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arXiv 1502.02434cond-mat.mtrl-sciphysics.chem-ph
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EuVO4的高压粉末X射线衍射研究

High-pressure powder x-ray diffraction study of EuVO4

Alka B. Garg, D. Errandonea

摘要:

用同步辐射高压X射线粉末衍射技术研究了正钒酸铕的高压结构行为。角色散X射线衍射测量进行了在室温下高达34.7 GPa使用金刚石砧室,扩大了以前的实验中报道的压力范围。我们证实了锆石-白钨矿相变的发生在6.8 GPa和共存的低压和高压相高达10.1 GPa。此外,在23.4 GPa下发现白钨矿-辉锑铅矿转变的明显证据。该fergusonite结构保持稳定高达34.7 GPa,在目前的测量达到的最高压力。从8.1到12.8 GPa也观察到EuVO 4的部分分解,然而,这一事实并不排除EuVO 4的不同晶体结构的识别。不同阶段的晶体结构已Rietveld细化,并已确定其状态方程(EOS)。计算结果与实验数据和理论计算结果进行了比较。

英文摘要:

The high-pressure structural behavior of europium orthovanadate has been studied using in-situ, synchrotron based, high-pressure x-ray powder diffraction technique. Angle-dispersive x-ray diffraction measurements were carried out at room temperature up to 34.7 GPa using a diamond-anvil cell, extending the pressure range reported in previous experiments. We confirmed the occurrence of zircon-scheelite phase transition at 6.8 GPa and the coexistence of low- and high-pressure phases up to 10.1 GPa. In addition, clear evidence of a scheelite-fregusonite transition is found at 23.4 GPa. The fergusonite structure remains stable up to 34.7 GPa, the highest pressure reached in the present measurements. A partial decomposition of EuVO4 was also observed from 8.1 to 12.8 GPa, however, this fact did not preclude the identification of the different crystal structures of EuVO4. The crystal structures of the different phases have been Rietveld refined and their equations of state (EOS) have been determined. The results are compared with the previous experimental data and theoretical calculations.

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