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首页> 外文期刊>Journal of Molecular Structure >Infrared and Raman spectroscopic characterization of the carbonate mineral huanghoite - And in comparison with selected rare earth carbonates
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Infrared and Raman spectroscopic characterization of the carbonate mineral huanghoite - And in comparison with selected rare earth carbonates

机译:碳酸盐矿物黄铁矿的红外和拉曼光谱表征-并与精选的稀土碳酸盐进行比较

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摘要

Raman spectroscopy complimented with infrared spectroscopy has been used to study the rare earth based mineral huanghoite with possible formula given as BaCe(CO_3)_2F and compared with the Raman spectra of a series of selected natural halogenated carbonates from different origins including bastnasite, parisite and northupite. The Raman spectrum of huanghoite displays three bands are at 1072, 1084 and 1091 cm~(-1) attributed to the CO_3~(2-) symmetric stretching vibration. The observation of three symmetric stretching vibrations is very unusual. The position of CO_3~(2-) symmetric stretching vibration varies with mineral composition. Infrared spectroscopy of huanghoite show bands at 1319, 1382, 1422 and 1470 cm~(-1). No Raman bands of huanghoite were observed in these positions. Raman spectra of bastnasite, parisite and northupite show a single band at 1433, 1420 and 1554 cm~(-1) assigned to the ν_3 (CO_3)~(2-) antisymmetric stretching mode. The observation of additional Raman bands for the ν_3 modes for some halogenated carbonates is significant in that it shows distortion of the carbonate anion in the mineral structure. Four Raman bands for huanghoite are observed at 687, 704, 718 and 730 cm~(-1)and assigned to the (CO_3)~(2-) ν_2 bending modes. Raman bands are observed for huanghoite at around 627 cm~(-1) and are assigned to the (CO_3)~(2-) ν_4 bending modes. Raman bands are observed for the carbonate ν_4 in phase bending modes at 722 cm~(-1) for bastnasite, 736 and 684 cm~(-1) for parisite, 714 cm~(-1) for northupite. Raman bands for huanghoite observed at 3259, 3484 and 3589 cm~(-1) are attributed to water stretching bands. Multiple bands are observed in the OH stretching region for bastnasite and parisite indicating the presence of water and OH units in their mineral structure. Vibrational spectroscopy enables new information on the structure of huanghoite to be assessed.
机译:拉曼光谱法与红外光谱法相辅相成,已被用于研究稀土基矿物黄铁矿,其可能的分子式为BaCe(CO_3)_2F,并与一系列来自不同来源的精选天然卤代碳酸盐的拉曼光谱进行了比较,这些碳酸盐包括矿渣,黄铁矿和诺苏石。黄土岩的拉曼光谱在1072、1084和1091 cm〜(-1)处有3个能带,这是由于CO_3〜(2-)对称拉伸振动引起的。观察到三个对称的拉伸振动非常不寻常。 CO_3〜(2-)对称拉伸振动的位置随矿物成分的变化而变化。黄ho石的红外光谱显示在1319、1382、1422和1470 cm〜(-1)处的谱带。在这些位置上没有观察到黄铝矿的拉曼带。菱铁矿,绢云母和褐铁矿的拉曼光谱在1433、1420和1554 cm〜(-1)处有一个单一的谱带,分配给ν_3(CO_3)〜(2-)反对称拉伸模式。对于某些卤代碳酸盐,ν_3模式的其他拉曼谱带的观察很重要,因为它显示出矿物结构中碳酸盐阴离子的变形。分别在687、704、718和730 cm〜(-1)处观察到4个针对黄hoite的拉曼谱带,并将其指定为(CO_3)〜(2-)ν_2弯曲模式。在约627 cm〜(-1)处观察到黄土矿的拉曼带,并将其指定为(CO_3)〜(2-)ν_4弯曲模式。碳酸盐ν_4的拉曼谱带在相弯曲模式下观察到,对于菱铁矿为722 cm〜(-1),对于方铁矿为736和684 cm〜(-1),对于褐铁矿为714 cm〜(-1)。在3259、3484和3589 cm〜(-1)处观察到的黄海岩拉曼谱带归因于水拉伸带。在OH伸展区中观察到了多个韧带和头孢母虫的条带,表明矿物质结构中存在水和OH单元。振动光谱法可以评估有关黄铁矿结构的新信息。

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