Issue |
A&A
Volume 641, September 2020
|
|
---|---|---|
Article Number | A92 | |
Number of page(s) | 14 | |
Section | Planets and planetary systems | |
DOI | https://doi.org/10.1051/0004-6361/202038187 | |
Published online | 14 September 2020 |
Characterization of the K2-38 planetary system
Unraveling one of the densest planets known to date★,★★
1
Instituto de Astrofísica de Canarias,
38205
La Laguna,
Tenerife, Spain
e-mail: btoledo@iac.es
2
Universidad de La Laguna, Departamento de Astrofísica,
38206
La Laguna,
Tenerife, Spain
3
Observatoire Astronomique de l’Université de Genève,
51 chemin des Maillettes,
1290
Versoix, Switzerland
4
Instituto de Astrofísica e Ciências do Espaço, Universidade do Porto, CAUP, Rua das Estrelas,
4150-762
Porto, Portugal
5
Departamento de Física e Astronomia, Faculdade de Ciências, Universidade do Porto, Rua do Campo Alegre,
4169-007
Porto, Portugal
6
INAF Osservatorio Astrofisico di Torino,
Via Osservatorio 20,
10025
Pino Torinese, Italy
7
Centro de Astrobiología (CSIC-INTA),
Carretera de Ajalvir km 4,
28850
Torrejón de Ardoz,
Madrid, Spain
8
Consejo Superior de Investigaciones Científicas,
28006
Madrid, Spain
9
INAF Osservatorio Astronomico di Trieste,
Via G. Tiepolo 11,
34143
Trieste, Italy
10
Centro de Astrobiología (CAB, CSIC-INTA), Dpto. de Astrofísica, ESAC campus 28692 Villanueva de la Cañada,
Madrid, Spain
11
Scuola Normale Superiore,
Piazza dei Cavalieri, 7,
56126
Pisa, Italy
12
European Southern Observatory,
Alonso de Córdova 3107,
Vitacura Casilla
19001,
Santiago 19,
Chile
13
European Southern Observatory,
Karl-Schwarzschild-Str. 2,
85748
Garching bei München, Germany
14
INAF Osservatorio Astronomico di Palermo,
Piazza del Parlamento 1,
90134
Palermo, Italy
15
Instituto de Astrofísica e Ciências do Espaço, Universidade de Lisboa,
Edifício C8,
1749-016
Lisboa, Portugal
16
Departamento de Física da Faculdade de Ciências da Universidade de Lisboa,
Edifício C8,
1749-016
Lisboa, Portugal
17
Physikalisches Institut & Center for Space and Habitability, Universität Bern,
Gesellschaftsstrasse 6,
3012
Bern,
Switzerland
18
INAF Osservatorio Astronomico di Brera,
Via E. Bianchi 46,
23807
Merate, Italy
19
INAF Osservatorio Astronomico di Padova,
Vicolo dell’Osservatorio 5,
35122
Padova, Italy
20
Centro de Astrofísica da Universidade do Porto,
Rua das Estrelas,
4150-762
Porto, Portugal
21
Institute for Fundamental Physics of the Universe,
Via Beirut 2,
34151
Miramare,
Trieste, Italy
22
Fundación Galileo Galilei, INAF,
Rambla José Ana Fern2ndez Pérez 7,
38712
Breña Baja, Spain
Received:
17
April
2020
Accepted:
26
June
2020
Context. An accurate characterization of the known exoplanet population is key to understanding the origin and evolution of planetary systems. Determining true planetary masses through the radial velocity (RV) method is expected to experience a great improvement thanks to the availability of ultra-stable echelle spectrographs.
Aims. We took advantage of the extreme precision of the new-generation echelle spectrograph ESPRESSO to characterize the transiting planetary system orbiting the G2V star K2-38 located at 194 pc from the Sun with V ~ 11.4. This system is particularly interesting because it could contain the densest planet detected to date.
Methods. We carried out a photometric analysis of the available K2 photometric light curve of this star to measure the radius of its two known planets, K2-38b and K2-38c, with Pb = 4.01593 ± 0.00050 d and Pc = 10.56103 ± 0.00090 d, respectively. Using 43 ESPRESSO high-precision RV measurements taken over the course of 8 months along with the 14 previously published HIRES RV measurements, we modeled the orbits of the two planets through a Markov chain Monte Carlo analysis, significantly improving their mass measurements.
Results. Using ESPRESSO spectra, we derived the stellar parameters, Teff = 5731 ± 66, log g = 4.38 ± 0.11 dex, and [Fe/H] = 0.26 ± 0.05 dex, and thus the mass and radius of K2-38, M⋆ = 1.03−0.02+0.04 M⊕ and R⋆ = 1.06−0.06+0.09 R⊕. We determine new values for the planetary properties of both planets. We characterize K2-38b as a super-Earth with RP = 1.54 ± 0.14 R⊕ and Mp = 7.3−1.0+1.1 M⊕, and K2-38c as a sub-Neptune with RP = 2.29 ± 0.26 R⊕ and Mp = 8.3−1.3+1.3 M⊕. Combining the radius and mass measurements, we derived a mean density of ρp = 11.0−2.8+4.1 g cm−3 for K2-38b and ρp = 3.8−1.1+1.8 g cm−3 for K2-38c, confirming K2-38b as one of the densest planets known to date.
Conclusions. The best description for the composition of K2-38b comes from an iron-rich Mercury-like model, while K2-38c is better described by a rocky-model with H2 envelope. The maximum collision stripping boundary shows how giant impacts could be the cause for the high density of K2-38b. The irradiation received by each planet places them on opposite sides of the radius valley. We find evidence of a long-period signal in the RV time-series whose origin could be linked to a 0.25–3 MJ planet or stellar activity.
Key words: techniques: radial velocities / techniques: photometric / instrumentation: spectrographs / stars: individual: K2-38 / planets and satellites: detection / planets and satellites: composition
The ESPRESSO RVs used in this paper are only available at the CDS via anonymous ftp to cdsarc.u-strasbg.fr (130.79.128.5) or via http://cdsarc.u-strasbg.fr/viz-bin/cat/J/A+A/641/A92
© ESO 2020
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