Uncovering the Origins of Super-Earths and Giant Planets

Uncovering the Origins of Super-Earths and Giant Planets

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Formation clues from exoplanet demographics

4 of 18

4 of 18

Formation clues from exoplanet demographics

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Uncovering the Origins of Super-Earths and Giant Planets

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  1. 1 Intro
  2. 2 Dust growth and transport: key process for planet formation
  3. 3 Planet formation: Likely a bottom up process
  4. 4 Formation clues from exoplanet demographics
  5. 5 Why does dust content matter for gas accretion?
  6. 6 Dust-to-gas ratio and dust opacity A function of location in the disk, especially if the fragmentation threshold varies with composition
  7. 7 Disk opacity is starkly different from ISM opacity
  8. 8 Gas giants at intermediate distances
  9. 9 Super-Earths are the most common planets in the galaxy. They are even more common around M stars than FGK stars.
  10. 10 The process of pebble accretion
  11. 11 Pebble accretion efficiency: key to converting dust to planets
  12. 12 Pebble accretion efficiency as a function of stellar mass
  13. 13 Super-Earth formation in actively heated regions of the disk
  14. 14 Giant planet core formation in the passively heated regions of the disk
  15. 15 Comparison to observations: We need early-stage disk demographics
  16. 16 What conditions favor the formation of cold giant planets?
  17. 17 Placing constraints on Kepler-167's disk properties
  18. 18 How giant planet hosting disks can form super-Earths

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