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Treading in the Limited Stability Regime of Lanthanum Strontium Ferrite - Reduction, Phase Change and Exsolution

机译:在镧系铁铁铁氧体的有限稳定性制度践踏,相变和exolution

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We present an in situ investigation of the iron exsolution from lanthanum strontium ferrite perovskites. Using in situ X-ray diffraction experiments at the synchrotron, the exact onset of exsolution was determined by a change in the lattice parameter before any iron reflexes become visible. For an initially orthorhombic thin film, on the other hand, a phase transition to a fluorite/rock-salt structure is observed to occur during the exsolution. Also, a difference in the iron oxidation states between bulk and surface is found since photoelectron spectroscopy and X-ray absorption spectroscopy both indicate the existence of the Fe(III)/Fe(II) couple in oxidation/reduction cycles, whereas magnetic measurements would suggest Fe(IV)/Fe(III).
机译:我们提出了从镧锶铁素体钙钛矿的铁爆炸的原位调查。在同步rotron的原位X射线衍射实验中,通过在任何铁反射变得可见之前的晶格参数的变化来确定eX的精确开始。另一方面,对于初始正交的薄膜,观察到在exolution期间发生对萤石/岩盐结构的相转变。此外,发现体和表面之间的铁氧化状态的差异,因为光电子谱和X射线吸收光谱都表明氧化/减少循环中的Fe(III)/ Fe(II)耦合的存在,而磁测量将建议Fe(iv)/ Fe(iii)。

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