All the clusters studied in this work have been classified as belonging to types I or II of Ruprecht (1966). There exist previous results only about Hogg15 and Melotte 105, which can be compared with the present ones. Precisely, the latter cluster was selected not only because of its compactness but also because it was observed by Santos & Bica (1993) at La Silla (Chile) using the same spectroscopic technique, so that it can be used as control cluster. The five remaining clusters BH132, BH217, Lyngå11, Pismis21 and Ruprecht 144 have not been previously studied and their reddenings and ages have been determined here for the first time. Lyngå11, Pismis21 and Ruprecht144 are mentioned in early catalogation or morphological classification works (Pismis 1959; Lyngå 1965; Ruprecht 1966).
The integrated spectrum of Ruprecht144, corrected for E(B-V) = 0.25, is
compared to that of the Y3A template (100 Myr) in Fig. 1. Notice that
this template presents TiO bands not observed in Ruprecht144. Notice
also that at
100 Myr very populous LMC clusters may present
strong TiO bands. This phenomenon appears to be associated to AGB stars
(BA87, Bica et al. 1990). Owing to statistical effects in non-massive clusters,
the effect is not expected in Galactic open clusters. Indeed, the best
match is found for the Y3B template (100 Myr)
adopting E(B-V) = 0.32
0.02 (Fig. 1). The age derived from the Balmer
lines is slightly larger (Table 5). CaII triplet EWs yield [
]
=
-0.1
0.2.
We have simultaneously determined the age and reddening for Melotte105, also
known as Collinder 246 (Collinder 1931), using the template Y3B (100 Myr). The
best template match yields E(B-V) = 0.31
0.02. Figure 2 shows the observed
cluster spectrum, the spectrum corrected for the derived interstellar reddening
E(B-V) = 0.31, and the template Y3B which best matches the cluster spectrum.
An alternative match using the template Y2 (50 Myr) is also shown. The derived
metallicity from CaII triplet
EWs is [
]
= 0.0
0.2. The age and reddening here derived are
in excellent agreement with the values found by Santos & Bica (1993) using
the same technique. On the other hand, using UBV photoelectric photometry
Sher (1965) estimated the same age (
100 Myr) and a somewhat larger
mean reddening E(B-V) = 0.38. The non-uniform reddening determined
photoelectrically by Sher (1965) may be reflecting the existence of internal
dust associated to the cluster. If this is the case, the spectroscopic
reddening should be lower than the photometric one since the less reddened
stars of a given spectral type should contribute to the integrated light
with larger fluxes in comparison with the most reddened stars of the same
spectral type. In other words, as stated by Santos & Bica (1993), it appears
highly probable that the lower reddening derived from the integrated spectrum
indicates an internal reddening, in the present case, of
0.07 mag.
Based on CCD UBV data Kjeldsen & Frandsen (1991) derived an age of
150 Myr and a quite larger reddening E(B-V) = 0.52. The difference
found in the cluster reddening may be explained by the fact that Kjeldsen &
Frandsen (B-V) colours are shifted by approximately 0.1 mag with respect to
those of Sher (1965). Finally, Balona & Laney (1995) obtained E(b-y) = 0.32
from uvby photometry, equivalent to E(B-V) = 0.43, if the relation E(B-V) = 1.35
E(b-y) derived by Crawford (1978) is used. This reddening differs scarcely by
0.05 mag from that of Sher (1965), while the age estimated by Balona & Laney
(250
Myr) is somewhat larger than the present one.
BH132 was first recognized as an open cluster by van den Bergh & Hagen
(1975). Figure 3 shows
the integrated cluster spectrum, corrected for E(B-V) = 0.28,
compared to the Y4 template (500 Myr). Note that although a general resemblance
between these two spectra is apparent, neither the Balmer jump nor the
H
line show a good agreement. Besides, the CaII K line in BH132
appears to be more diluted, which cannot be a metallicity effect since CaII
triplet near 8600 Å appears to be similar in both the template and BH132
spectra. This difference would be explained if BH132 were younger than
the Y4 template. The best match
is found for the Y3B template (100 Myr), using E(B-V) = 0.60 (Fig. 3). Note that
the spectral properties of this cluster are very similar to those of Ruprecht
144 and Melotte105. Equivalent widths of TiO and CaII triplet features
(Table 4) are compatible with the cluster having a nearly solar metal content.
Hogg15, also known as BH139 (van den Bergh & Hagen 1975) or ESO95SC15
(Lauberts 1982), was first
recognized as an open cluster by Hogg (1965a, 1965b). Photoelectric UBV
photometry by Moffat (1974)
yields E(B-V) = 1.16
0.03, a distance of 4.2 kpc, and an age
8 Myr.
Therefore, Hogg15 is one of the few clusters known to lie in the inner
arm -II, much further behind the Coalsack than the adjacent cluster NGC4609,
which is located at about 1.3 kpc from the Sun and is reddened by E(B-V) =
0.36 (Feinstein & Marraco 1971). The above reddening and age of Hogg15 are
in very good agreement with the results obtained from integrated spectroscopy.
We show in
Fig. 4 two template matches. The template match with YB.LMC (6-9 Myr) gives
E(B-V) = 0.70
0.05, whereas YA.LMC (3-6 Myr) yields E(B-V) = 1.05
0.05.
The latter is clearly the best match so that Hogg15 is confirmed as a highly
reddened young open cluster. We point out that we also dispose of the
near-IR spectrum for Hogg15, but we limit our comparison in Fig. 4 to the
range in common with the available template. The derived metallicity is
[
]
= -0.2
0.2. Moffat (1974) and Smith et al. (1994) have
discussed the possibility that the WN6 star HDE311884 could be a cluster
member. The cluster age is clearly compatible with such possibility (cf.
Paczinski 1973).
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Figure 9:
Same as Fig. 8 for
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Figure 11:
Same as Fig. 10 for
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Pismis21 was first recognized as an open cluster by Pismis (1959). Notice
the extreme absorption effects in the observed spectrum (Fig. 5). We also
show the foreground reddening corrected spectrum for E(B-V) = 1.50
0.03
and the Y2 template (50 Myr) which best
matches the spectrum. Although the age from Balmer lines is slightly greater
(Table 5), Pismis21 is found to be a moderately young highly reddened open
cluster. The derived metallicity is [
]
= 0.0
0.2.
We show in Fig. 6 two template matches. The template match with Y3B (100 Myr)
gives E(B-V) = 0.17
0.03, whereas Y4 (500 Myr) yields E(B-V) = 0.12
0.03. An inspection of the spectra reveals that the incipient 4000-Å
break favours Y4 as a match, as well as the general spectral distribution.
More details on the Balmer jump and 4000-Å break as a function of age
are given in Bica et al. (1994). Since the Balmer-line method also gives an
age closer to Y4 (Table 5), we
adopt the latter match as the best solution. The derived metallicity from CaII
triplet and TiO features is [
]
= +0.1
0.2.
This cluster was first recognized by van den Bergh & Hagen (1975), and is
also known as ESO333SC2 (Lauberts 1982). The
solution for BH217 yields an age of about 50 Myr and E(B-V) =
0.80
0.03 by template match (Fig. 7). The age derived from the Balmer lines
is only slightly lower (Table 5) and no metallicity could be derived
for this cluster. The spectral features of BH217 are quite similar to those
of the more reddened cluster Pismis21 (Fig. 5).
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