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A vibrational spectroscopic study of hydrated Fe3+ hydroxyl-sulphates; polymorphic minerals butlerite and parabutlerite

机译:水合Fe3 +羟基硫酸盐的振动光谱研究;多态矿物钙钠钙石和钙钠钙石

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摘要

Raman and infrared spectra of two polymorphous minerals with the chemical formula Fe3+(SO4)(OH)•2H2O, monoclinic butlerite and orthorhombic parabutlerite, are studied and the spectra assigned. Observed bands are attributed to the (SO4)2- stretching and bending vibrations, hydrogen bonded water molecules, stretching and bending vibrations of hydroxyl ions, water librational modes, Fe-O and Fe-OH stretching vibrations, Fe-OH bending vibrations and lattice vibrations. The O-H...O hydrogen bond lengths in the structures of both minerals are calculated from the wavenumbers of the stretching vibrations. One symmetrically distinct (SO4)2- unit in the structure of butlerite and two symmetrically distinct (SO4)2- units in the structure of parabutlerite are inferred from the Raman and infrared spectra. This conclusion agrees with the published crystal structures of both mineral phases.
机译:研究了两种化学式为Fe3 +(SO4)(OH)·2H2O的多晶矿物的拉曼光谱和红外光谱,并确定了光谱。观察到的谱带归因于(SO4)2-的拉伸和弯曲振动,氢键水分子,氢氧根离子的拉伸和弯曲振动,水自由模式,Fe-O和Fe-OH的拉伸振动,Fe-OH的弯曲振动和晶格振动。两种矿物的结构中的O-H ... O氢键长度是由拉伸振动的波数计算得出的。从拉曼光谱和红外光谱中推断出一种在堇青石结构中的对称对称的(SO 4)2-单元,以及在一个偏硅藻土结构中的对称对称的两个(SO 4)2-单元。该结论与两种矿物相的已公开晶体结构一致。

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