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Relationship between Crystalline Size and Bond Lengths in Boehmite

机译:勃姆石中晶体尺寸与键长之间的关系

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Boehmite with a crystallite size between 1 and 27 nm was prepared by annealing a boehmite precipitate under hydrothermal conditions at different temperatures. The crystalline structure, measured with X-ray powder diffraction, was refined with the Rietveld method. From the refinement bond lengths and bond angles between oxygen and aluminum atoms were calculated, which revealed that boehimite bond lengths atoms were calculated, which revealed that boehmite bond lengths and local symmetry depended on crystal dimensions. When boehmite's crystallite size decreased, Al-OH interaction increased, and the local octahedral symmetry tended to be tetrahedral. The hyrogen bond, sustaining boehmite's crystalline structure, and the bonds between oxygen atoms and hydroxyls inside the octahedra double layers, building the crystalline structure, became weaker as crystallite size decreased, which could explain why boehmite's transformation temperature into a transitional alumina also decreased with crystallite size. Alumina crystallite size also depended of the corresponding size of boehmite. It was shown that desorbed water from annealed samples came from the crystal surface and not from the bulk.
机译:通过在水热条件下在不同温度下退火勃姆石沉淀来制备微晶尺寸在1-27nm之间的勃姆石。用Rietveld方法精制通过X射线粉末衍射测量的晶体结构。通过精炼键长和氧原子与铝原子之间的键角,可以计算出勃姆石键长原子,这表明勃姆石键长和局部对称性取决于晶体尺寸。当勃姆石的微晶尺寸减小时,Al-OH相互作用增加,并且局部八面体对称趋向于四面体。维持勃姆石晶体结构的氢键以及八面体双层内部的氧原子与羟基之间的键(构成晶体结构)随着晶粒尺寸的减小而变弱,这可以解释为什么勃姆石向过渡氧化铝的转化温度也随晶粒的降低而降低尺寸。氧化铝微晶尺寸也取决于勃姆石的相应尺寸。结果表明,退火样品的解吸水来自晶体表面,而不是来自块体。

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