Abstract
Presolar grains of the mainstream, Y and Z type are believed to have an
origin in carbon stars. We compared the C and Si isotopic ratios of these grains
[1] with the results of theoretical models for the envelope compositions of
AGB stars. Two sets of models (FRANEC, Monash) use a range of stellar
masses (1.5 to 5 MÖ), metallicities, different prescriptions for mass loss, and
two sets of neutron-capture cross-sections for the Si isotopes [2, 3]. They
predict that the shifts in Si isotopic ratios and the increase of 12C/13C in the
envelope during third dredge-up are higher for higher stellar mass, lower
metallicity, and lower mass loss rate. The Guber et al. [3] cross-sections result
in larger shift in the 30Si/28Si ratios and smaller shifts in the 29Si/28Si ratios
than the Bao et al. [2] cross-sections. Because the 22Ne neutron source
dominates Si nucleosynthesis, the effect of the 13C source is negligible.
Original language | Undefined/Unknown |
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Pages (from-to) | A198 |
Number of pages | 1 |
Journal | Meteoritics and Planetary Science |
Volume | 41 |
Issue number | suppl. |
Publication status | Published - 2006 |