Bibcode
Löbling, L.; Boffin, H. M. J.; Jones, D.
Referencia bibliográfica
Astronomy and Astrophysics, Volume 624, id.A1, 26 pp.
Fecha de publicación:
4
2019
Revista
Número de citas
5
Número de citas referidas
4
Descripción
Context. Barium stars are peculiar red giants characterized by an
overabundance of the elements synthesized in the slow neutron-capture
nucleosynthesis (s-process elements) along with an enrichment in carbon.
These stars are discovered in binaries with white dwarf companions. The
more recently formed of these stars are still surrounded by a planetary
nebula. Aims: Precise abundance determinations of the various
s-process elements, of further key elements that act as indicators for
effectiveness of nucleosynthesis on the asymptotic giant branch and,
especially, of the lightest, short-lived radionuclide technetium will
establish constraints for the formation of s-process elements in
asymptotic giant branch stars as well as mass transfer through, for
example, stellar wind, Roche-lobe overflow, and common-envelope
evolution. Methods: We performed a detailed spectral analysis of
the K-type subgiant central star of the planetary nebula Hen 2-39 based
on high-resolution optical spectra obtained with the Ultraviolet and
Visual Echelle Spectrograph at the Very Large Telescope using local
thermodynamic equilibrium model atmospheres. Results: We confirm
the effective temperature of Teff = (4350 ± 150) K for
the central star of the planetary nebula Hen 2-39. It has a photospheric
carbon enrichment of [C/H] = 0.36 ± 0.08 and a barium
overabundance of [Ba/Fe] = 1.8 ± 0.5. We find a deficiency for
most of the iron-group elements (calcium to iron) and establish an upper
abundance limit for technetium (log ɛTc < 2.5).
Conclusions: The quality of the available optical spectra is not
sufficient to measure abundances of all s-process elements accurately.
Despite large uncertainties on the abundances as well as on the model
yields, the derived abundances are most consistent with a progenitor
mass in the range 1.75-3.00 M⊙ and a metallicity of
[Fe/H] = -0.3 ± 1.0. This result leads to the conclusion that the
formation of such systems requires a relatively large mass transfer that
is most easily obtained via wind-Roche lobe overflow.
Based on data products from observations made with ESO Telescopes at the
La Silla Paranal Observatory under program ID 093.D-0332(A).
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