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arXiv 0708.0028cond-mat.mtrl-sci
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SrMoO4的高压X射线衍射研究及压力诱导的结构变化

High-pressure x-ray diffraction study of SrMoO4 and pressure-induced structural changes

Daniel Errandonea, Ravhi S. Kumar, Xinghua Ma, Chaoyang Tu

摘要:

利用角色散X射线衍射研究了在25 GPa压力下SrMoO 4的结构。在12.2(9)GPa下观察到白钨矿结构的环境相到单斜的富铝尖晶石相的相变,晶胞参数a = 5.265(9)A,b = 11.191(9)A,c = 5.195(5)A,β = 90.9,Z = 4。在相变时没有明显的体积塌陷。未观察到额外的相变,并且在释放压力时恢复初始相,这意味着所观察到的结构修饰是可逆的。报道的过渡似乎是一个铁弹二阶变换产生的结构,是一个单斜畸变的低压相和以前观察到的化合物同构SrMoO 4。提出了一种可能的转变机制,并根据现有的数据和朗道理论讨论了它的性质。最后,报告了状态方程和研究晶体的各向异性压缩性的Sr-O和Mo-O键的压缩方面进行了讨论。

英文摘要:

SrMoO4 was studied under compression up to 25 GPa by angle-dispersive x-ray diffraction. A phase transition was observed from the scheelite-structured ambient phase to a monoclinic fergusonite phase at 12.2(9) GPa with cell parameters a = 5.265(9) A, b = 11.191(9) A, c = 5.195 (5) A, and beta = 90.9, Z = 4 at 13.1 GPa. There is no significant volume collapse at the phase transition. No additional phase transitions were observed and on release of pressure the initial phase is recovered, implying that the observed structural modifications are reversible. The reported transition appeared to be a ferroelastic second-order transformation producing a structure that is a monoclinic distortion of the low-pressure phase and was previously observed in compounds isostructural to SrMoO4. A possible mechanism for the transition is proposed and its character is discussed in terms of the present data and the Landau theory. Finally, the EOS is reported and the anisotropic compressibility of the studied crystal is discussed in terms of the compression of the Sr-O and Mo-O bonds.

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