Li Shu, Di Jing-ru, Wang Xiao-juan, Cao Bai-hui
Guang Pu Xue Yu Guang Pu Fen Xi. 2016 Sep;36(9):2978-83.
A new kind of imitation of turquoise named “Violet” and “White buffalo” which is a type of associated mineral of turquoise have appeared on the market recently and are becoming increasingly popular. Conventional instruments, X-ray fluorescence spectrometer, Infrared spectrometer, X-ray powder diffraction, Scanning electronic microscope, UV-Vis have been employed to discuss the gemmological characteristics of this kind of imitation of turquoise in this paper, to study their chemical composition, mineral composition, microstructure, spectral characteristics and color emerging mechanism. The X-ray fluorescence spectrum shows that the chemical composition of the sample is complicated. The basic elements of different-colour samples are basically identical which contains of Ca, Al, P, Cu, Si, K, Fe, Ba. It can be deduced from the intensity of infrared absorption bend that the major anion group of this kind of imitation of tuequoise is PO3-4. The analysis for X-ray powder diffraction data indicated that the major mineral of the sample is crandallite and woodhouseite. Meanwhile, the scanning electron microscopy showed that the structure of the dense sample is determined by numerous of scaly, leaf-shaped and irregular granular aggregates. With the study of absorption spectrum, the conclusion is drawn that Fe3+ electronic transitions are the main factor for coloring of the sample and color varies with the content of Fe3+.
一种名为“紫罗兰”和“白野牛”的新型绿松石仿制品最近出现在市场上,它们是绿松石的一种伴生矿物,且越来越受欢迎。本文采用常规仪器,如X射线荧光光谱仪、红外光谱仪、X射线粉末衍射仪、扫描电子显微镜、紫外可见光谱仪,来探讨这种绿松石仿制品的宝石学特征,研究其化学成分、矿物成分、微观结构、光谱特征及呈色机理。X射线荧光光谱表明样品的化学成分复杂。不同颜色样品的基本元素基本相同,包含Ca、Al、P、Cu、Si、K、Fe、Ba。从红外吸收峰强度可推断出这种绿松石仿制品的主要阴离子基团是PO₄³⁻。对X射线粉末衍射数据的分析表明样品的主要矿物是磷铝石和羟磷铝石。同时,扫描电子显微镜显示致密样品的结构由大量鳞片状、叶状和不规则粒状聚集体组成。通过对吸收光谱的研究得出结论,Fe³⁺电子跃迁是样品呈色的主要因素,颜色随Fe³⁺含量的变化而变化。