DISCOVERY AND VALIDATION OF A HIGH-DENSITY SUB-NEPTUNE FROM THE K2 MISSION
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Author
Espinoza, NestorBrahm, Rafael
Jordan, Andres
Jenkins, James S.
Rojas, Felipe
Jofre, Paula
Madler, Thomas
Rabus, Markus

Chaname, Julio
Pantoja, Blake
Soto, Maritza G.
Morzinski, Katie M.

Males, Jared R.

Ward-Duong, Kimberly
Close, Laird M.

Affiliation
Univ Arizona, Steward ObservIssue Date
2016-10-10Keywords
planets and satellites: compositionplanets and satellites: detection
planets and satellites: fundamental parameters
planets and satellites: terrestrial planets
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IOP PUBLISHING LTDCitation
DISCOVERY AND VALIDATION OF A HIGH-DENSITY SUB-NEPTUNE FROM THE K2 MISSION 2016, 830 (1):43 The Astrophysical JournalJournal
The Astrophysical JournalRights
© 2016. The American Astronomical Society. All rights reserved.Collection Information
This item from the UA Faculty Publications collection is made available by the University of Arizona with support from the University of Arizona Libraries. If you have questions, please contact us at repository@u.library.arizona.edu.Abstract
We report the discovery of K2-56b, a high-density sub-Neptune exoplanet, made using photometry from Campaign 4 of the two-wheeled Kepler (K2) mission, ground-based radial velocity (RV) follow-up from HARPS and high-resolution lucky and adaptive optics imaging obtained using AstraLux and MagAO, respectively. The host star is a bright (V - 11.04, K-s - 9.37), slightly metal-poor ([Fe/H] - -0.15 +/- 0.05 dex) solar analogue located at 152.1(-7.4)(+9.7) pc from Earth, for which we find a radius of R-* = 0.928(-04040)(+0.055) and a mass of M-* = 0.961(-0.029)(+0.032) M-circle dot. A joint analysis of the K2 photometry and HARPS RVs reveal that the planet is in a approximate to 42 day orbit around its host star, has a radius of 2.23(011)(+0.14)R(circle plus), and a mass of 16.3(6.1)(+6.0) M-circle plus. Although the data at hand put the planet in the region of the massradius diagram where we could expect planets with a pure rock (i.e., magnesium silicate) composition using two-layer models (i.e., between rock/iron and rock/ice compositions), we discuss more realistic three-layer composition models which can explain the high density of the discovered exoplanet. The fact that the planet lies in the boundary between "possibly rocky" and "non-rocky" exoplanets makes it an interesting planet for future RV follow-up.ISSN
1538-4357Version
Final published versionSponsors
CONICYT-PCHA/Doctorado Nacional.; FONDECYT [1130857]; Ministry for the Economy, Development, and Tourism Programa Iniciativa Cientifica Milenio [IC 120009]; BASAL CATA [PFB-06]; NASA Science Mission directorate; ESO programmes [096.C-0499(A), 096.C-0417(A), 096.D-0402(A)]Additional Links
http://stacks.iop.org/0004-637X/830/i=1/a=43?key=crossref.2397df04f9f37c10f54db77ec5ee83f5ae974a485f413a2113503eed53cd6c53
10.3847/0004-637X/830/1/43