Removal of Hot Saturns in Mass-Radius Plane by Runaway Mass Loss
arXiv:2211.11770 · doi:10.3847/2041-8213/acbd35
Abstract
The hot Saturn population exhibits a boundary in mass-radius space, such that no planets are observed at a density less than 0.1 g cm. Yet, planet interior structure models can readily construct such objects as the natural result of radius inflation. Here, we investigate the role XUV-driven mass-loss plays in sculpting the density boundary by constructing interior structure models that include radius inflation, photoevaporative mass loss and a simple prescription of Roche lobe overflow. We demonstrate that planets puffier than 0.1 g cm experience a runaway mass loss caused by adiabatic radius expansion as the gas layer is stripped away, providing a good explanation of the observed edge in mass-radius space. The process is also visible in the radius-period and mass-period spaces, though smaller, high-bulk-metallicity planets can still survive at short periods, preserving a partial record of the population distribution at formation.
11 pages, 5 figures, Accepted to ApJ Letters. This revision includes the effect of orbital evolution resulting from Roche lobe overflow; the overall conclusions are the same
References in corpus (20)
- Atmospheric Escape from Hot Jupiters
- Growth Model Interpretation of Planet Size Distribution
- The active lives of stars: a complete description of rotation and XUV evolution of F, G, K, and M dwarfs
- A new equation of state for dense hydrogen-helium mixtures
- Heating efficiency in hydrogen-dominated upper atmospheres
- A remnant planetary core in the hot-Neptune desert
- Mass-radius relationships for irradiated ocean planets
- Four Sub-Saturns with Dissimilar Densities: Windows into Planetary Cores and Envelopes
- An Ultra-Hot Neptune in the Neptune desert
- Primordial Radius Gap and Potentially Broad Core Mass Distributions of Super-Earths and Sub-Neptunes
- The Upper Edge of the Neptune Desert Is Stable Against Photoevaporation
- From Hot Jupiters to Super-Earths via Roche Lobe Overflow
- Creating the Radius Gap without Mass Loss
- Irradiation-driven escape of primordial planetary atmospheres II. Evaporation efficiency of sub-Neptunes through hot Jupiters
- Two young planetary systems around field stars with ages between 20-320 Myr from TESS
- Irradiation-driven escape of primordial planetary atmospheres I. The ATES photoionization hydrodynamics code
- Slow Cooling and Fast Reinflation for Hot Jupiters
- Sculpting the sub-Saturn Occurrence Rate via Atmospheric Mass Loss
- Three Hot-Jupiters on the upper edge of the mass-radius distribution: WASP-177, WASP-181 and WASP-183
- Qatar Exoplanet Survey: Qatar-8b, 9b and 10b --- A Hot Saturn and Two Hot Jupiters
Cited by in corpus (11)
- Planetary Population Synthesis and the Emergence of Four Classes of Planetary System Architectures
- Helium in Exoplanet Exospheres: Orbital and Stellar Influences
- Understanding the Planetary Formation and Evolution in Star Clusters(UPiC)-I: Evidence of Hot Giant Exoplanets Formation Timescales
- Discovery and characterization of a dense sub-Saturn TOI-6651b
- Inflated hot Jupiters: Inferring average atmospheric velocity via Ohmic models coupled with internal dynamo evolution
- Atmospheric Mass Loss from TOI-1259 A b, a Gas Giant Planet With a White Dwarf Companion
- TOI-1199 b and TOI-1273 b: Two new transiting hot Saturns detected and characterized with SOPHIE and TESS
- Ground-Based Reconnaissance Observations of 21 Exoplanet Atmospheres with the Exoplanet Transmission Spectroscopy Imager
- Confirmation of the hot super-Neptune TOI-672 b with NIRPS and HARPS and Insights into the Neptunian desert around M dwarfs
- Evolution of the ZTF SLRN-2020 star-planet merger
- A sub-Saturn Mass-Radius Desert for Planets with Equilibrium Temperature Less than 600 K