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Crystal-chemical study of wavellite from Zbirov, Czech Republic

机译:来自捷克共和国Zbirov的波形石的晶体化学研究

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The crystal chemistry of wavellite from Zbirov (Czech Republic), ideally Al_3(PO_4)_2(OH,F)_3?5H_2O, was addressed by means of a multi-methodological approach based on electron microprobe analysis (EMPA) using wave-dispersive spectroscopy, single-crystal X-ray diffraction, powder and single-crystal infrared spectroscopy and Raman spectroscopy. The EMPA data showed the presence of significant F replacing OH in the sample studied. The structure was solved in the Pcmn orthorhombic space group, with the following unit-cell constants: a = 9.6422(7), b = 17.4146(15), c = 7.0094(2) A, V - 1176.98(10) A3. Phosphorus atoms display tetrahedral (PO_4) coordination, while Al cations display octahedral coordination. The mineral framework can be viewed as the repetition of cationic arrays made up of AlO_6 polyhedra, bridged by PO_4 groups and further joined by O-H---O hydrogen bonds. The single-crystal unpolarized Fourier transform infrared (FTIR) spectrum shows combination bands indicating the presence of both OH and H_2O in the structure. Both FTIR and Raman spectra show a broad absorption extending from 3600 to 2800 cm~(-1) resulting from the overlapping of several components due to the water molecules and the OH group. The frequencies observed are comparable to those expected on the basis of the Libowitzky relationship for the range of D-K---A bond systems in the structure.
机译:通过基于电子微探针分析(EMPA)的多色方法,采用波色散光谱法,研究了Zbirov(捷克共和国)的波形石的结晶化学,理想情况下为Al_3(PO_4)_2(OH,F)_3?5H_2O ,单晶X射线衍射,粉末和单晶红外光谱以及拉曼光谱。 EMPA数据表明,在研究的样品中存在大量的F取代OH。在具有以下晶胞常数的Pcmn正交空间组中解析了结构:a = 9.6422(7),b = 17.4146(15),c = 7.0094(2)A,V-1176.98(10)A3。磷原子显示四面体(PO_4)配位,而Al阳离子显示八面体的配位。矿物骨架可以看作是由AlO_6多面体组成的阳离子阵列的重复,这些阳离子阵列由PO_4基团桥接,并进一步由O-H--O氢键连接。单晶非偏振傅立叶变换红外(FTIR)光谱显示组合带,表明结构中同时存在OH和H_2O。 FTIR和拉曼光谱都显示出从3600到2800 cm-1(-1)的宽吸收,这归因于由于水分子和OH基团的几种组分的重叠。在结构中D-K --- A键体系的范围内,观察到的频率与基于Libowitzky关系所预期的频率相当。

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