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首页> 外文期刊>Journal of Geosciences >Molecular structure of the phosphate mineral koninckite - a?vibrational spectroscopic?study
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Molecular structure of the phosphate mineral koninckite - a?vibrational spectroscopic?study

机译:磷酸盐矿物孔雀石的分子结构-振动光谱研究

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摘要

We have undertaken a?study of the mineral koninckite from Litoxc5xa1ice (Czech Republic), a?hydrated ferric phosphate, using a?combination of scanning electron microscopy with electron probe micro-analyzer (wavelength-dispersive spectroscopy) and vibrational spectroscopy. Chemical analysis shows that studied koninckite is a?pure phase with an empirical formula?Fe3+0.99(PO4)1.00xe2x88x992.75 H2O, with minor enrichment in Al, Ca, Ti, Si, Zn, and K (averages 0.00X apfu). Raman bands and shoulders at 3495, 3312, 3120, and 2966 cm-1 and infrared bands and shoulders at 3729, 3493, 3356, 3250, 3088, 2907, and 2706 cm-1 are assigned to the xcexbd OH stretching of structurally distinct differently hydrogen bonded water molecules, A?Raman band at 1602 cm-1 and shoulders at 1679, 1659, 1634, and 1617 cm-1 and infrared bands at 1650 and 1598 cm-1 are assigned to the ?2 (?) H2O bending vibrations of structurally distinct differently hydrogen bonded water molecules. Raman shoulders at 1576, 1554, 1541, 1532, and 1520 cm-1 and infrared shoulders at 1541 and 1454 cm-1 may be probably connected with zeolitically bonded water molecules located in the channels. Raman bands and shoulders at 1148, 1132, 1108, 1063, 1048, and 1015 cm-1 and an infrared band and shoulders at 1131, 1097, 1049, and 1017 cm-1 are assigned to the ?3 PO43- triply degenerate antisymmetric stretching vibrations. A?Raman band and a?shoulder at 994 and 970 cm-1, respectively, and an infrared band and a?shoulder at 978 and 949 cm-1, respectively, are assigned to the ?1 PO43- symmetric stretching vibrations. Infrared shoulders at 873, 833, and 748 cm-1 are assigned to libration modes of water molecules. Raman bands and shoulders at 670, 648, 631, 614, 600, 572, and 546 cm-1 and infrared bands at 592 and 534 cm-1 are assigned to the ?4 (?) PO43- triply degenerate out-of-plane bending vibrations; weak band at 570 cm-1 may coincide with the ? Fe-O bending vibration. Raman bands and shoulders at 453, 443, 419, and 400 cm-1 are assigned to the ?2 (?) PO43- doubly degenerate in-plane bending vibrations. Raman bands at 385, 346, 324, 309, 275, 252, and 227 cm-1 are assigned to the ? Fe-O stretching vibrations in FeO6 octahedra. Raman bands at 188, 158, 140, 112, 89, and 73 cm-1 are assigned to lattice?vibrations.
机译:我们使用扫描电子显微镜与电子探针显微分析仪(波长色散光谱法)和振动光谱法的组合,对来自Lito xc5 xa1ice(捷克共和国)的水合磷酸铁矿进行了研究。化学分析表明,研究的孔雀石为纯相,经验公式为Fe3 + 0.99(PO4)1.00 xe2 x88 x992.75 H2O,其中Al,Ca,Ti,Si,Zn和K(平均0.00 apfu)。在3495、3312、3120和2966 cm-1处的拉曼带和肩部以及在3729、3493、3356、3250、3088、2907和2706 cm-1处的红外带和肩部被指定为 xce xbd OH拉伸在结构上截然不同的氢键水分子,分别将1602 cm-1处的A3拉曼谱带和1679、1659、1634和1617 cm-1处的肩峰以及1650和1598 cm-1处的红外谱带分配给了α2(?)。结构不同的氢键水分子的H2O弯曲振动。 1576、1554、1541、1532和1520 cm-1处的拉曼肩部和1541和1454 cm-1处的红外肩部可能与位于通道中的沸石键合水分子相连。将拉曼谱带和肩部分别位于1148、1132、1108、1063、1048和1015 cm-1处,并将红外谱带和肩部分别位于1131、1097、1049和1017 cm-1处,以?3 PO43进行三次简并反对称拉伸振动。分别在994和970 cm-1处的λ拉曼谱带和λ肩,以及在978和949 cm-1处的红外谱带和λ肩被分配给λ1PO43对称拉伸振动。将873、833和748 cm-1处的红外肩膀分配给水分子的释放模式。分别在670、648、631、614、600、572和546 cm-1处的拉曼谱带和肩部以及在592和534 cm-1处的红外谱带被分配给π4(π)PO43-平面外三次退化弯曲振动; 570 cm-1处的弱带可能与? Fe-O弯曲振动。拉曼带和肩带分别在453、443、419和400 cm-1处分配给α2(α)PO43-双重简并面内弯曲振动。将385、346、324、309、275、252和227 cm-1的拉曼带分配给? FeO6八面体中的Fe-O拉伸振动。将188、158、140、112、89和73 cm-1处的拉曼带分配给晶格振动。

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