Ionized envelopes around protoplanets and the role of radiative feedback in gas accretion

Abstract

Planetary growth within protoplanetary disks involves accreting material from their surroundings, yet the underlying mechanisms and physical conditions of the accreting gas remain debated. This study aims to investigate the dynamics and thermodynamic properties of accreting gas giants, and to characterize the envelope that forms near the planet during accretion. We employ three-dimensional hydrodynamical simulations of a Jupiter-mass planet embedded in a viscous gaseous disk. Our models incorporate a non-isothermal energy equation to compute gas and radiation energy diffusion and include radiative feedback from the planet. Results indicate that gas accretion occurs supersonically towards the planet, forming an ionized envelope that extends from the planetary surface up to 0.2 times the Hill radius in the no-feedback model, and up to 0.4 times the Hill radius in the feedback model. The envelope's radius, or ionization radius, acts as a boundary halting supersonic gas inflow and is pivotal for estimating accretion rates and H$\alpha$ emission luminosities. Including radiative feedback increases accretion rates, especially within the ionization radius and from areas to the right of the planet when the star is positioned to the left. The accretion luminosities calculated at the ionization radius are substantially lower than those calculated at the Hill radius, highlighting potential misinterpretations in the non-detection of H$\alpha$ emissions as indicators of ongoing planet formation.