The Astrophysical Journal Letters (Jan 2024)

TOI-1685 b Is a Hot Rocky Super-Earth: Updates to the Stellar and Planet Parameters of a Popular JWST Cycle 2 Target

  • Jennifer A. Burt,
  • Matthew J. Hooton,
  • Eric E. Mamajek,
  • Oscar Barragán,
  • Sarah C. Millholland,
  • Tyler R. Fairnington,
  • Chloe Fisher,
  • Samuel P. Halverson,
  • Chelsea X. Huang,
  • Madison Brady,
  • Andreas Seifahrt,
  • Eric Gaidos,
  • Rafael Luque,
  • David Kasper,
  • Jacob L. Bean

DOI
https://doi.org/10.3847/2041-8213/ad5b52
Journal volume & issue
Vol. 971, no. 1
p. L12

Abstract

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We present an updated characterization of the TOI-1685 planetary system, which consists of a P _b = 0.69 day ultra-short-period super-Earth planet orbiting a nearby ( d = 37.6 pc) M2.5V star (TIC 28900646, 2MASS J04342248+4302148). This planet was previously featured in two contemporaneous discovery papers, but the best-fit planet mass, radius, and bulk density values were discrepant, allowing it to be interpreted either as a hot, bare rock or a 50% H _2 O/50% MgSiO _3 water world. TOI-1685 b will be observed in three independent JWST Cycle 2 programs, two of which assume the planet is a water world, while the third assumes that it is a hot rocky planet. Here we include a refined stellar classification with a focus on addressing the host star’s metallicity, an updated planet radius measurement that includes two sectors of TESS data and multicolor photometry from a variety of ground-based facilities, and a more accurate dynamical mass measurement from a combined CARMENES, InfraRed Doppler, and MAROON-X radial velocity data set. We find that the star is very metal-rich ([Fe/H] ≃ +0.3) and that the planet is systematically smaller, lower mass, and higher density than initially reported, with new best-fit parameters of R _pl = 1.468 ${}_{-0.051}^{+0.050}$ R _⊕ and M _pl = ${3.03}_{-0.32}^{+0.33}$ M _⊕ . These results fall in between the previously derived values and suggest that TOI-1685 b is a hot rocky planet with an Earth-like density ( ρ _pl = 5.3 ± 0.8 g cm ^−3 , or 0.96 ρ _⊕ ), high equilibrium temperature ( T _eq = 1062 ± 27 K), and negligible volatiles, rather than a water world.

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