Table 3
Atmospheric parameters and chemical composition of our sample of hot sdOs.
Feige 34 | Feige 67 | AGK+81°266 | LS II+18°9 | Haas (1997) a | Bauer & Husfeld (1995) b | ||
|
|||||||
Teffc (K) | 62 550 ± 600 | 61 050 ± 520 | 61 860 ± 870 | 60 010 ± 800 | 60 000 ± 4000 | 75 000 ± 5000 | |
log gc (cm s-2) | 5.99 ± 0.03 | 5.95 ± 0.03 | 6.07 ± 0.04 | 6.00 ± 0.06 | ... | 5.2 ± 0.2 | |
RVd (km s-1) | 11.0 ± 7.7 | 27.0 ± 7.8 | −27.8 ± 7.8 | −49.5 ± 12.3 | ... | ... | |
|
|||||||
Element | Abundance (log N(X)/N(H)) | Solare | |||||
|
|||||||
Hed | −1.79 ± 0.04 | −1.59 ± 0.04 | −2.9 ± 0.2 | −1.87 ± 0.07 | ... | −1.27 ± 0.25 | −1.07 |
C | ≲−6.7 | ≲−8.0 | ≲−6.7 | ≲−6.7 | ... | ≲−4.50 | −3.56 |
N | −4.9 ± 0.3 | −4.9 ± 0.3 | −6.0 ± 0.3 | −4.9 ± 0.3 | ... | −4.85 ± 0.5 | −4.17 |
O | −5.5 ± 0.5 | −5.5 ± 0.5 | ≲−6.4 | −5.5 ± 0.5 | ... | ... | −3.31 |
Mg | ≲−5.0 | ≲−5.0 | ≲−5.0 | ≲−5.0 | ... | ... | −4.40 |
Si | −6.2 ± 0.3 | ≲−6.2 | −5.0 ± 0.3 | −6.2 ± 0.3 | ... | ≲−5.5 | −4.49 |
P | −6.7 ± 0.5 | −6.7 ± 0.5 | −5.5 ± 0.5 | −6.7 ± 0.5 | ... | ... | −6.59 |
S | −5.6 ± 0.3 | −5.6 ± 0.3 | −5.3 ± 0.3 | −5.6 ± 0.3 | ... | ... | −4.86 |
Cr | ≲−5.3 | ≲−5.3 | ≲−5.3 | ≲−5.3 | ... | ... | −6.36 |
Mn | ≲−5.6 | ≲−5.6 | ≲−5.3 | ≲−5.6 | ... | ... | −6.57 |
Fe | −3.1 ± 0.3 | −3.1 ± 0.3 | −3.1 ± 0.3 | −3.1 ± 0.3 | −3.5 | ... | −4.50 |
Co | ≲−5.8 | ≲−5.8 | ≲−5.8 | ≲−5.8 | ... | ... | −7.01 |
Ni | −4.0 ± 0.3 | −4.0 ± 0.3 | −4.0 ± 0.3 | −4.0 ± 0.3 | −3.9 | ... | −5.77 |
Notes.
For Feige 34, Feige 67, and LS II+18°9, parameters such as log g and abundances of He, C, and N were kept fixed to the values derived by Bauer & Husfeld (1995) for Feige 67.
For Feige 67.
Our results are the averaged values of the different fits presented in Table 2.
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