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論文

Influences of hydration-dehydration on local structure in layered perovskite LaSr$$_{3}$$Fe$$_{3}$$O$$_{10}$$

八木 祐太朗*; 脇田 雄大*; 籠宮 功*; 松江 郁弥*; 柿本 健一*; 松村 大樹; 米田 安宏

ChemistrySelect (Internet), 7(21), p.e202104575_1 - e202104575_7, 2022/06

 被引用回数:0 パーセンタイル:0(Chemistry, Multidisciplinary)

The layered perovskite LaSr$$_{3}$$Fe$$_{3}$$O$$_{10}$$ (LSF) easily hydrates under ambient air. The hydrated LSF transports hydroxides in the middle-temperature range of 100 $$^circ$$C - 250 $$^circ$$C. This study used X-ray absorption fine structure analysis on normal and hydrated LSF from room temperature to 350 $$^circ$$C to evaluate the relationship between local structures and ion transport characteristics. The H$$_{2}$$O molecules are mainly intercalated into rock-salt interlayers, which are close to the La1 and O3 sites. The generated OH$$^{-}$$ ions are found at O3 sites, which are closer to Sr ions than La ions. The intercalated H$$_{2}$$O molecules and formed OH$$^{-}$$ ions expand the spaces of the rock-salt interlayers. The temperature dependence of the local crystal structure was also studied in this study. According to the findings, the presence of OH$$^{-}$$ ions on the O3 sites, which are closer to Sr ions, plays a significant role in OH$$^{-}$$ transport in the medium temperature range.

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