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Cr+3 Distribution in Al1 and Al2 Sites of Alexandrite (BeAl2O4: Cr3+) Induced by Annealing, Investigated by Optical Spectroscopy

机译:光谱法研究退火引起的翠翠石(BeAl2O4:Cr3 +)在Al1和Al2位的Cr + 3分布

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In order to investigate optical properties of alexandrite, the present work deals with the influence of thermal annealing on optical absorption and luminescence spectra of natural samples. The exposure time to heat treatment at 1000oC is taken into account. Possible migration of Cr3+ ions from Al1 (inversion site) to Al2 (reflection site) is detected. Sample composition is obtained through Scanning Electron Microscopy (SEM) measurements and points to a rearrangement of Cr+3 and Fe3+ ions in the alexandrite crystalline structure, un-der thermal annealing influence. This feature may be used to control the optical properties of natural alexan-drite, which can be associated to the observed laser emission effect.
机译:为了研究变石的光学性质,本工作涉及热退火对天然样品的光吸收和发光光谱的影响。考虑了在1000oC下的热处理时间。检测到Cr3 +离子可能从Al1(反转位点)迁移到Al2(反射位点)。通过扫描电子显微镜(SEM)测量获得样品成分,并指出在热退火影响下,变石中Cr + 3和Fe3 +离子的重排。该特征可用于控制天然亚历克斯晶体的光学性质,其可与观察到的激光发射效果相关。

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