Table 11
Comparison of the supernova yields to the measured abundances.
Parameter | DDTc | DDTa | WDD2 | W7 | Measured |
|
|||||
NGC 5044 | |||||
f | 0.84 | 0.83 | 0.83 | 0.84 | |
![]() |
38% | 31% | 36% | 39% | |
C/Fe | 0.19 | 0.19 | 0.19 | 0.21 | 1.5 ± 0.3 |
N/Fe | 0.22 | 0.23 | 0.22 | 0.22 | 1.5 ± 0.2 |
O/Fe | 0.6 | 0.6 | 0.6 | 0.6 | 0.60 ± 0.03 |
Mg/Fe | 0.47 | 0.48 | 0.49 | 0.48 | 0.73 ± 0.05 |
Si/Fe | 0.67 | 0.50 | 0.74 | 0.66 | 0.788 ± 0.012 |
S/Fe | 0.76 | 0.51 | 0.74 | 0.62 | 0.843 ± 0.016 |
Ar/Fe | 0.58 | 0.36 | 0.49 | 0.38 | 0.789 ± 0.013 |
Ca/Fe | 0.96 | 0.56 | 0.71 | 0.47 | 1.86 ± 0.13 |
Ni/Fe | 1.01 | 1.11 | 1.16 | 2.48 | 1.60 ± 0.05 |
|
|||||
NGC 5813 | |||||
f | 0.80 | 0.79 | 0.80 | 0.80 | |
![]() |
32% | 25% | 32% | 33% | |
C/Fe | 0.23 | 0.23 | 0.24 | 0.25 | 1.7 ± 0.4 |
N/Fe | 0.27 | 0.27 | 0.28 | 0.27 | 1.8 ± 0.3 |
O/Fe | 0.73 | 0.73 | 0.73 | 0.73 | 0.73 ± 0.04 |
Mg/Fe | 0.57 | 0.57 | 0.59 | 0.59 | 0.86 ± 0.06 |
Si/Fe | 0.73 | 0.57 | 0.81 | 0.73 | 0.99 ± 0.03 |
Ca/Fe | 0.98 | 0.60 | 0.74 | 0.51 | 1.9 ± 0.5 |
|
|||||
M 87a | |||||
f | 0.84 | 0.83 | 0.83 | 0.84 | |
![]() |
38% | 31% | 36% | 39% | |
C/Fe | 0.19 | 0.19 | 0.19 | 0.21 | 0.74 ± 0.13 |
N/Fe | 0.22 | 0.23 | 0.22 | 0.22 | 1.62 ± 0.21 |
O/Fe | 0.6 | 0.6 | 0.6 | 0.6 | 0.60 ± 0.03 |
Ne/Fe | 0.92 | 0.95 | 0.93 | 0.91 | 1.25 ± 0.12 |
Mg/Fe | 0.47 | 0.48 | 0.49 | 0.48 | 0.60 ± 0.06 |
Notes. Yields based on the models by Badenes et al. (2003), Iwamoto et al. (1999) and Nomoto et al. (2006). Abundance ratios in proto-solar units by Lodders (2003). The ratio of the iron created by supernovae type Ia to the total amount of iron (see Eq. (5)), f, is calculated based on the O/Fe ratio using the assumption that all oxygen and iron have been created by supernovae.
Values measured by Werner et al. (2006) are compared with the models used in this work.
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