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IR and UV spectral studies for rare earths-doped tellurite glasses

机译:稀土掺杂碲酸盐玻璃的红外和紫外光谱研究

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Infrared absorption spectra were measured for pure TeO_2 glasses and doped with 10-wt percent of different rare-earth oxides, La_2O_3, CeO_2, Pr_2O_3, Sm_2O_3, Nd_2O_3, and Yb_2O_3. The recorded bands were attributed to the different modes of vibrations of Te-O band. Rare earths connected to the chains of TeO_4 groups are identified on the basis of the simultaneous presence of the bands at approx 660 to 625 cm~(-1). Quantitative justification of these absorption bands shows that the values of the experimental wave number for most recorded absorption bands agree well with the theoretical ones. Optical absorption spectra show that the absorption edge has a tail extending towards lower energies. The edge shifts towards higher energies for all rare earths-doped glasses. The degree of the edge shift was found to be depending on the ionic radius of the rare earths and is mostly related to the structural rearrangement and the relative concentrations of the glass basic units. By increasing the ionic radius of the rare earths, the optical energy gap decreases, while the width of the localized states is increased.
机译:测量了纯TeO_2玻璃的红外吸收光谱,并掺有10wt%的不同稀土氧化物La_2O_3,CeO_2,Pr_2O_3,Sm_2O_3,Nd_2O_3和Yb_2O_3。记录的带归因于Te-O带的不同振动模式。根据在大约660至625 cm〜(-1)波段的同时存在,确定与TeO_4基团的链相连的稀土。这些吸收带的定量证明表明,大多数记录的吸收带的实验波数值与理论值相吻合。光学吸收光谱表明,吸收边缘的尾巴朝着较低的能量延伸。对于所有掺稀土的玻璃,边缘都向更高的能量转移。发现边缘位移的程度取决于稀土的离子半径,并且主要与玻璃重晶单元的结构重排和相对浓度有关。通过增加稀土的离子半径,光能隙减小,而局部态的宽度增加。

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