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.

Publication Details

Journal
Springer Link (Chiba Institute of Technology)
Published
2025-09-08
DOI
https://doi.org/10.1051/0004-6361/202555298/pdf
Primary Topic
Geochemistry and Geologic Mapping
Type
article
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article

Off-centre convective zones in mass accreting stellar models

Springer Link (Chiba Institute of Technology)
Geochemistry and Geologic Mapping
article

Off-centre convective zones in mass accreting stellar models

article en

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.

Springer Link (Chiba Institute of Technology)
Openalex Percentile: Top 51%
Geochemistry and Geologic Mapping
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