Superionic and metallic states of water and ammonia at giant planet conditions

被引:411
作者
Cavazzoni, C
Chiarotti, GL
Scandolo, S
Tosatti, E
Bernasconi, M
Parrinello, M
机构
[1] Ist Nazl Fis Mat, I-34014 Trieste, Italy
[2] Scuola Int Super Studi Avanzati, I-34014 Trieste, Italy
[3] SISSA, I-34014 Trieste, Italy
[4] Abdus Salaam Int Ctr Theoret Phys, I-34014 Trieste, Italy
[5] Univ Milan, Dipartimento Sci Mat, I-20126 Milan, Italy
[6] INFM, I-20126 Milan, Italy
[7] Max Planck Inst Festkorperforsch, D-70569 Stuttgart, Germany
关键词
D O I
10.1126/science.283.5398.44
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 phase diagrams of water and ammonia were determined by constant pressure ab initio molecular dynamic simulations at pressures (30 to 300 gigapascal) and temperatures (300 to 7000 kelvin) of relevance for the middle ice layers of the giant planets Neptune and Uranus. Along the planetary isentrope water and ammonia behave as fully dissociated ionic, electronically insulating fluid phases, which turn metallic at temperatures exceeding 7000 kelvin for water and 5500 kelvin for ammonia. At lower temperatures, the phase diagrams of water and ammonia exhibit a superionic solid phase between the solid and the ionic liquid. These simulations improve our understanding of the properties of the middle ice Layers of Neptune and Uranus.
引用
收藏
页码:44 / 46
页数:3
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