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现代地质 ›› 2025, Vol. 39 ›› Issue (01): 158-166.DOI: 10.19657/j.geoscience.1000-8527.2025.004

• 宝石地质学 • 上一篇    下一篇

不同色调红宝石的致色成因研究

刘富康1(), 郭颖1(), 赵贝2, 刘美颖3   

  1. 1.中国地质大学(北京)珠宝学院,北京 100083
    2.中国地质大学(北京)水资源与环境学院,北京 100083
    3.国家珠宝玉石首饰检验集团有限公司北京实验室,北京 102600
  • 出版日期:2025-02-10 发布日期:2025-02-20
  • 通信作者: 郭 颖,男,教授,博士生导师,1973年出生,宝石学专业,主要从事翡翠、和田玉、绿松石等宝玉石的岩石学、矿物学及宝石学的研究工作。Email: guoying@cugb.edu.cn
  • 作者简介:刘富康,女,博士,1995年出生,宝石学专业,主要从事宝石色度学研究工作。Email: 2916207845@qq.com

Chromogenic Mechanisms of Rubies with Varying Color Tones

LIU Fukang1(), GUO Ying1(), ZHAO Bei2, LIU Meiying3   

  1. 1. School of Gemmology, China University of Geosciences (Beijing), Beijing 100083, China
    2. School of Water Resources and Environment, China University of Geosciences (Beijing), Beijing 100083, China
    3. National Gemstone Testing Center Beijing Lab, Beijing 102600, China
  • Published:2025-02-10 Online:2025-02-20

摘要:

红宝石作为重要的宝石材料,其颜色特征受到广泛关注,探索红宝石颜色与其化学成分之间的关系对于宝石学基础研究以及深入理解矿物生成机制都具有重要作用。本研究对30颗刻面红宝石(包括正红色、偏紫色和偏粉色)进行了紫外-可见光光谱、X射线荧光光谱及颜色特征分析。研究发现,红宝石颜色与其化学成分紧密相关,红宝石颜色的呈现主要受控于Cr含量,同时受到Fe、V和Ti等元素的影响。Cr3+的d-d电子跃迁4A24T2引起的吸收在偏紫色红宝石中最为显著;而Cr3+的d-d电子跃迁4A24T1和Cr3+的荧光发射峰引起的吸收在偏粉色红宝石中最为显著。紫外-可见光光谱中412 nm和548 nm处的吸收强度可有效指示红宝石中紫色调的浓淡,该两波长处的吸收强度越高,红宝石紫色调越浓。紫外-可见光光谱中的412 nm可作为红宝石颜色参数Lb的指示波长,该波长处的吸收强度与红宝石的明度L呈显著负相关关系,与红宝石的b值呈显著正相关关系。这一发现为红宝石颜色特征的定量分析提供了新的视角。

关键词: 红宝石, 致色成因, 颜色, 紫外-可见吸收光谱, X射线荧光光谱

Abstract:

Rubies, as significant gemstone materials, have garnered extensive attention for their color characteristics. Exploring the relationship between the color of rubies and their chemical composition is essential for foundational research in gemology and for a deeper understanding of mineral formation mechanisms. This study analyzed 30 faceted rubies (including vivid red, slight purple, and slight pink hues) using UV-Visible spectroscopy, X-ray fluorescence spectroscopy, and color characteristic analysis. The findings indicate that the color of rubies is closely related to their chemical composition, primarily controlled by the Cr content, along with influences from elements such as Fe, V, and Ti. The absorption due to the d-d electron transition (4A24T2) of Cr3+is most prominent in rubies with a slight purple hue, whereas the absorption related to the d-d electron transition (4A24T1) and the fluorescence emission peak of Cr3+ is most significant in rubies with a slight pink hue. Additionally, the absorption intensities at 412 nm and 548 nm in the UV-Visible spectrum effectively indicate the intensity of the purple tone in rubies; higher absorption intensities at these wavelengths correlate with a more pronounced purple hue. The 412 nm wavelength serves as an indicator wavelength for the color parameters L and b of rubies, demonstrating a significant negative correlation with the brightness parameter L and a significant positive correlation with the b value. This finding provides a new perspective for the quantitative analysis of ruby color characteristics.

Key words: ruby, chromogenic origin, color, UV-Visible spectroscopy, X-ray fluorescence spectroscopy

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