TY - JOUR
T1 - Refining the transit-timing and photometric analysis of TRAPPIST-1
T2 - Masses, Radii, densities, dynamics, and ephemerides
AU - Agol, Eric
AU - Dorn, Caroline
AU - Grimm, Simon L.
AU - Turbet, Martin
AU - Ducrot, Elsa
AU - Delrez, Laetitia
AU - Gillon, Michaël
AU - Demory, Brice Olivier
AU - Burdanov, Artem
AU - Barkaoui, Khalid
AU - Benkhaldoun, Zouhair
AU - Bolmont, Emeline
AU - Burgasser, Adam
AU - Carey, Sean
AU - De Wit, Julien
AU - Fabrycky, Daniel
AU - Foreman-Mackey, Daniel
AU - Haldemann, Jonas
AU - Hernandez, David M.
AU - Ingalls, James
AU - Jehin, Emmanuel
AU - Langford, Zachary
AU - Leconte, Jérémy
AU - Lederer, Susan M.
AU - Luger, Rodrigo
AU - Malhotra, Renu
AU - Meadows, Victoria S.
AU - Morris, Brett M.
AU - Pozuelos, Francisco J.
AU - Queloz, Didier
AU - Raymond, Sean N.
AU - Selsis, Franck
AU - Sestovic, Marko
AU - Triaud, Amaury H.M.J.
AU - Van Grootel, Valerie
N1 - Publisher Copyright:
© 2021. The Author(s).
PY - 2021/2
Y1 - 2021/2
N2 - 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 Earthlike 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.
AB - 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 Earthlike 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.
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U2 - 10.3847/PSJ/abd022
DO - 10.3847/PSJ/abd022
M3 - Article
AN - SCOPUS:85102358014
SN - 2632-3338
VL - 2
JO - Planetary Science Journal
JF - Planetary Science Journal
IS - 1
M1 - 1
ER -