BULK COMPOSITION OF GJ 1214b AND OTHER SUB-NEPTUNE EXOPLANETS

GJ 1214b stands out among the detected low-mass exoplanets, because it is, so far, the only one amenable to transmission spectroscopy. Up to date there is no consensus about the composition of its envelope although most studies suggest a high molecular weight atmosphere. In particular, it is unclear if hydrogen and helium are present or if the atmosphere is water dominated. Here, we present results on the composition of the envelope obtained by using an internal structure and evolutionary model to fit the mass and radius data. By examining all possible mixtures of water and H/He, with the corresponding opacities, we find that the bulk amount of H/He of GJ 1214b is at most 7% by mass. In general, we find the radius of warm sub-Neptunes to be most sensitive to the amount of H/He. We note that all (Kepler-11b,c,d,f, Kepler-18b, Kepler-20b, 55Cnc-e, Kepler-36c, and Kepler-68b) but two (Kepler-11e and Kepler-30b) of the discovered low-mass planets so far have less than 10% H/He. In fact, Kepler-11e and Kepler-30b have 10%-18% and 5%-15% bulk H/He. Conversely, little can be determined about the H2O or rocky content of sub-Neptune planets. We find that although a 100% water composition fits the data for GJ 1214b, based on formation constraints the presence of heavier refractory material on this planet is expected, and hence, so is a component lighter than water required. The same is true for Kepler-11f. A robust determination by transmission spectroscopy of the composition of the upper atmosphere of GJ 1214b will help determine the extent of compositional segregation between the atmosphere and the envelope.

[1]  Nikole K. Lewis,et al.  SPITZER TRANSITS OF THE SUPER-EARTH GJ1214b AND IMPLICATIONS FOR ITS ATMOSPHERE , 2012, 1301.6763.

[2]  E. Guinan,et al.  Atmospheric Loss of Exoplanets Resulting from Stellar X-Ray and Extreme-Ultraviolet Heating , 2003 .

[3]  D. Sokoloff,et al.  Sunspot cycles and Grand Minima, Solar and Stellar Variability: Impact on Earth and Planets , 2010 .

[4]  M. Marley,et al.  Line and Mean Opacities for Ultracool Dwarfs and Extrasolar Planets , 2007, 0706.2374.

[5]  Sara Seager,et al.  THE OPTICAL AND NEAR-INFRARED TRANSMISSION SPECTRUM OF THE SUPER-EARTH GJ 1214b: FURTHER EVIDENCE FOR A METAL-RICH ATMOSPHERE , 2011, 1109.0582.

[6]  S. Seager,et al.  THREE POSSIBLE ORIGINS FOR THE GAS LAYER ON GJ 1214b , 2009, 0912.3243.

[7]  M. R. Haas,et al.  A closely packed system of low-mass, low-density planets transiting Kepler-11 , 2011, Nature.

[8]  J. Fortney,et al.  THE NATURE OF THE ATMOSPHERE OF THE TRANSITING SUPER-EARTH GJ 1214b , 2010, 1001.0976.

[9]  J. Koppenhoefer,et al.  Optical to near-infrared transit observations of super-Earth GJ 1214b: water-world or mini-Neptune? , 2011, 1111.2628.

[10]  H. F. Astrophysics,et al.  Internal structure of massive terrestrial planets , 2005, astro-ph/0511150.

[11]  T. Guillot,et al.  Composition and fate of short-period super-Earths: The case of CoRoT-7b , 2009, 0907.3067.

[12]  Howard Isaacson,et al.  ALL SIX PLANETS KNOWN TO ORBIT KEPLER-11 HAVE LOW DENSITIES , 2013, 1303.0227.

[13]  S. Seager,et al.  A FRAMEWORK FOR QUANTIFYING THE DEGENERACIES OF EXOPLANET INTERIOR COMPOSITIONS , 2009, 0912.3288.

[14]  Norman Murray,et al.  BROADBAND TRANSMISSION SPECTROSCOPY OF THE SUPER-EARTH GJ 1214b SUGGESTS A LOW MEAN MOLECULAR WEIGHT ATMOSPHERE , 2011, 1104.0011.

[15]  Tilman Spohn,et al.  Rocky super-Earth interiors. Structure and internal dynamics of CoRoT-7b and Kepler-10b , 2012 .

[16]  M. Ikoma,et al.  IN SITU ACCRETION OF HYDROGEN-RICH ATMOSPHERES ON SHORT-PERIOD SUPER-EARTHS: IMPLICATIONS FOR THE KEPLER-11 PLANETS , 2012, 1204.5302.

[17]  Jonathan J. Fortney,et al.  HOW THERMAL EVOLUTION AND MASS-LOSS SCULPT POPULATIONS OF SUPER-EARTHS AND SUB-NEPTUNES: APPLICATION TO THE KEPLER-11 SYSTEM AND BEYOND , 2012, 1205.0010.

[18]  et al,et al.  The CoRoT space mission : early results Special feature Transiting exoplanets from the CoRoT space mission VIII . CoRoT-7 b : the first super-Earth with measured radius , 2009 .

[19]  K. Lodders Solar System Abundances and Condensation Temperatures of the Elements , 2003 .

[20]  David Charbonneau,et al.  THE GJ1214 SUPER-EARTH SYSTEM: STELLAR VARIABILITY, NEW TRANSITS, AND A SEARCH FOR ADDITIONAL PLANETS , 2010, 1012.0518.

[21]  Jacob L. Bean,et al.  A ground-based transmission spectrum of the super-Earth exoplanet GJ 1214b , 2010, Nature.

[22]  Diana Valencia,et al.  Detailed Models of Super-Earths: How Well Can We Infer Bulk Properties? , 2007, 0704.3454.

[23]  “Hot Jupiters” , 2006 .

[24]  A. Watson,et al.  The dynamics of a rapidly escaping atmosphere: Applications to the evolution of Earth and Venus , 1981 .

[25]  Gilles Chabrier,et al.  An Equation of State for Low-Mass Stars and Giant Planets , 1995 .

[26]  T. Guillot On the radiative equilibrium of irradiated planetary atmospheres , 2010, 1006.4702.

[27]  S. Seager,et al.  Ocean Planet or Thick Atmosphere: On the Mass-Radius Relationship for Solid Exoplanets with Massive Atmospheres , 2007, 0710.4941.

[28]  Wolfgang Wagner,et al.  A Fundamental Equation for Water Covering the Range from the Melting Line to 1273 K at Pressures up to 25 000 MPa , 1989 .

[29]  T. Barman,et al.  HIGH-RESOLUTION, DIFFERENTIAL, NEAR-INFRARED TRANSMISSION SPECTROSCOPY OF GJ 1214b , 2011, 1104.1173.

[30]  David R. Alexander,et al.  Low-Temperature Rosseland Opacities , 1975 .

[31]  R. Redmer,et al.  THERMAL EVOLUTION AND STRUCTURE MODELS OF THE TRANSITING SUPER-EARTH GJ 1214b , 2010, 1010.0277.

[32]  Xavier Bonfils,et al.  A super-Earth transiting a nearby low-mass star , 2009, Nature.

[33]  J. Fortney,et al.  OBSERVATIONAL EVIDENCE FOR A METAL-RICH ATMOSPHERE ON THE SUPER-EARTH GJ1214b , 2011, 1103.2370.

[34]  W. Hubbard,et al.  Structure and evolution of Uranus and Neptune , 1980 .