 |  |
Astron. Astrophys. 342, 799-808 (1999)
2. Observations
In order to study the first overtone rotation-vibration bandheads
of SiO we observed the spectral range from 3.94 to
m for a sample of 23 oxygen-rich
late-type giants, most of which are Mira or Semiregular (SR)
variables. Also two Irregular variables have been included. The
sources have been selected due to their variability types, their
bright L-magnitude ( ), the existence
of reliable JHKLM as well as IRAS 12 and
m photometry and the existence of a
good IRAS-LRS spectrum. As it is shown in Table 1 the stars cover
a large variety of photometric periods and infrared colors. Due to
their pulsational properties at least most of them are expected to be
situated on the AGB (e.g. Alvarez et al. 1997).
![[TABLE]](img17.gif)
Table 1. -values, pulsational and photometric properties of the observed stars. and are the temperatures from a fit of two blackbodies, while corresponds to the effective temperature derived from the (J-K) color (see text).
The spectra have been observed in June 1993 with the cooled grating
spectrograph IRSPEC at the ESO NTT and reduced with MIDAS. They are
composed of 5 overlapping parts corresponding to different grating
positions. The final resolution is approximately 4000. To eliminate
atmospheric features and effects of detector response, spectra of
nearby O and B stars were taken at the same time and included into the
reduction. The hot objects were mainly used for the determination of
the stellar continua, since, apart from
Brackett- , they do not show any
distinct features in the studied wavelength range. However, concerning
the overall slopes of the measured energy distributions we did not
always get consistent results. Thus, we decided to use normalized
spectra divided by a polynomial fit to the wavelength ranges
m, m
m, m
m, m
m, and
m, where there are no strong SiO or
OH features. In this context it should be mentioned that in stars with
strong SiO bands the absorption will extend into all the defined
continuum regions at m, since there
is no frequency not affected by SiO at our resolution. Nevertheless,
this effect can easily be corrected, if one compares the data to
results from theoretical calculations, as it is discussed in
Sect. 4.1. Another problem may be caused by the presence of a large
number of stellar water lines in the whole spectral range between 3.94
and m (Aringer et al. 1997b). But
water absorption will only appear in the coolest objects and never
become very strong. In addition, we do not expect it to change the
overall slope of the continuum.
Since the stars in our sample are extremely bright in the infrared,
the signal/noise ratio is always very high. In addition, almost all of
the objects have been observed more than once (usually 3 to 4 times).
The different spectra, which have been averaged in order to get the
final data, are generally identical concerning their features. But -
even after a careful reduction - there were some variable spikes
produced by the detector. Because of their fixed positions the
stronger ones could be easily identified and removed using the O and B
stars. Nevertheless, the weak ones and those, which did not appear in
the spectra of the hot objects, remain in the final data. A good
example is the relatively strong spike at
m that can be seen in some of our
stars (see Fig. 1).
![[FIGURE]](img29.gif) |
Fig. 1. Observed IRSPEC spectra of 23 AGB stars including first overtone bandheads of SiO.
|
The normalized spectra of all objects are shown in Fig. 1. In most
of them one can see the first three bandheads of the main isotope
28Si16O situated at
m (V = 2
0),
m (V = 3
1) and
m (V = 4
2) as the dominant feature. But
there are also stars like X Hya, R Oph, RR Sgr and S Vir, all of which
are Mira variables, having only a very weak or no SiO absorption. Some
of them show Brackett- emission at
m, which is a sign for the appearance
of atmospheric shock waves. The distinct depression between 3.96 and
m is caused by OH (e.g. Decin et al.
1997). It can only be seen in objects with intense SiO bands. Finally,
as it has already been mentioned, there are a lot of H2O
lines in the whole observed spectral range, which become important for
the coolest stars with . However,
they will not give rise to any remarkable intense features (Aringer et
al. 1997b). Instead, they are expected to reduce the continuum flux
level and introduce many small absorption dips into the spectrum.
Isotopic bandheads of SiO are situated at
m (V = 2
0, 29SiO),
m (V = 2
0, 30SiO),
m (V = 3
1, 29SiO),
m (V = 3
1, 30SiO) and
m (V = 4
2, 29SiO). According to
our synthetic spectra published in Paper I, the most distinct of them
are expected at 4.0687 and m.
Especially at the first of these positions, there is a quite strong
feature that can be seen in all sources with large SiO absorption. But
also the second band, which appears to be weaker, seems to be present
at least in some of the stars. However, it should be noted that around
4.07 as well as around m an
accumulation of some intense OH lines can be found (e.g. Decin et al.
1997). Thus, we assume these features to be formed by 29SiO
and OH together. The remaining isotopic bands are only very weak or
not visible. This is especially true for 30SiO, because its
bandheads fall into an area with intense absorption from the main
isotope. Maybe they produce small peaks seen in the spectra of some
objects like SU Sgr. But that could also be due to another species
like water in the earth's or stellar atmosphere. A possible exception
concerning the appearance of isotopic bands is the strange spectrum of
RR Aql showing intense features at all of their positions.
In order to evaluate the intensity of the SiO absorption we have
measured , which is the sum of the
equivalent widths corresponding to the V = 2
0, V = 3
1 and V = 4
2 bandheads of the main isotope.
This has been done exactly in the same way as in Paper I for the
synthetic spectra. The results are listed in Table 1. The typical
uncertainty of these values, which is mainly due to the definition of
the local continuum around the bandheads, amounts to
Å.
© European Southern Observatory (ESO) 1999
Online publication: February 23, 1999
helpdesk.link@springer.de  |