Calibrations obtained from the procedure described above are given in Table 3. These calibrations supersede all counterparts that have previously been derived from Taylor's [Fe/H] catalogs. The notation "[Fe/H](q)'' is used in Table 3 to designate metallicities derived from the calibrations. The metallicity limits within which the calibrations apply are given (with other information) in Table 3's footnotes.
The values of S in the
CN calibration require comment. [34, Taylor
(1991]) presented a calibration in which S depends on color. By
contrast, [45, Twarog & Anthony-Twarog (1996]) found no evidence for a color
dependence that is statistically significant. As part of the new analysis,
preliminary solutions were performed to investigate this problem. The
results of the solutions revealed three intervals in the color (45-48), with
S and Z being essentially constant within each interval but differing
between intervals. For the final results given in Table 3, t tests show
that the values of S and Z differ between the first and second intervals with
confidence levels of at least 99.9%. The same is true for the second and
third intervals.
The first three lines of Table 3 contain results for the three color intervals. The fourth line contains averages for use near the boundary between the first and second color intervals. In the same way, the fifth line applies for the boundary between the second and third intervals. These latter relations are based on a guess that relatively smooth transitions between color intervals are more likely than abrupt changes between them.
Somewhat to the author's surprise, S decreases as one goes from the first color interval to the second, but then increases again as one goes from the second interval to the third. The reason for this kind of variation is not known. Given the results of the statistical tests quoted above, however, the existence of the variation seems to be reasonably well established.
Values of the following rms error are given in the fifth column of Table 3:
| (3) |
One would like to know how well the errors listed in Table 3 compare to the
errors given for values of [Fe/H] in Taylor's catalogs. The largest of the
Table 3 errors are for
and [M/H], and are quite comparable to
the rms error range for a single determination of [Fe/H] [35, (Taylor 1994,
1999b]). The smallest of the Table 3 errors are for G and
Fe
, and would be typical for stars with values of [Fe/H] that have
been determined several times. The small sizes of the latter errors suggest that the
isoabundance relations for G and
Fe
are correct.
It is also of interest to find out whether net values of
can be
decreased by averaging results from two (or more) calibrations. This is
possible only if the datum from each calibration is an independent sample of
underlying random effects. That condition is not met if there are internal
correlations in the data; if (say)
and
are
correlated, f(q) and F(Q) are effectively identical samples of underlying
random effects, and their average conveys no more information than f(q) or
F(Q) alone. To check for correlations of this sort, the two-error
least-squares algorithm described in Sect. 3.2 was applied to residuals from
the Table 3 relations. For the following parameter pairs, correlations
with a confidence level of 3.5
or better were found:
No corresponding correlation was obtained for G and
Fe
. However, the number of stars for which both parameters
are available is relatively small. Larger numbers of data could be
used to test these parameters against
CN. Since correlations were
found when both G and
Fe
were tested in this way, it appears
safest to assume that the G and
Fe
residuals are
correlated.
Recall now that the M1 calibration is intended only to answer a question
about
Leo (see Sect. 2). In the present context, that calibration may
be set aside. Apparently results for the other three evolved-star calibrations
cannot be meaningfully averaged. The same appears to be true for results for
the two calibrations for dwarfs. To avoid misleading appearances, it is
probably best not to average results from two or more calibrations at any point
in an analysis.
Copyright The European Southern Observatory (ESO)