Off-centre convective zones in mass accreting stellar models

We report the physical origin of transient off-centre convective zones (oCZs) that arise in mass accreting stellar models. Using detailed MESA simulations of binary evolution, we find that these oCZs are not numerical artefacts, but emerge due to a local increase in density near the retreating edge of the convective core. The density enhancement raises the local opacity, which amplifies the radiative temperature gradient ∇ rad . If this gradient surpasses the Ledoux threshold ∇ L , defined by both thermal and compositional stratification, the region becomes convectively unstable. The resulting oCZs are detached from the convective core and transient: mixing within the oCZ erases the local gradient in mean molecular weight and leaves a sharp ∇ μ discontinuity at the boundary, thus stabilising the adjacent layers. This mechanism naturally explains the presence and evolution of oCZs, as previously reported in massive interacting stars.

Authors

Publication Details

Journal
Astronomy and Astrophysics
Published
2025-08-29
DOI
https://doi.org/10.1051/0004-6361/202555298
Citations
2
Primary Topic
Astrophysics and Star Formation Studies
Type
article
Field-Weighted Citation Impact
2.31

Funders

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article

Off-centre convective zones in mass accreting stellar models

A. Miszuda
2 citations
Astronomy and Astrophysics
Astrophysics and Star Formation Studies
2.31
article

Off-centre convective zones in mass accreting stellar models

A. Miszuda
article en
2 citations

Abstract

We report the physical origin of transient off-centre convective zones (oCZs) that arise in mass accreting stellar models. Using detailed MESA simulations of binary evolution, we find that these oCZs are not numerical artefacts, but emerge due to a local increase in density near the retreating edge of the convective core. The density enhancement raises the local opacity, which amplifies the radiative temperature gradient ∇ rad . If this gradient surpasses the Ledoux threshold ∇ L , defined by both thermal and compositional stratification, the region becomes convectively unstable. The resulting oCZs are detached from the convective core and transient: mixing within the oCZ erases the local gradient in mean molecular weight and leaves a sharp ∇ μ discontinuity at the boundary, thus stabilising the adjacent layers. This mechanism naturally explains the presence and evolution of oCZs, as previously reported in massive interacting stars.

Astronomy and AstrophysicsVol. 701
Narodowe Centrum Nauki
Openalex Percentile: Top 10%
Astrophysics and Star Formation Studies
2.31
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