Characterising TOI-732 b and c: New insights into the M-dwarf radius and density valley

Abstract

TOI-732 is an M dwarf hosting two transiting planets that are located on the two opposite sides of the radius valley. By doubling the number of available space-based observations and increasing the number of radial velocity (RV) measurements, we aim at refining the parameters of TOI-732 b and c. We also use the results to study the slope of the radius valley and the density valley for a well-characterised sample of M-dwarf exoplanets. We performed a global MCMC analysis by jointly modelling ground-based light curves and CHEOPS and TESS observations, along with RV time series both taken from the literature and obtained with the MAROON-X spectrograph. The slopes of the M-dwarf valleys were quantified via a Support Vector Machine (SVM) procedure. TOI-732 b is an ultrashort-period planet (P0.77 d) with a radius Rb=1.325-0.058+0.057 R and a mass Mb=2.460.19 M (mean density b=5.8-0.8+1.0 g cm-3), while the outer planet at P12.25 d has Rc=2.39-0.11+0.10 R, Mc=8.04-0.48+0.50 M, and thus c=3.24-0.43+0.55 g cm-3. Also taking into account our interior structure calculations, TOI-732 b is a super-Earth and TOI-732 c is a mini-Neptune. Following the SVM approach, we quantified dRp,valley/dP=-0.065-0.013+0.024, which is flatter than for Sun-like stars. In line with former analyses, we note that the radius valley for M-dwarf planets is more densely populated, and we further quantify the slope of the density valley as dvalley/dP=-0.02-0.04+0.12. Compared to FGK stars, the weaker dependence of the position of the radius valley on the orbital period might indicate that the formation shapes the radius valley around M dwarfs more strongly than the evolution mechanisms.

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