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作 者:王亚芳[1,2] 杨百瑞[3] Peter Townsend
机构地区:[1]中国地质大学(北京)矿物材料国家专业实验室,北京100083 [2]中国地质大学(北京)材料科学与工程学院,北京100083 [3]北京师范大学物理学系,北京100875 [4]School of Science and Technology,University of Sussex
出 处:《人工晶体学报》2010年第B06期217-220,共4页Journal of Synthetic Crystals
基 金:中国地质大学(北京)矿物材料国家专业实验室项目(09A005)资助
摘 要:本文测量了磷光发光材料CaSO4∶Dy,Li和CaSO4∶Tm,Li经X射线辐照后在低温区域(25~280K)的三维热释光光谱。结果表明:两种样品的发光光谱分别由稀土元素Dy的特征发光(470nm,570nm,655nm)和Tm的特征发光(340nm,360nm,455nm,480nm)组成;发光峰分别出现在40K,100K,200K和240K,主要是由基体材料CaSO4∶Li决定的;两种样品在240K附近的热释光发光峰温有5K左右的差别,这表明掺稀土元素的CaSO4样品其热释光发光所涉及的俘获中心是受稀土元素扰动的,可能和稀土元素的半径相关。The thermoluminescence (TL) spectra of CaSO4: Dy, Li and CaSO4: Tm, Li were collected at the low temperature range from 25 K to 280 K after irradiated by X rays. The result shows that the emission bands of CaSO4: Dy, Li are the characteristic emissions of Dy^3+ , which are 470 nm,570 nm and 655 nm. As for CaSO4: Tm, Li, they are 340 nm,360 nm, 455 nm and 480 nm. The peak temperatur6s' of the two samples are 40 K, 100 K,200 K and 240 K which are mainly controlled by CaSO4:Li. There is a 5 K shift of the glow peak which is around 240 K between two samples. These data stro.ngly suggest that the trapping and recombination sites may be modulated by the size of rare earth dopants.
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