School of Chemistry, Physics and Mechanical Engineering, Science and Engineering Faculty, Queensland University of Technology, GPO Box 2434, Brisbane, Queensland 4001, Australia.
Spectrochim Acta A Mol Biomol Spectrosc. 2013 Dec;116:491-6. doi: 10.1016/j.saa.2013.07.048. Epub 2013 Aug 2.
We have undertaken a vibrational spectroscopic study of paravauxite the Siglo XX mine, Bustillo Province, northern of Potosí department, Bolivia. This mine is important source for rare and unusual secondary phosphate minerals and is the type locality for a number of rare phosphates such as vauxite, sigloite, metavauxite and for jeanbandyite. The chemical formula of the studied sample was determined as Fe(2+)(0.9)5, Al(0.07)Σ1.02 (Al)2.09 (PO4)1:97 (OH)1.98 · 7.90(H2O). The Raman spectrum is dominated by an intense Raman band at 1020 cm(-1) assigned to the PO4(3-) ν1 symmetric stretching mode. Low intensity Raman bands found at 1058, 1115 and 1148 cm(-1) are assigned to the PO4(3-) ν3 antisymmetric stretching vibrations. Raman bands of paravauxite at 537, 570, 609 and 643 cm(-1) are assigned to the ν4 PO4(3-) bending modes whilst the Raman bands at 393 and 420 cm(-1) are due to the ν2 PO4(3-) bending modes. The Raman spectral profile of paravauxite in the hydroxyl stretching region is broad with component bands resolved at 3086, 3215, 3315, 3421, 3505 and 3648 cm(-1). Vibrational spectroscopy enables the assessment of the molecular structure of paravauxite to be undertaken.
我们对来自玻利维亚波托西省北部布斯特略省西格罗 XX 矿的磷钙铝石进行了振动光谱研究。该矿是罕见和不寻常的次生磷酸盐矿物的重要来源,是许多稀有磷酸盐的产地,如磷钙铝石、硅钙铝石、磷钙铝矾和杰恩钡矿。研究样品的化学公式被确定为 Fe(2+)(0.9)5, Al(0.07)Σ1.02 (Al)2.09 (PO4)1:97 (OH)1.98 · 7.90(H2O)。拉曼光谱主要由一个位于 1020 cm(-1)的强拉曼带主导,该带归因于 PO4(3-) ν1 对称伸缩模式。在 1058、1115 和 1148 cm(-1)处发现的低强度拉曼带归因于 PO4(3-) ν3 反对称伸缩振动。磷钙铝石在 537、570、609 和 643 cm(-1)处的拉曼带归因于 ν4 PO4(3-)弯曲模式,而在 393 和 420 cm(-1)处的拉曼带归因于 ν2 PO4(3-)弯曲模式。磷钙铝石在羟基伸缩区域的拉曼光谱谱带较宽,可分辨出 3086、3215、3315、3421、3505 和 3648 cm(-1)处的组分带。振动光谱使我们能够对磷钙铝石的分子结构进行评估。