Morales Miguel A, Schwegler Eric, Ceperley David, Pierleoni Carlo, Hamel Sebastien, Caspersen Kyle
Department of Physics, National Center of Supercomputing Applications, and Institute of Condensed Matter Theory, University of Illinois at Urbana-Champaign, Urbana, IL 61801, USA.
Proc Natl Acad Sci U S A. 2009 Feb 3;106(5):1324-9. doi: 10.1073/pnas.0812581106. Epub 2009 Jan 26.
The properties of hydrogen-helium mixtures at Mbar pressures and intermediate temperatures (4000 to 10000 K) are calculated with first-principles molecular dynamics simulations. We determine the equation of state as a function of density, temperature, and composition and, using thermodynamic integration, we estimate the Gibbs free energy of mixing, thereby determining the temperature, at a given pressure, when helium becomes insoluble in dense metallic hydrogen. These results are directly relevant to models of the interior structure and evolution of Jovian planets. We find that the temperatures for the demixing of helium and hydrogen are sufficiently high to cross the planetary adiabat of Saturn at pressures approximately 5 Mbar; helium is partially miscible throughout a significant portion of the interior of Saturn, and to a lesser extent in Jupiter.
通过第一性原理分子动力学模拟计算了兆巴压力和中等温度(4000至10000K)下氢 - 氦混合物的性质。我们确定了作为密度、温度和成分函数的状态方程,并使用热力学积分估算混合吉布斯自由能,从而确定在给定压力下氦在致密金属氢中变得不溶时的温度。这些结果与木星行星内部结构和演化模型直接相关。我们发现,氦和氢的分层温度足够高,在大约5兆巴的压力下穿过土星的行星绝热线;在土星内部的很大一部分区域,氦是部分可混溶的,在木星中的可混溶程度较小。