2015ApJ...812..164L


Query : 2015ApJ...812..164L

2015ApJ...812..164L - Astrophys. J., 812, 164 (2015/October-3)

Giant impact: an efficient mechanism for the devolatilization of super-earths.

LIU S.-F., HORI Y., LIN D.N.C. and ASPHAUG E.

Abstract (from CDS):

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). ApJ99962\subject_ section 078 Exoplanets

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

Simbad objects: 6

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Number of rows : 6
N Identifier Otype ICRS (J2000)
RA
ICRS (J2000)
DEC
Mag U Mag B Mag V Mag R Mag I Sp type #ref
1850 - 2026
#notes
1 Kepler-36c Pl 19 25 00.0428079600 +49 13 54.630900876           ~ 133 1
2 Kepler-36b Pl 19 25 00.0428079600 +49 13 54.630900876           ~ 163 1
3 Kepler-36 Er* 19 25 00.0428079600 +49 13 54.630900876   12.795 12.174 12.094   F2 251 1
4 Kepler-11 Er* 19 48 27.6226218768 +41 54 32.903163504   14.635 13.838 13.742   G2V 377 1
5 Kepler-11c Pl 19 48 27.6226218768 +41 54 32.903163504           ~ 119 1
6 Kepler-11b Pl 19 48 27.6226218768 +41 54 32.903163504           ~ 159 1

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