The creation of sub-Neptune planets involving hydrogen atmospheres and magma oceans.Sub-Neptunes are a class of exoplanets with sizes between Earth and Neptune, and they are the most common type of planet found in our galaxy. They are thought to have a rocky or icy core surrounded by a thick hydrogen and helium atmosphere. The formation of these planets is a delicate dance between the growth of a solid core and the accretion of gas from the protoplanetary disk. Recent research suggests that the interaction between a magma ocean on the core's surface and the hydrogen atmosphere is crucial, potentially even generating water and other volatiles that shape the planet's final composition.
The concept of sub-Neptunes as a distinct class emerged from exoplanet discoveries in the 2010s, particularly from the Kepler mission. The specific role of magma-ocean and hydrogen-atmosphere interactions in their formation has been developed in the late 2010s and 2020s through theoretical models and laboratory experiments.
The formation begins with the accretion of rocky and icy planetesimals into a solid core, typically 2-5 times the mass of Earth. Once the core reaches a critical mass, it begins to gravitationally attract gas from the surrounding protoplanetary disk, forming a hydrogen-dominated atmosphere. However, the process is not just a simple accumulation of gas. The hot magma ocean on the core's surface reacts with the hydrogen atmosphere, producing water vapor and other compounds. This chemical interaction can significantly alter the atmospheric composition and the planet's overall volatile budget. The heat from the magma ocean, sustained by accretion and radioactive decay, can also delay the cooling and contraction of the atmosphere, keeping the planet inflated for longer periods. This explains why many sub-Neptunes have lower densities than expected.
Understanding sub-Neptune formation is essential for interpreting exoplanet observations, particularly the mass-radius relationships obtained from transit and radial velocity measurements. It also informs the search for habitable planets, as many sub-Neptunes may be mini-Neptunes with thick atmospheres rather than rocky super-Earths.
The magma ocean on a young sub-Neptune can be so hot that it vaporizes rock, creating a silicate atmosphere that mixes with the hydrogen, making the planet's atmosphere a bizarre hybrid of gas and rock vapor.




















