A&A 487, 645-657 (2008)
DOI: 10.1051/0004-6361:20078876
S. Ramstedt1 - F. L. Schöier1,2 - H. Olofsson1,2 - A. A. Lundgren3
1 - Stockholm Observatory, AlbaNova University Center, 106 91 Stockholm, Sweden
2 - Onsala Space Observatory, 439 92 Onsala, Sweden
3 - European Southern Observatory, Casilla 19001, Santiago 19, Chile
Received 19 October 2007 / Accepted 30 May 2008
Abstract
Context. In the recent literature there has been some doubt as to the reliability of CO multi-transitional line observations as a mass-loss-rate estimator for AGB stars.
Aims. Using new well-calibrated CO radio line observations, the main aim of the work presented here is to carefully evaluate the reliability of CO mass-loss-rate estimates for intermediate- to high-mass-loss-rate AGB stars with different photospheric chemistries.
Methods. Mass-loss rates for 10 intermediate- to high-mass-loss-rate AGB stars are derived using a detailed non-LTE, non-local radiative transfer code based on the Monte-Carlo method to model the CO radio line intensities. The circumstellar envelopes are assumed to be spherically symmetric and formed by constant mass-loss rates. The energy balance is solved self-consistently and the effects of dust on the radiation field and thermal balance included. An independent estimate of the mass-loss rate is also obtained from the combination of dust radiative transfer modelling with a dynamical model of the gas and dust particles.
Results. We find that the CO radio line intensities and shapes are successfully reproduced for the majority of our objects when assuming a constant mass-loss rate. Moreover, the CO line intensities are only weakly dependent on the adopted micro-turbulent velocity, in contrast to recent claims in the literature. The two methods used in the present work to derive mass-loss rates are consistent within a factor of 3 for intermediate- to high-mass-loss-rate objects, indicating that this is a lower limit to the uncertainty in present mass-loss-rate estimates. We find a tentative trend with chemistry. Mass-loss rates from the dust/dynamical model are systematically higher than those from the CO model for the carbon stars and vice versa for the M-type stars. This could be ascribed to a discrepancy in the adopted CO/H2-abundance ratio, but we caution that the sample is small and systematic errors cannot be excluded.
Key words: stars: AGB and post-AGB - stars: carbon - stars: late-type - stars: mass-loss
Although mass loss on the AGB can reach rates as high as 10
yr-1, the wind speed is quite low (
30 km s-1). The temperature of the outer parts of the atmosphere is low enough for dust to condense. These facts, combined with a high stellar luminosity (
10
), have lead to the conclusion that the winds of AGB stars are, at least partly, dust-driven, i.e., the mass loss from the star is driven by radiation pressure on grains and the gas is dragged away from the star by momentum-coupling between the grains and the gas (e.g., Lamers & Cassinelli 1999). The effects of the gas-dust interaction on the mass loss and wind formation have been studied by several authors (e.g., Simis et al. 2001; Habing 1996). Time-dependent dynamical models studying the effects of stellar pulsations (Bowen 1988) and further including detailed time-dependent dust formation (Höfner et al. 1995) have progressed to dynamical models in which the motion of the gas and dust particles is calculated and the radiative transfer is solved (Sandin & Höfner 2003). These models work well for carbon stars and support the dust-driven wind scenario, but the formation of silicate grains close enough to the star to drive mass-loss rates of the observed magnitude still poses a problem for M-type stars (Höfner & Andersen 2007; Woitke 2006).
Most likely, the average mass-loss rate increases as the star evolves along the AGB (Schöier & Olofsson 2001; Habing 1996). In addition to this steady increase, modulations of the mass-loss rate on shorter time scales are present (Habing 1996). Indications of this can be seen in observations of circumstellar CO line emission around some AGB stars with double-component line profiles (Knapp et al. 1998; Winters et al. 2003) and in observations of stellar and ambient Galactic light scattered by dust in circumstellar envelopes (CSEs) (Mauron & Huggins 2000,2001,2006). A process which can have a strong effect on the mass-loss properties of an AGB-star is the He-shell flash (or thermal pulse) (Olofsson et al. 2000; Steffen & Schönberner 2000; Schöier et al. 2005a; Olofsson et al. 1993). Other processes may be important during the very last stages when the star sheds the remaining few tenths of a solar mass of its hydrogen envelope (during a few hundred years) before it leaves the AGB (Skinner et al. 1997). Finally, the presence of a binary companion may influence the magnitude as well as the characteristics (e.g., the geometry) of the mass loss.
To make progress in the study of AGB stars, it is important to establish reliable mass-loss-rate estimators, which can be used primarily over a wide range of mass-loss rates and time scales and for different chemical types (M-, S-, and C-stars). Estimating AGB mass-loss rates through observations of circumstellar CO radio line emission, in combination with modelling of the radiative transfer, is considered to be one of the most reliable methods. Carbon monoxide line emission has also been used in a number of studies aimed at tracing the mass-loss history (Kemper et al. 2003; Schöier et al. 2002; Decin et al. 2007; Teyssier et al. 2006) and at identifying drastic mass-loss-rate changes at the end of the AGB (Heske et al. 1990; Justtanont et al. 1996). Detailed studies of the mass-loss properties of carbon stars (Schöier et al. 2002; Schöier & Olofsson 2001), M-type AGB stars (González Delgado et al. 2003; Olofsson et al. 2002), and S-type AGB stars (Ramstedt et al. 2006) have been performed on samples dominated by low-mass-loss-rate objects. It was concluded that for these types of objects the CO radio line emission is a good mass-loss-rate estimator, although not entirely free of problems.
It has been known for some time that for the higher mass-loss-rate objects the situation is less clear (Schöier & Olofsson 2001; Kastner 1992; Sahai 1990). A higher mass-loss rate leads to a decrease in the drift velocity between the dust and the gas and therefore a less efficient heating of the gas through collisions with dust grains. Since CO line emission is also a dominant coolant, the effect of an
increased mass-loss rate is increased cooling of the circumstellar gas. This, in combination with saturation of the spectral lines, leads to a
situation where the integrated CO line intensities are less dependent on
the mass-loss rate when it exceeds about
10
yr-1; the higher the frequency of the
lines the lower the mass-loss rate when the effect sets in. This
makes CO line emission a questionable mass-loss-rate estimator at mass-loss
rates in excess of 10
yr-1, an unfortunate
effect since we know that mass-loss rates up to
10
yr-1 are reached during the very final
stage, and this is also when the stars make their largest
contribution to the return of nuclear-processed material to the interstellar medium. In addition, Kemper et al. (2003) concluded that standard circumstellar radiative transfer models could not explain some CO line intensity ratios, and that the mass-loss-rate estimate is sensitively dependent on the (unknown) local turbulent line width.
An alternative way to estimate the mass-loss rate, not subject to the same problems, is to combine modelling of the dust radiative transfer with solving the coupled equations of motion for the gas and the dust particles (Habing et al. 1994). The gas expansion velocity is a strong function of the dust-to-gas mass-loss-rate ratio and therefore a solution to the kinematical equations that fits the gas expansion velocity and the dust optical depth, obtained through dust radiative transfer modelling, results in an independent estimate of the mass-loss rate.
Presented here are a detailed radiative transfer modelling of primarily new, well-calibrated, and high signal-to-noise ratio observations of CO
,
,
,
,
and
emission from a sample of 10 well-studied high-mass-loss-rate AGB stars and the resulting mass-loss-rate estimates. In addition, dust emission modelling combined with a dynamical model give independent estimates of the mass-loss rates. The dust emission modelling also provides the dust information necessary for the CO modelling, e.g., the dust radiation field. By obtaining the mass-loss rates for the stars using two independent methods, we can evaluate the reliability of the mass-loss-rate estimators and also look for trends with e.g. mass-loss rate and chemistry. A similar investigation comparing mass-loss-rates derived from ISO-SWS observations of the silicate dust features with mass-loss rates from CO modelling found in the literature on a sample of low-mass-loss-rate M-type AGB stars has been performed by Heras & Hony (2005).
The sample and the observational data are presented in Sects. 2 and 3. In Sect. 4 the adopted circumstellar model is discussed. In Sect. 5 the CO radiative transfer model is described and CO as a mass-loss-rate estimator is discussed. In Sect. 6, we describe how dust radiative transfer and the dynamical model is used to estimate mass-loss rates. The results are presented in Sect. 7 and outlined for each individual object in Sect. 8. In Sect. 9 we discuss and compare the two methods, and in Sect. 10 we give our conclusions.
The sample, presented in Table 1, consists of 10 well-studied AGB stars, with intermediate to high mass-loss rates. They are chosen with a spread in mass-loss rate, to allow studies of possible trends. Dependences on chemistry can also be investigated, since half of the stars were chosen to have a photospheric C/O-ratio >1 (carbon stars) and the other half C/O < 1 (M-type).
Source | Spec. | Var. | P | ![]() |
D | ||
Type | Type | [ days] |
![]() |
[ pc] | |||
LP And | C | Mira | 620 | 8200 | 620 | ||
CW Leo | C | Mira | 630 | 8300 | 120 | ||
RW LMi | C | SRa | 640 | 8500 | 390 | ||
V384 Per | C | Mira | 535 | 7000 | 590 | ||
AFGL 3068 | C | Mira | 696 | 9300 | 1090 | ||
TX Cam | M | Mira | 557 | 11900 | 440 | ||
GX Mon | M | Mira | 527 | 11100 | 630 | ||
WX Psc | M | Mira | 660 | 14600 | 720 | ||
IK Tau | M | Mira | 500 | 10400 | 300 | ||
IRC-10529 | M | Mira | 680 | 15100 | 890 |
Bolometric luminosities are estimated using the period-luminosity relation of Feast et al. (2006) for the carbon stars, and that of Whitelock et al. (1994) for the M-type stars. Periods are mainly taken from the Combined General Catalogue of Variable stars (Samus et al. 2004). The periods for LP And, AFGL 3068, and IK Tau are from Men'shchikov et al. (2006), Le Bertre (1992), and González Delgado et al. (2003), respectively. Distances are derived by fitting the spectral energy distribution (SED) calculated with DUSTY (Sect. 6.1) to observed fluxes from the near-IR to the mm-range (Sect. 3.2 and Appendix B).
When estimating the physical properties of the CSEs, e.g., mass-loss rates and kinetic temperatures, it is very important to have well-calibrated data for all lines (Schöier & Olofsson 2001). CO
(115.271 GHz) data was obtained in December 2003 using the Onsala Space Observatory (OSO) 20 m telescope
. The James Clerk Maxwell Telescope
(JCMT) located on Mauna Kea was used to collect CO
(230.538 GHz),
(345.796 GHz),
(461.041 GHz), and
(691.473 GHz) line emission from the sample sources. The observations were performed in June, July, and October 2003.
All observations were made in a dual-beamswitch mode,
where the source is alternately placed in the signal and the reference
beam, using a beam throw of about
at JCMT and
at OSO.
This method produces very flat baselines. Regular pointing checks made on strong continuum sources (JCMT) or SiO masers (OSO) were found to be consistent with the pointing model within
3
.
The data was reduced in a standard way using XS by removing a first order polynomial fitted to the emission-free channel ranges and then binned in order to improve the signal-to-noise ratio. The intensity scale is given in main-beam-brightness temperature,
,
where
is the
antenna temperature corrected for atmospheric attenuation using the
chopper-wheel method, and
is the main-beam
efficiency. The adopted main-beam efficiencies are given in Table 2.
The uncertainty in the absolute intensity scale is estimated to be about
20% for all lines except the CO
lines, where we estimated a higher uncertainty of about
30%.
Source | OSO | JCMT | ||||
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![]() |
![]() |
![]() |
||
LP And | 63 | 104 | 124a | 143a | 139 | |
CW Leo | 386 | 689 | 1070a | 1230a | ![]() |
|
RW LMi | 108 | 123 | 244a | 246a | ![]() |
|
V384 Per | 35 | 63 | 40 | 79 | ![]() |
|
AFGL 3068 | 48 | 72 | 73 | 93 | 55 | |
TX Cam | 20 | 61 | 71 | 149 | ![]() |
|
GX Mon | 31 | 61 | 80 | 79 | ![]() |
|
WX Psc | 44 | 81 | 70 | 84 | 23 | |
IK Tau | 46 | 95 | 125a | 130 | ![]() |
|
IRC-10529 | 16 | 45 | 27 | 22 | ![]() |
The observed spectra are presented in Figs. 3, 4, and C.1-C.8, and velocity-integrated intensities are reported in Table 3.
The SEDs are constructed from JHKLM-band, sub-millimetre, and millimetre photometric flux densities from the literature, together with IRAS data. SCUBA data (at 450 and 850 m) was downloaded from the JCMT archive for CW Leo, AFGL 3068, and RW LMi. All fluxes and references are presented in Appendix B.
To check the dust radiative transfer model results, IRAS and ISO spectroscopic data were used. IRAS-LRS spectra were downloaded for all stars in the sample. An absolute calibration correction was applied according to Volk & Cohen (1989) and Cohen et al. (1992). The ISO LWS and SWS Highly Processed Data Products (HPDP) were downloaded and not processed further. LWS spectra were available for all stars except GX Mon. SWS spectra were found for TX Cam and WX Psc (SWS spectra for carbon stars were not searched for). For IK Tau, only a grating scan covering the wavelength range
29-49
m was available, and for IRC-10529, the SWS spectrum is very noisy above 28
m.
Even in this simple model there are a number of uncertainties that will affect the strengths and the shapes of the CO lines and the shape of the SED, e.g., the thermodynamics of the gas, the CO chemistry, the dust composition, the optical properties of the dust, and the grain size distribution. In addition, there can be major deviations from this model due to e.g. non-isotropic, time-variable mass loss and a clumpy medium. Finally, the objects are long-period variables and the data are sometimes taken at different epochs. In many cases it may be impossible to disentangle which of these assumptions and effects, if any, are affecting the emerging radiation. This taken into account, the most reasonable approach is to choose the simplified circumstellar model and analyze all stars using the same method.
Only a short description of the radiative transfer analysis of the circumstellar CO radio line emission is given here, since the adopted model has been described in detail in previous articles (Schöier & Olofsson 2001, for carbon stars; and Olofsson et al. 2002, for M-type stars).
The non-LTE radiative transfer code is based on the Monte Carlo method. 41 rotational levels are included in each of the two lowest vibrational states (v=0 and v=1) in the excitation analysis of the CO molecule. Energy levels and radiative transition probabilities, as well as collisional rate coefficients for collisions between CO and
,
are taken from Schöier et al. (2005b)
. An ortho-to-para ratio of 3 is adopted when weighting together collisional rate coefficients for CO in collisions with ortho- and para-H2. Radiation from the central source (assumed to be a blackbody), thermal dust grains (Sect. 6.1), and the cosmic microwave background is included.
The energy balance equation for the gas is solved self-consistently, by including line cooling from CO and
and cooling due to the adiabatic expansion of the gas. The dominant gas-heating mechanism is collisions between the
molecules and the dust grains. Photoelectric heating is also included and it is mostly important in the outer parts of the CSE. The free parameters describing the dust are combined in the parameter, h, defined as
The radial distribution of CO is estimated using the model presented in Mamon et al. (1988). It includes photodissociation, shielding, and chemical exchange reactions. The photospheric abundance of CO relative to
is assumed to be
for the carbon stars (Zuckerman & Dyck 1986) and
for the M-type stars (Kahane & Jura 1994). The luminosity was estimated using a period-luminosity relation (see Sect. 2), and the inner radius of the CSE was taken from the SED fitting. It was shown in Schöier & Olofsson (2001) that, in the intermediate- to high-mass-loss-rate stars, the CO radio line intensities are essentially unaffected by a change in these parameters. The main reason is that in the higher-mass-loss-rate CSEs, CO is collisionally excited out to large radii. The mass-loss rate and h are the remaining free parameters in the CO line modelling.
Dust radiative transfer through a spherically symmetric envelope possesses scaling properties (Ivezic & Elitzur 1997). This fact is put to use in the publicly available radiative transfer code
DUSTY adopted here to model the observed continuum emission. The scaling properties of the solution makes DUSTY ideal for studying a large sample of stars, since only one model grid, although large, needs to be calculated for each dust type.
The most important parameter in the dust radiative transfer modelling is the dust optical depth
In the modelling, the dust optical depth, specified at 10 m, is varied in the range 0.1-10 in steps of
10%. In addition, the dust temperature at the inner radius of the dust envelope
,
and the stellar effective temperature
,
are varied. These are the three adjustable parameters in the analysis. The SED model result depends only weakly on the other input parameters, which are fixed at reasonable values. The size of the envelope is fixed at
/
to make sure that the whole envelope extent determined from the CO emission (
;
see Table 3 in Schöier & Olofsson 2001) is covered. Using an even larger size does not affect the result.
The temperature at the inner radius should be close to (or lower than) the dust condensation temperature. In the modelling it is varied in the range 300-1500 K, in steps of 100 K.
The canonical dust condensation temperature of carbonaceous dust grains is 1500 K, while the condensation temperature for the silicate grains is expected to be somewhat lower.
However, prompt dust formation is an oversimplification. Given the complex chemistry close to the star, where shocks are present and grain growth is important, the dust-to-gas ratio probably depends on the radius. The dust temperature at the inner radius should therefore be treated as a measure of the characteristic radius where dust formation is essentially completed.
The stellar effective temperature is varied in the range 1800-2400 K (also in steps of 100 K),
characteristic of high-mass-loss-rate AGB stars, but lower than that of AGB stars with optically thin dust envelopes (e.g., Lambert et al. 1986;
Bergeat et al. 2001; Heras & Hony 2005).
When scaling the result from DUSTY, the interstellar extinction is taken into account. It is calculated from the galactic longitude for each star, using Eq. (8) in Groenewegen et al. (1992).
When light is scattered by a dust particle, some of its momentum is given to the scattering particle. For particles with an arbitrary shape, the efficiency factor for this momentum transfer depends on the orientation of the particle and on the polarization of the light. However, for spherical particles, as assumed here, it is independent of both. The dimensionless efficiency factor is given by the momentum fraction taken from the incident beam divided by the geometrical cross section of a particle:
The radiation pressure efficiency
is determined and averaged over the photon spectrum,
rapidly decreases and reaches its terminal value,
,
at
20-30
.
Equations (4) to (6) are solved in an iterative way, for different mass-loss rates, until the dust density structure is consistent with the optical depth derived in the dust radiative transfer model, and a fit to the observed gas expansion velocity is found. In this way, an independent estimate of the mass-loss rate is obtained.
Bains et al. (2003) investigated maser emission towards four AGB stars and derived velocity profiles for their circumstellar envelopes. In Fig. 1, our result for IK Tau is overlayed and shown to be consistent with their data.
![]() |
Figure 1: The velocity profile for IK Tau from the dynamical model overlayed with the velocity data obtained from mapping of maser emission (see Bains et al. 2003, and references therein). H2O masers (circles) and OH maser (squares) have been used. The expansion velocity derived from the CO data is marked by a diamond. |
Only two parameters are adjustable when fitting the model to the observed integrated line intensities: the mass-loss rate, ,
and the h-parameter. Models are calculated for a large number of mass-loss rates and h-parameters for each star and the best-fit model is found using
-statistics. The reduced
for the best-fit model is estimated from
We are able to successfully model the CO line emission from all stars in our sample, both carbon stars and M-type stars, using a constant mass-loss rate. (The
line of WX Psc poses a problem that will be further discussed in Sect. 8.2.3.) The results are presented in Table 4. Figure 2 shows
-maps for all our sample stars. The difficulty in setting an upper limit on the mass-loss rate for high-mass-loss-rate stars using CO radio line intensities only is apparent. The saturation of the optically thick CO lines weakens significantly the dependence of the line intensity on the amount of CO in the envelope.
Source | ![]() |
h | ![]() |
![]() |
N |
![]() |
![]() |
||||
LP And | 7 | 2.0 | 14.0 | 0.5 | 5 |
CW Leo | 20 | 1.0 | 14.5 | 0.1 | 4 |
RW LMi | 5 | 1.5 | 17.0 | 0.7 | 4 |
V384 Per | 3 | 1.0 | 14.5 | 2.7 | 4 |
AFGL 3068 | 20 | 2.0 | 14.0 | 0.9 | 5 |
TX Cam | 7 | 1.0 | 18.5 | 3.0 | 4 |
GX Mon | 20 | 0.5 | 18.7 | 0.1 | 4 |
WX Psc | 40 | 0.4 | 19.3 | 1.0 | 4 |
IK Tau | 10 | 0.3 | 19.0 | 0.4 | 4 |
IRC-10529 | 16 | 0.2 | 14.0 | 3.8 | 4 |
In some cases, better constraints on the mass-loss rate can be set by including the shape of the line profile. Changing the mass-loss rate results in a changing photodissociation radius (see, e.g., model by Stanek et al. 1995), and this may result in a change of the line profile. Visual inspection of the line profiles (within the range of the innermost contour of the -maps) was used to pick the best model presented in Table 4 and when determining the error bars in Fig. 7. In principle, it is possible to account for the shape of the line profile in a more quantitative way, i.e. by dividing the line into several velocity bins and calculating an error using
-statistics. However, this is problematic since the resulting
-values become very sensitive to very small variations in the line-profile shape which may not be possible to account for by changing the free parameters in the adopted model. Also, in cases like TX Cam (Fig. 4), a fit to the line-profile shape can never be found within the adopted model, either the adopted distance or the photodissociation radius must be changed (see Sect. 8.2.1 for a discussion of this).
Figures 3 and 4 give the comparisons between the observed and the best-fit model CO lines for the carbon star LP And and the M-type star TX Cam, respectively. These results are discussed in Sects. 8.1.1 and 8.2.1, respectively. The results for the remaining stars are shown in Appendix C. The differences between the integrated line intensities in the best-fit model and the observed lines are presented in Table C.1.
The observational constraints in the form of SEDs, covering the wavelength range
1-1300
m, are analyzed using
-statistics. When combining the measured fluxes into an SED, the variability of the star must be taken into account. This is particularly important for fluxes measured at shorter wavelengths, where the amplitude of the variation is larger. To assess how strongly the fluxes are affected, the mean and deviation was calculated from several measurements performed at different epochs. As a result a 60% uncertainty was assumed for the J-band (1.24
m), 50% for the H-band (1.63
m), 40% for the K-band (2.19
m), and 30% for the L- and M-bands (3.79 and 4.64
m, respectively). At wavelengths longer than 5
m, a calibration uncertainty of 20% was added to
the total error budget and it dominates the error (since there is limited information on the variability at these wavelengths). In some cases where there are many fluxes measured at roughly the same wavelength, we introduce an average value to avoid a bias in the
calculation at certain wavelengths. (This is the reason why some of the fluxes presented in Table B.1 are not included in the analysis.) The SEDs constructed from the photometric flux densities are thus averages, where the variability of the star at different wavelengths is reflected in the error bars (typically larger uncertainties at shorter wavelengths). The best-fit model is found from minimizing
Table 5 lists the results from the dust modelling, the dust temperature at the inner radius
,
dust optical depth at 10
m
,
from fitting the SED, and the number of observational constraints N.
-maps, at constant best-fit stellar effective temperature, showing the level of consistency between the modelled SED and the photometric fluxes, when varying the dust temperature at the inner radius and the optical depth at 10
,
are displayed in Fig. 5. The SEDs from the dust-radiative-transfer model, with the observed photometric fluxes, are shown in Fig. 6.
are generally close to 1 and the dust optical depth at
is rather well constrained for most sources (see Fig. 5).
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Figure 3:
The observed CO
![]() ![]() ![]() ![]() ![]() ![]() ![]() |
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Figure 4:
The observed CO
![]() ![]() ![]() ![]() ![]() ![]() |
Source | ![]() |
![]() |
![]() |
![]() |
N |
[K] | [K] | ||||
LP And | 2400 | 1100 | 0.55 | 1.6 | 11 |
CW Leo | 2000 | 1500 | 1.2 | 2.4 | 12 |
RW LMi | 2400 | 1200 | 0.6 | 0.9 | 11 |
V384 Per | 1800 | 1000 | 0.2 | 0.9 | 10 |
AFGL 3068 | 2400 | 1500 | 4.0 | 5.3 | 11 |
TX Cam | 2200 | 800 | 0.4 | 0.5 | 9 |
GX Mon | 1800 | 500 | 0.3 | 4.9 | 9 |
WX Psc | 1800 | 1000 | 3.0 | 1.1 | 12 |
IK Tau | 2400 | 1200 | 1.2 | 0.9 | 12 |
IRC-10529 | 1800 | 800 | 3.0 | 3.1 | 10 |
Low resolution spectra in the wavelength range 7.5-23 m covering the silicate features at around 10 and 20
m, were measured with the Low Resolution Spectrograph (LRS) as part of the IRAS mission. Later, the Short Wavelength Spectrometer (SWS) and the Long Wavelength Spectrometer (LWS) onboard ISO measured medium and high resolution spectra in the wavelength range 2.38-45.2
m and 43-197
m, respectively. Short wavelength spectrometer spectra also cover the silicate features and LWS spectra show the slope of the SED at longer wavelengths and is particularly sensitive to the cold dust.
The strengths of the silicate features are very sensitive to the dust optical depth (see for instance Fig. 1 in van Loon 2006) and in turn the dust mass-loss rate. As a consistency check, the IRAS-LRS spectra and SWS spectra are plotted for the M-type stars in the lowest panel of Fig. 6. The carbon stars all have the SiC feature at 11 m (e.g., Speck et al. 1997). However, since SiC grains compose a small fraction of the total dust content (
10%) and have a minor effect on the overall SED except for the 11
m feature (Suh 2000), we have not included SiC in the dust model and consequently the observed spectra for the carbon stars are not shown. LWS spectra are available for all stars but one, and they are also plotted in Fig. 6.
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Figure 5:
![]() ![]() ![]() ![]() ![]() |
A fit to the LRS and SWS spectra has not been attempted because of the difficulty in including them in a proper best-fit analysis. One complication is that the spectral shape and strength of the 9.7 m silicate feature can change with the pulsational phase in stars with clear features and definite bolometric variability (Monnier et al. 1998). This is likely valid for all M-type stars in our sample. Also, since these spectra are reasonably well fitted (see Fig. 6), we expect the change in the resulting dust optical depth and inner radius, if the spectra were fitted in more detail (such as silicate features), to be small. A small change in the optical depth will result in an even smaller change in the estimated mass-loss rate from the dynamical model (see Table 7).
For some stars (CW Leo, RW LMi, AFGL 3068, and IRC-10529) there is a slight discrepancy between the slope of the LWS spectrum and that of the best-fit model. To perfectly reproduce the slope of the LWS spectra and the photometric fluxes at longer wavelengths, a varying mass-loss rate of these stars would probably have to be invoked. This has already been suggested for CW Leo by Groenewegen (1997), who found that the dust density far from the star was underestimated by the best-fit r-2 model. Other possible causes could be a difference between the optical properties of the model dust and the actual dust surrounding the star (see e.g. Figs. 1 and 6 in Suh 2000), or the uncertainty in the long-wavelength dependence of the dust opacity. The fluxes beyond 800
m might also be affected by other processes than the dust emission, e.g., free-free emission and molecular line emission (Dehaes et al. 2007; Groenewegen 1997). Bearing in mind the uncertainties in the circumstellar model (Sect. 4) and our aim to analyze all stars with the same assumptions we find that the LRS, SWS, and LWS data are well reproduced by our best-fit models.
In the dynamical model, the density structure is calculated from the conservation of mass and the model is iterated until this gives an optical depth that agrees with the dust continuum optical depth obtained from the SED modelling (within one percent) and the resulting terminal gas expansion velocity from solving Eqs. (4) and (5) corresponds to the observed expansion velocity within 0.1%.
Table 6 lists mass-loss rates,
,
,
and
for the best-fit dynamical model.
All sources in the sample are well-studied both at IR and radio wavelengths. As established already in Sects. 7.1 and 7.2, we are able to reasonably successfully model the CO line emission (the integrated intensities and the line shapes) and the SEDs for all 10 stars using a constant mass-loss rate.
In the following discussion it should be kept in mind that the different methods measure the mass-loss rate at different epochs and over different time intervals. The size of the CO line emitting region decreases with the J-number and hence the different lines measure the mass-loss rate at slightly different epochs. The same is true for the SEDs where the emission at different wavelenghts (apart from the photospheric contribution) comes from different parts of the CSE. The estimated mass-loss rate should be considered as an average and it is a complicated synthesis of the different epochs and time scales.
The derived mass-loss rate from the CO modelling is
yr-1, while the dynamical model gives a mass-loss rate of
yr-1, a factor of 2.5 larger. The model lines agree very well with all five observed lines,
(Fig. 3). Previous mass-loss-rate estimates from CO radio lines have resulted in mass-loss rates close to our results,
yr-1 (CO/H
)
(Teyssier et al. 2006), and
yr-1 (Schöier & Olofsson 2001), both assuming a distance of 630 pc. Men'shchikov et al. (2006) estimated the mass-loss rate to be
yr-1 from a dust radiative transfer model, assuming a distance of 740 pc and a dust-to-gas mass ratio of 0.0039. The corresponding mass-loss rate at the distance used and the dust-to-gas ratio obtained in our model, would be
yr-1, in fairly good agreement with our result.
Neri et al. (1998) found a slight asymmetry in the CSE from maps of the CO(
)
emission. Mauron & Huggins (2006), using optical images in scattered light, suggested that the envelope around LP And may have an interesting structure, but concluded that the signal-to-noise in their data is too low to make any firm statement.
Source | ![]() |
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LP And | 17 | 3.1 | 1 | 0.09 | 2.5 |
CW Leo | 21 | 1.9 | 2 | 0.05 | 1.1 |
RW LMi | 17 | 1.3 | 2 | 0.08 | 3.3 |
V384 Per | 5 | 6.5 | 2 | 0.11 | 1.6 |
AFGL 3068 | 62 | 0.7 | 3 | 0.02 | 3.1 |
TX Cam | 3 | 10.6 | 4 | 0.11 | 0.5 |
GX Mon | 2 | 12.6 | 10 | 0.09 | 0.1 |
WX Psc | 18 | 4.3 | 3 | 0.06 | 0.5 |
IK Tau | 7 | 7.3 | 2 | 0.10 | 0.7 |
IRC-10529 | 26 | 2.9 | 2 | 0.06 | 1.6 |
Being the closest carbon star, CW Leo is certainly the most well-studied. We estimate the mass-loss rate to be
yr-1 from the CO line modelling and
yr-1 from the dynamical model.
Previous estimates of its mass-loss rate from CO is
yr-1 (Teyssier et al. 2006) and
yr-1 (Schöier & Olofsson 2001), both assuming a distance of 120 pc. Groenewegen et al. (1998) did a very thorough investigation of the CO radio line emission toward CW Leo and estimated the present day mass-loss rate to (
yr-1 and the distance to lie between 110 and 135 pc.
Several reports on structures in the circumstellar environment around CW Leo can be found in the literature (e.g., Mauron & Huggins 1999; Fong et al. 2006). Optical images show arc-like structures on arcsecond scales in the CSE, but whether this is due to changes in the mass-loss rate over time, is still under debate (e.g., Leão et al. 2006, and references therein).
The best-fit CO model gives a mass-loss rate of
yr-1. However, as can be seen in Fig. C.3, the model
,
and
lines are all 15-20% weaker than the observed lines, while the model
line is 65% stronger than the observed line. This results in a rather high
.
The most likely explanation is a calibration error in the
line. The mass-loss rate from the dynamical model is higher,
yr-1. Schöier & Olofsson (2001) estimated
yr-1 at 560 pc from CO line modelling.
Our model of the CO line emission reproduces all five lines for a constant mass-loss rate of
yr-1 with a
.
The dynamical model gives
yr-1, slightly more than a factor of three higher. Earlier estimates of the mass-loss rate from CO line modelling have resulted in
yr-1 (Teyssier et al. 2006) at 1000 pc and
yr-1 (Woods et al. 2003) at 820 pc. Teyssier et al. (2006) deduced a much lower temperature in the outer envelope than we calculate in our model and this is the reason for the discrepancy between the estimates.
There is no doubt that the CSE around this source is asymmetric and have density structures that cannot be reconciled with a spherically symmetric CSE (Mauron & Huggins 2006). Radial CO (
)
visibility profiles show a compact inner envelope surrounded by a large outer shell. The outer shell is strongly bipolar and there are even indications that it might be detached (Neri et al. 1998).
We find the CO line data to be consistent with a mass-loss rate of
yr-1. From the dynamical model the mass-loss rate is estimated to be
yr-1. Teyssier et al. (2006) found it necessary to infer a change in the mass-loss rate about 250 years ago to fit the CO intensity measured at offset positions; the mass-loss rate has decreased from
yr-1 to
yr-1. The two component structure was already noticed by Neri et al. (1998) when first inspecting the interferometric data. Schöier & Olofsson (2001) estimated
yr-1 from CO line modelling using the same distance as Teyssier et al. (2006), 440 pc.
The best-fit CO model gives
yr-1 (the same rate was derived by González Delgado et al. 2003), but the model does not reproduce the shape of the observed line profiles (Fig. 4). The observed
and
lines are flat-topped, which suggests unresolved, optically thin emission, while the model gives double-peaked lines, which suggests resolved, optically thin emission. The observed
and
lines are parabolic and thus optically thick, while the model produces an optically thin, resolved
line and a flat-topped
line. The simplest explanation would be that the distance is underestimated. A larger distance requires a higher mass-loss rate to reproduce the line intensities and hence gives line profiles that better reproduce the observed ones. An increased distance also decreases the angular size, but this is partly counteracted by the fact that the CO photodissociation radius increases with the mass-loss rate. Another explanation could be that the size of the CO envelope in this object is smaller than the photodissociation radius given by the model of Mamon et al. (1988). Decreasing the size of the CO envelope solves the problem with the model producing resolved lines. Also, a smaller radius will require a higher mass-loss rate to reproduce the observed intensities. This also increases the optical depth. However, the dynamical model estimate of the mass-loss rate is
yr-1, a little more than a factor of 2 less than the CO modelling.
The dynamical model gives a mass-loss rate estimate (
yr-1) one order of magnitude lower than the CO model (
yr-1). The best-fit SED model found according to the strategy described above gives a dust temperature at the inner radius of 500 K. Figure 5 shows the
-maps from the SED-fitting and in the case of GX Mon, the model is not very well constrained. The major dust condensation phase in M-type stars is thought to occur at temperatures between 1200 K and 800 K (Whittet 2003). With the low dust optical depth derived for GX Mon a high dust-to-gas ratio (
)
is needed to accelerate the gas to the measured expansion velocity. (Setting
K, requires a higher optical depth to fit the model to the observed fluxes (
)
and results in
yr-1 from the dynamical model, somewhat more in line with the CO results. The measured expansion velocity would be reached with
). A possible explanation for the low temperature at the inner radius is that the star has undergone a rather drastic decrease in the mass-loss rate recently. The dust envelope from an earlier epoch would have moved outward and cooled to the temperature obtained from the modelling, and the photometric fluxes would thus probe this ``older'' shell. In such a case the dynamical model would produce an erroneous result.
The
,
and
lines are well-fitted by a constant mass-loss rate of
yr-1. We are, however, not able to fit the
line using this model. The problem of not being able to model higher-frequency CO lines from this source using a constant mass-loss rate has been previously noted by Kemper et al. (2003), Teyssier et al. (2006), and Decin et al. (2007). The difficulty of getting well-calibrated data for these higher frequency lines should be kept in mind when drawing conclusions based on this kind of data. As an example, the integrated intensity in the
line in this work is a factor of two stronger than that reported by Kemper et al. (2003). A model fitting only our
line results in
yr-1. Decin et al. (2007) introduce a rather complicated mass-loss history, and estimate the mass-loss rate to be
yr-1 in the region where the
line is mainly coming from. Higher transition CO lines are within the range of archived ISO LWS spectra (43-197
m). The CO
and
lines were modelled using our best-fit model. The resulting peak intensities (
W cm-2 (km s)-1 and
W cm-2 (km s)-1, respectively) would result in a
(the resolution-corrected
noise level is
10-23 W cm-2 (km s-1)). None of the CO lines within the range of the ISO LWS were detected, and this is in line with the weakness of the observed
line. Thus, the results reported by us and previous authors suggest a recent decrease in the mass-loss rate in this source. From the dynamical model we find
yr-1.
Modelling IK Tau with a constant mass-loss rate of
yr-1 gives a good fit to the four available CO lines (Fig. C.7). This rate is a factor of two higher than that found by Teyssier et al. (2006) at a somewhat smaller distance of 250 pc. The dynamical model gives
yr-1.
When modelling IRC-10529, we encounter a similar problem as for V384 Per. We find that the best-fit CO model with
yr-1 has a
.
The
and
lines are fitted within the observational uncertainties, but the model
line is 45% too weak, and the
line is 40% too strong (Fig. C.8). We do not find it likely that this is due to modulations in the mass-loss rate, since the emitting regions for the
and
lines overlap to a large extent. It is more likely due to observational problems. The dynamical model gives
yr-1, in good agreement with the estimate from the CO model.
The model CO line intensities dependence on the h-parameter and
is displayed in Fig. 2. A further discussion on how the resulting line intensities depend on various input parameters can be found in Schöier & Olofsson (2001).
To evaluate the sensitivity of the results of the dynamical model to the different derived or assumed input parameters, we varied the parameters in Eqs. (4) and (5) by 50%. Shown in Table 7 is the needed change of the dust-to-gas ratio,
,
and the mass-loss rate,
,
to reach the observed expansion velocity and derived optical depth for RW LMi. As can be seen, the dynamical model results are strongly dependent on the assumed dust parameters, which are not well known.
A trend with mass-loss rate can be seen in the dynamical model. For TX Cam, an intermediate-mass-loss-rate object (
yr-1 from the dynamical model), an increase in the mass-loss rate by 50% leads to an increased expansion velocity by 6%. For RW LMi, a high-mass-loss-rate object (
yr-1) the same increase in the mass-loss rate will lead to a decrease in the expansion velocity by 15%. This is due to the fact that a higher mass-loss rate leads to a higher dust optical depth resulting in a radiation field that decreases more rapidly with radius and with it the radiation pressure efficiency. Nevertheless, this does not lead to a problem finding the correct mass-loss rate. In some cases, two mass-loss rates give the same expansion velocity, but there is only one solution that produces the correct dust optical depth.
We have decided not to display any error bars on the estimates from the dynamical model in Fig. 7. The reason for this is that the resulting (formal) error bars given by the dust radiative transfer model (variations in inner radius and optical depth, Fig. 5) are small and ignores the substantial uncertainties in the adopted dust parameters.
Parameter | Change | ![]() |
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L | +50% | +50% | -35% |
-50% | -50% | +100% | |
M* | +50% | -25% | +30% |
-50% | +30% | -30% | |
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+50% | +50% | -35% |
-50% | -50% | +125% | |
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+50% | -35% | +60% |
-50% | +105% | -55% | |
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+50% | +35% | +10% |
-50% | -40% | -10% | |
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+50% | +50% | -35% |
-50% | -50% | +100% |
It is very difficult to assess which method is the most reliable for estimating mass-loss rates, since both are dependent on a number of assumptions, which are more or less well-founded. For instance, the dynamical model assumes an entirely dust driven wind, while recent results suggest that there might be other factors at play (Höfner & Andersen 2007; Woitke 2006).
In all cases but GX Mon, for which we have good reasons to believe that the dynamical model gives an erroneous result (see Sect. 8.2.2 for an explanation), the mass-loss rates estimated from the dynamical model and the CO line modelling agree within a factor of 3. A comparison is shown in Fig. 7, where the full drawn line marks the one-to-one relation, while the dashed lines subtend the range within a factor of 3. (Error bars represents the range within the innermost contour in the
-maps from the CO model. Here the shape of the line profiles have also been taken into account.) Since the two methods give independent estimates of the mass-loss rate, this result can be used as a guideline to the uncertainty in the mass-loss-rate estimates within the adopted circumstellar model. Heras & Hony (2005) found in their comparison of mass-loss rates derived from ISO-SWS and CO mass-loss rates taken from the literature for low-mass-loss-rate M-type stars that the estimated mass-loss rates can differ up to a factor of ten.
In principle, it is possible to check whether the dust results obtained from the dynamical model (
,
,
)
are consistent with those used in the CO radiative transfer modelling (h,
). However, we do not expect to get a perfect agreement since in the CO radiative transfer modelling the h-parameter is adjusted until the radial kinetic temperature profile results in reasonable relative strengths of the CO lines. Hence, it is affected by possible missing heating and cooling terms in the description of the thermodynamics of the circumstellar gas. However, as outlined in Sect. 5, this does not affect the mass-loss-rate estimates.
For the carbon stars in our sample the dust-to-gas ratio, ,
is estimated to be
.
Groenewegen et al. (1998) derived dust-to-gas ratios for a sample of 36 carbon stars and found a rather constant value of 0.0025 up to
where a strong increase with period is found. This agrees rather well with our results. However for AFGL 3068 they find
,
in strong excess of our result. For the M-type stars we find somewhat larger dust-to-gas ratios,
(GX Mon excluded). Justtanont et al. (1994) modelled three thick M-type CSEs and found
.
The CO mass-loss-rate estimate is lower than the estimate from the dynamical model for all five carbon stars, see Fig. 7. The opposite can be seen for the M-type stars, where the CO model gives a mass-loss-rate estimate higher than the dynamical model for three out of four M-type stars (GX Mon excluded). Keeping in mind that the sample presented here is too small to make a general statement, we suggest that a possible explanation to this is that the adopted CO/H2-ratio is too low, on average, for the M-type stars and too high for the carbon stars. This is also in line with recent chemical models (Cherchneff 2006), where a non-equilibrium chemical model gives a CO-abundance of
in M-type stars (
)
at 5 stellar radii. For the carbon stars (
), the resulting CO-abundance at the same distance from the star is found to be
.
Adopting these abundances would require a higher mass-loss rate for the carbon stars and a lower mass-loss rate for the M-type stars to reproduce the observed CO line intensities.
Kemper et al. (2003) made non-LTE radiative transfer modelling of CO
to
emission toward a sample of AGB stars and red supergiants. In a line ratio diagram they compared modelled line intensity ratios, for standard CSEs with different mass-loss rates, to those found from observations (Fig. 4 in their paper). Kemper et al. found that they could not reproduce the observed line intensity ratios. On the contrary, the standard model described above (Sect. 5) generally gives a very good fit to the observed line intensities as indicated by a
of the order of unity for the majority of the sample sources. This is also illustrated in Fig. 8 where line intensity ratios calculated from our standard model using
km s-1 and h = 0.5 for a range of mass-loss rates are compared to the observations. The model CSE was placed at a distance of 1 kpc. The interconnected stars are the results from the standard model and the squares show the observed line ratios.
Kemper et al. (2003) also found that the magnitude of the stochastic velocity strongly affects the line intensities, since it determines the size of the region where the line is formed (
,
since
is the local thermal broadening and
). We have performed the same test as in their Fig. 10, changing the turbulent velocity from 0.05 to 2 km s-1, to see how this affects the intensity of the CO(
)
line. We used the same standard model as above with a mass-loss rate of
yr-1. Kemper et al. (2003) saw a decrease in intensity from around
K at
km s-1 to
K at
km s-1. We, however, see the opposite trend and a much weaker effect;
K at
km s-1 to
K at
km s-1. It is difficult to outline exactly how the line intensity is affected by the turbulent velocity, as it also affects the excitation of the molecules. However, to a first approximation, with an increased turbulent width the number of molecules per unit velocity interval decreases. On the other hand, as already mentioned above, it also increases the size of the interacting region. Under certain circumstances (spherically symmetric CSE, constant excitation temperature,
)
these two effects cancel out and the line intensity becomes independent of the turbulent velocity (see for example Morris 1975; Olofsson et al. 1982).
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Figure 8: Observed line intensity ratios for the sample sources (squares) compared with predictions from the standard model for various mass-loss rates (stars). |
In conclusion, we are not able to reproduce the results reported by Kemper et al. (2003) using our model. We confirmed our result using two additional codes; an accelerated Monte Carlo code (Hogerheijde & van der Tak 2000) and an Accelerated Lambda Iteration (ALI) code (Maercker et al. 2008). The results from the excitation analysis were then combined with different ray tracers (the one used in this paper and the code described in Hogerheijde & van der Tak 2000) to get the resulting line profiles. All results were in good agreement with ours.
We have presented mass-loss-rate estimates, derived using two independent methods, for a sample of 10 intermediate- to high-mass-loss-rate, well-studied AGB stars, and we arrive at the following conclusions:
Acknowledgements
The authors acknowledge support from the Swedish Research Council. 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. Finally the authors would like to thank Franz Kerschbaum for providing us with a compilation of near-IR data needed for the dust radiative transfer modelling.
Knapp & Morris (1985) derived a theoretical mass-loss-rate formula in terms of the CO(
)
line intensity, valid for optically thick CO emission. The formula relates the mass-loss rate to a number of easily determined observables;
for the CO(1-0) line, and
.
The distance D and CO abundance
also enter the formula. It was derived using a fixed CO envelope size. This formula was used in e.g. Olofsson et al. (1993) to estimate mass-loss rates for a sample of carbon stars. Later, Schöier & Olofsson (2001) could compare their results on the sample, derived using the same radiative transfer model as in this work, to those estimated using the formula. They found that the formula underestimated the mass-loss rates compared to what was found from the radiative transfer analysis, on average by a factor of four, but the discrepancy was found to increase even more for lower mass-loss-rate objects. The reason is that the emission from the low-mass-loss-rate objects is not optically thick and it is more sensitive to the size of the CO envelope. However, the usefulness of simple formulae of this sort can not be disputed.
In order to improve the results by Knapp & Morris (1985), we set up a grid with 60 model stars, whose properties were varied in
(1, 3, 10, 30, and
yr-1),
(5, 10, 15, and
),
and
(1, 3, and
). Following Schöier & Olofsson (2001), the value of h was assumed to be 0.2 for
in the range up to
yr-1, 0.5 for 1-
yr-1, and 1.5 for the mass-loss rate
yr-1. For each star, the velocity integrated intensities in CO (
,
,
,
)
were calculated for a 20 m class telescope (the corresponding beam sizes were 33
,
16.5
,
11
,
and 8.5
). The distance to the stars were set to 1 kpc. The output from the modeling was fitted to Eq. (A.1) and the errors were
minimized using a Levenberg-Marquardt method (Press et al. 1992),
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Figure A.1: Mass-loss rates derived using Eq. (A.1) and the parameters in Table A.1 versus the mass-loss rates estimated using the Monte Carlo model for the same stars. Red triangles represent carbon stars, blue squares, M-type stars, and green dots represent S-type stars. |
Transition | sJ | ![]() |
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The SEDs used as constraints in the dust emission modelling are constructed from JHKLM-band, sub-millimetre, and millimetre photometric flux densities from the literature, together with IRAS data. All flux densities used are listed in Table B.1. Values in italics were omitted from the analysis to avoid a bias in the -analysis at certain wavelengths. Values in italics marked with a dagger were omitted since the reported errors were
50%.
Wavelength | LP And | CW Leo | V384 Per | AFGL 3068 | RW LMi | TX Cam | GX Mon | WX Psc | IK Tau | IRC-10529 |
[![]() |
||||||||||
1.24 | 1.6a | 4.0d | 13e | ![]() |
5.8h | 280a | 49j | 3.2i | 250i | 2.4i |
1.63 | 11a | 58d | 53e | ![]() |
39h | 590a | 120j | 32i | 730i | 20i |
2.19 | 55a | 520d | 170e | ![]() |
180h | 780a | 200j | 130i | 1200i | 78i |
3.79 | 450a | 10 000d | 520e | 9.6g | 970h | 750a | 580j | 620i | 1900i | 290i |
4.64 | ![]() |
19 000d | ![]() |
55g | ![]() |
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410j | 800i | 1800i | 340i |
8.55 | ![]() |
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290k | ![]() |
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850k | ![]() |
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8.57 | ![]() |
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700k | ![]() |
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9.56 | ![]() |
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360k | ![]() |
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1100k | ![]() |
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11.21 | ![]() |
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400k | 3900k | ![]() |
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1000k | ![]() |
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12 | 960b | 48 000b | 540b | 1700b | 3300b | 1600b | 1600b | 1200b | 4600b | 1300b |
12.45 | ![]() |
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470k | ![]() |
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360k | ![]() |
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25 | 470b | 23 000b | 200b | 780b | 1200b | 640b | 360b | 970b | 2400b | 1100b |
60 | 110 b | 5700b | 40b | 250b | 270b | 130b | 110b | 220b | 330b | 220b |
100 | 36b | 920b | 12b | 74b | 86b | 39b | 40b | 72b | 100b | 64b |
400 | ![]() |
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3.0m | ![]() |
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450 | 0.35
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13o | ![]() |
2.2o | 2.4o | ![]() |
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1.2
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600 | 0.41f | ![]() |
0.11
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0.67f | ![]() |
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800 | 0.25f | 6.7l | 0.21f | 0.33f | 0.78l | ![]() |
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0.25l | ![]() |
850 | ![]() |
12o | ![]() |
0.59o | 0.97o | ![]() |
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1100 | 0.081f | 1.9l | 0.045f | 0.17f | 0.16l | ![]() |
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0.082l | ![]() |
1200 | ![]() |
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0.24c | ![]() |
0.10c |
1300 | ![]() |
1.5n | ![]() |
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0.29n | ![]() |
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0.059c | 0.037n | ![]() |
References: a Bagnulo (1996); b Beichman et al. (1988), IRAS Point Source Catalogue; c Dehaes et al. (2007); d Epchtein et al. (1985); e Gezari et al. (1987); f Groenewegen et al. (1993); g Jones et al. (1990); h Kerschbaum & Hron (1994); i Le Bertre (1993); j Lepine et al. (1995); k Marengo et al. (1999); l Marshall et al. (1992); m Sopka et al. (1985); n Walmsley et al. (1991); o JCMT archival data.
|
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Figure C.1:
The observed CO
![]() ![]() ![]() ![]() ![]() ![]() ![]() |
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Figure C.2:
The observed CO
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Figure C.3:
The observed CO
![]() ![]() ![]() ![]() ![]() ![]() ![]() |
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Figure C.4:
The observed CO
![]() ![]() ![]() ![]() ![]() ![]() ![]() ![]() |
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Figure C.5:
The observed CO
![]() ![]() ![]() ![]() ![]() ![]() ![]() |
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Figure C.6:
The observed CO
![]() ![]() ![]() ![]() ![]() ![]() ![]() ![]() ![]() |
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Figure C.7:
The observed CO
![]() ![]() ![]() ![]() ![]() ![]() ![]() |
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Figure C.8:
The observed CO
![]() ![]() ![]() ![]() ![]() ![]() ![]() |
Source | OSO | JCMT | ||||
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||
LP And | 3.2 | 5.4 | 15.8 | 4.2 | -0.6 | |
CW Leo | 4.8 | -7.3 | -15.6 | -11.7 | ![]() |
|
RW LMi | -16.6 | 37.4 | -1.6 | 6.2 | ![]() |
|
V384 Per | -22.3 | -20.3 | 63.8 | -15.3 | ![]() |
|
AFGL 3068 | 6.3 | -4.2 | 11.0 | -13.3 | 34.6 | |
TX Cam | -7.7 | 56.9 | 40.2 | -18.9 | ![]() |
|
GX Mon | 1.6 | -3.4 | -1.9 | 3.4 | ![]() |
|
WX Psc | -3.2 | -14.8 | 23.8 | 6.8 | 273.7 | |
IK Tau | -3.3 | -1.4 | 9.2 | 16.4 | ![]() |
|
IRC-10529 | -3.5 | -44.8 | 11.9 | 38.9 | ![]() |