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首页> 外文期刊>Journal of Colloid and Interface Science >XPS study of the major minerals in bauxite: Gibbsite, bayerite and (pseudo-)boehmite
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XPS study of the major minerals in bauxite: Gibbsite, bayerite and (pseudo-)boehmite

机译:XPS研究铝土矿中的主要矿物:菱铁矿,钙铝石和(假)勃姆石

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摘要

Synthetic corundum (Al2O3), gibbsite (Al(OH)(3)), bayerite (Al(OH)(3)), boehmite (AlO(OH)) and pseudoboehmite (AlO(OH)) have been studied by high resolution XPS. The chemical compositions based on the XPS survey scans were in good agreement with the expected composition. High resolution A12p scans showed no significant changes in binding energy, with all values between 73.9 and 74.4 eV. Only bayerite showed two transitions, associated with the presence of amorphous material in the sample. More information about the chemical and crystallographic environment was obtained from the 0 Is high resolution spectra. Here a clear distinction could be made between oxygen in the crystal structure, hydroxyl groups and adsorbed water. Oxygen in the crystal structure was characterised by a binding energy of about 530.6 eV in all minerals. Hydroxyl groups, present either in the crystal structure or on the surface, exhibited binding energies around 531.9 eV, while water on the surface showed binding energies around 533.0 eV. A distinction could be made between boehmite and pseudoboehmite based on the slightly lower ratio of oxygen to hydroxyl groups and water in pseudoboehmite. (c) 2005 Elsevier Inc. All rights reserved.
机译:通过高分辨率XPS研究了合成刚玉(Al2O3),菱镁石(Al(OH)(3)),三钠铝石(Al(OH)(3)),勃姆石(AlO(OH))和假勃姆石(AlO(OH)) 。根据XPS调查扫描得出的化学成分与预期成分非常吻合。高分辨率A12p扫描显示结合能没有明显变化,所有值在73.9和74.4 eV之间。只有三钠铝石显示出两个转变,这与样品中无定形物质的存在有关。从0 Is高分辨率光谱获得了有关化学和晶体学环境的更多信息。在此可以对晶体结构中的氧,羟基和吸附的水进行明确区分。晶体结构中的氧的特征是所有矿物中的结合能约为530.6 eV。存在于晶体结构或表面上的羟基显示出约531.9 eV的结合能,而表面上的水显示出约533.0 eV的结合能。基于假勃姆石中氧与羟基和水的比率稍低,可以将勃姆石和假勃姆石区分开。 (c)2005 Elsevier Inc.保留所有权利。

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