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Infrared and Raman spectroscopic characterization of the carbonate bearing silicate mineral aerinite – Implications for the molecular structure

机译:含碳酸盐的硅酸盐矿物铜铁矿的红外和拉曼光谱表征–对分子结构的影响

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摘要

The mineral aerinite is an interesting mineral because it contains both silicate and carbonate units which is unusual. It is also a highly colored mineral being bright blue/purple. We have studied aerinite using a combination of techniques which included scanning electron microscopy, energy dispersive X-ray analysis, Raman and infrared spectroscopy. Raman bands at 1049 and 1072 cm−1 are assigned to the carbonate symmetric stretching mode. This observation supports the concept of the non-equivalence of the carbonate units in the structure of aerinite. Multiple infrared bands at 1354, 1390 and 1450 cm−1 supports this concept. Raman bands at 933 and 974 cm−1 are assigned to silicon–oxygen stretching vibrations. Multiple hydroxyl stretching and bending vibrations show that water is in different molecular environments in the aerinite structure.
机译:矿物铜铁矿是一种有趣的矿物,因为它含有硅酸盐和碳酸盐单元,这是不寻常的。它也是一种高度着色的矿物,呈亮蓝色/紫色。我们使用包括扫描电子显微镜,能量色散X射线分析,拉曼光谱和红外光谱在内的多种技术组合研究了堇青石。将1049和1072 cm-1处的拉曼带分配给碳酸盐对称拉伸模式。该观察结果支持了在堇青石结构中碳酸盐单元不等价的概念。 1354、1390和1450 cm-1的多个红外波段支持此概念。 933和974 cm-1处的拉曼谱带被分配给硅氧拉伸振动。多次羟基拉伸和弯曲振动表明,水在硅藻土结构中处于不同的分子环境中。

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