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Artículo

A fading radius valley towards M dwarfs, a persistent density valley across stellar types

Venturini, J.; Ronco, María PaulaIcon ; Guilera, Octavio MiguelIcon ; Haldemann, J.; Mordasini, C.; Miller Bertolami, Marcelo MiguelIcon
Fecha de publicación: 05/2024
Editorial: EDP Sciences
Revista: Astronomy and Astrophysics
ISSN: 0004-6361
Idioma: Inglés
Tipo de recurso: Artículo publicado
Clasificación temática:
Astronomía

Resumen

The radius valley separating super-Earths from mini-Neptunes is a fundamental benchmark for theories of planet formation and evolution. Observations show that the location of the radius valley decreases with decreasing stellar mass and with increasing orbital period. Here, we build on our previous pebble-based formation model. Combined with photoevaporation after disc dispersal, it has allowed us to unveil the radius valley as a separator between rocky and water-worlds. In this study, we expand our model for a range of stellar masses spanning from 0.1 to 1.5 M⊙. We find that the location of the radius valley is well described by a power-law in stellar mass as Rvalley = 1.8197 M⋆0.14(+0.02/−0.01), which is in excellent agreement with observations. We also find very good agreement with the dependence of the radius valley on orbital period, both for FGK and M dwarfs. Additionally, we note that the radius valley gets filled towards low stellar masses, particularly at 0.1–0.4 M⊙, yielding a rather flat slope in Rvalley − Porb. This is the result of orbital migration occurring at lower planet mass for less massive stars, which allows for low-mass water-worlds to reach the inner regions of the system, blurring the separation in mass (and size) between rocky and water worlds. Furthermore, we find that for planetary equilibrium temperatures above 400 K, the water in the volatile layer exists fully in the form of steam, puffing the planet radius up (as compared to the radii of condensed-water worlds). This produces an increase in planet radii of ∼30% at 1 M⊕ and of ∼15% at 5 M⊕ compared to condensed-water worlds. As with Sun-like stars, we find that pebble accretion leaves its imprint on the overall exoplanet population as a depletion of planets with intermediate compositions (i.e. water mass fractions of ∼0 − 20%), carving an planet-depleted diagonal band in the mass-radius (MR) diagrams. This band is better visualised when plotting the planet’s mean density in terms of an Earth-like composition. This change in coordinates causes the valley to emerge for all the stellar mass cases.
Palabras clave: Planets and satellites: formation , Planets and satellites: interiors , Planets and satellites: composition
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info:eu-repo/semantics/openAccess Excepto donde se diga explícitamente, este item se publica bajo la siguiente descripción: Creative Commons Attribution 2.5 Unported (CC BY 2.5)
Identificadores
URI: http://hdl.handle.net/11336/246240
URL: https://www.aanda.org/10.1051/0004-6361/202349088
DOI: http://dx.doi.org/10.1051/0004-6361/202349088
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Articulos(IALP)
Articulos de INST.DE ASTROFISICA LA PLATA
Citación
Venturini, J.; Ronco, María Paula; Guilera, Octavio Miguel; Haldemann, J.; Mordasini, C.; et al.; A fading radius valley towards M dwarfs, a persistent density valley across stellar types; EDP Sciences; Astronomy and Astrophysics; 686; L9; 5-2024; 1-17
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