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The debris disk - Terrestrial planet connection

  • Sean N. Raymond
  • , Philip J. Armitage
  • , Amaya Moro-Martín
  • , Mark Booth
  • , Mark C. Wyatt
  • , John C. Armstrong
  • , Avi M. Mandell
  • , Franck Selsis
  • CNRS-OASU
  • Laboratoire d'Astrophysique de Bordeaux
  • Centro de Astrobiología (INTA-CSIC)
  • Princeton University
  • University of Cambridge
  • Weber State University
  • NASA Goddard Space Flight Center

Research output: Chapter in Book/Report/Conference proceedingConference contributionpeer-review

1 Scopus citations

Abstract

The eccentric orbits of the known extrasolar giant planets provide evidence that most planet-forming environments undergo violent dynamical instabilities. Here, we numerically simulate the impact of giant planet instabilities on planetary systems as a whole. We find that populations of inner rocky and outer icy bodies are both shaped by the giant planet dynamics and are naturally correlated. Strong instabilities - those with very eccentric surviving giant planets - completely clear out their inner and outer regions. In contrast, systems with stable or low-mass giant planets form terrestrial planets in their inner regions and outer icy bodies produce dust that is observable as debris disks at mid-infrared wavelengths. Fifteen to twenty percent of old stars are observed to have bright debris disks (at λ ∼ 70μm) and we predict that these signpost dynamically calm environments that should contain terrestrial planets.

Original languageEnglish
Title of host publicationThe Astrophysics of Planetary Systems
Subtitle of host publicationFormation, Structure, and Dynamical Evolution
EditorsAlessandro Sozzetti, Mario Lattanzi, Alan Boss
Pages82-88
Number of pages7
EditionS276
DOIs
StatePublished - Oct 2010

Publication series

NameProceedings of the International Astronomical Union
NumberS276
Volume6
ISSN (Print)1743-9213
ISSN (Electronic)1743-9221

Keywords

  • Debris disks
  • Formation
  • Methods
  • N-body simulations
  • Planetary systems

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