Errandonea D, MacLeod S G, Ruiz-Fuertes J, Burakovsky L, McMahon M I, Wilson C W, Ibañez J, Daisenberger D, Popescu C
Departamento de Física Aplicada-ICMUV, Universidad de Valencia, MALTA Consolider Team, Edificio de Investigación, C/Dr. Moliner 50, 46100 Burjassot, Valencia, Spain.
J Phys Condens Matter. 2018 Jul 25;30(29):295402. doi: 10.1088/1361-648X/aacac0. Epub 2018 Jun 6.
The phase diagram of zinc (Zn) has been explored up to 140 GPa and 6000 K, by combining optical observations, x-ray diffraction, and ab initio calculations. In the pressure range covered by this study, Zn is found to retain a hexagonal close-packed (hcp) crystal symmetry up to the melting temperature. The known decrease of the axial ratio (c/a) of the hcp phase of Zn under compression is observed in x-ray diffraction experiments from 300 K up to the melting temperature. The pressure at which c/a reaches [Formula: see text] (≈10 GPa) is slightly affected by temperature. When this axial ratio is reached, we observed that single crystals of Zn, formed at high temperature, break into multiple poly-crystals. In addition, a noticeable change in the pressure dependence of c/a takes place at the same pressure. Both phenomena could be caused by an isomorphic second-order phase transition induced by pressure in Zn. The reported melt curve extends previous results from 24 to 135 GPa. The pressure dependence obtained for the melting temperature is accurately described up to 135 GPa by using a Simon-Glatzel equation: [Formula: see text], where P is the pressure in GPa. The determined melt curve agrees with previous low-pressure studies and with shock-wave experiments, with a melting temperature of 5060(30) K at 135 GPa. Finally, a thermal equation of state is reported, which at room-temperature agrees with the literature.
通过结合光学观测、X射线衍射和从头算计算,对锌(Zn)的相图进行了高达140吉帕和6000开尔文的研究。在本研究涵盖的压力范围内,发现锌在达到熔化温度之前一直保持六方密堆积(hcp)晶体对称性。在从300开尔文到熔化温度的X射线衍射实验中,观察到了锌hcp相在压缩下轴向比(c/a)的已知减小。c/a达到[公式:见正文](≈10吉帕)时的压力受温度影响较小。当达到这个轴向比时,我们观察到高温下形成的锌单晶会破碎成多个多晶体。此外,在相同压力下,c/a的压力依赖性发生了明显变化。这两种现象可能都是由锌中压力诱导的同构二阶相变引起的。报道的熔化曲线扩展了先前从24吉帕到135吉帕的结果。通过使用西蒙 - 格拉策尔方程:[公式:见正文],其中P是吉帕为单位的压力,在高达135吉帕的范围内准确描述了熔化温度的压力依赖性。确定的熔化曲线与先前的低压研究以及冲击波实验一致,在135吉帕时的熔化温度为5060(30)开尔文。最后,报道了一个热状态方程,其在室温下与文献一致。