Weck Gunnar, Queyroux Jean-Antoine, Ninet Sandra, Datchi Frédéric, Mezouar Mohamed, Loubeyre Paul
CEA, DAM, DIF, F-91297 Arpajon, France.
Université Paris Saclay, Lab Matiere Condit Extremes, CEA, F-91680 Bruyeres Le Chatel, France.
Phys Rev Lett. 2022 Apr 22;128(16):165701. doi: 10.1103/PhysRevLett.128.165701.
Structural transformation of hot dense water ice is investigated by combining synchrotron x-ray diffraction and a laser-heating diamond anvil cell above 25 GPa. A transition from the body-centered-cubic (bcc) to face-centered-cubic (fcc) oxygen atoms sublattices is observed from 57 GPa and 1500 K to 166 GPa and 2500 K. That is the structural signature of the transition to fcc superionic (fcc SI) ice. The sign of the density discontinuity at the transition is obtained and a phase diagram is disclosed, showing an extended fcc SI stability field. Present data also constrain the stability field of the bcc superionic (bcc SI) ice up to 100 GPa at least. The current understanding of warm dense water ice based on ab initio simulations is discussed in the light of present data.
通过结合同步加速器X射线衍射和激光加热金刚石对顶砧池,在25吉帕以上的压力下研究了热致密水冰的结构转变。观察到从57吉帕和1500开尔文到166吉帕和2500开尔文,体心立方(bcc)氧原子亚晶格向面心立方(fcc)氧原子亚晶格的转变。这是向fcc超离子(fcc SI)冰转变的结构特征。获得了转变时密度不连续的符号,并揭示了相图,显示出扩展的fcc SI稳定场。目前的数据还至少将bcc超离子(bcc SI)冰的稳定场限制到了100吉帕。根据目前的数据讨论了基于从头算模拟对温暖致密水冰的当前理解。