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Correlation between crystallite sizxes and microstrains in TiO_2 nanopowders

机译:TiO_2纳米粉体中晶粒尺寸与微应变的相关性

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Nanopowders of TiO_2 doped with by V, Nb, Ta were obtained by laser-induced pyrolysis. The profiles of the diffraction peaks were Fourier analysed with a single-peak method and the microtructural parameters (average crysallite size) and <ε~2>~1/2 (mean-square root microstrain) were estimated. A linear correlation between <ε~2>~1/2 and 1/ was observed in both aatase and rutile phases. For a given crystallite size, the microstrains as well as the dispersion of data were larger in anatase then in rutile. Indeed, one of the factos inducing the anatase-to-rutile transformation may be the presence of larer microstrains in anatase. In rutile, the high correlation found between <ε~2>~1/2 and 1/ suggests tat in this phade the microsrains present in the structre are due only to the geometricla constraints of the suface. Indeed, for infinite crystallite size no microstrains are expected. In anatase, microsrains depend also on the specific cation present in the crsytallite.
机译:通过激光诱导的热解,获得了掺有V,Nb,Ta的TiO_2纳米粉体。用单峰方法对衍射峰的轮廓进行傅里叶分析,并估计微结构参数(平均冰晶石尺寸)和<ε〜2>〜1/2(均方根微应变)。在锐钛矿相和金红石相中均观察到ε2〜1/2 M与1 / M之间的线性相关。对于给定的微晶尺寸,锐钛矿中的微应变以及数据的分散度大于金红石中的。实际上,诱导从锐钛矿到金红石转化的事实之一可能是锐钛矿中存在较大的微菌株。在金红石中,在<ε〜2>〜1/2 和1 / 之间发现的高度相关性表明,在该阶段中,存在于结构中的微应变仅是由于表面的几何约束。实际上,对于无限的微晶尺寸,没有微应变是可以预期的。在锐钛矿中,微应变也取决于存在于冰晶石中的特定阳离子。

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