GIANT IMPACT

AN EFFICIENT MECHANISM for the DEVOLATILIZATION of SUPER-EARTHS

Shang Fei Liu, Yasunori Hori, D. N C Lin, Erik Asphaug

Research output: Contribution to journalArticle

34 Citations (Scopus)

Abstract

Mini-Neptunes and volatile-poor super-Earths coexist on adjacent orbits in proximity to host stars such as Kepler-36 and Kepler-11. Several post-formation processes have been proposed for explaining the origin of the compositional diversity between neighboring planets: mass loss via stellar XUV irradiation, degassing of accreted material, and in situ accumulation of the disk gas. Close-in planets are also likely to experience giant impacts during the advanced stage of planet formation. This study examines the possibility of transforming volatile-rich super-Earths/mini-Neptunes into volatile-depleted super-Earths through giant impacts. We present the results of three-dimensional hydrodynamic simulations of giant impacts in the accretionary and disruptive regimes. Target planets are modeled with a three-layered structure composed of an iron core, silicate mantle, and hydrogen/helium envelope. In the disruptive case, the giant impact can remove most of the H/He atmosphere immediately and homogenize the refractory material in the planetary interior. In the accretionary case, the planet is able to retain more than half of the original gaseous envelope, while a compositional gradient suppresses efficient heat transfer as the planetary interior undergoes double-diffusive convection. After the giant impact, a hot and inflated planet cools and contracts slowly. The extended atmosphere enhances the mass loss via both a Parker wind induced by thermal pressure and hydrodynamic escape driven by the stellar XUV irradiation. As a result, the entire gaseous envelope is expected to be lost due to the combination of those processes in both cases. Based on our results, we propose that Kepler-36b may have been significantly devolatilized by giant impacts, while a substantial fraction of Kepler-36c's atmosphere may remain intact. Furthermore, the stochastic nature of giant impacts may account for the observed large dispersion in the mass-radius relationship of close-in super-Earths and mini-Neptunes (at least to some extent).

Original languageEnglish (US)
Article number164
JournalAstrophysical Journal
Volume812
Issue number2
DOIs
StatePublished - Oct 20 2015

Fingerprint

planet
planets
Neptune
Neptune (planet)
envelopes
atmosphere
atmospheres
irradiation
hydrodynamics
refractory materials
degassing
helium
heat transfer
silicate
escape
convection
proximity
silicates
hydrogen
Earth mantle

Keywords

  • equation of state
  • hydrodynamics
  • planets and satellites: formation
  • planets and satellites: interiors
  • stars: individual (Kepler-36, Kepler-11)

ASJC Scopus subject areas

  • Nuclear and High Energy Physics

Cite this

GIANT IMPACT : AN EFFICIENT MECHANISM for the DEVOLATILIZATION of SUPER-EARTHS. / Liu, Shang Fei; Hori, Yasunori; Lin, D. N C; Asphaug, Erik.

In: Astrophysical Journal, Vol. 812, No. 2, 164, 20.10.2015.

Research output: Contribution to journalArticle

Liu, Shang Fei ; Hori, Yasunori ; Lin, D. N C ; Asphaug, Erik. / GIANT IMPACT : AN EFFICIENT MECHANISM for the DEVOLATILIZATION of SUPER-EARTHS. In: Astrophysical Journal. 2015 ; Vol. 812, No. 2.
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