Journal
ASTROPHYSICAL JOURNAL
Volume 551, Issue 2, Pages 1065-1072Publisher
IOP PUBLISHING LTD
DOI: 10.1086/320235
Keywords
dust, extinction; meteors, meteoroids; novae, cataclysmic variables; nuclear reactions, nucleosynthesis, abundances
Categories
Ask authors/readers for more resources
We report the discovery of five SiC grains and one graphite grain isolated from the Murchison carbonaceous meteorite whose major-element isotopic compositions indicate an origin in nova explosions. The grains are characterized by low C-12/C-13 (4-9) and N-14/N-15 (5-20) ratios, large excesses in Si-30 (Si-30/ Si-28 ratios range to 2.1 times solar), and high Al-26/Al-27 ratios. These isotopic signatures are theoretically predicted for the ejecta from ONe novae and cannot be matched by any other stellar sources. Previous studies of presolar grains from primitive meteorites have shown that the vast majority formed in red giant outflows and supernova ejecta. Although a classical nova origin was suggested for a few presolar graphite grains on the basis of Ne-22 enrichments, this identification is somewhat ambiguous since it is based on only one trace element. Our present study presents the first evidence for nova grains on the basis of major element isotopic compositions of single grains. We also present the results of nucleosynthetic calculations of classical nova models and compare the predicted isotopic ratios with those of the grains. The comparison points toward massive ONe novae if the ejecta are mixed with material of close-to-solar composition.
Authors
I am an author on this paper
Click your name to claim this paper and add it to your profile.
Reviews
Recommended
No Data Available