Cavazzoni C, Chiarotti G L, Scandolo S, Tosatti E, Bernasconi M, Parrinello M
Istituto Nazionale per la Fisica della Materia (INFM) and International School for Advanced Studies (SISSA), Via Beirut 4, I-34014 Trieste, Italy.
Science. 1999 Jan 1;283(5398):44-6. doi: 10.1126/science.283.5398.44.
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.
通过在与巨行星海王星和天王星中间冰层相关的压力(30至300吉帕斯卡)和温度(300至7000开尔文)下进行恒压从头算分子动力学模拟,确定了水和氨的相图。沿着行星等熵线,水和氨表现为完全离解的离子性、电子绝缘流体相,在温度超过7000开尔文(水)和5500开尔文(氨)时变为金属相。在较低温度下,水和氨的相图在固体和离子液体之间呈现出超离子固相。这些模拟增进了我们对海王星和天王星中间冰层性质的理解。