Bibcode
Guenther, E. W.; Barragán, O.; Dai, F.; Gandolfi, D.; Hirano, T.; Fridlund, M.; Fossati, L.; Chau, A.; Helled, R.; Korth, J.; Prieto-Arranz, J.; Nespral, D.; Antoniciello, G.; Deeg, H.; Hjorth, M.; Grziwa, S.; Albrecht, S.; Hatzes, A. P.; Rauer, H.; Csizmadia, Sz.; Smith, A. M. S.; Cabrera, J.; Narita, N.; Arriagada, P.; Burt, J.; Butler, R. P.; Cochran, W. D.; Crane, J. D.; Eigmüller, Ph.; Erikson, A.; Johnson, J. A.; Kiilerich, A.; Kubyshkina, D.; Palle, E.; Persson, C. M.; Pätzold, M.; Sabotta, S.; Sato, B.; Shectman, St. A.; Teske, J. K.; Thompson, I. B.; Van Eylen, V.; Nowak, G.; Vanderburg, A.; Winn, J. N.; Wittenmyer, R. A.
Referencia bibliográfica
Astronomy and Astrophysics, Volume 608, id.A93, 10 pp.
Fecha de publicación:
12
2017
Revista
Número de citas
61
Número de citas referidas
57
Descripción
Aims: Planets in the mass range from 2 to 15 M⊕
are very diverse. Some of them have low densities, while others are very
dense. By measuring the masses and radii, the mean densities, structure,
and composition of the planets are constrained. These parameters also
give us important information about their formation and evolution, and
about possible processes for atmospheric loss. Methods: We
determined the masses, radii, and mean densities for the two transiting
planets orbiting K2-106. The inner planet has an ultra-short period of
0.57 days. The period of the outer planet is 13.3 days. Results:
Although the two planets have similar masses, their densities are very
different. For K2-106b we derive
Mb=8.36-0.94+0.96 M⊕,
Rb = 1.52 ± 0.16 R⊕, and a high
density of 13.1-3.6+5.4 g cm-3. For
K2-106c, we find Mc=5.8-3.0+3.3
M⊕, Rc=2.50-0.26+0.27
R⊕ and a relatively low density of
2.0-1.1+1.6 g cm-3. Conclusions:
Since the system contains two planets of almost the same mass, but
different distances from the host star, it is an excellent laboratory to
study atmospheric escape. In agreement with the theory of
atmospheric-loss processes, it is likely that the outer planet has a
hydrogen-dominated atmosphere. The mass and radius of the inner planet
is in agreement with theoretical models predicting an iron core
containing 80-30+20% of its mass. Such a high
metal content is surprising, particularly given that the star has an
ordinary (solar) metal abundance. We discuss various possible formation
scenarios for this unusual planet.
The results are partly based on observations obtained at the European
Southern Observatory at Paranal, Chile in program 098.C-0860(A). This
paper includes data gathered with the 6.5 m Magellan Telescopes located
at Las Campanas Observatory, Chile. The article is also partly based on
observations with the TNG, NOT. This work has also made use of data from
the European Space Agency (ESA) mission Gaia (http://https://www.cosmos.esa.int/gaia),
processed by the Gaia Data Processing and Analysis Consortium (DPAC, http://https://www.cosmos.esa.int/web/gaia/dpac/consortium).The
RV measurements are only available at the CDS via anonymous ftp to http://cdsarc.u-strasbg.fr (http://130.79.128.5) or via http://cdsarc.u-strasbg.fr/viz-bin/qcat?J/A+A/608/A93
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