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高压下 FeVO 的稳定性:X 射线衍射和第一性原理研究。

Stability of FeVO under Pressure: An X-ray Diffraction and First-Principles Study.

机构信息

CONACYT - División de Materiales Avanzados , IPICYT , Camino a la presa San José 20155 , San Luis Potosí , S. L. P. 78216 , Mexico.

Departamento de Física Aplicada-ICMUV , Universidad de Valencia, MALTA Consolider Team, Edificio de Investigación , C. Dr. Moliner 50 , 46100 Burjassot , Spain.

出版信息

Inorg Chem. 2018 Jul 2;57(13):7860-7876. doi: 10.1021/acs.inorgchem.8b00984. Epub 2018 Jun 13.

Abstract

The high-pressure behavior of the crystalline structure FeVO has been studied by means of X-ray diffraction using a diamond-anvil cell and first-principles calculations. The experiments were carried out up to a pressure of 12.3 GPa, until now the highest pressure reached to study an FeVO compound. High-pressure X-ray diffraction measurements show that the triclinic P1̅ (FeVO-I) phase remains stable up to ≈3 GPa; then a first-order phase transition to a new monoclinic polymorph of FeVO (FeVO-II') with space group C2/ m is observed, having an α-MnMoO-type structure. A second first-order phase transition is observed around 5 GPa toward the monoclinic ( P2/ c) wolframite-type FeVO-IV structure, which is stable up to 12.3 GPa in coexistence with FeVO-II'. The unit cell volume reductions for the first and second phase transitions are Δ V = -8.5% and -13.1%. It was observed that phase transitions are irreversible and both high-pressure phases remain stable once the pressure is released. Calculations were performed at the level of the generalized gradient approximation plus Hubbard correction (GGA+ U) and with the hybrid Heyd-Scuseria-Ernzerhof (HSE06) exchange-correlation functional in order to have a good representation of the pressure behavior of FeVO. We found that theoretical results follow the pressure evolution of structural parameters of FeVO, in good agreement with the experimental results. Also, we analyze FeVO-II (orthorhombic Cmcm, CrVO-type structure) and -III (orthorhombic Pbcn, α-PbO-type structure) phases and compare our results with the literature. Going beyond the experimental results, we study some possible post-wolframite phases reported for other compounds and we found a phase transition for FeVO-IV to raspite (monoclinic P2/ c) type structure (FeVO-V) at 36 GPa (Δ V = -8.1%) and a further phase transition to the AgMnO-type (monoclinic P2/ c) structure (FeVO-VI) at 66.5 GPa (Δ V = -3.7%), similar to the phase transition sequence reported for InVO.

摘要

采用金刚石对顶砧高压装置和第一性原理计算,研究了 FeVO 晶体结构的高压行为。实验压力高达 12.3 GPa,这是迄今为止研究 FeVO 化合物的最高压力。高压 X 射线衍射测量表明,三方晶系 P1̅(FeVO-I)相在 ≈3 GPa 以下保持稳定;然后观察到一个一级相变到一个新的单斜晶 FeVO(FeVO-II')多型体,具有α-MnMoO 型结构。在 5 GPa 左右观察到第二个一级相变,向单斜(P2/ c)钨铁矿型 FeVO-IV 结构转变,该结构在与 FeVO-II'共存的情况下在 12.3 GPa 以下稳定。对于第一个和第二个相变,单元体积减少量分别为 Δ V = -8.5%和-13.1%。观察到相变是不可逆的,一旦压力释放,两种高压相都保持稳定。计算是在广义梯度近似加 Hubbard 修正(GGA+ U)和混合 Heyd-Scuseria-Ernzerhof(HSE06)交换相关泛函的水平上进行的,以便对 FeVO 的压力行为进行很好的描述。我们发现,理论结果与 FeVO 的结构参数的压力演化一致,与实验结果吻合良好。此外,我们分析了 FeVO-II(正交晶系 Cmcm,CrVO 型结构)和 -III(正交晶系 Pbcn,α-PbO 型结构)相,并将我们的结果与文献进行了比较。超越实验结果,我们研究了其他化合物报道的一些可能的后钨铁矿相,我们发现 FeVO-IV 向锐钛矿(单斜 P2/ c)型结构(FeVO-V)的相变在 36 GPa(Δ V = -8.1%)和进一步的相变向 AgMnO 型(单斜 P2/ c)结构(FeVO-VI)在 66.5 GPa(Δ V = -3.7%),类似于 InVO 报道的相变序列。

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