僧帽石MgAlBO4的偏振单晶拉曼光谱

Chris L. Hayward , Stephen P. Best , Robin J.H. Clark , Nancy L. Ross , Rob Withnall
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引用次数: 4

摘要

在1300-10 cm−1范围内,在80 K下收集了僧伽罗石的偏振单晶拉曼光谱。对橄榄石结构类型因子群分析预测的36个一阶拉曼谱带进行了观测和赋值。在具有橄榄石结构的晶体中,僧伽罗石的晶胞体积最小,而且比硅酸盐橄榄石扭曲得更严重。这导致了振动光谱中与畸变相关的结果,例如每种模式的波数范围更大,对称BO4模式的拉曼强度降低。在796-468 cm−1区域的强拉曼带被分配给BO4旋转/平移,这使AlO键变形,而位于M1位点的铝原子却没有位移。涉及M1阳离子位移的拉曼主动模式与FGA不相容。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Polarised single crystal Raman spectroscopy of sinhalite, MgAlBO4

Polarised single-crystal Raman spectra for sinhalite have been collected at 80 K over the range 1300-10 cm−1. All 36 of the first-order Raman bands predicted by the factor group analysis (FGA) of the olivine structure type have been observed and assigned. Sinhalite has the smallest unit cell volume of any crystal with the olivine structure and is significantly more distorted than are the silicate olivines. This leads to distortion-related consequences in the vibrational spectra, such as greater wavenumber ranges for each type of mode and reduced Raman intensity for symmetric BO4 modes. Intense Raman bands in the region 796-468 cm−1 are assigned to BO4 rotations/translations which deform the AlO bond without displacement of the aluminium atoms which lie on the M1 sites. Raman-active modes involving M1 cation displacements are incompatible with the FGA.

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