The Covariation of Color and Orange Fluorescence Instabilities in Yellow Sapphires

Author:

Yang Yunqi12,Wang Chaowen123ORCID,Wang Chengsi12,Shen Xibing45,Yin Ke4,Chen Tao12,Shen Andy Hsitien12ORCID,Algeo Thomas J.678ORCID,Hong Hanlie47

Affiliation:

1. Gemmological Institute, China University of Geosciences, Wuhan 430074, China

2. Hubei Gems and Jewelry Engineering Technology Research Center, Wuhan 430074, China

3. Department of Geosciences and Engineering, Delft University of Technology, 2628 CN Delft, The Netherlands

4. School of Earth Sciences, China University of Geosciences, Wuhan 430074, China

5. School of Resources and Environment, Beibu Gulf University, Qinzhou 535011, China

6. Department of Geosciences, University of Cincinnati, Cincinnati, OH 45221-0013, USA

7. State Key Laboratory of Biogeology and Environmental Geology, China University of Geosciences, Wuhan 430074, China

8. State Key Laboratory of Geological Processes and Mineral Resources, China University of Geosciences, Wuhan 430074, China

Abstract

In recent years, some sapphires were found to fade in sunlight and to increase their color after UV irradiation. This unstable color phenomenon is attributed to the photochromism of corundum. The photochromic effect seriously affects the grading and evaluation of sapphires, although its mechanism is still uncertain. Here, we performed a set of photochromic experiments on sapphire specimens using a 254 nm shortwave UV light source and a D65 light source (which simulates sunlight) to generate different color states exhibiting characteristic absorption, emission, and excitation spectra. We observed that, for different color states, variation in the intensity of the absorption band at ~460 nm was consistent with that of orange fluorescence at 500–800 nm. This observation indicates a relationship between color instability and orange fluorescence. Peaks in excitation spectra at 320, 420, 490, 560, and 637 nm provide insight into the source(s) of excited orange fluorescence, which are related to different types of F-centers and Mg-trapped holes. We propose an explanation for the photochromic phenomenon: the color of photochromic yellow sapphire is the result of a variety of defects that release orange fluorescence simultaneously. Further, we hypothesize that the mechanism of photochromism in yellow sapphires is linked to electron transfer between F-centers and Mg-trapped holes.

Funder

National Science Foundation of China

Chinese Scholarship Council

Hubei Gems and Jewelry Engineering Technology Research Center

Publisher

MDPI AG

Subject

Geology,Geotechnical Engineering and Engineering Geology

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