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Table 2:

Comparison of results obtained with representative cases from two different model atmosphere sets (ATLAS, and MARCS), assuming a solar oxygen abundance of $\log~\epsilon_{\rm O}=8.66$ (Asplund et al. 2004).
$T_{\rm {eff}}$(K)$\setminus$log g 5500$\setminus$4.5 6500$\setminus$2.0 6500$\setminus$4.0
  $\Delta\log~\epsilon_{\rm O}$ $\Delta\log~\epsilon_{\rm O}$ $\Delta\log~\epsilon_{\rm O}$
  (ATLAS) (ATLAS) (ATLAS)
[Fe/H] = 0.0 -0.20/-0.11 -0.83/-0.86 -0.53/-0.45
[Fe/H] =-1.0 -0.14/-0.05 -0.64/-0.67 -0.36/-0.31
[Fe/H] =-2.0 -0.11/-0.03 -0.32/-0.35 -0.20/-0.15
[Fe/H] =-2.5 -0.12/-0.03 -0.28/-0.26 -0.27/-0.16
[Fe/H] =-3.5 -0.43/-0.10 -0.26/-0.18 -0.87/-0.54
  $\Delta\log~\epsilon_{\rm O}$ $\Delta\log~\epsilon_{\rm O}$ $\Delta\log~\epsilon_{\rm O}$
  (MARCS) (MARCS) (MARCS)
[Fe/H] = 0.0 -0.18/-0.10 -0.88/-0.92 -0.50/-0.44
[Fe/H] =-1.0 -0.12/-0.05 -0.63/-0.66 -0.34/-0.29
[Fe/H] =-2.0 -0.11/-0.03 -0.30/-0.31 -0.19/-0.14
[Fe/H] =-2.5 -0.16/-0.04 -0.42/-0.33 -0.56/-0.34
[Fe/H] =-3.5 -0.52/-0.14 -0.88/-0.53 -1.21/-0.85

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