Refining the Transit-timing and Photometric Analysis of TRAPPIST-1: Masses, Radii, Densities, Dynamics, and Ephemerides

Author:

Agol EricORCID,Dorn CarolineORCID,Grimm Simon L.ORCID,Turbet MartinORCID,Ducrot ElsaORCID,Delrez LaetitiaORCID,Gillon MichaëlORCID,Demory Brice-OlivierORCID,Burdanov ArtemORCID,Barkaoui KhalidORCID,Benkhaldoun ZouhairORCID,Bolmont EmelineORCID,Burgasser AdamORCID,Carey SeanORCID,de Wit JulienORCID,Fabrycky DanielORCID,Foreman-Mackey DanielORCID,Haldemann JonasORCID,Hernandez David M.ORCID,Ingalls JamesORCID,Jehin EmmanuelORCID,Langford ZacharyORCID,Leconte JérémyORCID,Lederer Susan M.ORCID,Luger RodrigoORCID,Malhotra RenuORCID,Meadows Victoria S.ORCID,Morris Brett M.ORCID,Pozuelos Francisco J.ORCID,Queloz DidierORCID,Raymond Sean N.ORCID,Selsis FranckORCID,Sestovic MarkoORCID,Triaud Amaury H. M. J.ORCID,Grootel Valerie VanORCID

Abstract

Abstract We have collected transit times for the TRAPPIST-1 system with the Spitzer Space Telescope over four years. We add to these ground-based, HST, and K2 transit-time measurements, and revisit an N-body dynamical analysis of the seven-planet system using our complete set of times from which we refine the mass ratios of the planets to the star. We next carry out a photodynamical analysis of the Spitzer light curves to derive the density of the host star and the planet densities. We find that all seven planets’ densities may be described with a single rocky mass–radius relation which is depleted in iron relative to Earth, with Fe 21 wt% versus 32 wt% for Earth, and otherwise Earth-like in composition. Alternatively, the planets may have an Earth-like composition but enhanced in light elements, such as a surface water layer or a core-free structure with oxidized iron in the mantle. We measure planet masses to a precision of 3%–5%, equivalent to a radial-velocity (RV) precision of 2.5 cm s−1, or two orders of magnitude more precise than current RV capabilities. We find the eccentricities of the planets are very small, the orbits are extremely coplanar, and the system is stable on 10 Myr timescales. We find evidence of infrequent timing outliers, which we cannot explain with an eighth planet; we instead account for the outliers using a robust likelihood function. We forecast JWST timing observations and speculate on possible implications of the planet densities for the formation, migration, and evolution of the planet system.

Publisher

American Astronomical Society

Subject

Space and Planetary Science,Earth and Planetary Sciences (miscellaneous),Geophysics,Astronomy and Astrophysics

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