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TOI-4010: A System of Three Large Short-period Planets with a Massive Long-period Companion

  • Authors: Michelle Kunimoto, Andrew Vanderburg, Chelsea X. Huang, M. Ryleigh Davis, Laura Affer, Andrew Collier Cameron, David Charbonneau, Rosario Cosentino, Mario Damasso, Xavier Dumusque, A. F. Martnez Fiorenzano, Adriano Ghedina, R. D. Haywood, Florian Lienhard, Mercedes López-Morales, Michel Mayor, Francesco Pepe, Matteo Pinamonti, Ennio Poretti, Jesús Maldonado, Ken Rice, Alessandro Sozzetti, Thomas G. Wilson, Stéphane Udry, Jay Baptista, Khalid Barkaoui, Juliette Becker, Paul Benni, Allyson Bieryla, Pau Bosch-Cabot, David R. Ciardi, Karen A. Collins, Kevin I. Collins, Elise Evans, Trent J. Dupuy, Maria V. Goliguzova, Pere Guerra, Adam Kraus, Jack J. Lissauer, Daniel Huber, Felipe Murgas, Enric Palle, Samuel N. Quinn, Boris S. Safonov, Richard P. Schwarz, Avi Shporer, Keivan G. Stassun, Jon M. Jenkins, David W. Latham, George R. Ricker, Sara Seager, Roland Vanderspek, Joshua Winn, Zahra Essack, Hannah M. Lewis, Mark E. Rose

Michelle Kunimoto et al 2023 The Astronomical Journal 166 .

  • Provider: AAS Journals

Caption: Figure 12.

Mass–radius diagram for planets with density known to better than 50% precision (﹩{\sigma }_{{\rho }_{p}}/{\rho }_{p}\lt 0.5﹩), plotted alongside the three transiting, short-period TOI-4010. Planets are colored by equilibrium temperature, which we recalculated assuming an albedo of 0 for uniformity. Mass–radius curves from Zeng et al. (2018) assuming 1000 K surface temperature for Earth-like rocky cores with no atmosphere or 0.1%, 1%, and 2% H2 envelopes by mass are overlaid in green, along with water-rich cores with 0.1%, 0.3%, and 1% H2 envelopes by mass (blue) and a pure rock composition (red).

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