Table A.2.
Errors in the abundance of zinc determined from the two Zn I lines used in this study and different spectral line quality (A–C, see Sect. 3).
| Element | Line λ, nm | Line quality | σ(Teff) dex | σ(log g) dex | σ(ξt) dex | σ(cont) dex | σ(fit) dex | σ(A)tot dex |
|---|---|---|---|---|---|---|---|---|
| Zn I | 472.21 | A | ±0.03 | ∓0.04 | ∓0.11 | 0.04 | 0.06 | 0.14 |
| B | ±0.03 | ∓0.04 | ∓0.11 | 0.04 | 0.08 | 0.15 | ||
| C | ±0.03 | ∓0.04 | ∓0.11 | 0.04 | 0.09 | 0.16 | ||
| Zn i | 481.05 | A | ±0.03 | ∓0.03 | ∓0.11 | 0.05 | 0.05 | 0.14 |
| B | ±0.03 | ∓0.03 | ∓0.11 | 0.05 | 0.06 | 0.14 | ||
| C | ±0.03 | ∓0.03 | ∓0.11 | 0.05 | 0.08 | 0.15 |
Notes. The ± or ∓ sign reflects the change in elemental abundance that occurs due to increase (top sign) or decrease (bottom sign) in a given atmospheric parameter. For example, an increase in the effective temperature leads to an increase in the abundance of zinc (±), while increasing microturbulence velocity results in a decreasing zinc abundance (∓).
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