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Astron. Astrophys. 359, 586-596 (2000) 4. Model results4.1. The
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Fig. 2. Multi-transition 12CO and 13CO millimetre wave line emission observed towards the high mass loss rate Mira variable CW Leo. The observed spectra (histograms) have been overlayed with the model prediction (full line) using a mass loss rate of 1.5![]() ![]() ![]() ![]() ![]() ![]() ![]() ![]() ![]() ![]() ![]() |
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Fig. 3. Multi-transition 12CO and 13CO millimetre wave line emission observed towards the optically bright carbon star U Hya. The observed spectra (histograms) have been overlayed with the model prediction (full line) using a mass loss rate of 1.0![]() ![]() ![]() ![]() ![]() ![]() ![]() ![]() ![]() ![]() ![]() |
The derived envelope parameters, used as input for the
13CO modelling, are presented in Table 3. We believe
that, within the adopted circumstellar model, the estimated mass loss
rates are generally accurate to within
50% (neglecting errors introduced by
the uncertain CO abundance and the distance estimates). In the models
presented here only 12CO line cooling was included. For the
J-stars, cooling from 13CO will be important (scales with
the isotope ratio for these low mass loss rate objects), but it will
not affect the derived mass loss rate since the heating must be
increased, i.e., the kinetic temperature structure will not change
significantly, in order to maintain a good fit (Schöier &
Olofsson 2000). See also the discussion in Ryde et al. (1999) for
the high mass loss rate object IRAS 15194-5115, where radio and
far-IR 12CO and 13CO data are modelled.
When comparing our mass loss rate estimate for CW Leo to those
obtained from other detailed radiative transfer models (Kastner 1992;
Crosas & Menten 1997; Groenewegen et al. 1998) we find a very
good agreement, within 20%, when adjustments for differences in
and distance have been made. Kastner
(1992) also modelled the high mass loss rate object RW LMi
(a.k.a. CIT 6) obtaining (when corrected for the difference in
distance) a mass loss rate in excellent agreement with our estimate.
Sopka et al. (1989) used a much simpler radiative transfer model
to derive the mass loss rate for a number of AGB stars, of which four
overlap with our survey. For RW LMi they derived a mass loss rate
in excellent agreement with that obtained from our model. For
LP And, V384 Per, and V Cyg, however, there are
discrepancies of about a factor of two to three. It should be noted
though that Sopka et al. (1989) based their mass loss rate
estimates on observations of a single line,
J
1
0,
using a single telescope (OSO). For LP And, the source with the
largest discrepancy, we observe a
12CO(J
1
0)
line that is almost a factor of two stronger using the same
telescope.
Once the general characteristics of the CSE have been determined from the 12CO analysis, the observed 13CO line emission is modelled. Again, the observed intensities, as well as the line shapes, are generally well reproduced by the model. As for the 12CO modelling, this is illustrated for two of our sample stars, CW Leo (Fig. 2) and U Hya (Fig. 3).
The abundance of 13CO is usually (the J-stars provide an
exception) much smaller than that of 12CO, which leads to
significantly different excitation conditions for the rarer
isotopomer. For instance, the model 13CO line intensities
are more sensitive to the assumed properties of the central source of
emission, since radiative pumping via the first excited vibrational
state becomes important. Indeed, the 13CO
J1
0
and
J
2
1
transitions have inverted populations over parts of the envelope even
for a high mass loss rate object as CW Leo, Fig. 2. For the high
mass loss rate objects, however, the part over which there is a weak
maser acting is very small and the emission emanating from this region
is not detected in our observations. For thinner envelopes the part of
the envelope where the lowest rotational levels are inverted is larger
due to the fact that the pumping emission can penetrate further out
into the wind. In the case of U Hya, changing the inner radius of
the CSE or the luminosity of the star by
50% will change the estimated
13CO abundance by
20%.
In our modelling of the 13CO line emission we have
assumed that the 13CO envelope size is equal to that of
12CO. This is based upon the model results by Mamon
et al. (1988). In this model both the effects of
photodissociation and of chemical fractionation were included.
Chemical fractionation of CO occurs through the exchange reaction
(Watson et al. 1976)
+
+
+
,
where
35 K.
Below this temperature, the backward reaction is suppressed and
production of 13CO from 12CO is favoured. This
reaction can effectively produce 13CO in the outer, cool
parts of circumstellar envelopes. Mamon et al. (1988) concluded
that the difference between the 12CO and 13CO
abundance distributions, when tested over a large mass loss rate
interval, is always small, no more than 10 to 20%. Without the effect
of chemical fractionation the 13CO envelope would be
significantly smaller. This is due to the fact that CO is
photodissociated in lines and thereby exhibits considerable
self-shielding. Thus, the shielding is higher the higher the optical
depth, and hence it is less efficient for the less abundant
13CO. Using OSO we have obtained a brightness distribution
map of the
13CO(J
1
0)
emission around CW Leo. It is found that the model, with an
assumed 13CO envelope size equal to that of
12CO, reproduces the observed radial brightness
distribution within the observational errors, Fig. 2. A 20% smaller
13CO envelope gives the same
12CO/13CO-ratio but fails to reproduce the
observed radial brightness distribution within the observational
errors. This shows the importance of chemical fractionation, at least
in the cool outer parts of dense CSEs. In the case of the thin
molecular envelope around U Hya a 20% smaller 13CO
envelope size would increase the derived 13CO abundance by
about 20%. This illustrates that in the case of a thin CSE the CO
molecules are effectively excited to the photodissociation radius,
i.e., photodissociation determines the size of the emitting region,
whereas in a dense CSE excitation sets the size of the emitting
region.
In Table 4 we list the observed integrated
12CO/13CO line intensity ratios. They are
corrected for the differences in line strengths and beam-filling
factors (assuming the sources to be unresolved the combined effect
gives a correction, i.e., the
observed ratio is lowered by a factor of 0.87). Although we note that
some of our CSEs are resolved, we have nevertheless treated all our
sources in the same manner. Here we have chosen to integrate the
emission over the entire line in order to achieve better
signal-to-noise ratios. For optically thin lines this ratio should
provide a first order estimate of the abundance ratio. A narrow
velocity interval centered on the systemic velocity, where optical
depth effects are smallest, should give somewhat higher line intensity
ratios than those presented here. Nine of our sample stars have been
detected in the
13CO(J
1
0)
and/or the
13CO(J
2
1)
line. A simple comparison of the 12CO/13CO line
intensity ratios and the 12C/13C-ratios derived
by Lambert et al. (1986) shows a tight correlation of the form
(in the cases where more than one value is available in Table 4
we have used an average),
Thus, a straightforward use of line intensity ratios would lead to 12C/13C-ratios that, on the average, agree with those of Ohnaka & Tsuji (1996). However, any optical depth effects would lower the observed line intensity ratio.
In Table 3 we present the
12CO/13CO-ratios derived using our radiative
transfer code. They span a large range, from 2.5 to 90 (steps of 5 in
the 12CO/13CO-ratio was used to find the best
fit 13CO model, except for the J-stars where a smaller
step-size of 0.5 was used). For most of our observed stars the isotope
ratio obtained from the detailed radiative transfer is higher than
those estimated from simple line intensity ratios. The discrepancy is
fairly small for the objects with thin CSEs, but it increases with the
thickness of the CSE
(/
)
and reaches a factor of six for the high mass loss rate objects,
Fig. 4. This reflects that even for low to intermediate mass loss rate
objects there are optical depth effects, and a detailed modelling is
needed to derive reliable isotope ratios. In Table 3 we present,
for each star, the maximum tangential optical depth in the
12CO(J
2
1)
transition obtained in the modelling. The radial variation of the
tangential optical depth is shown for the high mass loss rate object
CW Leo in Fig. 2 and for the low mass loss rate object U Hya
in Fig. 3. The optical depth in the
12CO(J
1
0)
line is significantly lower.
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Fig. 4. The ratio between the 12CO/13CO-ratio obtained from the radiative transfer analysis and that obtained from the observed line intensity ratios (in the cases where more than one value is available in Table 4 we have used an average) as a function of the density of the shell (![]() ![]() ![]() |
The estimated 13CO abundance depends on the adopted
12CO abundance (assumed to be equal for all stars). We find
that to a first approximation it scales with
, since a lower (higher)
leads to a higher (lower) mass loss
rate to fit the 12CO line intensities and hence a lower
(higher) 13CO abundance to fit the 13CO line
intensities. This means that to a first approximation the estimated
12CO/13CO-ratios are only very weakly dependant
on the adopted 12CO abundance. We have varied some of the
other parameters in the model (see above), and conclude that in doing
so the derived 12CO/13CO-ratio changes by about
20%. With an additional uncertainty of
15% in the relative calibration of
the 12CO and 13CO data (the relative calibration
is usually better than the absolute calibration for any given
telescope), we estimate that the 12CO/13CO-ratio
is uncertain by about
30%. In the
cases were the 12CO/13CO-ratio estimate relies
on observations of just one line the uncertainty may be as high as
50% depending on the quality of the
data.
We compare first our derived 12CO/13CO-ratio for CW Leo with those found by others. Crosas & Menten (1997) derived, using a radiative transfer model similar to ours, an isotope ratio of 50, i.e., the same as we do. Greaves & Holland (1997) found a lower ratio of 32, and also a much lower ratio (24) for LP And, using a simple radiative transfer model. Kahane et al. (1992) found the 12C/13C-ratio to be 44 based on observations of optically thin lines. Kahane et al. (1992) also determined the 12C/13C-ratio for RW LMi obtaining a value of 31, in good agreement with our 12CO/13CO estimate for this object. Sopka et al. (1989) estimated 12CO/13CO-ratios for four of our stars that are all lower than our derived values. This is most probably an effect of the difference in the treatment of the radiative transfer. We also note that Dufour et al. (2000, in prep.), derive somewhat lower 12CO/13CO-ratios for the three J-stars.
For our sample stars we compare the circumstellar 12CO/13CO-ratios obtained from the modelling with the photospheric 12C/13C-ratios estimated by Lambert et al. (1986) in Fig 5. A good correlation of the form
is obtained. Lambert et al. (1986) give an uncertainty in
their estimated 12C/13C-ratios of about
40%. Included in our sample are stars
that have had a drastic change in their mass loss rate. For R Scl
and S Sct, stars with known detached CSEs (probably) produced
during a period of intense mass loss, we have performed the analysis
using the envelope parameters determined by Olofsson et al.
(1996). These results are included in Fig 5. We note here that
our results suggest that the 12C/13C-ratios in
the detached shells (with ages of about 103 and
104 yr for R Scl and S Sct, respectively) are the
same as the present ones in the photospheres.
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Fig. 5. Comparison between the estimated circumstellar 12CO/13CO-ratio obtained using our detailed radiative transfer code, and the photospheric 12C/13C-ratio estimated by Lambert et al. (1986). An open triangle indicate a lower limit and the solid line represents a 1:1 correlation. Note that at 12C/13C![]() |
© European Southern Observatory (ESO) 2000
Online publication: July 7, 2000
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