Jupiter's Interior with an Inverted Helium Gradient
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arXiv
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| Format: | Preprint |
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2025
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| _version_ | 1866917972821409792 |
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| author | Nettelmann, Nadine Fortney, Jonathan J. |
| author_facet | Nettelmann, Nadine Fortney, Jonathan J. |
| contents | Jupiter's gravity field observed by NASA's Juno spacecraft indicates that the density in the 10--100 GPa region is lower than one would expect from a H/He adiabat with 0.5-5x solar water abundance as has been observationally inferred in Jupiter's atmosphere, supported by the 2--4$\times$ solar enrichment in the heavy noble gases and other volatiles observed by the Galileo entry probe. Here, we assume that Jupiter's envelope harbors a radiative window at ~0.975-0.99 RJ. This outer stable layer (OSL) delays particle exchange and accelerates the cooling of the deep interior. Consequently, the He-depletion at the Mbar-level where H/He phase separation occurs would be stronger than seen in the atmosphere. We find that the inverted He-gradient across the OSL leads to atmospheric heavy element abundances that are up to dZatm=0.03 (+2x solar) higher than for adiabatic models. With an additional inverted Z-gradient, Zatm up to 3x solar is possible. Models with 1x solar Zatm have a dilute core confined to the inner 0.2-0.3 MJ (0.4-0.5 RJ), smaller than in adiabatic models. Models with 3x solar Zatm have a largely homogeneous-Z interior at 1x solar. The low observed atmospheric Ne/He ratio suggests that Ne is transported through the OSL as efficiently as He is and at an enhanced diffusivity as is characteristic of double diffusive convection. Better knowledge of the H/He-EOS in the 10--100 GPa region and of the H/He phase diagram is needed to understand Jupiter's interior structure. |
| format | Preprint |
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arxiv_https___arxiv_org_abs_2504_00228 |
| institution | arXiv |
| publishDate | 2025 |
| record_format | arxiv |
| spellingShingle | Jupiter's Interior with an Inverted Helium Gradient Nettelmann, Nadine Fortney, Jonathan J. Earth and Planetary Astrophysics Jupiter's gravity field observed by NASA's Juno spacecraft indicates that the density in the 10--100 GPa region is lower than one would expect from a H/He adiabat with 0.5-5x solar water abundance as has been observationally inferred in Jupiter's atmosphere, supported by the 2--4$\times$ solar enrichment in the heavy noble gases and other volatiles observed by the Galileo entry probe. Here, we assume that Jupiter's envelope harbors a radiative window at ~0.975-0.99 RJ. This outer stable layer (OSL) delays particle exchange and accelerates the cooling of the deep interior. Consequently, the He-depletion at the Mbar-level where H/He phase separation occurs would be stronger than seen in the atmosphere. We find that the inverted He-gradient across the OSL leads to atmospheric heavy element abundances that are up to dZatm=0.03 (+2x solar) higher than for adiabatic models. With an additional inverted Z-gradient, Zatm up to 3x solar is possible. Models with 1x solar Zatm have a dilute core confined to the inner 0.2-0.3 MJ (0.4-0.5 RJ), smaller than in adiabatic models. Models with 3x solar Zatm have a largely homogeneous-Z interior at 1x solar. The low observed atmospheric Ne/He ratio suggests that Ne is transported through the OSL as efficiently as He is and at an enhanced diffusivity as is characteristic of double diffusive convection. Better knowledge of the H/He-EOS in the 10--100 GPa region and of the H/He phase diagram is needed to understand Jupiter's interior structure. |
| title | Jupiter's Interior with an Inverted Helium Gradient |
| topic | Earth and Planetary Astrophysics |
| url | https://arxiv.org/abs/2504.00228 |