Published December 10, 2011 | Version v1
Journal article

THE MASS OF CoRoT-7b

  • 1. Thüringer Landessternwarte, D-07778 Tautenburg (Germany)
  • 2. European Space Agency, ESTEC, SRE-SA, P.O. Box 299, NL-2200AG, Noordwijk (Netherlands)
  • 3. School of Physics and Astronomy, Raymond and Beverly Sackler Faculty of Exact Sciences, Tel Aviv University, Tel Aviv (Israel)
  • 4. Observatoire de la Côte d'Azur, BP 4229, F-06304 Nice Cedex 4 (France)
  • 5. Institut d'Astrophysique de Paris, UMR 7095 CNRS, Université Pierre and Marie Curie, 98bis boulevard Arago, F-75014 Paris (France)
  • 6. Rheinisches Institut für Umweltforschung, Universität zu Köln, Abt. Planetenforschung, Aachener Str. 209, D-50931 Köln (Germany)
  • 7. Observatoire de l'Université de Genève, 51 chemin des Maillettes, 1290 Sauverny (Switzerland)
  • 8. Observatoire de Haute Provence, F-04670 Saint Michel l'Observatoire (France)
  • 9. Laboratoire d'Astrophysique de Marseille, CNRS and University of Provence, 38 rue Frédéric Joliot-Curie, F-13388 Marseille Cedex 13 (France)
  • 10. Instituto de Astrofísica de Canarias, E-38205 La Laguna, Tenerife (Spain)
  • 11. University of Vienna, Institute of Astronomy, Türkenschanzstr. 17, A-1180, Vienna (Austria)
  • 12. IAG, University of São Paulo (Brazil)

Description

The mass of CoRoT-7b, the first transiting super-Earth exoplanet, is still a subject of debate. A wide range of masses have been reported in the literature ranging from as high as 8 M⊕ to as low as 2.3 M⊕. This range in mass is largely due to the activity level of the star that contributes a significant amount of radial velocity (RV) 'jitter' and how the various methods correct this jitter. Although most mass determinations give a density consistent with a rocky planet, the lower value permits a bulk composition that can be up to 50% water. We present an analysis of the CoRoT-7b RV measurements that uses very few and simple assumptions in treating the activity signal. By analyzing those RV data for which multiple measurements were made in a given night, we remove the activity related RV contribution without any a priori model. We argue that the contribution of activity to the final RV curve is negligible and that the K-amplitude due to the planet is well constrained. This yields a mass of 7.42 ± 1.21 M⊕ and a mean density of ρ = 10.4 ± 1.8 gm cm–3. CoRoT-7b is similar in mass and radius to the second rocky planet to be discovered, Kepler-10b, and within the errors they have identical bulk densities—they are virtual twins. These bulk densities lie close to the density-radius relationship for terrestrial planets similar to what is seen for Mercury. CoRoT-7b and Kepler-10b may have an internal structure more like Mercury than the Earth.

Availability note (English)

Available from http://dx.doi.org/10.1088/0004-637X/743/1/75

Additional details

Identifiers

Publishing Information

Journal Title
Astrophysical Journal
Journal Volume
743
Journal Issue
1
Journal Page Range
[11 p.]
ISSN
0004-637X
CODEN
ASJOAB

INIS

Country of Publication
United States
Country of Input or Organization
International Atomic Energy Agency (IAEA)
INIS RN
43094595
Subject category
S79: ASTROPHYSICS, COSMOLOGY AND ASTRONOMY;
Descriptors DEI
ACTIVITY LEVELS; AMPLITUDES; BULK DENSITY; EARTH PLANET; MERCURY PLANET; RADIAL VELOCITY; STARS
Descriptors DEC
DENSITY; PHYSICAL PROPERTIES; PLANETS; VELOCITY