首页> 外文会议>12th International Clay Conference Jul 22-28, 2001 Bahia Blanca, Argentina >FT-Raman spectroscopy and SEM of gibbsite, bayerite, boehmite and diaspore in relation to the characterization of bauxite
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FT-Raman spectroscopy and SEM of gibbsite, bayerite, boehmite and diaspore in relation to the characterization of bauxite

机译:三水铝石,三水铝石,勃姆石和水铝石的FT-拉曼光谱和SEM与铝土矿的表征有关

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Gibbsite, bayerite, boehmite and diaspore were investigated using FT-Raman spectroscopy in conjunction with scanning electron microscopy (SEM) in order to provide information for the characterization of bauxite. The Raman spectrum of gibbsite shows four strong, sharp bands at 3617, 3522, 3433 and 3364 cm~(-1) and the spectrum of bayerite shows seven bands at 3664, 3652, 3552, 3542, 3450, 3438, and 3420 cm~(-1) in the hydroxyl stretching region. Four broad and weak bands are observed at 3371, 3220, 3085 and 2989 cm~(-1) for boehmite, and five broad bands are observed at 3445, 3363, 3226, 3119 and 2936 cm~(-1) for diaspore in the hydroxyl stretching region. The hydroxyl stretching bands are related to the surface structure of these minerals. The Raman spectra of bayerite, gibbsite and diaspore are complex while the Raman spectrum of boehmite only shows three major bands in the hydroxyl deformation and water bending, and low frequency regions. These bands are assigned to hydroxyl deformation and translational, and Al-O modes of the alumina phases. The present results in relation to the characterization of bauxite are interpreted.
机译:使用傅立叶变换拉曼光谱结合扫描电子显微镜(SEM)研究了菱镁矿,三羟铝石,勃姆石和辉石,以提供表征铝土矿的信息。三水铝石的拉曼光谱在3617、3522、3433和3364 cm〜(-1)处显示出四个强而尖的带,而三羟铝石的光谱在3664、3652、3552、3542、3450、3438和3420 cm〜处显示了七个带。 (-1)在羟基拉伸区域。在勃姆石中,在3371、3220、3085和2989 cm〜(-1)处观察到四个宽带和弱带,而在渗铝中,在3445、3363、3226、3119和2936 cm〜(-1)处观察到五个宽带。羟基拉伸区。羟基拉伸带与这些矿物质的表面结构有关。钙铝石,三水铝石和水辉石的拉曼光谱很复杂,而勃姆石的拉曼光谱仅在羟基变形和水弯曲以及低频区域显示三个主要谱带。这些条带分配给氧化铝相的羟基变形和平移以及Al-O模式。解释了有关铝土矿表征的现有结果。

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