Volume 531, July 2011
|Number of page(s)||11|
|Section||Planets and planetary systems|
|Published online||07 July 2011|
On the mass determination of super-Earths orbiting active stars: the CoRoT-7 system
Instituto de Astronomia, Geofísica e Ciências Atmosféricas (IAG) – Universidade de São Paulo, Rua do Matão, 1226 Cep:05508–090 São Paulo, Brazil
2 Observatório Astronómico de Córdoba, Universidad Nacional de Córdoba, Argentina
Received: 3 November 2010
Accepted: 18 March 2011
Context. Star activity makes the mass determination of CoRoT-7b and CoRoT 7c uncertain. Investigators of the CoRoT team proposed several solutions, but all but one of them are larger than the initial determinations of 4.8 ± 0.8 MEarth for CoRoT-7b and 8.4 ± 0.9 MEarth for CoRoT 7c.
Aims. This investigation uses the excellent HARPS radial velocity measurements of CoRoT-7 to redetermine the planet masses and to explore techniques for determining mass and orbital elements of planets discovered around active stars when the relative variation in the radial velocity due to the star activity cannot be considered as just noise and can exceed the variation due to the planets.
Methods. The main technique used here is a self-consistent version of the high-pass filter used by Queloz et al. (2009, A&A, 506, 303) in the first mass determination of CoRoT-7b and CoRoT-7c. The results are compared to those given by two alternative techniques: (1) the approach proposed by Hatzes et al. (2010, A&A, 520, A93) using only those nights in which two or three observations were done; (2) a pure Fourier analysis. In all cases, the eccentricities are taken equal to zero as indicated by the study of the tidal evolution of the system. The periods are also kept fixed at the values given by Queloz et al. Only the observations done in the time interval BJD 2 454 847 − 873 are used because they include many nights with multiple observations; otherwise, it is not possible to separate the effects of the rotation fourth harmonic (5.91 d = Prot/4) from the alias of the orbital period of CoRoT-7b (0.853585 d).
Results. The results of the various approaches are combined to give planet mass values 8.0 ± 1.2 MEarth for CoRoT-7b and 13.6 ± 1.4 MEarth for CoRoT 7c. An estimation of the variation of the radial velocity of the star due to its activity is also given.
Conclusions. The results obtained with three different approaches agree to give higher masses than those in previous determinations. From the existing internal structure models they indicate that CoRoT-7b is a much denser super-Earth. The bulk density is 11 ± 3.5 g cm-3, so CoRoT-7b may be rocky with a large iron core.
Key words: planets and satellites: detection / planets and satellites: fundamental parameters
© ESO, 2011
Current usage metrics show cumulative count of Article Views (full-text article views including HTML views, PDF and ePub downloads, according to the available data) and Abstracts Views on Vision4Press platform.
Data correspond to usage on the plateform after 2015. The current usage metrics is available 48-96 hours after online publication and is updated daily on week days.
Initial download of the metrics may take a while.