Department of Physics, College of Science, National University of Defense Technology, Changsha 410073, Hunan, People's Republic of China.
Sci Rep. 2013 Nov 20;3:3272. doi: 10.1038/srep03272.
The structure and phase transition of high-pressure ice are of long-standing interest and challenge, and there is still a huge gap between theoretical and experimental understanding. The quantum nature of protons such as delocalization, quantum tunneling and zero-point motion is crucial to the comprehension of the properties of high-pressure ice. Here we investigated the temperature-induced phase transition and oxygen K-edge x-ray absorption spectra of ice VII, VIII and X using ab initio path-integral molecular dynamics simulations. The tremendous difference between experiments and the previous theoretical predictions is closed for the phase diagram of ice below 300 K at pressures up to 110 GPa. Proton tunneling assists the proton-ordered ice VIII to transform into proton-disordered ice VII where only thermal activated proton-transfer cannot occur. The oxygen K edge with its shift is sensitive to the order-disorder transition, and therefore can be applied to diagnose the dynamics of ice structures.
高压冰的结构和相变一直以来都备受关注,也是一个极具挑战的研究领域,理论和实验之间的理解仍然存在巨大差距。质子的量子特性,如离域、量子隧穿和零点运动,对于理解高压冰的性质至关重要。在此,我们使用从头算路径积分分子动力学模拟研究了冰 VII、VIII 和 X 的温度诱导相变和氧 K 边 X 射线吸收光谱。实验与之前理论预测之间存在巨大差异,这种差异在高达 110GPa 压力下 300K 以下冰的相图中得到了弥补。质子隧穿有助于质子有序冰 VIII 转变为质子无序冰 VII,而在后者中,质子只能通过热激活转移。氧 K 边的位移对有序-无序转变很敏感,因此可以用于诊断冰结构的动力学。