Fe abundances were derived using a rather large number of lines, typically
20 and
30-40 for TO-stars and subgiants respectively. Full
details about the line list, including gf's, EWs and abundances from
individual lines, will be given in separate papers (in preparation).
The Fe abundance obtained for dwarfs in NGC 6397 (
,
where
this error bar is the internal error as given by the standard deviation of the
mean) is in good agreement with that determined from subgiants
(
). The average of the two groups is
(this is the internal error of our analysis, obtained by combining
results for TO-stars and subgiants; systematic errors, within the abundance
scale defined by observations of the field stars, are mainly due to
uncertainties in the adopted temperature; again combining results for TO stars
and subgiants, that may be considered as independent each other, they are
dex). This value is less than that derived from giants in Carretta &
Gratton (1997):
), and Zinn & West (1984:
). However it agrees very well with the value obtained by
Minniti et al. (1993:
), and the recent, comprehensive
analysis of giants and subgiants by Castilho et al. (2000:
).
The equilibrium of ionization is not well reproduced: abundances from neutral
Fe lines are 0.11 dex larger than those from singly ionized Fe lines. The same
result is obtained for NGC 6752 and our field stars. Note that a smaller
difference (0.07 dex) in the same sense is also present in our solar reference
analysis (in that case we obtained
from Fe I lines,
and 7.45 from Fe II lines using the solar model atmosphere from Kurucz 1993,
with no overshooting). We then think most of the difference for the Sun is due
to either the adopted gf's values (these are laboratory values taken from
recent literature) or to the model atmospheres (models might underestimate the
temperature gradient in real atmospheres, perhaps due to an inappropriate
consideration of convection). The residual difference for the program stars
might be due to the adoption of slightly too high
's
(
40-50 K) or too low gravities (by
0.1 dex). Note that it cannot be due
to departures from LTE, because the expected dominating effect
(overionization: Idiart & Thévenin 1999; Gratton et al. 1999) would lead to
larger abundances from Fe II lines than from Fe I ones (opposite to
observations).
The star-to-star scatter in [Fe/H] values is extremely small: the rms
scatter is only 0.04 dex (i.e. 10%) for NGC 6397. This seems a very
homogeneous cluster as far as Fe abundances are considered.
![]() |
Figure 5: Same as Fig. 3, but for the region including the 7771-74 Å OI triplet in NGC 6752 TO-stars (stars are ordered according to decreasing Na abundances). The position of the O lines is marked |
On the other side, the [Fe/H] value for NGC 6752 (
,
internal error; systematic error is again
dex), obtained both from
TO and subgiant stars, which agree completely, coincides with that derived
from giants by Carretta & Gratton (1997:
); it is
somewhat larger than the value quoted by Zinn & West (
)
and
Minniti et al. (1993:
). The spectra of NGC 6752 have a
S/N lower than those in NGC 6397, since we chose to observe more stars, even at
a lower S/N. The scatter of abundances for individual lines (from 0.12 to 0.27
dex) is larger than that obtained for stars in NGC 6397, roughly in agreement
with the lower S/N.
For field stars we may compare the present Fe abundances with those derived by
Carretta et al. (2000). Limiting ourselves to only those stars for
which Carretta et al. considered high dispersion abundances, the present Fe
abundances are smaller on average by
dex (11 stars,
dex). The slightly lower metal abundances are due to lower
's adopted in the present paper.
Copyright ESO 2001