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High-pressure phase behavior of MnTiO_3: Decomposition of perovskite into MnO and MnTi_2O_5

机译:MnTiO_3的高压相行为:钙钛矿分解为MnO和MnTi_2O_5

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The phase relations and compression behavior of MnTiO_3 perovskite were examined using a laser-heated diamond-anvil cell, X-ray diffraction, and analytical transmission electron microscopy. The results show that MnTiO_3 perovskite becomes unstable and decomposes into MnO and orthorhombic MnTi_2O_5 phases at above 38 GPa and high temperature. This is the first example of ABO_3 perovskite decomposing into AO + AB_2O_5 phases at high pressure. The compression behavior of volume, axes, and the tilting angle of TiO_6 octahedron of MnTiO_3 perovskite are consistent with those of other A~(2+)B~(4+)O_3 perovskites, although no such decomposition was observed in other perovskites. FeTiO_3 is also known to decompose into two phases, instead of transforming into the CaIrO_3-type post-perovskite phase and we argue that one of the reasons for the peculiar behavior of titanate is the weak covalency of the Ti-O chemical bonds.
机译:MnTiO_3钙钛矿的相关系和压缩行为使用激光加热的金刚石-砧室,X射线衍射和分析型透射电子显微镜检查。结果表明,在高于38 GPa的高温下,MnTiO_3钙钛矿变得不稳定,分解为MnO和正交晶MnTi_2O_5相。这是ABO_3钙钛矿在高压下分解为AO + AB_2O_5相的第一个示例。 MnTiO_3钙钛矿的TiO_6八面体的体积,轴和倾斜角的压缩行为与其他A〜(2+)B〜(4+)O_3钙钛矿的压缩行为一致,尽管在其他钙钛矿中未观察到这种分解。还已知FeTiO_3分解成两相,而不是转变成CaIrO_3型钙钛矿后相,并且我们认为钛酸酯特殊行为的原因之一是Ti-O化学键的弱共价性。

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