The debris disk - terrestrial planet connection
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 wavelengths of ~70 microns) and we predict that these signpost dynamically calm environments that should contain terrestrial planets.
Keywords
Cite
@article{arxiv.1104.2898,
title = {The debris disk - terrestrial planet connection},
author = {Sean N. Raymond and Philip J. Armitage and Amaya Moro-Martín and Mark Booth and Mark Wyatt and John C. Armstrong and Avi M. Mandell and Franck Selsis},
journal= {arXiv preprint arXiv:1104.2898},
year = {2015}
}
Comments
Contribution to proceedings of IAU 276: Astrophysics of Planetary Systems