Silane-Methane Competition in Sub-Neptune Atmospheres As A Diagnostic Of Metallicity And Magma Oceans

editorAstrobiology16 hours ago2 Views

Silane-Methane Competition in Sub-Neptune Atmospheres As A Diagnostic Of Metallicity And Magma Oceans

Envelope composition in the H–He–C–N–O–Si chemical system of TOI-421b (𝑅MEB = 1.65𝑅⊕, 𝑅𝑃 = 2.64𝑅⊕, 𝑀𝑃 = 6.7𝑀⊕, 𝑇MEB = 3000 K) as a function of H mass fraction. Elemental budgets, reactions, gas solubility laws, and real gas equations are described in Sect. 2. MEB partial pressures of the considered gases for (a) 1× solar metallicity and 100% mantle melt (IW–6.2 to IW–5.7), (b) 100× solar metallicity and 100% mantle melt (IW–5.5 to IW–5.2), (c) 1× solar metallicity and 1% mantle melt (IW–3.4 to IW–3.1), and (d) 100× solar metallicity and 1% mantle melt (IW–2.3 to IW–1.6). Full range of MEB partial pressures is shown in Fig. A2. The corresponding partitioning of volatile elements in magma and real gas fugacity coefficients are given in Fig. B1 and Fig. B2, respectively. — astro-ph.EP

The James Webb Space Telescope is characterising the atmospheres of sub-Neptunes. The presence of magma oceans on sub-Neptunes is expected to strongly alter the chemistry of their envelopes (100 bar-100 kbar) and atmospheres (1 mbar-100 bar).

At the magma ocean-envelope boundary (MEB, >10 kbar), gas properties deviate from ideality, yet the effects of real gas behaviour on chemical equilibria remain underexplored.

Here, we compute equilibrium between magma-gas and gas-gas reactions using real gas equations of state in the H-He-C-N-O-Si system for TOI-421 b, a canonical hot sub-Neptune potentially hosting a magma ocean. We find that H and N are the most soluble in magma, followed by He and C.

We fit real gas equations of state to experimental data on SiH4, and show that, for a fully molten mantle, SiH4 dominates at the MEB under accreted gas metallicity of 1× solar, but is supplanted by CH4 at 100× solar. Lower mantle melt fractions lower both magma-derived Si abundances in the envelope and the solubility of H and He in magma, yielding H2– and He-rich envelopes.

Projecting equilibrium chemistry through the atmosphere (1 mbar-100 bar), we find that condensation of β-quartz ‘clouds’ depletes Si-bearing gases, although SiH4 remains abundant at solar metallicity. SiH4/CH4 ratios increase with mantle melt fraction and decrease with metallicity. These effects also deplete H2 via CH4 and SiH4 formation and the dissolution of H2 into magma.

The competition between SiH4 and CH4 presents a diagnostic of metallicity and magma oceans. The corollary is that H2– and He-rich, SiH4– and CH4-poor (<5%) atmospheres may indicate a limited role or absence of magma oceans on sub-Neptunes.

Kaustubh Hakim, Dan J. Bower, Fabian Seidler, Paolo A. Sossi

Comments: 15 pages, 13 figures, submitted
Subjects: Earth and Planetary Astrophysics (astro-ph.EP)
Cite as: arXiv:2508.19235 [astro-ph.EP] (or arXiv:2508.19235v1 [astro-ph.EP] for this version)
https://doi.org/10.48550/arXiv.2508.19235
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Submission history
From: Kaustubh Hakim
[v1] Tue, 26 Aug 2025 17:55:13 UTC (643 KB)
https://arxiv.org/abs/2508.19235

Astrobiology

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