摘要
比较了一些白钨矿结构的钨、钼酸盐晶体(如未掺杂的CaWO4、PbWO4、CaMoO4、Pb-MoO4晶体)的透射光谱,发现这些晶体的光吸收边的相对位置用普遍认同的观点,即白钨矿结构的钨、钼酸盐晶体的光吸收边起源于具有Td对称性的W(Mo)O2-4基团内的电子从t1轨道向2e轨道的转移激发,不能给出圆满阐释,而应代之以新的观点。作者认为这类晶体的光吸收边可能起因于D2d对称的W(Mo)O2-4基团内的电子从1a2轨道向2b1轨道的转移激发,并借助于离子极化的模型对这些未掺杂晶体以及分别掺La、Mo和Nb的PbWO4晶体的光吸收边的相对位置进行了定性解释。
The transmission spectra and optical absorption edges (OAEs) of some scheelite structured crystals, such as undoped CaWO 4, PbWO 4, CaMoO 4 and PbMoO 4 crystals, were comparatively studied. It was found that the relative location of their OAEs can not be explained from a widely adopted viewpoint that the OAEs originate from electron transfer from t 1 orbital to 2e orbital of W(Mo)O 2- 4 group with T d symmetry. But it can be explained with the electron transfer from 1a 2 orbital to 2b 1 orbital within the W(Mo)O 2- 4 group with D 2d symmetry. The OAEs of the above mentioned crystals and the PbWO 4 crystals doped with lanthanum, niobium and molybdenum respectively were interpreted briefly from the present viewpoint and the ion polarization model.
出处
《光学学报》
EI
CAS
CSCD
北大核心
1998年第11期1591-1596,共6页
Acta Optica Sinica
基金
国家自然科学基金
关键词
白钨矿结构
钨酸盐
钼酸盐
晶体
光吸收边
scheelite structure, tungstate crystal, molybdate crystal, doped tunsgate crystal, optical absorption edge.