January 27, 2009
Helium And the Formation Of Jovian Planets
Models of how Saturn and Jupiter formed may soon take on a different look.
By determining the properties of hydrogen-helium mixtures at the millions of atmospheres of pressure present in the interior of Saturn and Jupiter, physicists at Lawrence Livermore National Laboratory and the University of Illinois at Urbana-Champaign have determined the temperature at a given pressure when helium becomes insoluble in dense metallic hydrogen. The results are directly relevant to models of the interior structure and evolution of Jovian planets.
However, scientists have struggled to determine what conditions are needed for the two elements to mix.
Using first-principle molecular dynamics simulations, Miguel Morales, a DOE Stewardship Science graduate fellow from David Ceperley's group at the University of Illinois worked with LLNL's Eric Schwegler, Sebastien Hamel, Kyle Caspersen and Carlo Pierleoni from the University of L'Aquila in Italy to determine the equation of state of the hydrogen-helium system at extremely high temperatures (4,000-10,000 degrees Kelvin), similar to what would be found in the interior of Saturn and Jupiter.
The team used LLNL's extensive high-performance computing facilities to conduct simulations over a wide range of density, temperature and composition to locate the equation of state of the two elements.
"Our simulation results are consistent with the idea that a large portion of the interior of Saturn has conditions such that hydrogen and helium phase separate," Morales said. "This can account for the apparent discrepancy between the current evolutionary models for Saturn and observational data."
In addition to being made mostly of hydrogen and helium, a characteristic of Jovian planets is that they radiate more energy than they take in from the sun. Various models of their evolution and structure have been developed to describe a relation between the age, volume and mass of the planet and its luminosity.
While this model works for Jupiter by modeling the energy radiation left over from its formation 4.55 billion years ago, it doesn't exactly work for Saturn. Instead, the model seriously underestimates the current luminosity of Saturn.
So the researchers decided to try something different. They determined where helium and hydrogen mix as well as at what temperature they don't mix.
It turned out the temperature where the two elements don't mix is high enough that helium is "partially mixable over a significant fraction of the interior of the Jovian planets with the corresponding region of Saturn being larger than in Jupiter," Schwegler said. "This, in fact, could change the current interior models of Saturn and Jupiter."
The new findings appeared in the Jan. 26 online edition of the journal, Proceedings of the National Academy of Sciences.
Image 1: As Jupiter and Saturn cool, the interior of the planets will approach temperatures where hydrogen and helium no longer mix. This process, which is likely to have already occurred in Saturn, could lead to the formation of helium droplets that would "rain down" towards the center of the planet and provide an additional source of heat. Illustration by Jonathan DuBois
Image 2: First-principle simulations have been used to directly determine the miscibility of helium (gold balls) in dense metallic hydrogen (white balls) under the extreme conditions that are present in the interiors of the Jovian planets. Illustration by Kwei-Yu Chu
On the Net:
- Lawrence Livermore National Laboratory
- University of Illinois at Urbana-Champaign
- Proceedings of the National Academy of Sciences