金红石的变形与显微组织

M. Blanchin, L. Bursill, C. Lafage
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引用次数: 17

摘要

对金红石的力学性能进行了研究,特别是在温度变化(纯金红石)、内在非化学计量(低氧压下还原的纯金红石)和外在非化学计量(掺杂铬和氧化铝的金红石)下压缩弹性极限的行为。得到的数值范围很广,这可以通过属于{101}和{110}滑移系统的位错与杂质、非化学计量的小而扩展的缺陷和沉淀的相互作用来理解。中分辨率透射电子显微镜和高分辨率电子显微镜已被用于将力学行为与微观结构联系起来。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Deformation and microstructure of rutile
Studies of the mechanical properties of rutiles are described, in particular the behaviour of the elastic limit under compression with respect to variations in temperature (pure rutile), intrinsic non-stoichiometry (pure rutile reduced under low oxygen pressure) and extrinsic non-stoichiometry (rutile doped with chromia and alumina). A wide range of values is obtained, which may be understood in terms of the interaction of dislocations belonging to the slip systems {101} <1̄01> and {110} <001> with impurities, non-stoichiometric small and extended defects and precipitates. Transmission electron microscopy at medium resolution as well as high-resolution electron microscopy have been used to relate mechanical behaviour with microstructure.
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