Garg Alka B, Errandonea D, Rodríguez-Hernández P, López-Moreno S, Muñoz A, Popescu C
J Phys Condens Matter. 2014 Jul 2;26(26):265402. doi: 10.1088/0953-8984/26/26/265402.
We report a high-pressure experimental and theoretical investigation of the structural properties of zircon-type HoVO4. Angle-dispersive x-ray diffraction measurements were carried out under quasi-hydrostatic and partial non-hydrostatic conditions up to 28 and 23.7 GPa, respectively. In the first case, an irreversible phase transition is found at 8.2 GPa. In the second case, the onset of the transition is detected at 4.5 GPa, a second (reversible) transition is found at 20.4 GPa, and a partial decomposition of HoVO4 was observed. The structures of the different phases have been assigned and their equations of state (EOS) determined. Experimental results have also been compared to theoretical calculations which fully agree with quasi-hydrostatic experiments. Theory also suggests the possibility of another phase transition at 32 GPa; i.e. beyond the pressure limit covered by present experiments. Furthermore, calculations show that deviatoric stresses could trigger the transition found at 20.4 GPa under non-hydrostatic conditions. The reliability of the present experimental and theoretical results is supported by the consistency between the values yielded for transition pressures and EOS parameters by the two methods.
我们报道了对锆石型HoVO₄结构性质的高压实验和理论研究。分别在准静水和部分非静水条件下进行了角度色散X射线衍射测量,压力分别高达28 GPa和23.7 GPa。在第一种情况下,在8.2 GPa处发现了不可逆的相变。在第二种情况下,在4.5 GPa处检测到相变的开始,在20.4 GPa处发现了第二次(可逆)相变,并且观察到HoVO₄发生了部分分解。已确定了不同相的结构及其状态方程(EOS)。实验结果也与理论计算进行了比较,理论计算与准静水实验完全一致。理论还表明在32 GPa处可能发生另一个相变;即超出了当前实验所涵盖的压力极限。此外,计算表明偏应力可能会在非静水条件下引发在20.4 GPa处发现的相变。两种方法得出的转变压力和EOS参数值之间的一致性支持了当前实验和理论结果的可靠性。