塔吉克斯坦Kuh-i-Lal粉红色尖晶石的显色机理和光谱热变化

Yicen Liu, Li-jian Qi, D. Schwarz, Zhengyu Zhou
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引用次数: 0

摘要

采用光致发光、中红外、紫外/可见光谱等方法研究了塔吉克斯坦帕米尔高原Kuh-i-Lal地区粉色尖晶石的显色机理。这包括研究加热到从300°C到1000°C一系列温度后光谱的变化。采用激光烧蚀-电感耦合等离子体质谱法测定了样品中的微量元素。结果表明,这种颜色是由cr3 +、fe3 +、v3 +和fe2 + - fe3 +间价电荷转移机制的自旋允许跃迁共同作用的结果。光致发光光谱表明,在热处理过程中,N 1峰(687 nm)的强度以及r线和N线的全宽半最大值随温度的升高而增大。在750°-825°C范围内加热后,温度与r线和n线的积分面积之比之间存在线性关系。中红外光谱显示,在加热过程中,581 cm -1 (ν 3)处的波段逐渐消失,这可能与尖晶石晶格中八面体M-O和四面体T-O键长变化有关。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Color Mechanism and Spectroscopic Thermal Variation of Pink Spinel Reportedly from Kuh-i-Lal, Tajikistan
The color mechanism of pink spinel from Kuh-i-Lal in the Pamir Mountains of Tajikistan was studied using photo luminescence, mid-infrared, and ultraviolet/visible spectroscopy. This included studying the variations in spectra after heating to a series of temperatures ranging from 300° to 1000°C. Laser ablation–inductively coupled plasma–mass spectrometry was used to measure the trace elements present. The results reveal that the color is caused by the combined effect of spin-allowed transitions of Cr 3+ , Fe 3+ , V 3+ , and Fe 2+ -Fe 3+ intervalence charge transfer mechanisms. The photoluminescence spectra show that during heat treatment, the intensity of the N 1 peak (687 nm) and the full width half maximum of the R-line and N-lines increase with temperature. Following heating in the range of 750°–825°C, there is a linear relationship between temperature and the ratio of integral areas of the R-line and N-lines. The mid-infrared spectra indicate that the band at 581 cm –1 ( ν 3 ) gradually disappears during the heating process, which is likely related to the variation of octahedral M-O and tetrahedral T-O bond length in the spinel lattice.
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