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首页> 外文期刊>Spectrochimica acta, Part A. Molecular and biomolecular spectroscopy >Assessment of the molecular structure of the borate mineral boracite Mg _3B _7O _(13)Cl using vibrational spectroscopy
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Assessment of the molecular structure of the borate mineral boracite Mg _3B _7O _(13)Cl using vibrational spectroscopy

机译:用振动光谱法评估硼酸盐矿物硼铁矿Mg _3B _7O _(13)Cl的分子结构

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摘要

Boracite is a magnesium borate mineral with formula: Mg _3B _7O _(13)Cl and occurs as blue green, colorless, gray, yellow to white crystals in the orthorhombic - pyramidal crystal system. An intense Raman band at 1009 cm ~(-1) was assigned to the BO stretching vibration of the B _7O _(13) units. Raman bands at 1121, 1136, 1143 cm ~(-1) are attributed to the in-plane bending vibrations of trigonal boron. Four sharp Raman bands observed at 415, 494, 621 and 671 cm ~(-1) are simply defined as trigonal and tetrahedral borate bending modes. The Raman spectrum clearly shows intense Raman bands at 3405 and 3494 cm ~(-1), thus indicating that some Cl anions have been replaced with OH units. The molecular structure of a natural boracite has been assessed by using vibrational spectroscopy.
机译:硼铁矿是一种硼酸镁矿物,分子式为:Mg _3B _7O _(13)Cl,在正交晶-金字塔形晶体系统中以蓝绿色,无色,灰色,黄色至白色晶体形式存在。将B _7O _(13)单元的BO拉伸振动分配给1009 cm〜(-1)的拉曼带。拉曼能带在1121、1136、1143 cm〜(-1)处归因于三角硼的面内弯曲振动。分别在415、494、621和671 cm〜(-1)处观察到四个尖锐的拉曼带,简单地定义为三角形和四面体硼酸盐弯曲模式。拉曼光谱清楚地显示在3405和3494 cm〜(-1)处有很强的拉曼带,因此表明某些Cl阴离子已被OH单元取代。天然硼铁矿的分子结构已经通过使用振动光谱法进行了评估。

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