首页> 外文OA文献 >Raman spectroscopic study of the uranyl minerals vanmeersscheite U(OH)4(UO2)3(PO4)2(OH)2.4H2O and arsenouranylite Ca(UO2)(UO2)3(AsO4)2(OH)2.(OH)2.6H2O
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Raman spectroscopic study of the uranyl minerals vanmeersscheite U(OH)4(UO2)3(PO4)2(OH)2.4H2O and arsenouranylite Ca(UO2)(UO2)3(AsO4)2(OH)2.(OH)2.6H2O

机译:拉曼光谱研究了铀矿矿物中的凡尔赛石U(OH)4 (UO2)3(PO4)2(OH)2 .4H2O和亚砷铝石Ca(UO2)(UO2)3(AsO4)2(OH)2。 (OH)2.6水

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摘要

Raman and infrared spectra of secondary uranyl phosphate vanmeersscheite and Raman spectrum of secondary uranyl arsenate arsenuranylite were recorded and interpreted and the spectra related to the structure of the minerals. Observed bands were attributed to the stretching and bending vibrations of uranyl, phosphate and/or arsenate units and OH (H2O and OH-) units. Phosphuranylite sheet topology is characteristic for both minerals. U-O bond lengths in uranyl were calculated from the spectra and compared with those inferred for vanmeersscheite from the X-ray single crystal structure analysis. O-H...O hydrogen bonds in both minerals were also inferred using the Libowitzky empirical relation.
机译:记录并解释了仲铀酰磷酸铀锰铁矿的拉曼光谱和红外光谱,以及砷酸铀酰仲砷锰矿的拉曼光谱和与矿物结构有关的光谱。观察到的谱带归因于铀酰,磷酸根和/或砷酸根和OH(H2O和OH-)单元的拉伸和弯曲振动。两种矿物均具有辉绿岩片状拓扑。从光谱中计算出铀酰中的U-O键长度,并将其与X射线单晶结构分析推断出的钒钙锰矿的长度进行比较。两种矿物中的O-H ... O氢键也可以通过Libowitzky经验关系来推断。

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