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The molecular structure of the vanadate mineral mottramite PbCu(VO4)(OH) from Tsumeb, Namibia – a vibrational spectroscopic study

机译:纳米比亚楚梅布的钒酸盐矿物蒙脱石PbCu(VO4)(OH)的分子结构–振动光谱研究

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摘要

We have studied a mineral sample of mottramite PbCu(VO4)(OH) from Tsumeb, Namibia using a combination of scanning electron microscopy with EDX, Raman and infrared spectroscopy. Chemical analysis shows principally the elements V, Pb and Cu. Ca occurs as partial substitution of Pb as well as P and As in substitution to V. Minor amounts of Si and Cr were also observed. The Raman band of mottramite at 829 cm-1, is assigned to the ν1 symmetric (VO-4) ) stretching mode. The complexity of the spectra is attributed to the chemical composition of the Tsumeb mottramite. The ν3 antisymmetric vibrational mode of mottramite is observed as very low intensity bands at 716 and 747 cm-1. The series of Raman bands at 411, 439, 451 cm-1 and probably also the band at 500 cm-1 are assigned to the (VO-4) ν2 bending mode. The series of Raman bands at 293, 333 and 366 cm-1 are attributed to the (VO-4) ) ν4 bending modes. The ν3, ν3 and ν4 regions are complex for both minerals and this is attributed to symmetry reduction of the vanadate unit from Td to Cs.
机译:我们使用扫描电子显微镜,EDX,拉曼光谱和红外光谱技术研究了纳米比亚Tsumeb的芒硝PbCu(VO4)(OH)矿物样品。化学分析主要显示元素V,Pb和Cu。 Ca作为Pb的部分取代以及P和As替代V的一部分。还观察到少量的Si和Cr。在829 cm-1处,蒙脱石的拉曼光谱带被指定为ν1对称(VO-4)拉伸模式。光谱的复杂性归因于Tsumeb硅镁土的化学成分。在716和747 cm-1处观察到的陨石的ν3反对称振动模式为非常低的强度带。将411、439、451 cm-1处的拉曼带系列以及可能还有500 cm-1处的拉曼带分配给(VO-4)ν2弯曲模式。 293、333和366 cm-1处的拉曼谱带系列归因于(VO-4))ν4弯曲模式。两种矿物的ν3,ν3和ν4区域都很复杂,这归因于钒酸盐单元从Td到Cs的对称还原。

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