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論文

Crystal structure and cation distribution of the X-type hexaferrite Sr$$_{2}$$Co$$_{2}$$Fe$$_{28}$$O$$_{46}$$

駒淵 舞*; 漆原 大典*; 浅香 透*; 福田 功一郎*; 大原 高志; 宗像 孝司*; 石川 喜久*

Journal of the Physical Society of Japan, 89(3), p.034601_1 - 034601_5, 2020/03

 被引用回数:0 パーセンタイル:22.58(Physics, Multidisciplinary)

The crystal structure of an X-type hexaferrite Sr$$_{2}$$Co$$_{2}$$Fe$$_{28}$$O$$_{46}$$ was investigated by the X-ray and neutron diffraction methods for a single crystal. Sr$$_{2}$$Co$$_{2}$$Fe$$_{28}$$O$$_{46}$$ has the crystal structure described as a space group $$Roverline{3}m$$ ($$Z = 3$$) and its lattice constants are $$a$$ = 5.9165(2) ${AA}$; and $$c$$ = 84.1395(33) ${AA}$; at 843 K. Co ions are almost localized in the octahedral site ($$9d$$) in the middle of S$$^{*}$$S$$^{*}$$ blocks. In addition, the adjacent octahedral and tetrahedral sites to $$9d$$ site contain the significant number of Co$$^{2+}$$.

論文

High oxide-ion conductivity in Si-deficient La$$_{9.565}$$(Si$$_{5.826}$$[]$$_{0.174}$$)O$$_{26}$$ apatite without interstitial oxygens due to the overbonded channel oxygens

藤井 孝太郎*; 八島 正知*; 日比野 圭祐*; 白岩 大裕*; 福田 功一郎*; 中山 享*; 石沢 伸夫*; 花島 隆泰*; 大原 高志

Journal of Materials Chemistry A, 6(23), p.10835 - 10846, 2018/06

 被引用回数:24 パーセンタイル:70.61(Chemistry, Physical)

Apatite-type rare earth silicates are attractive materials with exhaust application such as solid-oxide fuel cells, due to its extremely high oxide-ion conductivity below 600$$^{circ}$$C. Interstitial (excess) oxygens have been believed to be responsible for the high conductivity in apatite-type materials. On the contrary, the present study clearly reveals the presence of Si vacancies [] in La-rich La$$_{9.565}$$(Si$$_{5.826}$$[]]$$_{0.174}$$)O$$_{26}$$ instead of the interstitial oxygens, by single-crystal neutron and X-ray diffraction analyses, density measurements and ${{it ab initio}}$ electronic calculations.

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