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Dependence of boehmite thermal evolution on its atom bond lengths and crystallite size

机译:勃姆石热演化对其原子键长和微晶尺寸的依赖性

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The thermal properties of boehmite with a crystallite size between 1 and 27 nm were analyzed by thermogravimetry and differential thermal analysis, and correlated with its crystallography, crystallite morphology, and the atom bond lengths determined by refining its crystalline structure with the Rietveld method. Boehmite's thermal evolution depended on atom bond lengths: the dehydratation temperature was determined by the interaction between an aluminum atom and the oxygen atom of hydroxyl. After dehydratation, the number of hydroxyls in crystals was larger than expected from stoichiometry, because oxygen atoms on crystal surfaces perpendicular to the (020) plane reacted with hydrogen and hydroxyls in environment. The transition temperature from boehmite into #gamma#-alumina was determined by the hydrogen bond in boehmite. The transformation temperature from transitional aluminas into #alpha#-Al_2O_3 also varied with boehmite's crystallite size; however, it was not determined by the amount of hydroxyls in transitional aluminas, but probable by the aluminum-oxygen bonds in boehmite.
机译:通过热重分析和差热分析来分析微晶尺寸为1至27 nm的勃姆石的热性能,并将其与晶体学,微晶形态以及通过Rietveld方法精炼其晶体结构所确定的原子键长相关。勃姆石的热演化取决于原子键的长度:脱水温度由铝原子和羟基的氧原子之间的相互作用决定。脱水后,晶体中的羟基数量比化学计量法预期的要多,这是因为垂直于(020)平面的晶体表面上的氧原子与环境中的氢和羟基反应。从勃姆石到#γ#-氧化铝的转变温度由勃姆石中的氢键确定。从过渡氧化铝到#alpha#-Al_2O_3的转变温度也随勃姆石的微晶尺寸而变化。然而,它不是由过渡氧化铝中的羟基含量决定的,而是由勃姆石中的铝-氧键决定的。

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