Open Access
Table 1
H-He EOSs used in interior models.
Name of the H-He EOS | H EOS | He EOS | H-He interactions | Notes/references |
---|---|---|---|---|
MGF16+MH13 | MGF16-H | SCvH95-He | Included in the H EOS but fixed at Y = 0.245 | Derived by Miguel et al. (2016) from Militzer & Hubbard (2013) |
MH13* | -- | -- | -- | Adjusted from MGF16+MH13 to fit a Y = 0.245 adiabat from Militzer et al. (2022) |
CD21 | CD21-H | CMS19-He | Included in the H EOS but fixed at Y = 0.245 | Derived by Chabrier & Debras (2021) from Militzer & Hubbard (2013) |
HG23+CMS19 | CMS19-H | CMS19-He | HG23 | H and He EOSs from Chabrier et al. (2019) and non-ideal mixing effects from Howard & Guillot (2023) |
HG23+MLS22 | MLS22-H | CMS19-He | HG23 | H EOS from Mazevet et al. (2022) and non-ideal mixing effects from Howard & Guillot (2023) |
SCvH95 | SCvH95-H | SCvH95-He | None | H and He EOSs from Saumon et al. (1995) |
Notes. Concerning the heavy elements, the EOSs used for ices and rocks are respectively those of water and dry sand from Lyon & Johnson (1992).
Current usage metrics show cumulative count of Article Views (full-text article views including HTML views, PDF and ePub downloads, according to the available data) and Abstracts Views on Vision4Press platform.
Data correspond to usage on the plateform after 2015. The current usage metrics is available 48-96 hours after online publication and is updated daily on week days.
Initial download of the metrics may take a while.