Magma Ocean Interactions Can Explain JWST Observations Of The sub-Neptune TOI-270 d

editorAstrobiologyYesterday2 Views

Magma Ocean Interactions Can Explain JWST Observations Of The sub-Neptune TOI-270 d

Schematic of the modeling framework used in this study. Chemical equilibrium between the core, mantle and atmosphere is calculated using the model from H. E. Schlichting & E. D. Young (2022). Upper atmospheric temperature profiles are calculated using HELIOS (M. Malik et al. 2017). Fastchem cond (J. W. Stock et al. 2022) is used to find equilibrium chemical abundances throughout the upper atmosphere, accounting for rainout condensation. After iterating between HELIOS and Fastchem cond until convergence is reached, we account for photochemical processes and vertical mixing using Photochem (N. F. Wogan et al. 2023, 2025). — astro-ph.EP

Sub-Neptunes with substantial atmospheres may possess magma oceans in contact with the overlying gas, with chemical interactions between the atmosphere and magma playing an important role in shaping atmospheric composition.

Early JWST observations have found high abundances of carbon- and oxygen-bearing molecules in a number of sub-Neptune atmospheres, which may result from processes including accretion of icy material at formation or magma-atmosphere interactions. Previous work examining the effects of magma-atmosphere interactions on sub-Neptunes has mostly been limited to studying conditions at the atmosphere-mantle boundary, without considering implications for the upper atmosphere which is probed by spectroscopic observations.

In this work, we present a modeling architecture to determine observable signatures of magma-atmosphere interactions. We combine an equilibrium chemistry code which models reactions between the core, mantle and atmosphere with a radiative-convective model that determines the composition and structure of the observable upper atmosphere.

We examine how different conditions at the atmosphere-mantle boundary and different core and mantle compositions impact the upper atmospheric composition. We compare our models to JWST NIRISS+NIRSpec observations of the sub-Neptune TOI-270 d, finding that our models can provide a good fit to the observed transmission spectrum with little fine-tuning.

This suggests that magma-atmosphere interactions may be sufficient to explain high abundances of molecules such as H2O, CH4 and CO2 in sub-Neptune atmospheres, without additional accretion of icy material from the protoplanetary disk. Although other processes could lead to similar compositions, our work highlights the need to consider magma-atmosphere interactions when interpreting the observed atmospheric composition of a sub-Neptune.

Matthew C. Nixon, R. Sander Somers, Arjun B. Savel, Jegug Ih, Eliza M.-R. Kempton, Edward D. Young, Hilke E. Schlichting, Tim Lichtenberg, Luis Welbanks, William Misener, Anjali A. A. Piette, Nicholas F. Wogan

Comments: 19 pages, 8 figures. Revised version after responding to reviewer comments. Submitted to AAS journals
Subjects: Earth and Planetary Astrophysics (astro-ph.EP)
Cite as: arXiv:2510.07367 [astro-ph.EP] (or arXiv:2510.07367v1 [astro-ph.EP] for this version)
https://doi.org/10.48550/arXiv.2510.07367
Focus to learn more
Submission history
From: Matthew Nixon
[v1] Wed, 8 Oct 2025 18:00:00 UTC (1,367 KB)
https://arxiv.org/abs/2510.07367
Astrobiology, exoplanet,

0 Votes: 0 Upvotes, 0 Downvotes (0 Points)

Leave a reply

Recent Comments

No comments to show.
Join Us
  • Facebook38.5K
  • X Network32.1K

Stay Informed With the Latest & Most Important News

[mc4wp_form id=314]
Categories

Advertisement

Loading Next Post...
Follow
Search Trending
Popular Now
Loading

Signing-in 3 seconds...

Signing-up 3 seconds...