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Updated: Dec 16, 2025

Simulation of the Planetary Interior Differentiation Processes in the Laboratory
Published on: November 15, 2013
A remnant planetary core in the hot-Neptune desert
David J Armstrong1,2, Théo A Lopez3, Vardan Adibekyan4
1Centre for Exoplanets and Habitability, University of Warwick, Coventry, UK. d.j.armstrong@warwick.ac.uk.
TOI-849b, a dense exoplanet smaller than Neptune, is likely the remnant core of a gas giant. Its low mass suggests significant atmospheric loss, offering insights into planetary evolution.
Area of Science:
- Planetary Science
- Exoplanet Research
- Astrophysics
Background:
- Giant planet interiors and cores are poorly understood, with significant observational uncertainties.
- Exoplanets undergoing rare evolutionary processes, like those in the hot-Neptune desert, aid in studying planetary interiors.
- Planets like HD149026b, LTT9779b, and NGTS-4b highlight atmospheric loss and massive cores.
Purpose of the Study:
- To investigate the nature of the exoplanet TOI-849b, characterized by its small radius and large mass.
- To determine the composition and evolutionary history of TOI-849b using interior-structure models.
- To understand the mechanisms responsible for potential mass loss in giant planets.
Main Methods:
- Observation of the exoplanet TOI-849b.
- Analysis of TOI-849b's mass, radius, and density.
- Application of interior-structure models to constrain the gaseous envelope mass.
Main Results:
- TOI-849b has a radius smaller than Neptune but a mass of 7.7 Earth masses and a density similar to Earth's.
- Interior-structure models indicate a hydrogen and helium envelope comprising no more than 15% of the total planetary mass.
- The planet's characteristics suggest it was once a gas giant that lost substantial mass.
Conclusions:
- TOI-849b is likely the remnant core of a giant planet.
- Mass loss could have occurred through thermal self-disruption, giant planet collisions, or by avoiding substantial gas accretion.
- Photoevaporation can remove smaller hydrogen/helium envelopes over billions of years, implying TOI-849b's remaining atmosphere may be volatile-enriched.
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