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首页> 外文期刊>日本セラミックス協会学術論文誌 >Microstructure of Rare-Earth-Doped Ceria Prepared by Oxalate Coprecipitation Method
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Microstructure of Rare-Earth-Doped Ceria Prepared by Oxalate Coprecipitation Method

机译:草酸酯共沉淀法制备稀土掺杂二氧化铈的微观结构

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摘要

Rare-earth-doped ceria powders (Ce_(0.8)R_(0.2)o_(1.9), R =Yb, Y, Gd, Sm, Nd and La),prepared by oxalate coprecipitation, were sintered at 1600 deg C in air. All X-ray diffraction patterns of the samples could be indexed as those of a cubic fluorite structure. The measured lattice parameter and density were well explained by the oxygen vacancy model associated with the substitution of a rare-earth-dopant for cerium. The observation of rare-earth-doped ceria ceramics by high-resolution transmission electron microscopy indicated that no crystalline or amorphous secondary phase formed in the grain interior or at grain boundaries. The rare-earth-dopant elements dissolved uniformly in the bulk and at grain boundaries.
机译:稀土掺杂的二氧化铈粉(CE_(0.8)R_(0.2)O_(1.9),R = Yb,y,Gd,Sm,Nd和1a)在空气中以1600℃烧结。 样品的所有X射线衍射图形可以作为立方萤石结构的偏向。 测量的晶格参数和密度是通过与铈替代稀土掺杂剂相关的氧空位模型进行了很好的解释。 通过高分辨率透射电子显微镜观察稀土掺杂的二氧化铈陶瓷,表明在晶粒内部或晶状体边界中形成的结晶或无定形二次相。 稀土掺杂元素均匀地溶于块状和晶界。

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