Fluorescence plays an important role in determining the color appearance of fluorescing minerals. This paper discusses the color mechanism in the red spinel and the color effects from the light source as well as the background on the spinel color. Excitation-Emission Matrices (EEMs) fluorescence spectroscopy was utilized to characterize the fluorescence of natural Cr-doped magnesia-alumina spinel from Myanmar. EMP, LA-ICP-MS, and optical spectroscopy were applied to study the spinel's chemical compositions and color mechanism. X-Rite Ci-7800 spectrophotometer, which is useful to measure colors for fluorescing minerals, was employed to acquire color data of spinel in daylight and incandescent light. The results indicated the higher value of Cr/Fe makes pinkish-red spinel has a much stronger red fluorescence effect than dark-red spinel. The two narrow absorption bands at ~ 25,500 cm (with a broad absorption band at ~ 24,100 cm) and ~ 18,570 cm in the optical absorption spectrum are assigned to spin-allowed electronic d-d transitions A → T(F) and A → T(F) in Cr at the M site. The EEMs spectra of the pinkish-red spinels show twin emissions at 706 nm excited both by ~ 380 nm and ~ 535 nm radiations, which is the key to the bright neon red color in pinkish-red spinel. The colorimetry study suggests the strong red fluorescence produced by < 460 nm radiation contributes more than 10% lightness and chroma in pinkish-red spinel under daylight. The lightness and the chroma of the spinels grow with the decrease of the background grayscale. The differentiation of spinel colors in dark conditions is lower than that in a bright environment.
荧光在确定发荧光矿物的颜色外观方面起着重要作用。本文讨论了红色尖晶石中的颜色机制以及来自光源和尖晶石颜色背景的颜色效果。利用激发-发射矩阵(EEM)荧光光谱法对来自缅甸的天然 Cr 掺杂镁铝尖晶石的荧光进行了表征。采用电子探针(EMP)、激光剥蚀电感耦合等离子体质谱(LA-ICP-MS)和光谱法研究尖晶石的化学成分和颜色机制。采用 X-Rite Ci-7800 分光光度计(可用于测量发荧光矿物的颜色)在日光和白炽灯光下获取尖晶石的颜色数据。结果表明,较高的 Cr/Fe 比值使粉红色尖晶石比暗红色尖晶石具有更强的红色荧光效果。光学吸收光谱中两个狭窄的吸收带分别位于25500cm(24100cm 处有一个宽吸收带)和18570cm,归因于 Cr 在 M 位的自旋允许电子 d-d 跃迁 A→T(F)和 A→T(F)。粉红色尖晶石的 EEM 光谱显示在380nm 和~535nm 辐射激发下,在 706nm 处有两个发射峰,这是粉红色尖晶石中产生鲜艳霓虹红色的关键。色度学研究表明,在日光下,由<460nm 辐射产生的强红色荧光对粉红色尖晶石的明度和色度的贡献超过 10%。随着背景灰度值的降低,尖晶石的明度和色度增加。在暗环境下,尖晶石颜色的差异低于明亮环境。