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SEM, EDS and vibrational spectroscopic study of dawsonite NaAl(CO3)(OH)2

机译:片钠铝石NaAl(CO3)(OH)2的SEM,EDS和振动光谱研究

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摘要

In this work we have studied the mineral dawsonite by using a combination of scanning electron microscopy with EDS and vibrational spectroscopy. Single crystals show an acicular habitus forming aggregates with a rosette shape. The chemical analysis shows a phase composed of C, Al, and Na. Two distinct Raman bands at 1091 and 1068 cm are assigned to the CO ν symmetric stretching mode. Multiple bands are observed in both the Raman and infrared spectra in the antisymmetric stretching and bending regions showing that the symmetry of the carbonate anion is reduced and in all probability the carbonate anions are not equivalent in the dawsonite structure. Multiple OH deformation vibrations centred upon 950 cm in both the Raman and infrared spectra show that the OH units in the dawsonite structure are non-equivalent. Raman bands observed at 3250, 3283 and 3295 cm are assigned to OH stretching vibrations. The position of these bands indicates strong hydrogen bonding of the OH units in the dawsonite structure. The formation of the mineral dawsonite has the potential to offer a mechanism for the geosequestration of greenhouse gases.
机译:在这项工作中,我们通过结合扫描电子显微镜,EDS和振动光谱学研究了矿物钠铝矾石。单晶显示针状习性形成具有莲座状的聚集体。化学分析显示出由C,Al和Na组成的相。将在1091和1068 cm处的两个不同的拉曼带分配给COν对称拉伸模式。在反对称拉伸和弯曲区域的拉曼光谱和红外光谱中均观察到多个谱带,表明碳酸盐阴离子的对称性降低,并且碳酸盐阴离子在片钠铝石结构中很可能不相等。拉曼光谱和红外光谱都以950 cm为中心的多次OH变形振动表明,片钠铝石结构中的OH单元是不等价的。在3250、3283和3295 cm处观察到的拉曼带被指定为OH拉伸振动。这些带的位置表明片钠铝石结构中的OH单元具有很强的氢键。钠铝矾石矿物的形成可能为地质隔离温室气体提供一种机制。

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