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希腊劳里翁地区埃斯佩兰萨矿的锌羟碳矾Zn3(CO3,SO4)(OH)4的扫描电子显微镜、能量色散X射线光谱、拉曼光谱和红外光谱研究

SEM, EDX and Raman and infrared spectroscopic study of brianyoungite Zn3(CO3,SO4)(OH)4 from Esperanza Mine, Laurion District, Greece.

作者信息

Frost Ray L, López Andrés, Wang Lina, Scholz Ricardo, Sampaio Ney Pinheiro

机构信息

School of Chemistry, Physics and Mechanical Engineering, Science and Engineering Faculty, Queensland University of Technology, GPO Box 2434, Brisbane, Queensland 4001, Australia.

School of Chemistry, Physics and Mechanical Engineering, Science and Engineering Faculty, Queensland University of Technology, GPO Box 2434, Brisbane, Queensland 4001, Australia.

出版信息

Spectrochim Acta A Mol Biomol Spectrosc. 2015 Oct 5;149:279-84. doi: 10.1016/j.saa.2015.04.013. Epub 2015 Apr 23.

Abstract

The mineral brianyoungite, a carbonate-sulphate of zinc, has been studied by scanning electron microscopy (SEM) with chemical analysis using energy dispersive spectroscopy (EDX) and Raman and infrared spectroscopy. Multiple carbonate stretching modes are observed and support the concept of non-equivalent carbonate units in the brianyoungite structure. Intense Raman band at 1056 cm(-1) with shoulder band at 1038 cm(-1) is assigned to the CO3(2-) ν1 symmetric stretching mode. Two intense Raman bands at 973 and 984 cm(-1) are assigned to the symmetric stretching modes of the SO4(2-) anion. The observation of two bands supports the concept of the non-equivalence of sulphate units in the brianyoungite structure. Raman bands at 704 and 736 cm(-1) are assigned to the CO3(2-) ν4 bending modes and Raman bands at 507, 528, 609 and 638 cm(-1) are assigned to the CO3(2-) ν2 bending modes. Multiple Raman and infrared bands in the OH stretching region are observed, proving the existence of water and hydroxyl units in different molecular environments in the structure of brianyoungite. Vibrational spectroscopy enhances our knowledge of the molecular structure of brianyoungite.

摘要

矿物布氏锌矿,一种锌的碳酸盐 - 硫酸盐,已通过扫描电子显微镜(SEM)结合能谱分析(EDX)进行化学分析以及拉曼光谱和红外光谱进行了研究。观察到多个碳酸盐伸缩振动模式,支持了布氏锌矿结构中存在不等价碳酸盐单元的概念。在1056 cm(-1)处的强拉曼峰以及在1038 cm(-1)处的肩峰归属于CO3(2-) ν1对称伸缩振动模式。在973和984 cm(-1)处的两个强拉曼峰归属于SO4(2-)阴离子的对称伸缩振动模式。这两个峰的观察结果支持了布氏锌矿结构中硫酸盐单元不等价的概念。在704和736 cm(-1)处的拉曼峰归属于CO3(2-) ν4弯曲振动模式,在507、528、609和638 cm(-1)处的拉曼峰归属于CO3(2-) ν2弯曲振动模式。在OH伸缩振动区域观察到多个拉曼和红外峰,证明了布氏锌矿结构中不同分子环境下存在水和羟基单元。振动光谱增强了我们对布氏锌矿分子结构的认识。

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