P. M. Woods1,2 - F. L. Schöier3 - L.-Å. Nyman1,4 - H. Olofsson5
1 - European Southern Observatory, Alonso de Cordova 3107, Casilla 19001, Santiago 19, Chile
2 -
Department of Physics, UMIST, PO Box 88, Manchester M60 1QD, UK
3 -
Leiden Observatory, PO Box 9513, 2300 RA Leiden, The Netherlands
4 -
Onsala Space Observatory, 43992 Onsala, Sweden
5 -
Stockholm Observatory, AlbaNova, 10691 Stockholm,
Sweden
Received 25 September 2002 / Accepted 4 February 2003
Abstract
A millimetre molecular line survey of seven high
mass-loss rate carbon stars in both the northern and southern skies is
presented. A total of 196 emission lines (47 transitions) from 24
molecular species were detected. The observed CO emission is used to
determine mass-loss rates and the physical structure of the
circumstellar envelope, such as the density and temperature structure,
using a detailed radiative transfer analysis. This enables abundances
for the remaining molecular species to be determined. The derived
abundances generally vary between the sources by no more than a factor
of five indicating that circumstellar envelopes around carbon stars
with high mass-loss rates have similar chemical compositions. However,
there are some notable exceptions. The most striking difference
between the abundances are reflecting the spread in the
12C/13C-ratio of about an order of magnitude between the
sample stars, which mainly shows the results of nucleosynthesis.
The abundance of SiO also shows a variation of more than an order of
magnitude between the sources and is on average more than an order
of magnitude more abundant than predicted from photospheric chemistry
in thermal equilibrium. The over-abundance of SiO is consistent with
dynamical modelling of the stellar atmosphere and the inner parts of
the wind where a pulsation-driven shock has passed. This scenario is
possibly further substantiated by the relatively low amount of CS
present in the envelopes. The chemistry occurring in the outer
envelope is consistent with current photochemical models.
Key words: molecular processes - stars: abundances - stars: AGB and post-AGB - stars: carbon - circumstellar matter
The chemistry associated with carbon stars has long been known to be
rich and complex in comparison to the alternative O-rich regime (i.e.,
where
). This is in part due to the favourable bonding of
the carbon atom, enabling long chains and complex species to form.
Most of the current understanding of carbon stars has come from both
observational and theoretical work on the high-mass-losing carbon
star, IRC +10216. This source, which lies within 200 pc and
presents an ideal specimen for the study of carbon-rich envelopes, has
been mapped interferometrically in various molecular species
(e.g. Bieging & Tafalla 1993; Dayal & Bieging 1993, 1995;
Gensheimer et al. 1995; Guelin et al. 1993, 1996; Lucas et al. 1995;
Lucas & Guélin 1999) and has had models of its dust
(a good summary is given by Men'shchikov et al. 2001) and chemistry
(e.g. Millar et al. 2000) constructed. These tools have
produced groundbreaking results and have been used to set a paradigm
for what has come to be known as carbon
chemistry in connection with evolved stars.
However, the accuracy of employing IRC +10216 chemistry to
similar carbon stars has been little-tested due to the difficulties in
observing them. Much work has been done on the carbon-rich post-AGB
sources CRL 618 and CRL 2688, and the chemistry of
CRL 618 in particular has been modelled by
Woods et al. (2003). Detailed chemical studies of carbon stars on
the AGB have been few in number, but examples include the molecular
line survey of IRAS 15194-5115, a peculiar 13C-rich
star (Nyman et al. 1993). Carbon star surveys which include
molecular-line comparisons are fewer, and have been limited in the
number of lines observed. Olofsson et al. (1993a) detected some 40
stars in a handful of species other than CO. The sample of
Bujarrabal et al. (1994) included 16 carbon stars, with up to ten
molecular lines observed in each. A more recent survey by
Olofsson et al. (1998) detected 22 carbon stars in up to 6 molecular lines.
Table 1: Positions, luminosities, periods and calculated distances of the sample of carbon stars.
The survey work presented here purports to be the most complete and consistent molecular-line survey in AGB carbon stars to date, covering high mass-loss rate objects in both the northern and the southern sky. Previously unpublished spectra of five stars (IRAS 15082-4808, IRAS 07454-7112, CIT 6, AFGL 3068 and IRC +40540) are presented, and spectra taken towards IRC +10216 and IRAS 15194-5115 with the Swedish-ESO Submillimetre Telescope (SEST; Nyman et al. 1993) and IRC +10216 with the Onsala Space Observatory (OSO) 20 m telescope are used to supplement the survey. Comparison of data from IRC +10216 taken with both telescopes affords a high degree of confidence in the relative calibration that can be derived.
Up to 51 molecular lines were observed in the sample of 7 high-mass-losing carbon stars, of which 47 were clearly detected. Mass-loss rates, dust properties and the 12CO/13CO-ratio are calculated self-consistently using a radiative transfer method (Schöier & Olofsson 2000, 2001; Schöier et al. 2002). An approach similar to that of Nyman et al. (1993) is adopted to calculate fractional abundances (including upper limits), and a detailed analysis of the comparison between the calculated abundances is carried out. Hence, Sect. 2 details the observations carried out and the instrumentation used. Section 3 gives the observational results, including a presentation of various spectra. Section 4 details the NLTE radiative transfer code used to determine the envelope parameters and Sect. 5 explains the method of calculating chemical abundances. The results and deductions are discussed in Sect. 6.
Following the CO survey of Nyman et al. (1992), several carbon stars, which were bright in CO lines, were selected for a more comprehensive molecular line search. These stars are rare in that they are all losing mass at a very high rate, and hence are more likely to produce strong emission from a variety of molecular lines. The sample of seven carbon stars (Table 1) was observed using both the 15 m Swedish-ESO Submillimetre Telescope (Booth et al. 1989) during the period 1987-1996, and the Onsala 20 m telescope, in 1994. The SEST, situated on La Silla, Chile, was used to observe IRAS 07454-7112, IRAS 15082-4808, and IRAS 15194-5115. The 20 m telescope, located at the Onsala Space Observatory (OSO) in Sweden, observed the remaining three sources, CIT 6, AFGL 3068 and IRC +40540. Both telescopes were used to observe the well-studied carbon star, IRC +10216 in order to determine the relative calibration between the two telescopes.
The JCMT public archive was searched for
complementary line observations, in particular the CO lines used in
the radiation transfer modelling described in Sect. 4.
Lines for which multi-epoch observations are available in the JCMT
archive typically display intensities that are consistent to
20% (Schöier & Olofsson 2001). In addition, interferometric
observations of the CO(J=1-0) brightness distribution around some
of the sample stars have been performed
(Neri et al. 1998) using the
Plateu de Bure interferometer (PdBI), France. The data are publically
available and have been used in this paper.
The coordinates used for each individual source are listed in
Table 1. Also shown in Table 1 are
the adopted luminosities and distances to be used in the molecular
excitation analysis. For stars where a period has been determined
(see Table 1) the period-luminosity relation from
Groenewegen & Whitelock (1996) was used to estimate the corresponding
luminosity. If a reliable period is not available the total
bolometric luminosity was fixed to 9000 .
The distance
was then obtained from the luminosity using the observed bolometric
magnitude. Schöier & Olofsson (2001) used the same approach when
determining the distances to a large sample of optically bright carbon
stars and concluded that there were no apparent systematic effect when
comparing with estimates based upon Hipparcos parallaxes, although the
scatter is large and the distance estimate for an individual source is
subject to some uncertainty of up to a factor of
2. The effects
of the adopted distance on the molecular excitation will be addressed
in Sect. 5.5.
If, for simplicity, the central ratiation field is represented by one
or two blackbodies their properties can be determined from a fit to
the observed spectral energy distribution (SED) as described in
Kerschbaum (1999). A fit to the SED gives the two blackbody
temperatures (T* and
)
as well as their relative
luminosities (
/L*). The parameters obtained in this
fashion are presented in Table 1.
Table 2: Beam widths and efficiencies at selected frequencies.
The SEST is equipped with two acousto-optical spectrometers (HRS, 86 MHz bandwidth with 43 kHz channel separation and 80 kHz resolution; LRS, 500 MHz bandwidth with 0.7 MHz channel separation and a resolution of 1.4 MHz). The receivers used were dual polarization Schottky receivers at both 3 and 1.3 mm wavelength. Typical system temperatures above the atmosphere were 400-500 K and 1000-1800 K, respectively.
The OSO 20 m telescope uses two filterbanks (MUL B, 64 MHz bandwidth with a channel width of 250 kHz; MUL A, 512 MHz bandwidth and a channel width of 1 MHz). The receiver used was a horizontally, linearly polarised SIS receiver with a typical system temperature of 400-500 K above the atmosphere.
All observations were performed using the dual beam switching method,
which places the source alternately in two beams, and yields very flat
baselines. Beam separation was in both cases about 11
5.
Calibration was done with the standard chopper-wheel method. The
intensity scales of the spectra are given in main-beam brightness
temperature (the corrected antenna temperature,
,
divided by the main-beam efficiency,
). Main-beam
efficiencies and FWHM beam widths are given in Table
2 for both telescopes.
![]() |
Figure 1: Low-resolution spectra of IRAS 07454-7112, obtained with the SEST. |
![]() |
Figure 2: Low-resolution spectra of IRAS 07454-7112, obtained with the SEST. |
A total of 196 lines were detected in the sample. 47 transitions of
24 molecular species were detected, and upper limits for another 95
relevant transitions were also obtained, including another three
species (C2S, C3S and SO). Previously unpublished spectra are
shown in Figs. 1, 2 and
A.1-A.13. Table 3 lists the
detections in all seven sources, together with their peak and
integrated intensities. If a line has a hyperfine structure, the
frequency and intensity of the strongest component is listed, and the
integrated intensity is the sum over all hyperfine components. Values
of
for lines where no detection was made are the
rms noise values.
Almost all lines observed in IRC +10216 by the SEST were observed in the same source with the OSO 20 m telescope. The majority of those which were not are due to the lack of a 1.3 mm receiver at OSO. A large proportion of these lines were observed in the remaining six sources. The purpose of observing IRC +10216 twice, with different telescopes, was to ascertain the relative calibration between the two different setups, and hence gain a basis from which good comparisons could be made between the entire sample of carbon stars.
The 13CS (J=2-1) line observed in some of these sources is partially blended with the C3S (J=16-15) line (Kahane et al. 1988). The 13CS (J=2-1) integrated intensities include both these lines. It is assumed that the relative intensities of these two lines are constant in all the objects, and hence will not affect comparisons. The lines of two HC3N isotopes, HC13CCN and HCC13CN, lie very closely and are in all cases blended together. No attempt is made to separate the components.
There are four characteristic line profile shapes which give information on the source being observed. These lineshapes are most typically seen in CO emission since it is often strongest (for a comprehensive review of line profiles see Olofsson et al. 1993b). For optically thick emission the line profile can be described as parabolic for unresolved sources or flat-topped for resolved sources. A parabolic profile is shown by most of the 12CO emission lines in the sample except in IRC +10216 and IRAS 15194-5115, where the CO (J=1-0) emission shows a flat-topped profile.
When emission is optically thin, a flat-topped profile is seen for unresolved sources, and a double-peaked profile for a resolved source. Examples of these profiles can be seen in the 13CO emission towards IRAS 15082-4808 and IRC +10216. In the following calculations, all lines are assumed optically thin, except those from CO and HCN.
The values of the expansion velocity,
,
of the
circumstellar envelopes quoted in Table 4 are obtained from
the radiative transfer CO modelling of these sources (presented in
Sect. 4) where its value is adjusted until a good fit
to the observed line profiles is obtained. No trends in the widths of
the observed lines are present which lends further support to the
assumption adopted here that these envelopes are expanding at constant
velocities.
The integrated intensities for lines which were not detected are
determined using
![]() |
(1) |
Table 3: Detected lines.
Table 4: Summary of circumstellar properties derived from the CO modelling (see text for details).
The observed circumstellar CO line emission is modelled taking into account 50 rotational levels in each of the fundamental and first excited vibrational states. The energy levels and radiative transition probabilities from Chandra et al. (1996) are used. The recently published collisional rates of CO with H2 by Flower (2001) have been adopted assuming an ortho-to-para ratio of 3. For temperatures above 400 K the rates from Schinke et al. (1985) were used and further extrapolated to include transitions up to J=50. The collisional rates adopted here differ from those used in the previous modelling of some of these sources (Ryde et al. 1999; Schöier & Olofsson 2000; Schöier & Olofsson 2001) and account for the slightly different envelope parameters derived in the present analysis. The same set of collisional rates were used for all CO isotopomers.
The envelopes are assumed to be spherically symmetric and to expand at a constant velocity and the model includes the radiation emitted from the central star. Dust present around the star will absorb parts of the stellar radiation and re-emit it at longer wavelenghts. For simplicity, the central radiation field is represented by one or two blackbodies and is determined from a fit to the observed spectral energy distribution (SED) (Table 1). The inner radius of the circumstellar envelope is taken to reside outside that of the central blackbodies. This procedure provides a good description of the radiation field to which the envelope is subjected. For the sample stars, which have dense CSEs, the line intensities derived from the 12CO model are not sensitive to the adopted description of the stellar spectrum due to the high line optical depths. The stellar photons are typically absorbed within the first few shells in the model. A more detailed treatment of thermal emission from the dust present in the CSE, and the increase of total optical depth at the line wavelenghts, has been found to be of no major importance in deriving the envelope parameters for high mass-loss rate objects (Schöier et al. 2002).
The abundance of 12CO relative to H2 was fixed at
,
in agreement with Willacy & Cherchneff (1998) and the survey of
Olofsson et al. (1993a). The CO envelope size was estimated based
upon modelling results from Mamon et al. (1988), which have been shown to
compare well with observations (Schöier & Olofsson 2001). The same
envelope size was assumed for all CO isotopomers.
The 12CO data used in the analysis are presented in Schöier & Olofsson (2001) and Schöier et al. (2002) for CIT 6, IRC +10216, IRAS 15194-5115, and IRC +40540 and consist of both millimetre and sub-millimetre line data as well as far infra-red high-J transitions observed by ISO. The best fit 12CO model obtained for AFGL 3068 is overlayed onto observations and presented in Fig. 3. For IRAS 07454-7112 and IRAS 15082-4808 only J=1-0and J=2-1 line data as observed by the SEST, and presented here in Figs. 1, 2, A.1, A.2 and A.6-A.9, are available. Due to the limited number of constraints the h-parameter was assumed to be equal to 1.5, i.e., the dust properties were taken to be the same as for IRC +10216 and IRC +40540 for these two sources.
The CSEs of the sample stars have similar physical
properties. However, the stars presented here are losing mass at a
significantly higher rate than the average carbon star:
Schöier & Olofsson (2001) measure a median mass-loss rate for carbon
stars of 3
10-7
yr-1, based on a
sample of carbon stars complete within
600 pc from the
sun. This suggests that the stars in the sample presented here are
going through the super-wind phase of evolution
(e.g. Vassiliadis & Wood 1993) at the end of the AGB, and will soon
eject the entire stellar mantle.
![]() |
Figure 3: Multi-transition CO millimetre-wave line emission observed towards AFGL 3068. The observed spectra (histograms) have been overlayed with the best fit model results (solid lines). Also shown, lower right panel, is the observed radial brightness distribution (boxes with error bars) overlayed by the results from the model (full line), with the circular beam used in the radiative transfer analysis (dot-dashed line). The transition, telescope used, and the corresponding beamsize, are indicated for each observation. |
C18O emission was only detected towards IRC +10216 and a C16O/C18O-ratio of 1050 is derived, using four observational constraints (including three different transitions J=1-0, 2-1, 3-2) for C18O. This value is in excellent agreement with the 16O/18O-ratio of 1260 obtained by Kahane et al. (1992), using a combination of optically thin emission lines. In comparison, the value of this ratio in the solar neighbourhood is around 500. The 16O/18O-ratio and in particular the 17O/18O-ratio, which is not measured here, can be used as tracers of nucleosynthesis. Like the 12C/13C-ratio, these ratios are thought to increase as the star evolves along the AGB. Kahane et al. (1992) indeed find support for this scenario in a small sample of carbon-rich evolved stars.
The calculation of isotope ratios of various species (as shown in Table 8) shows in general that many lines are optically thick (i.e., the ratio derived from observations is lower than the 12CO/13CO abundance ratio derived from the radiative transfer analysis). Where this is the case, the abundance of the main isotope (viz., CN, CS and HC3N) has been calculated by scaling the abundance of the less abundant isotope by the 12CO/13CO-ratio. This is indicated by the bold-faced type in Table 7. The abundance of HCN is not calculated using Eq. (3) since the line is certainly optically thick, but in all cases only by scaling the abundance of H13CN by the calculated 12CO/13CO-ratio.
![]() |
Figure 4: The density (solid line) and kinetic temperature (dotted line) structures obtained from the CO excitation analysis for AFGL 3068. Also shown is the excitation temperature of the CO(J=2-1) line (dash-dotted line). |
When two or more transitions of the same molecule are observed, it is
possible to make an estimate of the rotation temperature
(
)
of that molecule using
Eq. (3). Assuming a molecular species to be excited over the
same radial range, and according to a single temperature, the
rotational temperature can be estimated. The results are shown in
Table 5. It is clear that the rotational temperatures
vary from source to source and between molecular species in the range
3-30 K, as to be expected. The average excitation temperature
is 8.7 K (averaged over the individual excitation temperatures for
all sources, rather than molecular species). A generic value of 10 K
was assumed for all the abundances estimated.
Table 5: Rotation temperatures.
All molecules are assumed to be linear, rigid rotators, except for SiC2 and C3H2 which are asymmetric tops and CH3CN, which is a prolate symmetric top. Einstein A-coefficients (where available) and energy levels are taken from Chandra & Rashmi (1998) for SiC2, from Vrtilek et al. (1987) for C3H2, and from Boucher et al. (1980) for CH3CN.
The partition function, Z, is calculated assuming that no molecules
have a hyperfine structure, i.e. as having simple rotational energy
diagrams. Hence the integrated intensities which are summed over all
hyperfine components are used. For C3H2, CH3CN and SiC2 we use the approximate expression for an asymmetric rotor
(Townes & Schawlow 1975) multiplied by 2 for C3H2, by 4 for
CH3CN (to account for spin statistics) and by 1/2 for SiC2 (since half of the energy levels are missing because of spin
statistics). It is assumed that all levels are populated according to
.
To calculate the radial extent of the molecules HCN, CN, C2H and CS
the photodissociation model of Huggins & Glassgold (1982) is
adopted. The photodissociation radius of a parent species
(
,
viz., HCN, C2H2, CS) is determined by
![]() |
(4) |
![]() |
(5) |
There will generally be a drift velocity between the dust and the gas
(e.g., Schöier & Olofsson 2001)
![]() |
(8) |
Table 6: Photodissociation rates.
The photodissociation radii of species formed in the photosphere were
chosen to be the e-folding radii of the initial abundances,
i.e.
,
where
is the
stellar radius. For the photodissociation products inner and outer
radii are chosen to be where the abundance has dropped to 1/e of its
peak value. The envelope sizes calculated by the simple
photodissociation model agree relatively well with observed values in
IRC +10216 and other objects, except in the case of SiS (see next
paragraph). Lindqvist et al. (2000) used a detailed radiative
transfer method and observed brightness distributions to derive
envelope sizes of HCN and CN. For IRC +10216 and
IRC +40540 they found envelope sizes of
4
1016 cm for HCN and
5
1016 cm
for CN, in excellent agreement with the values derived here from the
photodissociation model. In the case of CIT 6 the observed
HCN envelope size is larger than that calculated by a factor of
2. Envelope sizes and derived abundances are given in Table
7.
SiO and SiS are parent species with a radial extent depending on
photodissociation. The calculation of the SiS photodissociation radius
in IRC +10216, however, is not consistent with the radius
observed by Bieging & Tafalla (1993). Therefore the observed radius
for SiS in IRC +10216 was used in the abundance calculations,
and its radius was scaled for the other objects in the sample with the
factor
in
the same way as described in Sect. 5.4.2. The outer radius
calculated via the photodissociation model is actually slightly larger
than that observed. This gives credence to the idea that SiS freezes
out onto dust grains. SiO is treated in the same way as SiS since it
too is likely to freeze out onto grains. Hence the same envelope size
as SiS was adopted for this species.
Table 7: Abundances and sizes of emission regionsa.
The assumption of optically thin emission has a systematic effect on the derived abundances, in that the true abundance will be higher if there are opacity effects. As can be seen from Table 8, there can be a factor of 2-3 in error from this assumption.
The accuracy of the calculated abundances is dependent on various
assumptions. Due to the intrinsic difficulties in estimating distances
to the objects included in the sample, the typical uncertainty in the
adopted distance is a factor of 2. This influences the mass-loss
rates derived in the radiative transfer modelling such that the
adopted mass-loss rate will scale as D1-2. The calculation of the
limiting radii of a certain molecular distribution in the envelope is
also affected by inaccuracies in the distance estimate. Where radii
have been calculated by scaling observed radii in IRC +10216,
there comes an error which scales as D. The results from the
photodissociation model will have a lesser dependence, with D coming into the expression for the shielding distance, via
.
Hence the abundance, which is trivially derived from
Eq. (3), will vary as approximately D-1-0, giving
a factor of 2, possibly, in error.
In the present analysis an excitation temperature of 10 K was assumed
for all transitions. The error in abundance estimate due to this
assumption will depend on the excitation temperature of a particular
transition and the assumption of LTE, and is estimated to be not more
than a factor of 2.
Overall, it seems like an error of a factor of 5 is reasonable to expect in the abundances presented here, although it should be borne in mind that this could possibly rise to an order of magnitude. In the comparison of abundance ratios in Table 9, any difference less than a factor of 5 is treated as insignificant with respect to error margins.
In comparison with Nyman et al. (1993), derived abundance ratios
(Table 9) have increased in favour of IRAS
15194-5115 by up to a factor of approximately 4. Individual
abundances generally show a factor 2 increase for those in
IRAS 15914-5115, and a factor
2 decrease for
IRC +10216, over Nyman et al. (1993). In
Nyman et al. (1993), the distances adopted for IRC +10216
and IRAS 15194-5115 were approximately twice as large as
those here; however this has little effect on calculated abundances
since the distance ratio is more or less unchanged. However, the
calculated mass-loss rate of IRAS 15194-5115 in the previous
paper was larger than that of IRC +10216 by a factor of 2.5,
and here the recalculated mass-loss rates are the same for these two
objects. This would tend to increase the abundance ratios quoted by a
similar factor. The photodissociation radius depends on the mass-loss
rate and the dust parameters through the dust shielding
distance. Compared to Nyman et al. (1993) this paper uses different
mass-loss rates, a different gas-to-dust ratio (0.01 compared to
0.005), and the dust parameters are also slightly different due to the
determination of the h-factor in the radiative transfer
analysis. The scale factor that determines the inner and outer radii
of the species with a origin in circumstellar chemistry depends on the
ratio of the mass-loss rates. Thus the difference in relative mass
loss rates explains the factor of 4 difference in relative abundances
between IRAS 15914-5115 and IRC +10216 derived in
this paper compared to those derived in Nyman et al. (1993).
As discussed earlier in this paper the outer radii of SiS and SiO are
not determined through the photodissociation radius but scaled from
their observed radius in IRC +10216. In this way the calculated
abundances of SiO and SiS have increased in by a factor of 4-5 for
IRAS 15194-5115 compared to Nyman et al. (1993). For
IRC +10216 these species have the same abundance as calculated
previously, and they are in reasonable agreement with those reported
elsewhere in the literature. Bujarrabal et al. (1994) give
f(SiO) =
and f(SiS) =
,
which
are
4 times greater, using an outer radius half that quoted in
this paper and a distance of 200 pc. Better agreement is seen for
the other species which Bujarrabal et al. (1994) detect, with the
exception of HNC, which is a factor
6 in disagreement.
Cernicharo et al. (2000) also calculate abundances in
IRC +10216, and are within a factor 5 of those here.
Generally, it seems that IRC +10216 has lower abundances than IRAS 15194-5115, IRAS 15082-4808, IRAS 07454-7112 and CIT 6. However, it is very similar, physically and chemically, to AFGL 3068 and IRC +40540.
The three northern sources observed at OSO have also been studied in
the literature, and abundances derived. The
Bujarrabal et al. (1994) paper includes data relating to
CIT 6, AFGL 3068 and IRC +40540. All
abundances calculated by Bujarrabal et al. in these three sources are
greater than those derived here. Distances and mass-loss rates are
reasonably comparable between this paper and that. Generally, this
means that the calculated abundances in this paper are lower by a
factor of 2 in CIT 6, a factor of
5 in
AFGL 3068, and a factor of
3 in IRC +40540
compared to those derived in Bujarrabal et al. (1994).
Table 8: Molecular isotope abundance ratios.
Table 9: Abundance ratios, compared to IRC +10216 observed with the SEST.
In Table 10 the abundances obtained by
Willacy & Cherchneff (1998) for TE and non-equilibrium chemical modelling (shock
strength of 11.7 km s-1) are compared to the values obtained in
the analysis. Given the uncertanties, about a factor of five, the
abundances obtained from the observations clearly favour a scenario in
which a shock has passed through the inner (5
)
parts of the wind. The SiO and SiS abundances which are derived are
lower limits since they could be significantly depleted in the outer
envelope due to freeze-out onto dust grains. The average abundances
derived for HCN, CS, and SiO in the sample are
,
,
,
respectively. The SiO
abundance shows the largest spread among the sources reflecting its
sensitivity to the shock strength and possible variation in the
C/O-ratio among the sample sources. CS might, however, not be
particularly well suited as a probe of shocked
chemistry. Olofsson et al. (1993a) found, when modelling a large
sample of optically bright carbon stars, that in their photospheric
LTE models the CS abundance varied considerably with adopted stellar
temperature.
Many photochemical models have been developed for the outer envelope
of IRC +10216
(e.g. Millar & Herbst 1994; Doty & Leung 1998; Millar et al. 2000). The physical conditions in the outer parts of the
wind (100
)
allow for the penetration of ambient
ultraviolet radiation that induces a photochemistry. In
Table 11 the derived column densities for
IRC +10216 for a number of species produced in the envelope
are compared to those from the photochemical model of
Millar et al. (2000). In general the abundances agree well, given
the uncertainties.
It is remarkable that the abundances generally show relatively little
variation within the sample. Most apparent is the over-abundance of
Si-bearing molecules in CIT 6 (Sect. 6.3). Some of the
abundances of IRAS 15194-5115 also stand out and will be
separately discussed in Sect. 6.2. There are no apparent
trends with the stellar or circumstellar parameters. This would
suggest that the physical structure in these sources indeed is much
the same and that the initial atomic abundances are similar. When
comparing the present sample of carbon stars to the sample of
Olofsson et al. (1993a), which on the whole tend to have a low
mass-loss rate (10-7
yr-1), the agreement
in derived abundances for the star in common, CIT 6, is very
good. There is less than a factor 3 difference in the calculated
abundances of HCN, CN and CS. However, in general, the sample of low
mass-loss rate stars has calculated abundances which are
systematically an order of magnitude greater than those calculated
here. It must be noted that Olofsson et al. (1993a) use an
excitation temperature of 20 K, twice that used in this
analysis. Moreover, Schöier & Olofsson (2001) show that the
mass-loss rates in the low mass-loss rate objects in
Olofsson et al. (1993a) are underestimated by about a factor of 5
on average. This would explain the apparent discrepancy in calculated
abundances between the high mass-loss rate objects here and the lower
mass-loss rate objects in Olofsson et al. (1993a). Hence there
seems not to be a marked difference in the molecular composition of
high and low mass-loss carbon stars.
The large spread in the abundance of isotopomers containing 13C follows from the varying 12C/13C-ratio among the sample sources. The 12C/13C-ratio is related to the nucleosynthesis rather than the chemistry and reflects the evolutionary status of these stars. However, chemical fractionation may affect this ratio in certain molecules, in particular CO.
CN/HCN and HNC/HCN ratios can also be used to estimate the
evolutionary status of carbon stars. CN is produced via the
photodissociation of HCN by ultraviolet radiation, and as stellar
radiation increases with evolution from AGB star to PPN to PN, so the
CN/HCN ratio will increase
(e.g., Bachiller et al. 1997a; Cox et al. 1992). HNC, formed from
the dissociative recombination of HCNH+, behaves in a similar
way. In this sample there is a rather large spread in the CN/HCN
ratio, from 0.07-0.68, and a value of 1.82 for CIT 6 (see
Sect. 6.3). This large spread is in contrast to
Olofsson et al. (1993a), for example, who found a very narrow range
(CN/HCN 0.65-0.70) in low mass-loss stars. However, there is
excellent agreement with the results of
Lindqvist et al. (2000). For the carbon stars IRC +10216,
CIT 6 and IRC +40540 they derive ratios of 0.16, 1.5
and 0.17, respectively, in comparison with the 0.22, 1.82 and 0.15
derived here. A CN/HCN ratio of
0.5 is typical in C-rich AGB
stars (Bachiller et al. 1997b) , increasing to
5 in PPNe. In
fact, a ratio of 0.6-0.7 is predicted by the photodissociation model,
with only a weak dependence on mass-loss rate
(see Fig. 8 of Lindqvist et al. 2000). The HNC/HCN ratio seems to be split into
two ranges in the present sample of carbon stars. IRC +10216,
AFGL 3068 and IRC +40540 have HNC/HCN ratios of
0.005, whilst the remaining stars have ratios of 0.01-0.03. The
value derived for IRC +10216 is in agreement with that quoted
in Cox et al. (1992). This seems to indicate that the sample stars
are not well evolved, since a HNC/HCN ratio of
1 is expected in
PPNe (e.g., Cox et al. 1992). Having said this, the HNC/HCN
ratio does rapidly become of the order 1, as can be seen in models of
PPN chemistry (Woods et al. 2003).
Generally, it seems that to use the term carbon chemistry to refer to a paradigm of chemistry in C-rich evolved stars is reasonable. Of the sample stars here, given the variety of molecular species, there is very little difference in molecular abundances, save for two slightly curious sources, as detailed in the following subsections.
Table 10: Fractional abundances for IRC +10216 for species of photospheric origin.
The modelled 12CO/13CO ratio in this source agrees well with that carried out previously (Groenewegen et al. 1996; Schöier & Olofsson 2000). This ratio, however, does not agree with 12C/13C ratios derived from observations of other molecules and their 13C isotopes, both in this paper (Table 8) and elsewhere (Kahane et al. 1992; Groenewegen et al. 1996).
A further point worth note is the comparative over-abundance of Si-bearing species which possibly indicates a less efficient freeze-out onto dust grains in this particular source.
Table 11: Radial column densities (cm-2) for species of circumstellar origin towards IRC +10216.
The most striking difference between the abundances are reflecting the spread in the 12C/13C-ratio of about an order of magnitude between the sample stars. Also, the high abundance of SiO in the envelopes indicates that a shock has passed through the gas in the inner parts of the envelope. This is further corroborated by the relatively low amounts of CS and possibly HCN.
The abundances of species that are produced in the outer parts of the wind can be reasonably well explained by current photochemical models.
Acknowledgements
We are grateful to F. Kerschbaum for help with estimating some of the input parameters to the CO modelling. FLS is supported by the Netherlands Organization for Scientific Research (NWO) grant 614.041.004. The Swedish-ESO Submillimetre Telescope, SEST, is operated jointly by ESO and the Swedish National Facility for Radioastronomy, Onsala Space Observatory at Chalmers University of Technology. The OSO 20 m telescope is operated by the Swedish National Facility for Radioastronomy. This article made use of data obtained through the JCMT archive as Guest User at the Canadian Astronomy Data Center, which is operated by the Dominion Astrophysical Observatory for the National Research Council of Canada's Herzberg Institute of Astrophysics.
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Figure A.1: High-resolution spectra of IRAS 07454-7112, obtained with the SEST. |
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Figure A.2: High-resolution spectra of IRAS 07454-7112, obtained with the SEST. |
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Figure A.3: High-resolution spectra of CIT 6, obtained at OSO. |
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Figure A.4: Low-resolution spectra of CIT 6, obtained at OSO. |
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Figure A.5: Low-resolution spectrum of CIT 6, obtained at OSO. |
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Figure A.6: High-resolution spectra of IRAS 15082-4808, obtained with the SEST. |
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Figure A.7: High-resolution spectra of IRAS 15082-4808, obtained with the SEST. |
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Figure A.8: Low-resolution spectra of IRAS 15082-4808, obtained with the SEST. |
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Figure A.9: Low-resolution spectra of IRAS 15082-4808, obtained with the SEST. |
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Figure A.10: High-resolution spectra of AFGL 3068, obtained at OSO. |
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Figure A.11: Low-resolution spectra of AFGL 3068, obtained at OSO. |
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Figure A.12: High-resolution spectra of IRC +40540, obtained at OSO. |
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Figure A.13: Low-resolution spectra of IRC +40540, obtained at OSO. |