A diagram to determine the evaporation status of extrasolar planets
By A. Lecavelier, Des Etangs. 2006
219 citations recorded by the source corpus.
Aims. To describe the evaporation status of extrasolar planets, we consider an energy diagram in which the potential energy of the planets is plotted versus the energy received by the upper atmosphere. Methods. Here we present a basic method to estimate these quantities. For the potential energy, we include the modification of the gravity field by the tidal forces from the parent stars. Results. This description allows a rapid estimate of both the escape rate of the atmospheric gas and the lifetime of a planet against the evaporation process. In the energy diagram, we find an evaporation-forbidden region in which a gaseous planet would evaporate in less than 5 billion years. With their observed characteristics, all extrasolar planets are found outside this evaporation-forbidden region. The escape rates are estimated to be in the range 10 5 g s -1 to 10 12 g s -1 with a few cases above 10 11 g s -1 . The estimated escape rate for HD 209458 b is consistent with the lower limit of 10 10 g s -1 obtained from interpretation of the H I Lyman-α observations. This diagram suggests possibilities for the nature of the recently discovered Neptune-mass planets. We find that GJ 436 b, 55 Cnc e and HD 69830 b cannot be low mass gaseous planets. With a density that must be above 0.5 g cm -3 to survive evaporation, these planets must contain a large fraction of solid/liquid material. We find that GJ 876 d must have a density greater than ∼3 g cm -3 to survive the strong EUV energy flux from its nearby parent star. GJ 876 d must contain a large fraction of massive elements.
Subfields: Astronomy and Astrophysics, Instrumentation, Statistical and Nonlinear Physics
View Paper: https://www.semanticscholar.org/paper/024cc0e4a99f61397a86e15dd0ed466614e3f887
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Citations in the corpus
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- TIDAL EVOLUTION OF CLOSE-IN PLANETS (2010, background): “The orbits of these planets might have been circularized as the planet lost mass (e.g. Lammer et al. 2003; Lecavelier Des Etangs 2007), or the planetary radius expanded due to tidal heating (e.g. Bodenheimer et al. 2001; Gu et al. 2003).”
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- Planetary evaporation by UV and X‐ray radiation: basic hydrodynamics (2012, background): “Perhaps the simplest approach is to assume that every photon received at the planet’s surface is turned into mass-loss at some efficiency (Watson et al. 1981; Lecavelier des Etangs 2007).”
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