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A universal brown dwarf desert formed between planets and stars
Kaiming Cui1,2,3, Guang-Yao Xiao1, Fabo Feng1,4
1Tsung-Dao Lee Institute, Shanghai Jiao Tong University, Shanghai 201210, People's Republic of China.
Giant planets and brown dwarfs are key to understanding star formation. This study reveals a "brown dwarf desert" and identifies giant planets beyond the water-ice line, supporting dual formation scenarios.
Area of Science:
- Astronomy and astrophysics
- Exoplanetary science
- Stellar evolution
Background:
- Giant planets and brown dwarfs bridge the gap between planets and stars, with formation mechanisms requiring further investigation.
- Previous studies lacked comprehensive samples of wide-orbit giant planets and substellar companions, hindering boundary research.
- Radial velocity and astrometry data combined offer a larger, unified sample for analysis.
Purpose of the Study:
- To statistically analyze the occurrence rates of brown dwarfs and giant planets around FGK stars.
- To investigate the formation boundary between planets and stars.
- To test the dual formation hypothesis for substellar objects.
Main Methods:
- Combined analysis of radial velocity and astrometry data.
- Statistical analysis of a sample of 55 giant planets, brown dwarfs, and low-mass stellar companions.
- Population synthesis modeling.
Main Results:
- Identified a distinct brown dwarf desert around 30 Jupiter masses (MJ) with no observed decline up to 20 astronomical units (au).
- Discovered a population of giant planets and low-mass brown dwarfs beyond the water-ice line, contrary to previous predictions.
- Observed metallicity and eccentricity trends suggesting two distinct formation pathways.
Conclusions:
- The findings support the dual formation hypothesis for substellar objects.
- The study refines our understanding of the occurrence rates and formation mechanisms of giant planets and brown dwarfs.
- The identified brown dwarf desert and planetary population beyond the water-ice line provide crucial data for formation models.
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