The Hydrogen Secret of Young Sub-Neptunes ✛

Original: "Redefining interiors and envelopes: hydrogen-silicate miscibility and its consequences for the structure and evolution of sub-Neptunes"
arXiv:2509.13320 · 2025-09-16 · CC BY 4.0 · 1 min
In the depths of young sub-Neptunes, hydrogen and molten rock mix like cocoa in milk, forever changing the planet’s appearance.

Previous models depicted sub-Neptunes as a rocky ball wrapped in hydrogen. But new research has shown: in the depths of young sub-Neptunes, due to colossal pressure and temperatures above 4000°C, hydrogen and molten rocky material mix into a single liquid, like cocoa in hot milk. Up to a third of the planet’s mass may be hidden in this ‘cocktail’.

As it cools, the mixture separates: hydrogen slowly ‘sweats out’ into the atmosphere, like bubbles in a cooling drink. This gas release slows down the planet’s contraction, making young sub-Neptunes look suspiciously puffy. Telescopes can catch this process through atmospheric features.

After a billion years, almost all the hydrogen will evaporate, and the planet will resemble an adult counterpart. But its interior forever holds traces of that hot youth — like a hidden snapshot beneath the crust.

Without this hydrogen cushion, such planets would shrink twice as fast, and we simply wouldn’t notice their puffiness.

Without this hydrogen cushion, young sub-Neptunes would look almost twice as small — their puffiness gives away a turbulent past.

\frac{\partial P}{\partial m} = -\frac{Gm}{4\pi r^4}
Pressure increases toward the planet's center proportionally to the mass inside the radius
\Delta \hat{G}_{\text{mix}} = RT\left[(1-x_{\text{H}_2})\ln(1-x_{\text{H}_2}) + x_{\text{H}_2}\ln x_{\text{H}_2}\right] + (1-x_{\text{H}_2})x_{\text{H}_2}(A(1-x_{\text{H}_2})+Bx_{\text{H}_2})\left(1-\frac{T}{C}+\frac{P}{D}\right)
The mixing energy determines whether hydrogen and silicate mix at given temperature and pressure
Scientists
Christian DopplerD. B. McLaughlinDidier QuelozMichel MayorR. A. RossiterDavid Charbonneau
Concepts
sub neptune formation sub neptune hydrogen atmosphere mantle gas giant planetary interior subsurface ocean hydrogen envelope gas envelope habitability habitable zone olivine europa mercury thermocline dust liquid helium temperature neutron star interior crust super earth