Glass-liquid transition of water at high pressure

被引:60
作者
Andersson, Ove [1 ]
机构
[1] Umea Univ, Dept Phys, S-90187 Umea, Sweden
关键词
glass transition; pressure-induced amorphization; relaxation; DENSITY AMORPHOUS ICE; HYPERQUENCHED WATER; ENTHALPY; BEHAVIOR; STATE; GPA;
D O I
10.1073/pnas.1016520108
中图分类号
O [数理科学和化学]; P [天文学、地球科学]; Q [生物科学]; N [自然科学总论];
学科分类号
07 ; 0710 ; 09 ;
摘要
The knowledge of the existence of liquid water under extreme conditions and its concomitant properties are important in many fields of science. Glassy water has previously been prepared by hyperquenching micron-sized droplets of liquid water and vapor deposition on a cold substrate (ASW), and its transformation to an ultraviscous liquid form has been reported on heating. A densified amorphous solid form of water, high-density amorphous ice (HDA), has also been made by collapsing the structure of ice at pressures above 1 GPa and temperatures below approximately 140 K, but a corresponding liquid phase has not been detected. Here we report results of heat capacity C-p and thermal conductivity, in situ, measurements, which are consistent with a reversible transition from annealed HDA to ultraviscous high-density liquid water at 1 GPa and 140 K. On heating of HDA, the C-p increases abruptly by (3.4 +/- 0.2) J mol(-1) K-1 before crystallization starts at (153 +/- 1) K. This is larger than the C-p rise at the glass to liquid transition of annealed ASW at 1 atm, which suggests the existence of liquid water under these extreme conditions.
引用
收藏
页码:11013 / 11016
页数:4
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