天河石的颜色成因探讨

余红军, 沈锡田

余红军, 沈锡田. 天河石的颜色成因探讨[J]. 宝石和宝石学杂志, 2018, 20(2): 38-46. DOI: 10.15964/j.cnki.027jgg.2018.02.006
引用本文: 余红军, 沈锡田. 天河石的颜色成因探讨[J]. 宝石和宝石学杂志, 2018, 20(2): 38-46. DOI: 10.15964/j.cnki.027jgg.2018.02.006
YU Hongjun, Andy Hsitien Shen. Discussion of Colour Origin in Amazonite[J]. Journal of Gems & Gemmology, 2018, 20(2): 38-46. DOI: 10.15964/j.cnki.027jgg.2018.02.006
Citation: YU Hongjun, Andy Hsitien Shen. Discussion of Colour Origin in Amazonite[J]. Journal of Gems & Gemmology, 2018, 20(2): 38-46. DOI: 10.15964/j.cnki.027jgg.2018.02.006

天河石的颜色成因探讨

基金项目: 

中国地质大学(武汉)珠宝检测技术创新中心开放基金(文章编号GICTXM-S201420)

详细信息
    作者简介:

    余红军(1989-),男,硕士研究生,主要从事宝石学研究。

    通讯作者:

    沈锡田(1962-),男,博士生导师,教授,主要从事宝石学研究工作。E-mail:ahshen@foxmail.com

  • 中图分类号: TS93

Discussion of Colour Origin in Amazonite

  • 摘要: 在充分查阅了大量前人的资料的基础上,对5个天河石样品进行常规宝石学测试,并借助大型仪器对其进行深入的研究。激光剥蚀电感耦合等离子体技术测试发现,天河石的微量元素Fe、Rb和Pb的质量分数较多;显微红外光谱对结构水测试发现,在3 800~3 200 cm-1范围内显示有结构水和液态水的吸收;显微紫外-可见吸收光谱测试显示以380、625、740 nm为中心的强吸收。观察讨论天河石对可见光的吸收,结合热处理和辐照处理的结果,综合比较前人的研究结果,得出影响天河石颜色的三个吸收区域(625 nm中心、740 nm中心和380 nm中心)都是空穴缺陷造成的,与结构水并无直接的关系。
    Abstract: Based on the literatures, we studied gemmological characteristics of five amazonite samples, and conducted in-depth research with the help of advanced instrumentation. The contents of trace elements (Fe,Rb and Pb) were obtained by laser ablation inductively coupled plasma mass specrtrometry (LA-ICP-MS). We identified structural water and liquid water among 3 800~3 200 cm-1 using microscopic FTIR spectroscopy. We found three strong absorption centers at 380、625 nm and 740 nm by using microscopic UV-Vis spectrophotometer. Comparing the results from heat treatment and irradiation treatment, we concluded that the hole-related centers at 380, 640 nm and 725 nm caused its colour. The colour has no direct relation with the structural water.
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出版历程
  • 收稿日期:  2017-06-11

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