Liquid Water on Frozen Extrasolar Planets?
- Research areas:
- Year:
- 2008
- Authors:
-
- David Ehrenreich
- Alain Lecavelier des Etangs
- Jean-Philippe Beaulieu
- Olivier Grasset
- Editor:
- Fischer, D; Rasio, FA; Thorsett, SE; Wolszczan, A
- Volume:
- 398
- Series:
- ASTRONOMICAL SOCIETY OF THE PACIFIC CONFERENCE SERIES
- BibTex:
- Abstract:
- The detection of OGLE-2005-BLG-390Lb (Beaulieu et al. 2006) around an M star in the Galactic Bulge unveils the existence of cold (similar to 40 K) Earth-mass planets (Ehrenreich and Cassan 2007). Such planets could nevertheless host liquid water beneath a frozen surface, because of a strong radiogenic heating of the ice shell (Ehrenreich et al. 2006). Heating and cooling of the ice shell depend on the ice-to-rock ratio (I/R.) and the age of the planet planet. OGLE 390Lb now seems too old (similar to 10 Gyr) to host a subsurface ocean, for any tested I/R value. However, the heat production rate was larger in the past so that liquid water did flow for several billions of years underneath the ice shell.