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A&A 455, L25-L28 (2006)
DOI: 10.1051/0004-6361:20065697
Letter
Formation and structure of the three Neptune-mass planets system around HD 69830
Y. Alibert1, I. Baraffe2, W. Benz1, G. Chabrier2, C. Mordasini1, C. Lovis3, M. Mayor3, F. Pepe3, F. Bouchy4, D. Queloz3 and S. Udry31 Physikalisches Insitut, University of Bern, Sidlerstrasse 5, 3012 Bern, Switzerland
e-mail: yann.alibert@space.unibe.ch
2 CRAL, École Normale Supérieure, 46 allée d'Italie, 69007 Lyon, France
3 Observatoire de Genève, 51 Ch. des Maillettes, 1290 Sauverny, Switzerland
4 Institut d'Astrophysique de Paris, 98bis Bd Arago, 75014 Paris, France
(Received 26 May 2006 / Accepted 6 July 2006)
Abstract
Since the discovery of the first giant planet outside the solar system in 1995 (Mayor & Queloz 1995,
Nature, 378, 355), more than
180 extrasolar planets have been discovered. With improving detection capabilities, a new
class of planets with masses 5-20 times larger than the Earth, at close distance from their
parent star is rapidly emerging. Recently, the first system of three Neptune-mass planets
has been discovered around the solar type star HD 69830 (Lovis et al. 2006,
Nature, 441, 305). Here, we present and discuss a
possible formation scenario for this planetary system based on a consistent coupling between
the extended core accretion model and evolutionary models (Alibert et al. 2005a,
A&A, 434, 343; Baraffe et al. 2004,
A&A, 419, L13; Baraffe et al. 2006,
A&A, 450, 1221).
We show that the innermost planet formed from an embryo having started inside the iceline is composed
essentially of a rocky core surrounded by a tiny gaseous envelope. The two outermost planets
started their formation beyond the iceline and, as a consequence, accrete a substantial
amount of water ice during their formation. We calculate the present day thermodynamical
conditions inside these two latter planets and show that they are made of a rocky core
surrounded by a shell of fluid water and a gaseous envelope.
Key words: stars: planetary systems -- stars: planetary systems: formation
© ESO 2006
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