钙钛矿(结构)
材料科学
后钙钛矿
亚稳态
等温过程
矿物学
结晶学
热力学
化学
地质学
物理
地球化学
有机化学
地幔(地质学)
作者
D. P. Dobson,Richard J. McCormack,Simon A. Hunt,Michael W. Ammann,Donald J. Weidner,L. Li,Liping Wang
标识
DOI:10.1180/minmag.2012.076.4.09
摘要
Abstract Stable perovskite and metastable post-perovskite NaCoF3 were deformed in pure-shear geometry in a deformation-DIA press with radiographic monitoring of the sample strain. In isothermal experiments where there was no transformation, post-perovskite was found to be 5 times weaker than perovskite. In temperature-ramping experiments where post-perovskite transformed to perovskite during the deformation experiment the initial post-perovskite sample was 5–10 times weaker than perovskite under comparable conditions and their strengths converged during the transformation, being equal on completion of the transformation. These results confirm recent findings which show that postperovskite is weaker than perovskite, regardless of the prior history of the sample.
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