首页> 外文OA文献 >Chemistry, Raman and infrared spectroscopic characterization of the phosphate mineral reddingite: (MnFe)3(PO4)2(H2O,OH)3, a mineral found in lithium-bearing pegmatite
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Chemistry, Raman and infrared spectroscopic characterization of the phosphate mineral reddingite: (MnFe)3(PO4)2(H2O,OH)3, a mineral found in lithium-bearing pegmatite

机译:磷酸盐矿赤铁矿的化学,拉曼光谱和红外光谱表征:(MnFe)3(PO4)2(H2O,OH)3,一种在含锂伟晶岩中发现的矿物

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摘要

Detailed investigation of an intermediate member of the reddingite–phosphoferrite series, using infrared and Raman spectroscopy, scanning electron microcopy and electron microprobe analysis, has been carried out on a homogeneous sample from a lithium-bearing pegmatite named Cigana mine, near Conselheiro Pena, Minas Gerais, Brazil. The determined formula isudud(Mn1.60Fe1.21Ca0.01Mg0.01)∑2.83(PO4)2.12⋅(H2O2.85F0.01)∑2.86ududindicating predominance in the reddingite member. Raman spectroscopy coupled with infrared spectroscopy supports the concept of phosphate, hydrogen phosphate and dihydrogen phosphate units in the structure of reddingite-phosphoferrite. Infrared and Raman bands attributed to water and hydroxyl stretching modes are identified. Vibrational spectroscopy adds useful information to the molecular structure of reddingite–phosphoferrite.
机译:已对米纳斯州Conselheiro Pena附近含锂锂伟晶岩名为Cigana矿的均质样品进行了红外和拉曼光谱,扫描电子显微镜和电子微探针分析的赤铁矿-磷铁酸盐系列中间成员的详细研究。巴西吉拉斯州。所确定的公式为 ud ud(Mn1.60Fe1.21Ca0.01Mg0.01)∑2.83(PO4)2.12⋅(H2O2.85F0.01)∑2.86 ud udred表示赤铁矿成员中的优势。拉曼光谱法和红外光谱法一起支持在红铁矿-磷铁矿结构中使用磷酸根,磷酸氢根和磷酸二氢根单元的概念。确定了归因于水和羟基拉伸模式的红外和拉曼谱带。振动光谱为赤铁矿-磷铁氧体的分子结构增加了有用的信息。

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