Main sequence dynamo magnetic fields emerging in the white dwarf phase
Metadatos
Mostrar el registro completo del ítemAutor
Camisassa, Maria; Fuentes, José Rafael; Rebassa-Mansergas, A.; Torres, S.; Raddi, R.; Domínguez Aguilera, María InmaculadaEditorial
edp sciences
Materia
stars: evolution stars: interiors stars: magnetic field
Fecha
2024-11-26Referencia bibliográfica
Camisasa, M. et. al. A&A, 691, L21 (2024). [ https://doi.org/10.1051/0004-6361/202452539]
Patrocinador
RYC2021-032721-I, funded by MCIN/AEI/10.13039/501100011033 and by the European Union NextGenerationEU /PRTR; NASA Solar System Workings grant 80NSSC24K0927; FONDECYT (grant number 1221059) and eRO-STEP (grant SA 2131/15-2, project number 414059771); AGAUR/Generalitat de Catalunya grant SGR-386/2021, by the Spanish MINECO grant PID2020-117252GB-I00 and by PID2021-123110NB-I00 financed by MCIN/AEI/10.13039/501100011033/FEDER, UE; Munich Institute for Astro-, Particle and BioPhysics (MIAPbP), which is funded by the Deutsche Forschungsgemeinschaft (DFG, German Research Foundation) under Germany’s Excellence Strategy – EXC-2094 – 390783311Resumen
Recent observations of volume-limited samples of magnetic white dwarfs (WD) have revealed a higher incidence of magnetism in
older stars. Specifically, these studies indicate that magnetism is more prevalent in WDs with fully or partially crystallized cores than
in those with entirely liquid cores. This has led to the recognition of a crystallization-driven dynamo as an important mechanism for
explaining magnetism in isolated WDs. However, recent simulations have challenged the capability of this mechanism to generate
surface magnetic fields with the typical strengths detected in WDs. In this Letter, we explore an alternative hypothesis for the surface
emergence of magnetic fields in isolated WDs. Those with masses &0:55 M are the descendants of main sequence stars with convective
cores capable of generating strong dynamo magnetic fields. This idea is supported by asteroseismic evidence of strong magnetic
fields buried within the interiors of red giant branch stars. Assuming that these fields are disrupted by subsequent convective zones,
we estimated magnetic breakout times for WDs with carbon-oxygen (CO) cores and masses ranging from 0:57 M to 1:3 M . Due to
the significant uncertainties in breakout times stemming from the treatment of convective boundaries and mass-loss rates, we cannot
provide a precise prediction for the emergence time of the main sequence dynamo field. However, we can predict that this emergence
should occur during the WD phase for those objects with masses &0:65 M . We also find that the magnetic breakout is expected to
occur earlier in more massive WDs, which is consistent with observations of volume-limited samples and the well-established fact that
magnetic WDs tend to be more massive than non-magnetic ones. Moreover, within the uncertainties of stellar evolutionary models,
we find that the emergence of main sequence dynamo magnetic fields can account for a significant portion of the magnetic WDs.
Additionally, we estimated magnetic breakout times due to crystallization-driven dynamos in CO WDs; our results suggest that this
mechanism cannot explain the majority of magnetic WDs.





