Atmospheric Helium Abundances in the Giant Planets
N. Nettelmann, M. Cano Amoros, N. Tosi, J. J. Fortney, R. Helled

TL;DR
This study models atmospheric helium depletion in giant planets using phase diagrams and equations of state, revealing different internal structures and the importance of in-situ measurements for understanding their composition.
Contribution
It applies H/He phase diagrams and EOS models to explain helium depletion, offering new insights into the internal structures of Uranus, Neptune, and Saturn.
Findings
Strong helium depletion in ice giants if adiabatic.
Weak depletion in Uranus with a thermal boundary layer.
Possible dissimilar internal structures between Uranus and Neptune.
Abstract
Noble gases are accreted to the giant planets as part of the gas component of the planet-forming disk. While heavier noble gases can separate from the evolution of the hydrogen-rich gas, helium is thought to remain at the protosolar H/He ratio Yproto~0.27-0.28. However, spacecraft observations revealed a depletion in helium in the atmospheres of Jupiter, Saturn, and Uranus. For the gas giants, this is commonly seen as indication of H/He phase separation at greater depths. Here, we apply predictions of the H/He phase diagram and three H/He-EOS to compute the atmospheric helium mass abundance Yatm as a result of H/He phase separation. We obtain a strong depletion Yatm<0.1 for the ice giants if they are adiabatic. Introducing a thermal boundary layer at the Z-poor/Z-rich compositional transition with a temperature increase of up to a few 1000 K, we obtain a weak depletion in Uranus as…
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Taxonomy
TopicsAstro and Planetary Science · Spacecraft and Cryogenic Technologies · Planetary Science and Exploration
