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首页> 外文期刊>Hyperfine Interactions >Study of phase transition on nanocrystalline (La, Sr)(Mn, Fe)O system using high-pressure M?ssbauer spectroscopy and high-pressure X-ray diffraction
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Study of phase transition on nanocrystalline (La, Sr)(Mn, Fe)O system using high-pressure M?ssbauer spectroscopy and high-pressure X-ray diffraction

机译:高压M?ssbauer光谱和高压X射线衍射研究纳米晶(La,Sr)(Mn,Fe)O系统的相变

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摘要

Pressure-induced structural changes on nano-crystalline La0.8Sr0.2Mn0.8Fe0.2O3 were studied using high-pressure M?ssbauer spectroscopy and high-pressure X-ray diffraction. M?ssbauer measurements up to 10 GPa showed first order transition at 0.52 GPa indicating transformation of Fe4 + to high spin Fe3 + , followed by another subtle transition at 3.7 GPa due to the convergence of two different configurations of Fe into one. High-pressure X-ray diffraction measurements carried up to 4.3 GPa showed similar results at 0.6 GPa as well as 3.6 GPa. Attempts were made to explain the changes at 0.6 GPa by reorientation of grain/grain boundaries due to uniaxial stress generated on the application of pressure. Similarly variation at 3.6 GPa can be explained by orthorhombic to monoclinic transition.
机译:利用高压M研究了纳米晶La0.8 Sr0.2 Mn0.8 Fe0.2 O3 上压力引起的结构变化。 ssbauer光谱学和高压X射线衍射。高达10 GPa的M?ssbauer测量表明,在0.52 GPa处发生了一级转变,表明Fe4 + 向高自旋Fe3 + 转变,随后由于两种不同构型的收敛,在3.7 GPa下又发生了细微转变。铁合一。高达4.3 GPa的高压X射线衍射测量在0.6 GPa和3.6 GPa时显示出相似的结果。尝试解释由于施加压力时产生的单轴应力而导致的晶粒/晶粒边界的重新定向,从而解释了在0.6 GPa时的变化。类似地,在3.6 GPa的变化可以通过斜方晶向单斜晶过渡来解释。

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