金刚石顶砧
正交晶系
钙钛矿(结构)
化学
单斜晶系
体积模量
后钙钛矿
相变
结晶学
环境压力
相(物质)
粉末衍射
衍射
X射线晶体学
同步加速器
硅酸盐钙钛矿
热力学
晶体结构
光学
地质学
有机化学
物理
地幔(地质学)
古生物学
作者
Camilla Hjort Kronbo,Emma Ehrenreich-Petersen,Martin Ottesen,Francesca Menescardi,Davide Ceresoli,Martin Bremholm
出处
期刊:Inorganic Chemistry
[American Chemical Society]
日期:2022-11-16
卷期号:61 (48): 19088-19096
被引量:2
标识
DOI:10.1021/acs.inorgchem.2c02471
摘要
Using a recently developed method for in situ high-pressure, laser heating experiments in diamond anvil cells, we obtained a novel post-perovskite phase of SrOsO3. The phase transition from perovskite SrOsO3 was induced at 44 GPa and 1350 K in a diamond anvil cell and characterized with synchrotron powder X-ray diffraction. The newly obtained post-perovskite is quenchable and Le Bail refinements under ambient conditions yielded the unit cell parameters: a = 3.152(9) Å, b = 10.82(2) Å, c = 7.27(1) Å, V = 248.1(1) Å3. In addition, the compression of perovskite SrOsO3 at ambient temperature was investigated up to 66 GPa in a diamond anvil cell using synchrotron powder X-ray diffraction. The compression at ambient temperature showed that pressure alone does not induce the first-order phase transition to the post-perovskite structure. However, at 36 GPa, a continuous phase transition to monoclinic (P21/n) symmetry was detected, persistent up to 58 GPa, where the perovskite transitioned back to orthorhombic (Pbnm) symmetry. Fitting a third-order Birch-Murnaghan equation of state to the obtained P-V data for perovskite SrOsO3 yielded a bulk modulus of K0 = 187.4(15) GPa. Density functional theory calculations were performed to support the experimental findings in the compression study at ambient temperature. This work shows that transformations to the post-perovskite structure can be obtained for a wider range of perovskites than simple empirical rules otherwise suggest.
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