The TESS-Keck Survey. XVIII. A Sub-Neptune and Spurious Long-period Signal in the TOI-1751 System

Author:

Desai AnmolORCID,Turtelboom Emma V.ORCID,Harada Caleb K.ORCID,Dressing Courtney D.ORCID,Rice David R.ORCID,Murphy Joseph M. AkanaORCID,Brinkman Casey L.ORCID,Chontos AshleyORCID,Crossfield Ian J. M.,Dai FeiORCID,Hill Michelle L.ORCID,Fetherolf TaraORCID,Giacalone StevenORCID,Howard Andrew W.ORCID,Huber DanielORCID,Isaacson HowardORCID,Kane Stephen R.ORCID,Lubin JackORCID,MacDougall Mason G.ORCID,Mayo Andrew W.ORCID,Močnik TeoORCID,Polanski Alex S.ORCID,Rice MalenaORCID,Robertson PaulORCID,Rubenzahl Ryan A.ORCID,Van Zandt JudahORCID,Weiss Lauren M.ORCID,Bieryla AllysonORCID,Buchhave Lars A.ORCID,Jenkins Jon M.ORCID,Kostov Veselin B.ORCID,Levine Alan M.ORCID,Lillo-Box JorgeORCID,Paegert M.ORCID,Rabus MarkusORCID,Seager S.ORCID,Stassun Keivan G.ORCID,Ting Eric B.ORCID,Watanabe DavidORCID,Winn Joshua N.ORCID

Abstract

Abstract We present and confirm TOI-1751 b, a transiting sub-Neptune orbiting a slightly evolved, solar-type, metal-poor star (T eff = 5996 ± 110 K, log ( g ) = 4.2 ± 0.1 , V = 9.3 mag, [Fe/H] = −0.40 ± 0.06 dex) every 37.47 days. We use TESS photometry to measure a planet radius of 2.77 0.07 + 0.15 R . We also use both Keck/HIRES and APF/Levy radial velocities (RV) to derive a planet mass of 14.5 3.14 + 3.15 M , and thus a planet density of 3.6 ± 0.9 g cm−3. There is also a long-period (∼400 days) signal that is observed in only the Keck/HIRES data. We conclude that this long-period signal is not planetary in nature and is likely due to the window function of the Keck/HIRES observations. This highlights the role of complementary observations from multiple observatories to identify and exclude aliases in RV data. Finally, we investigate the potential compositions of this planet, including rocky and water-rich solutions, as well as theoretical irradiated ocean models. TOI-1751 b is a warm sub-Neptune with an equilibrium temperature of ∼820 K. As TOI-1751 is a metal-poor star, TOI-1751 b may have formed in a water-enriched formation environment. We thus favor a volatile-rich interior composition for this planet.

Funder

Heising-Simons Foundation

National Science Foundation

Alfred P. Sloan Foundation

National Aeronautics and Space Administration

David and Lucile Packard Foundation

Publisher

American Astronomical Society

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