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ZnAl2O4 as a potential sensor: variation of luminescence with thermal history

机译:ZnAl2O4作为电势传感器:发光随热历史的变化

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ZnAI2O4 spinel powders were prepared using the Pechini or co-precipitation synthetic route and were then treated at different temperatures (600-1350 °C). These powders were characterised by X-ray diffraction, scanning electron microscopy (SEM), diffuse reflectance and luminescence measurements. SEM investigations and the X-ray patterns showed that the spinel crystallite size was dependent on the synthetic route and the treatment temperature. In addition, the structural evolution was investigated by Rietveld refinements. The inversion rate decrease was correlated with the temperature, leading to a direct spinel phase for the sample treated at high temperature. Furthermore, luminescence measurements showed various emissions linked to the presence of defects in the matrix structure. The two main emissions observed were attributed to oxygen vacancy and Zn in the interstitial positions (as revealed by differential Fourier maps). The luminescence spectra exhibited strong differences between 1200 °C and 1350 °C At the higher temperature, the characteristic emission spectra can be attributed to the direct spinel phase. The indirect-direct spinel transformation can be monitored through the change in the optical properties and correlated to the thermal history of the sample.
机译:使用Pechini或共沉淀合成路线制备ZnAl2O4尖晶石粉末,然后在不同温度(600-1350°C)下处理。这些粉末通过X射线衍射,扫描电子显微镜(SEM),漫反射率和发光测量来表征。 SEM研究和X射线图表明,尖晶石微晶尺寸取决于合成路线和处理温度。此外,通过Rietveld改进对结构演变进行了研究。转化率的降低与温度相关,导致在高温下处理的样品直接成为尖晶石相。此外,发光测量显示各种发射与基质结构中缺陷的存在有关。观察到的两个主要排放物归因于间隙位置的氧空位和Zn(如差分傅里叶图所示)。发光光谱在1200°C和1350°C之间表现出很强的差异。在较高的温度下,特征发射光谱可归因于直接尖晶石相。间接-尖晶石转变可以通过光学性质的变化进行监测,并与样品的热历史相关。

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