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Astron. Astrophys. 359, 191-212 (2000)
Abundance evolution of intermediate mass elements (C to Zn) in the Milky Way halo and disk
A. Goswami 1 and
N. Prantzos 2
1 Indian Institute of Astrophysics, Bangalore, 560034, India (aruna@iiap.ernet.in)
2 Institut d'Astrophysique de Paris, C.N.R.S., 98 bis Bd. Arago, 75014 Paris, France (prantzos@iap.fr)
Received 25 January 2000 / Accepted 16 May 2000
Abstract
We present a comprehensive study of the evolution of the abundances
of intermediate mass elements, from C to Zn, in the Milky Way halo and
in the local disk. We use a consistent model to describe the evolution
of those two galactic subsystems. The halo and the disk are assumed to
evolve independently, both starting with gas of primordial
composition, and in different ways: strong outflow is assumed to take
place during the 1 Gyr of the halo
formation, while the disk is built by slowly infalling gas. This
description of the halo+disk evolution can correctly account for the
main observational constraints (at least in the framework of simple
models of galactic chemical evolution). We utilise then metallicity
dependent yields to study the evolution of all elements from C and Zn.
Comparing our results to an extensive body of observational data
(including very recent ones), we are able to make a critical analysis
of the successes and shortcomings of current yields of massive stars.
Finally, we discuss qualitatively some possible ways to interpret the
recent data on oxygen vs iron, which suggest that oxygen behaves
differently from the other alpha-elements.
Key words: nuclear reactions, nucleosynthesis,
abundances
stars:
abundances
Galaxy:
abundances
Galaxy:
evolution
Galaxy: general
Galaxy: halo
This article contains no SIMBAD objects.
Contents
- 1. Introduction
- 2. Yields of massive stars and supernova Ia
- 3. The model of galactic chemical evolution
- 4. Evolution of the halo and the disk
- 5. Abundance ratios in the halo and the local disk
- 5.1. Carbon and Nitrogen
- 5.2.
- elements O, Mg, Si, S, Ca, Ti
- 5.3. Sodium and Aluminium
- 5.4. Potassium, Scandium, Vanadium
- 5.5. Fe-peak elements: Cr, Mn, Co, Ni, Cu and Zn
- 5.6. Fluorine, Neon, Phosphorous, Chlorine, Argon
- 5.7. Chemical evolution with respect to Ca
- 6. Alternatives for Oxygen vs. Iron
- 7. Evolution of Mg isotopic ratios
- 8. Summary
- Acknowledgements
- References
© European Southern Observatory (ESO) 2000
Online publication: June 30, 2000
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