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Astron. Astrophys. 362, 273-280 (2000) 3. Discussion3.1. Spectral featuresThe spectrum shown in Fig. 1 exhibits many features. Some of them are weak or blended and their identifications are uncertain. However, some features are relatively strong and isolated from other lines. The last include absorption features at 4.27 and 13.68 µm, a broad emission band around 18.1 µm (which, however, most likely is an artifact produced by the glitches - see below), and the other two broad absorption bands at 3.02 and 9.7 µm. To see these and other tentative detections in more detail part of the SWS spectrum is enlarged in Fig. 2 where, for sake of comparison, a continuum-divided spectrum around 3 µm is shown in the lower left panel.
The suggestion of C-richness of IRAS 03201 comes from its
absorption feature around 3.0 µm. Systematic
spectrophotometric observation of cool stars in the
2-4 µm region by Merrill & Stein (1976a,
1976b) and Noguchi et al. (1977) revealed this feature in all the
observed carbon stars. Furthermore, Ridgway et al. (1978)
identified the absorption features around 3.0 µm in
spectra of carbon stars as different bands of
C2H2 and HCN molecules (see also Cernicharo et
al. 1999 for the most recent ISO results). This feature is thus a
strong indication of C-richness. The comparison of
3.0 µm band of IRAS 03201 with that of genuine
C-rich star IRC+10216 (Cernicharo et al. 1999) shows them to be
similar in shape and position, while there are significant differences
with the 3.0 µm water ice band observed in O-rich
stars (e.g. Sylvester et al. 1999). The 3.0 µm band
consists of two absorption valleys whose minima are at about 3.02 and
3.08 µm and the first one being deeper if it is due
to C-bearing molecules and is relatively irregular with predominantly
single minimum at about 3.05-3.10 µm if it is due to
water ice. The idea that the 3 µm feature in
IRAS 03201+5459 is C-based is further supported by the existence
of another feature at about 13.7 µm which is
detected in the ISO-SWS spectra of several C-rich stars (Yamamura et
al. 1998) and interpreted as a On the other hand, in the SWS 01 spectrum of IRAS 03201
there are a few features which usually occur in an O-rich environment.
The broad absorption feature at 9.7 µm is generally
accepted as a stretching band of amorphous silicate dust. It is seen
in O-rich AGB stars with optically thick circumstellar shells. Because
the oxygen atoms are thought to react effectively with carbon to form
CO, there is no excess of oxygen atoms to generate silicates in a
C-rich environment. As can be seen from the following model fitting,
the center of this feature actually is a little blue shifted (exact
center at 9.67 µm) in comparison with that expected
from the circumstellar silicates (David & Pegourie 1995).
It could mean that this band is due to some polluted silicate dust
other than the circumstellar silicates. Therefore the
possibility mentioned in the Introduction that the observed feature
could be due to interstellar absorption is investigated here in more
detail. Detailed maps in 12CO (Digel et al. 1996) showed
that there is an intervening cloud in direction of our source
(l = 143.59o, b = -1.46o)
which has a peak of 12CO emission at
l = 143.8o and b = -1.5o and
a line-of-sight velocity with respect to the local standard of rest,
There are at least four possible explanations of this discrepancy.
Firstly, the relation of Bachiller & Cernicharo (1986)
between 13CO column density and
Observations of dust in interstellar medium show that the structure of silicates remains mostly amorphous (Dorschner & Henning 1995). However, crystalline silicates are present in significant amounts around some late type stars including post-AGB sources and planetary nebulae (Waters et al. 1998a, Waters et al. 1998b, Cohen et al. 1999, Waters & Molster 1999, Molster et al. 1999b). Spectroscopic observations (Waters & Molser 1999) seem to suggest that crystalline silicates tend to appear only when the mass loss rate from the star is sufficiently high. These data also suggest that the process of crystallization takes place not only in the long-lived reservoir of orbiting matter left over from previous episodes of mass loss (e.g. the Red Rectangle - Waters et al. 1998a) but also in the outflows from late type stars (e.g. OH 32.8-0.3 - Waters & Molster 1999). Therefore the presence of crystalline silicate bands in our SWS 01 spectrum would suggest the existence of oxygen rich material concentrated around IRAS 03201. In spite of poor data quality in band 3, features of crystalline enstatite and/or forsterite at 21.5, 24.5 and relatively strong emission at about 18.1 µm seem to be present. For comparison, in Fig. 1 we have marked some positions (16.1, 18.1, 21.5, 23.6 and 24.5 µm) of crystalline silicate bands identified in the spectrum of AFGL 4106 by Molster et al. (1999a). Because the strength and shape of the 18.1 µm feature is rather unusual as compared to the already published ISO spectra with crystalline silicate signatures, we examined carefully the data from all detectors in band 3C. We found that there are two glitches: one at about 17.5 µm in the down scan (increasing wavelength with time of observation) and a second at about 18.5 µm in the up scan (decreasing wavelength). The extended tails which result from these glitches overlap (the down scan is particularly disturbed by this) and it is very difficult to find the continuum in the vicinity of 18 µm. Therefore, we think that the feature seen around 18.1 µm is most likely an artifact of data reduction. A small contribution from crystalline silicates could be present but it is impossible to prove this on the basis of our ISO data. In ISO SWS 01 spectrum of IRAS 03201, there is another O-bearing molecular absorption feature at 4.27 µm, identified as due to solid CO2. The identification is furthermore supported by the tentative detection of an absorption around 15.2 µm also due to solid CO2, and a tentatively detected absorption at 4.38 µm from solid 13CO2 (see Fig. 2). The narrowness of the feature with minimum around 4.27 µm suggests it is caused by polar (H2O and/or CH3OH-rich) CO2 ice (e.g. Ehrenfreund et al. 1999) while the wing on the short wavelength side of this feature is probably due to a non-polar component (e.g. Sandford & Allamandola 1990). Most likely, the CO2 ice bands in spectrum of IRAS 03201 come from the intervening cloud discussed above. The column density, N(CO2) (assuming band strength 7.8 10-17 cm molecule-1 - Gerakines et al. 1995) is only about 4 1016 cm-2, one of the smallest values found (see e.g. Table 7 of Gerakines et al. 1999). This could favour the explanation that the intervening cloud is not of high AV. The column density determination for 13CO2 is very uncertain since the feature at 4.38 µm is weak and the spectrum around it is noisy. However under the resolution and signal to noise ratio achieved in the case of IRAS 03201, we cannot conclude that solid and/or gaseous CO2 does not exist around the source itself. For example, relatively broad absorption feature around 4.2-4.3 µm and weak absorption around 14.97 µm have been detected the Red Rectangle, a C-rich object, (Waters et al. 1998a) and attributed to gas-phase CO2, although as they state the contribution from solid CO2 of circumstellar origin to the 4.27 µm band is also possible. The stretching-mode resonance of gaseous CO2 visible in range from about 4.20 to 4.35 µm with minimum around 4.23 µm has been detected in the O-rich star NML Cyg (Justtanont et al. 1996), in two O-rich Miras (Yamamura et al. 1999b) and in a few OH/IR stars (Sylvester et al. 1999). One more example of O-bearing molecular features in our spectrum is
the tentatively detected absorption feature around
7.3 µm due to the Summarizing above discussion all the O-based features detected in
the spectrum of IRAS 03201 could be, at least partly, of
interstellar origin. However, we were not able to prove that the
interstellar extinction is high enough to be responsible for the
observed strength of the 9.7 µm absorption feature.
Therefore, it seems plausible to consider that at least part of the
O-rich features are of circumstellar origin. The co-existence of both
O-bearing and C-bearing spectral features would suggest that the
object is chemically complex. An alternative possibility is that the
C-bearing molecules are produced at the outer
( 3.2. Spectral energy distributionIn order to investigate the nature of this object, we try to fit the spectral energy distribution (SED) by radiative transfer modelling. Without additional observations we are not able to solve the question of the location of O-rich material, i.e. whether this material is located in some kind of disk-like structure seen edge on or it is flowing outwards after a phase of O-rich mass loss. For the purpose of this paper we will consider only the later possibility. The basic idea of such a model is a solution of the radiative transfer through the dusty circumstellar envelope. The central star is assumed to radiate as a blackbody and to lose mass at constant rate with the resulting envelope expanding at constant velocity. Under these assumptions, the frequency-dependent radiative transfer equations are solved under the spherically-symmetric geometry simultaneously with the thermal balance equation for dust (Szczerba et al. 1997). The important parameters that determine the final SED include the properties of the star, the properties of the gas/dust envelope and the (dust) mass loss rate. They are adjusted in a reasonable range for an AGB star in order to fit the observed SED. Because no information is available on the expansion velocity of the circumstellar envelope, a typical value of 15 km s-1 is adopted. As a first step, a one-dust-component model is constructed in spite of the conflicting circumstellar spectral features. No reasonable fit to the SED could be found by assuming
circumstellar silicates (David & Pegourie 1995) as the dust
component in the circumstellar envelope, even when the parameters for
the model were changed over a wide range. The main shortcoming of the
silicate dust model lies in its producing too wide an SED in
comparison with the observed SED of IRAS 03201. On the other
hand, a reasonable fit to the continuum radiation is achieved by
assuming amorphous carbon (AC1 from Rouleau & Martin 1991) as the
dust component of the circumstellar envelope. The values of key
parameters for the best fit with AC1 are listed in Table 1. The
stellar effective temperature 3000 K and luminosity
8000 Table 1. Parameters for AC1 dust model. 3.3. Two-dust-component modelAccording to the theoretical study of stellar evolution in the AGB phase, when a carbon star forms there should be a period when the star has two dust components in the circumstellar envelope. When the third dredge-up process occurs, the newly produced carbon and other elements from the He-burning shell are convected to the surface of the stellar photosphere, which can then be brought to the circumstellar envelope by a stellar wind. When the O-rich star becomes C-rich after the fatal He-shell flash, both sorts of dust could co-exist in the circumstellar envelope. This phase is short (of order of hundred years - see e.g. Mowlavi 1999) and thus difficult to catch observationally, but, at least theoretically it is not impossible to find such object. We constructed a model based on such a theoretical scenario with a central star surrounded by an inner C-rich and an outer O-rich circumstellar shell. We assume that there is no gap between the two shells, which means the mass loss is continuous when the star changes chemical composition. The earlier mass loss process forms the outer O-rich shell and the later mass loss after the star becomes C-rich creates the inner C-rich shell. The basic framework of the model is then similar to that for one dust component, i.e. the frequency-dependent radiative transfer equations are solved under the spherically-symmetric geometry simultaneously with the thermal balance equation for a dusty envelope. As the mass loss rate and dust-to-gas ratio are dependent on each other, the mass loss rate is assumed to be the same for these two phases of mass loss process but the dust-to-gas ratios can differ. The best fit we can obtain by the two-dust model is an improvement
in comparison with the one-dust component model. Both the silicate
feature and the overall energy distribution can be approximately fit
simultaneously. The values of key parameters for this fit shown in
Fig. 4 are listed in Table 2. If the dust-to-gas ratios for
O-rich and C-rich stellar winds are the same then the O-rich mass loss
rate would be 1.6 times that for C-rich case. The thinner C-rich shell
close to the central star extends up to about
0.15
Table 2. Key parameters for two-dust (AC1+silicate) model Early in 1986, Little-Marenin (1986) and Willems & de Jong (1986) found nine stars which showed silicate emission at 9.7 µm but were optically identified as carbon stars. Some of these sources may be mis-identified, but several others do seem to have both the silicate and C-rich features (see e.g. Kwok et al. 1997for one of the most recent lists of such sources). Because the majority of these silicate carbon stars are 13C-enhanced J-type (Lambert et al. 1990, Le Bertre et al. 1990, Lloyd-Evans 1990), a binary model was proposed. However the presence of a mass-losing O-rich companion was ruled out observationally for a number of silicate carbon stars (Noguchi et al. 1990; Engels & Leinert 1994). In addition, an object with both O-rich and C-rich spectral features has been found in LMC (Trams et al. 1999). In a single-star model, such silicate carbon stars would have experienced O-rich mass loss which formed the O-rich shell that has already expanded to become optically thin at 9.7 µm, producing the emission feature. Their central stars have become C-rich after the third dredge-up process ejected the freshly produced C from the burning shell to the photosphere. Note, however, that Jura & Kahane (1999) found narrow emission lines of CO from two carbon-stars with oxygen-rich envelopes, which can be interpreted as an evidence of long-lived reservoir of orbiting gas in a thin disk. This gas, if O-rich and not seen exactly edge-on, could give rise to observed silicate emission. Despite the still ongoing discussion on the nature of silicate
carbon-stars, IRAS 03201+5459 might be related to this group of
sources. As opposed to previously known sources, the feature at
9.7 µm is in absorption rather than in emission.
That would mean the O-rich shell is still optically thick at
9.7 µm, if we follow the outflow scenario the object
is at earlier evolutionary stage than those with an emission feature
at 9.7 µm. Willems & de Jong (1986)
suggested that after the transition from O-rich to C-rich star there
is an interruption of mass loss. Investigation of the chemical
composition inside detached shells by Zuckerman (1993) suggested,
however, that such shells could be C-rich rather than O-rich. The
short timescales for O-rich and C-rich shells derived from the
modelling of SED for IRAS 03201 could be interpreted as a
signature of the mass loss during the ongoing thermal pulse. After the
transformation of the atmosphere from O-rich to C-rich the dust
composition changes correspondingly and the mass loss follows the
luminosity behaviour during the thermal pulse. If so, then in a short
time the mass loss rate would decrease significantly and the already
C-rich star in IRAS 03201 might appear as an object with silicate
emission and then as an optically identified C-star with a detached
shell and with no clear signature of O-richness inside the expanding
shell (see example of theoretical modelling of the AGB evolution by
Steffen et al. 1998). Taking into account the obtained circumstellar
3.4. Other possibilitiesThere could be an alternative scenario related to the nature of IRAS 03201. The broad features at 3 µm and 9.7 µm are seen simultaneously in the so-called BN Orion objects (Merrill & Stein 1976c, Willner et al. 1982). Such objects represent a very early stage of stellar evolution (Becklin & Neugebauer 1968) and are referred to protostars. The 3 µm feature in protostars is attributed to amorphous water ices (Gillet & Forrest 1973) and the 9.7 µm feature is attributed to the silicate particles as in the late-type O-rich stars. The spectrum of the protostellar object RAFGL 7009S by ISO-SWS in AOT 01 mode revealed the absorption features of CO2 at 4.27 µm and 15.21 µm (Ehrenfreund et al. 1997). So apparently all the strong spectral features present in IRAS 03201 can be explained if it is a protostar. However, the 3 µm feature observed in IRAS 03201 resembles that produced by C2H2 and HCN molecules in C-type stars instead of that of water ice in protostars. The SED does not support the protostar model either. The 2-10 µm region of SED can be fit roughly by a blackbody at a temperature of about 760 K which gives a little less emission in the longer wavelength than the observed spectrum. The blackbody-like SED is consistent with the characteristics of protostars, but this temperature is too high for protostars. One more possible explanation of IRAS 03201 nature is related to the fact that the spectral energy distribution of IRAS 03201 looks similar to that of late-type Galactic Wolf-Rayet (WR) stars (e.g. van der Hucht et al. 1996). In this group of objects the observed 9.7µm features are solely interpreted as due to the interstellar absorption. However, there are many differences between IRAS 03201 and the galactic Wolf-Rayet stars. For example, neither the 3.0 µm feature nor the CO2 absorption features have been detected in any of the WR stars. ![]() ![]() ![]() ![]() © European Southern Observatory (ESO) 2000 Online publication: October 30, 19100 ![]() |