A&A 368, 497-526 (2001)
DOI: 10.1051/0004-6361:20000554
A. B. Men'shchikov1,3 - Y. Balega2 - T. Blöcker3 - R. Osterbart3 - G. Weigelt3
1 -
Stockholm Observatory, 13336 Saltsjöbaden, Sweden
2 -
Special Astrophysical Observatory, Nizhnij Arkhyz,
357147 Karachaevo-Cherkesia, Russia
3 -
Max-Planck-Institut für Radioastronomie, Auf dem Hügel 69,
53121 Bonn, Germany
Received 13 July 2000 / Accepted 12 December 2000
Abstract
We present the first detailed, two-dimensional radiative transfer
model of the dusty envelope around the carbon star IRC
+10216.
Our goal was to find a self-consistent model of the star and its
envelope which takes into account as many observational constraints as
possible. The model reproduces very well the entire beam-matched
spectral energy distribution of IRC
+10216 from optical to centimeter
wavelengths (at several phases of stellar luminosity), observed
intensity profiles of the object at 1.25, 2.2, 10.5, 50, 100
m,
and 1.3mm, a 10.5
m lunar occultation intensity profile, our
high-resolution J, H, K, and
bispectrum
speckle-interferometry images, and visibilities in
J, H, K, L, M, and
N bands.
For the adopted distance of 130pc, the model of IRC
+10216 implies that
the object changes its luminosity between 13000 and 5200
,
its
effective temperature between 2800 and 2500K, and its radius between 500
and 390
.
There is a dense non-spherical dust shell around the star,
with outflow cavities at position angle PA
20
.
The
southern cavity with a full opening angle of 36
is
tilted toward us by 40
from the plane of sky, causing the
observed bipolar appearance of the object on a subarcsecond scale.
If the envelope's outflow velocity of 15kms-1 applies to the
material making up the dense core, then just
15 years ago the
star was losing mass at a rate of
9 10-5
yr-1.
Dust exists in the envelope of IRC
+10216 everywhere from the stellar
photosphere up to a distance of 3pc from the star. The total mass of
the envelope lost by the central star is 3
and the dust-to-gas
mass ratio is 0.004. The total optical depth
toward the star
in the visual is 40, in the polar cavities it is 10.
The innermost parts of the envelope are optically thick even at
10.7
m due to a strong resonance absorption of silicon carbide
grains at that wavelength. In addition to SiC dust, the model contains
inhomogeneous grains made of a mixture of SiC and incompletely
amorphous carbon with thin [Mg0.5Fe0.5]S mantles. This is the simplest dust
mixture required to fit all observations of IRC
+10216 and to correctly
interpret the well-known 11.3
m and 27
m emission bands.
The dust model found in this study can also be successfully applied to
many other carbon stars exhibiting broad emission features in the
10.3-12.6
m and 25-37
m wavelength regions.
An important and firm result of our modeling is that the brightest
compact peak observed in IRC
+10216 is not the direct light from the
underlying central star. In contrast to previous suggestions, the
brightest southern component, labeled A in our high-resolution
near-infrared images (Weigelt et al. 1998a,
Weigelt et al. 1998b; Osterbart et al. 2000), is only the radiation emitted
and scattered in the optically thinner southern cavity of the bipolar
dense shell moving away from the central star. The carbon star is at
the position of the fainter component B in our H and K images,
which is 0
21 away from A along the symmetry axis. Direct
stellar light (component B) is not seen at all in the Hubble Space
Telescope 0.8
m and 1.1
m images, being absorbed by the
dense dusty material. The even fainter components C and D in the Hand K images are probably due to smaller deviations of the dense
shell from the spherical shape. IRC
+10216 seems to have entered a phase
immediately before moving off the asymptotic giant branch and started
developing asymmetries in its envelope.
After the first study by Becklin et al. (1969) and a series of
photometric, spectroscopic, and polarimetric measurements by others
(Lockwood 1970; Miller 1970; Herbig & Zappala 1970; Shawl & Zellner 1970),
it has become clear that IRC
+10216 (CW Leo, AFGL 1381)
deserves special attention. An extended object
(
)
outside the galactic plane, IRC
+10216 was
the brightest source on the sky in the near infrared (IR). Its almost
featureless spectral energy distribution (SED) resembled that of a
650K blackbody (or 1200K at wavelengths below 1
m); its
brightness at 2.2
m varied by 2
with a period of
600 days; its small proper motion implied a distance
100pc. The 1
m linear polarization was in excess of
20% at a position angle PA
120
,
perpendicular
to the elongation of the optical image (PA
30
),
indicating scattering by solid particles in a non-spherical
environment. IRC
+10216 was identified as a longest-period, pulsating
carbon star surrounded by an opaque dust shell, perhaps in a state
preceding that of a planetary nebula.
During the three decades of studies, dust continuum radiative transfer
calculations have been repeatedly applied to this well-observed object
(Crabtree & Martin 1979; Mitchell & Robinson 1980; Rowan-Robinson & Harris 1983; Le Bertre 1987; Martin & Rogers 1987; Orofino et al. 1990; Griffin 1990; Lorenz-Martins & Lefèvre 1993; Winters et al. 1994; Sloan & Egan 1995; Bagnulo et al. 1995; Ivezic & Elitzur 1996; Groenewegen 1997) in order to understand in more detail physical,
chemical, and evolutionary properties of the star and its dusty
molecular envelope. All the models used an assumption of spherical
geometry which seemed to be justified for this object by the presence
of the large-scale (several arcminutes) apparently symmetric envelope.
The latter appears to have, however, not very smooth density
distribution in the deep optical images by Crabtree et al. (1987)
and Mauron & Huggins (1999), showing a series of incomplete
concentric shells at radii of
15-60
.
On the other hand, several speckle observations (McCarthy et al. 1980; Mariotti et al. 1983; Ridgway & Keady 1988; Dyck et al. 1991; Danchi et al. 1994) and
especially recent highest-resolution observations (Osterbart et al. 1997; Weigelt et al. 1998a,b; Haniff & Buscher 1998; Osterbart et al. 2000; Tuthill et al. 2000) have demonstrated that the inner dust shell of IRC
+10216
is actually non-spherical and extremely clumpy. This well-established
observational fact emphasizes the need of multidimensional radiative
transfer calculations for proper interpretation of the observations.
A lot of circumstellar structures seen in the high-resolution images of the last decade demonstrate that the spherical symmetry is no more a realistic basic assumption for understanding the observations. Clumpy and bipolar structures (often intrinsically related to the jets and outflows) are being widely observed in protostars, young stellar objects (YSO), protoplanetary nebulae, in the winds of evolved post-asymptotic giant branch (post-AGB) stars, and in active galactic nuclei. An axially symmetric geometry of an optically thick toroidal distribution of matter around a central energy source emerges as a good basic approximation for the modeling of the physically different non-spherical objects.
From a practical point of view, axisymmetric geometries are much more time-consuming for modeling, because of two additional parameters, the density structure in the polar direction and the viewing angle. Furthermore, to find a self-consistent and realistic model, one has to derive also the properties of dust grains, which makes the whole problem enormously difficult and requiring many more observational data sets to constrain the modeling. In a series of recent papers (Men'shchikov & Henning 1997; Men'shchikov et al. 1998; Men'shchikov et al. 1999; White et al. 2000), we applied our two-dimensional radiative transfer code to detailed modeling of toroidal envelopes around YSOs (L1551 IRS5, HL Tau) and around a close binary post-AGB star (the Red Rectangle). The models demonstrate that a derivation of reliable physical parameters requires using all available (spatial) information in a detailed radiative transfer modeling. The less constraints are used, the easier is to find a model and the higher is the risk that the model is unrealistic (Men'shchikov & Henning 2000). The common practice of sketchy fitting of SEDs alone can only give source parameters that are highly uncertain.
In the present study, we utilized our approach and two-dimensional
radiative transfer code to find a self-consistent model of the dusty
environment of IRC
+10216, which would match quantitatively all
available dust continuum observations. In Sect. 2, we
briefly describe the most substantial results obtained for IRC
+10216
during the three decades of very active studies, that will enable the
reader synthesize a large amount of information and follow easier our
subsequent discussion. In Sect. 3, all details of our
approach and radiative transfer model are described. In
Sect. 4, we confront the model with available
observations of IRC
+10216. In Sect. 5, we briefly touch upon
its present evolutionary state. In Sect. 6, we summarize
results obtained in this study.
In the years following the initial discovery, a great number of observations in a wider wavelength range and with higher sensitivity, spectral and angular resolution painted quite a detailed and complex (yet incomplete) picture of this carbon star.
GEOMETRY.
Although on scales of more than several arcseconds the envelope of
IRC
+10216 seems to have a roughly spherical shape,
large optical and
near-IR polarization measured by Dyck et al. (1971) and
Capps & Knacke (1976) suggested significant deviations from spherical
symmetry. Near-IR speckle interferometry by Mariotti et al. (1983),
Dyck et al. (1984), and Ridgway & Keady (1988) revealed
asymmetries in the envelope on subarcsecond scales and two scattering
lobes of a lower density. Polarimetric imaging by
Tamura et al. (1988) detected an extended envelope also in highly
polarized light. A weakly-bipolar reflection nebula
(Kastner & Weintraub 1994) or a geometrically thick disk
(Dyck et al. 1987) or a dusty torus (Skinner et al. 1998) must be
significantly inclined toward an observer. A complex, clumpy
subarcsecond structure in the near IR is changing on time scales of a
few years, as has been demonstrated by interferometric observations of
Weigelt et al. (1998a) and Haniff & Buscher (1998).
Osterbart et al. (2000) concluded that it is the southern scattering
lobe that dominates the optical Hubble Space Telescope (HST) and
near-IR images and polarization pattern. See also Sects. 3.2,
4.5.1, 4.5.2, 4.6, and
6.
DENSITY PROFILE.
Near-IR interferometry observations by McCarthy et al. (1980)
indicated large departures from the expected smooth
density distribution on an arcsecond scale.
Deviations indicating an enhancement by a factor of 3 were found also
over much larger distances by Bieging et al. (1984) and a flatter
density distribution
was
deduced by Fazio et al. (1980). Having analysed far-IR scans of the
envelope on large scales, Harvey et al. (1991) concluded that dust
density distribution is inconsistent with the picture of a smooth,
constant-velocity outflow. Keady & Ridgway (1993) presented evidence
for by a factor of 2-3 higher densities
1000 years ago. Two
periods of enhanced density
200 and 850 years ago were
identified by Groenewegen et al. (1997). Direct evidence of periodic
outbursts with higher densities on a time scale of 200-800 years was
found in deep optical images by Groenewegen et al. (1987) and
Mauron & Huggin (1999). See also Sects. 4.3,
4.4, 4.5.3, and 6.
MASS-LOSS RATE.
From a radiative transfer modeling of the CO line emission,
Groenewegen et al. (1998) derived a mass-loss rate of
1.5 10-4
yr-1. A similar estimate of
2 10-5
yr-1 was obtained by
Keady et al. (1988) and Kastner (1992). Somewhat higher
mass-loss rate of
3.25 10-5
yr-1 was derived
by Crosas & Menten (1997) from their modeling of the CO radiation,
whereas Truong-Bach et al. (1991) obtained
4 10-5
yr-1 for the outer envelope.
Molecular spectroscopy and a spectral synthesis modeling allowed
Keady & Ridgway (1993) to derive an upper limit of
4 10-5
yr-1.
Sahai (1987) estimated
4.8 10-5
yr-1 in
the outer envelope, whereas Knapp & Morris (1985) obtained
5.5 10-5
yr-1. Note that the above estimates
are based on different distances and need to be rescaled (see
Table 5). See also Sects. 4.4 and
6.
OUTFLOW VELOCITY. From molecular line observations, Morris et al. (1975) derived an expansion velocity of the envelope of 12kms-1. Betz et al. (1979) detected NH3 in the inner dense region, concluding that the gas flow was accelerated to 14kms-1 on subarcsecond scales. Olofsson et al. (1982) observed several molecules in the envelope with an outflow velocity of 14.4kms-1. Kuiper et al. (1976) resolved a large CO envleope expanding at 15kms-1 and Knapp & Morris (1985) obtained almost the same velocity of 15.2kms-1, whereas Knapp et al. (1982) measured an outflow velocity of 17kms-1. See also Sect. 3.2 and Appendix A.
COMPOSITION. A broad emission feature at about
11
m in the spectra of IRC
+10216 obtained by
Treffers & Cohen (1974) indicated that silicon carbide dust must be
present, as well as other carbonaceous particles with featureless
emissivity. A broad far-IR emission band beginning at 24
m was
discovered by Forrest et al. (1981). It was shown to extend beyond
37
m and peak at
30
m by Herter et al. (1982).
Magnesium sulfide dust grains were proposed by Goebel & Moseley (1985)
as the carrier of the band. See also Sects. 3.3.1,
3.3.4, 3.3.5, 3.3.6, 4.2,
and 6.
SIZES. Spectrophotometry of the 11
m feature by
Treffers & Cohen (1974) showed that there exist small grains with
radii
1
m. Near-IR low-resolution
spectra obtained by Witteborn et al. (1980) indicated a presence of
grains with radii
0.25
m. Jura (1983) argued
that grains are rather small, having
0.05
m, and
later Jura (1994) proposed that dust in the outer envelope has a
wide distribution of sizes, including both large and small grains
(
0.015
m,
0.5
m). See also
Sects. 3.3.1, 3.3.6, and 4.2.
CONDENSATION. Modeling of dust formation by McCabe (1982)
demonstrated that small SiC grains can condense very close to the
stellar photosphere (
1.5
,
1500K), whereas graphite grains form at
lower temperatures further away from the star
(5
20
,
1000K
600K). Danchi et al. (1990)
interpreted interferometry data as indicating that dust grains form
at higher temperatures (1000-1800K), and closer to the star
(1.5-3
)
than usually assumed. See also Sects. 3.3.2,
4.3, and 6.
EMISSIVITY. Submillimeter photometry by Phillips et al. (1982)
showed that the far-IR opacity of the grains is close to
.
Comparing the far-IR and
ultraviolet extinction of dust in the envelope, Jura (1983) argued
that
.
Photometry in the far IR by
Rengarajan et al. (1985) and at submm wavelengths by
Sopka et al. (1985) confirmed that the dust emissivity is rather
flat at long wavelengths (
to
). A similar result was also found by
Le Bertre (1987) from his radiative transfer fitting of the
observed SED. See also Sects. 3.3.3 and 4.2.
Huge amounts of detailed observational information for IRC
+10216
present a real challenge to theoretical models attempting to explain
the data in a consistent way. In addition to the usual difficulties and
uncertainties of modeling and interpretation, the star and its envelope
have significantly varied in time due to both periodic pulsations and
non-periodic, long-term changes. What we observe is a complex result
of a very long evolution of the central star, with its history recorded
in the structure and chemical composition of the parsec-sized
envelope.
Many usual simplifying assumptions are invalid for IRC
+10216:
(1) we clearly have a non-stationary, time-dependent problem,
(2) spherical symmetry cannot be adopted for dense inner regions
and even axial symmetry is questionable there,
(3) the mass-loss rate and the wind velocity are not constant,
(4) the envelope's density and chemical composition cannot be described
by simple power laws,
(5) dust grains are very likely to have inhomogeneous structure
and composition, non-spherical shapes, and different size distributions
in various parts of the envelope,
(6) the grains are accelerated by the radiation pressure to different
velocities, which leads to their collisions and possible growth by
coagulation or to destruction in the dense inner regions,
(7) the observational constraints used in models are not coeval.
The last point is potentially very troublesome, because of the observed non-periodic changes which imply that the data from different epochs may well be fundamentally incomparable. An important question is how far one can go making simplifying assumptions while modeling very complex phenomena. The finer details are observed, the more simplifications we have to abandon, and the more complex the models should become.
Having mentioned many difficulties which may complicate thorough
and detailed analyses, we are going to make a number of assumptions and
simplifications, which we believe are reasonable, and present a model
for IRC
+10216, which takes into account all existing dust
continuum observations. Our goal is to find a snapshot structure of the dusty envelope, consistent with the recent
high-resolution optical and near-IR images of the object
(Weigelt et al. 1998a,b; Haniff & Buscher 1998; Osterbart et al. 2000), as well as with most other measurements of the
dust radiation. Although our model describes only the present structure of the object (and as such is time-independent),
in Sect. 5 we consider its evolutionary implications. The
complex molecular chemistry of the envelope is largely ignored here and
the gas component is described by means of a spatially constant
dust-to-gas mass ratio. The assumed constancy of
may not be
realistic enough, thus contributing to the uncertainties of the derived
properties of the gaseous envelope (e.g., the total mass M of
the envelope, lost by the central star during its evolution).
We utilized our 2D radiative transfer code based on a ray-tracing method which provides an accurate solution to the frequency-dependent radiative transfer problem, including isotropic scattering (we refer to Men'shchikov & Henning 1997, for a detailed description). Large parameter space was explored in many hundreds of runs by changing model parameters and comparing their SEDs, images, and visibilities to available observational constraints (see Appendix B for details).
The model assumes axially-symmetric geometry shown schematically in
Figs. 1 and 2.
Departures from spherical
symmetry appear only on a subarcsecond scale, in the inner dense
core. In our recent images (Osterbart et al. 2000) the bipolar holes
appear very small, comparable to the stellar diameter (see also
Sect. 4.5). The perfect conical shape of the polar cavities
should be considered as only a first approximation to reality. In this
2D radiative transfer modeling, we had to ignore the possibility that
the immediate environment of IRC
+10216 may be three-dimensional. One
needs to keep this in mind, however, when comparing our results with
observations.
Although it may contradict intuitive perception, in our model the star
is located at the position of the fainter component B, whereas the
brightest peak A is produced by the hot dust emission from the far side
of the outflow cavity (Fig. 1). The even fainter
components C and D may be, for example, optically thinner zones due to
density fluctuations along a ring surrounding the outflow cavity
(Fig. 2). High-resolution observations, in particular a
1.1
m polarization map and the components' proper motions
presented in our previous paper (Osterbart et al. 2000), support
this picture. We have shown that the most natural and symmetric
velocity field can be derived if one assumes the star at the position
of B. In fact, only in this case, both symmetrically located components
C and D are moving away from B (within the plane of sky) with the
same apparent velocity
5kms-1; the component A is moving away from
the star with an apparent velocity of
14kms-1 (Table 2
in Osterbart et al. 2000). A velocity being different by factor of 3 is
most likely a pure projection effect implying that the radius-vectors
and
to C and D are more inclined toward the
observer than is the vector
to component A
(Fig. 2). The actual deprojected radial velocity
15kms-1 (see Appendix A) is
the same for all the components and equal to the general expansion
velocity of the envelope around IRC
+10216.
It is instructive to list here our general simplifying assumptions, which
are relevant (and essential) for the model:
(1) dust distribution is axially-symmetric close to the star,
(2) outer parts of the envelope are spherically-symmetric,
(3) dust density depends only on the radial coordinate,
(4) dust population consists of spherical, compact solid grains,
(5) size distribution of the grains can be described by a power law,
(6) wherever a dust component exists, its composition, structure, and grain
sizes are spatially invariant,
(7) light scattering by the dust particles is isotropic,
![]() |
Figure 1:
Geometry of the circumstellar envelope of IRC |
| Open with DEXTER | |
![]() |
Figure 2:
Three-dimensional representation of the innermost dense core of the
circumstellar envelope of IRC |
| Open with DEXTER | |
There are no good reasons to believe that the above statements are extremely good approximations. One cannot avoid using them, however, primarily because of the obvious lack of sufficiently detailed and reliable observational constraints. The influence of the assumptions on model results is quite uncertain apriori and, therefore, it must be carefully investigated.
Spectrophotometric observations of IRC
+10216 show an almost featureless
continuum with only a couple of clearly detected broad bands
(Sect. 2.2). The latter are the so-called 11.3
m emission
attributed to SiC grains (Treffers & Cohen 1974) and a very broad
emission band at
30
m, which is usually thought to be
produced by MgS grains (Goebel & Moseley 1985). Also clearly visible
is a 3.1
m absorption feature attributed to the absorption by
molecules (C2H2, HCN) in stellar photospheres
(Ridgway et al. 1978).
| T1(K) | R1( |
a( |
p | Composition | Reference |
| 1700 | 2 | Gr | Crabtree & Martin (1979) | ||
| 1500 | 1.5 | Gr+SiC | McCabe (1982) | ||
| 1500 | 1.9 | 1 | amC+SiC | Griffin (1990) | |
| 1500 | 3.4 | amC+SiC+MgS | Skinner et al. (1999) | ||
| 1300 | 2.5-3 | Danchi et al. (1990) | |||
| 1300 | 2.5 | amC | Winters et al. (1994) | ||
| 1100 | 2.2-3 | 0.008 | 1.3 | amC+SiC | Bagnulo et al. (1995) |
| 1075(5%) | 4.5(10%) | 0.16(6%) | amC+SiC | Groenewege (1997) | |
| 1000 | 4.0 | amC+SiC | Sloan & Egan (1995) | ||
| 1000 | 4.5 | 0.05 | 1 | amC | Martin & Rogers (1987) |
| 950(25%) | 6.6 | 1.3 | Le Bertre (1987) | ||
| 850 | 6 | 0.05 | 1.2 | amC+SiC | Lorenz-Martins & Lefèvre (1993) |
| 750 | 5.6 | 0.1 | 1 | amC | Rowan-Robinson & Harris (1983) |
| 750(7%) | 5.1-8.5 | amC+SiC | Ivezic & Elitzur (1996) | ||
| 600 | 20 | 0.05 | 2 | Gr+SiC | Mitchell & Robinson (1980) |
| 0.01 | amC+SiC | Sloan & Egan (1995) |
The continuum is undoubtedly produced by some kind of carbonaceous solid particles, although details of the chemical composition, internal structure of the dust material, and of the condensation process itself are still a matter of debate. Most frequently, the observations have been interpreted in terms of amorphous carbon grains (which are conglomerates of highly disordered planar graphitic structures), although it seems very unlikely that any single form of carbon may be able to explain all observations. Moreover, there are good reasons to believe that properties of circumstellar dust are extremely complex.
In the present modeling we assumed that dust is a mixture of compact
spherical solid particles of radius a, composed of inhomogeneous materials which include different forms of carbon,
silicon carbide, and magnesium-iron sulfides. Although polycyclic
aromatic hydrocarbon (PAH) molecules may also exist in the carbon-rich
envelope around IRC
+10216, the observations show no evidence of their
emission features. The three components considered in this work
constitute the simplest realistic set of materials; the addition of
other solids or PAHs would not be justified.
The radiative transfer code employed in this study
(Men'shchikov & Henning 1997) treats separately an arbitrary number
of dust components which may differ by the composition, structure,
shapes and sizes of grains.
Following Kim et al. (1994) and
Jura (1994), we adopted a size distribution in the form
,
which is
defined by the minimum grain radius and by the exponential cutoff
radius for the largest particles (
).
Although we explored a very large range of various grain parameters and
mixtures in the modeling, unknown details of the dust properties in
IRC
+10216 prevented us from using more complex dust models in final runs.
Laboratory experiments on dust condensation (Frenklach et al. 1989)
suggest that SiC may be the first material to nucleate from the gas
phase at fairly high temperatures
2000K, i.e.
very close to (or even inside of) the stellar photosphere. At lower
temperatures of
1500K (distances r of only a
few
)
these very small SiC particles may provide sites for
their further heterogeneous growth by the deposition of amorphous
carbon (diamond, for
1300K) layers. When
temperatures in the stellar wind drop to
1000-900K,
PAH molecules can form in the gas phase (Frenklach & Feigelson 1989).
Their clustering may produce more nucleation sites, provided that
chemical, thermal, and dynamic conditions in the wind are favorable for
the formation of high enough number density of PAHs. The existing SiC-C
core-mantle grains could also grow substantially by the deposition of
PAHs on their surfaces. At even larger distances from the star
(
10
), MgS could condense at temperatures
800K, as indicated by nucleation calculations
(Gail & Sedlmayr 1986).
Although laboratory experiments and theory suggest that condensation
temperatures as high as 2000K are possible for the abundant
refractory C and SiC dust, radiative transfer models have been adopting
much lower temperatures T1 at the inner dust boundary R1. It
is clear from Table 1, however, that the observationally
based model estimates of the dust temperature and the dust-free
zone radius in IRC
+10216 also substantially differ from each other.
Note a
very large scatter, by factors of
3-4 in the derived values
for the two key model parameters.
It is reasonable to consider
the factors as rough estimates of the absolute uncertainties, or
"error bars'', of typical simplified models that fit only SEDs.
Less
abundant (or more transparent) refractory components may condense at
higher temperatures, closer to the star than the models assume, yet
their presence in the "dust-free'' zone is almost impossible to deduce
from simple fitting of observed SEDs.
As usual, our model assumes that dust appears instantaneously at a
distance R1 from the star, where the gas temperature
equals to the expected nucleation temperature
of the
adopted dust component. In a multicomponent approach utilized in the
present study, different components of dust grains (having different
abundances) form in a considerable range of temperatures and distances
(factors of
3 and 10, correspondingly). The stellar surface
oscillates in our model between 1.8 and 2.3AU with the pulsational
period of the star. We put the inner boundary of the dusty envelope as
close as possible to the star, at
3.3AU
,
and
separated it from the latter for purely numerical reasons. This
particular choice of R1 does not influence the model results in
any way, because the innermost regions of the envelope
(
20AU) populated by SiC dust are optically thin.
Condensation temperature of SiC grains, the most refractory dust
component (
2000K), is higher than their
radiative equilibrium temperatures at the inner boundary
(
1000K), suggesting that SiC dust can indeed nucleate
even inside the stellar photosphere. At larger distances,
AU
,
carbonaceous
dust condenses in the stellar wind (
900K),
forming [SiC,C] conglomerates. The formation zone of magnesium-iron
sulfides, the least refractory material (
600 K), is located further downstream, at
45AU
.
Pre-existing [SiC,C] grains serve as the condensation sites for
[Mg,Fe]S mantles in our model.
Most previous radiative transfer calculations tried to fit the SED of
IRC
+10216 by postulating small spherical graphite or amorphous carbon
grains, with a power-law long-wavelength emissivity
(Table 1).
Recent
radiative transfer models that took into account near-IR
visibilities (in addition to the SED), derived somewhat larger grain
sizes, up to
0.2
m.
Some of the studies used
also pure SiC grains as a minor additional component necessary to
explain the 11.3
m emission feature. All of them adopted optical
constants of SiC published by Pegourie (1988); see, however,
Papoular et al. (1998) for a discussion of problems with derivation
of those constants. Lack of published measurements for MgS was the main
reason why this dust component has not been included in previous models,
despite the proposed association of the broad 30
m emission with
this material (Sect. 2.2).
In this study, relevant materials were identified using known optical
constants of different laboratory analogs of cosmic dust. Mie theory
was applied to compute the size- and wavelength-dependent absorption
and scattering efficiencies,
and
.
We utilized the optical constants of graphite
(Draine 1987), amorphous carbon AC1 (Rouleau & Martin 1991),
ACH2 (Zubko et al. 1996), carbon samples cel400, cel600, cel800,
cel1000 (Jaege et al. 1998),
-SiC (Choyke & Palik 1985; Pegourie 1988), and [Mg,Fe] sulfides of various compositions
([MgxFe1-x]S with x=0.9, 0.75, 0.5, 0.1, 0;
Begemann et al. 1994).
The optical data of the laboratory samples of [Mg,Fe] sulfides have
been measured by Begemann et al. (1994) in the wavelengths range
10-500
m. To enable calculations of the radiative
equilibrium dust temperatures, we extrapolated the optical constants to
the wavelengths 1.2-10
m using the Lorentz oscillator model in
the limit
,
where
is the
resonance frequency (e.g., Bohren & Huffman 1983. The data were
extended to the wavelength range 0.3-1.1
m using the optical
constants of troilite (FeS) measured by Egan & Hilgeman (1977).
A similar extrapolation to the wavelength range 17-300
m, in the
limit
,
was applied to the optical constants of
-SiC compiled for the wavelengths 0.04-17
m by
Choyke & Palik (1985). In this way, we were able to compute the
efficiencies
and
in the interval
0.3-300
m from the optical constants.
At longer wavelengths, we extrapolated
by a power law
with
2 for SiC and
1 for the other
materials. Although
at
in the ideal case of compact homogeneous
spherical grains, the latter simple model is unlikely to describe the
real cosmic dust in full detail. In fact, we know that the real dust
grains have various non-spherical shapes, rough surfaces, inhomogeneous
chemical composition, and aggregate (porous) structure. A lower
exponent approaching unity is more appropriate for coagulated particles
with fluffy structure
(Wright 1987; Ossenkopf 1993; Ossenkopf & Henning 1994; Henning & Stognienko 1996)
or layered materials (Tielens & Allamandola 1987). Moreover, a
lot of observational material has been accumulated over the last
decades indicating that
1 describes the optical
properties of circumstellar dust much better than
2 at long
wavelengths (cf. Table 1 for IRC
+10216).
In addition to the homogeneous spherical grains, we considered more realistic core-mantle particles and studied shape effects using the model of continuous distribution of ellipsoids (CDE, Bohren & Huffman 1983). To account for the composite, non-uniform internal structure of the real grains, we utilized the effective medium calculator, written by Volker Ossenkopf, which simulates the effects of pollution, porosity, and aggregation on the optical constants of the input materials (Ossenkopf 1991). We explored inclusions of one material into the other (Maxwell-Garnett effective medium) and of unorganized conglomerates (Bruggeman effective medium). Simple spherical impurities and their shapes in the extreme cases of disks and needles, have been investigated. Exploring the parameter space of the mixtures, we tried to keep a balance between the obvious complexity of the reality and simplifications necessary to avoid too many free parameters.
The broad emission band seen in IRC
+10216 and many other carbon
stars between 10
m and 13
m (Fig. 3) is
usually called the 11.3
m feature.
![]() |
Figure 3:
Silicon carbide feature and the 11.3 |
| Open with DEXTER | |
Blanco et al. (1994) attempted to explain them by a mixture of two
crystalline forms of silicon carbide,
- and
-SiC.
Kozasa et al. (1996) proposed core-mantle grains consisting of
-SiC cores and carbon mantles (or
-SiC inclusions in carbon
particles) as the most plausible carrier of the feature.
Papoular et al. (1998 )argued, however, that the shape effects alone
can explain the emission bands, favoring CDE as an adequate
approximation. Speck et al. (1999) concluded that it is actually
-SiC,
not
-SiC, that reproduces the observed shapes in carbon stars. None
of the above explanations is convincing, since they are based on a
highly simplified approach and a narrow wavelength range of just one
dust feature.
We addressed the problem anew, in the frame of our
detailed radiative transfer calculations, aiming to construct a dust
model that is consistent with both broad features observed in
IRC
+10216 as well as with all other observations of this object.
Note that the 11.3
m band in Fig. 3 is significantly
asymmetric and that continuum levels at the blue and red sides of the
feature (
9.5
m and 14
m, respectively) differ by
30-50%. This characteristic shape, which is also observed in
other carbon stars (see, e.g., V Cyg, RU Vir,
IRC+40540 in Yamamura et al. 1998), should be reproduced
by successful models.
Many mixtures of SiC with different samples of carbon (volume
fractions 0.01-0.99) have been tested in our study. Some of the
results are shown in Fig. 3, where we compare
shapes of the absorption efficiencies for small grains with the
Infrared Space Observatory (ISO) spectrum of IRC
+10216. It is quite clear
that the optical constants of SiC derived by Pegourie (1988)
cannot explain the observed 11.3
m feature. Both the spherical
grains and the CDE model predict much broader shapes of the band and
higher level of its red wing, opposite to what is observed. Spherical
-SiC grains with the optical constants published by
Choyke & Palik (1985) can also be ruled out as they produce a very
strong single resonance at 10.75
m. The CDE model applied to
their data predicts a flatter, much broader profile which looks
somewhat more similar to the observed band.
Yet, shapes of
-SiC grains in the CDE approximation cannot explain
the observations, as SiC is clearly not the only grain material present
in carbon stars. In fact, amounts of SiC must be small compared to
other carbonaceous dust, because of the great strength of its resonance
feature. If we added, however, any small amount of the CDE grains
to the most abundant carbon materials (featureless in this wavelength
region), there would be no asymmetry in the continuum levels at both
sides of the 11.3
m feature. This would be an obvious inconsistency
with the observations, implying that the CDE model is incapable of
explaining the 11.3
m feature, contrary to the conclusions of
Papoular et al. (1998). By the same reasons, any additional
component of spherical SiC grains would also fail to reproduce the
essential characteristics of the observed profile.
Results of our modeling plotted in Fig. 3 demonstrate
that inhomogeneous grains are the carrier of the band. We confirm
the general idea of Kozasa et al. (1996) that a composite material
containing both carbon and SiC is indeed responsible for the
observed profiles in carbon stars. The results disagree, however, with
their suggestion that carbon mantles or Maxwell-Garnett-type
-SiC impurities in amorphous carbon grains provide a good model for
the 11.3
m band. We have found that unorganized Bruggeman-type
aggregates of
-SiC (constants from Choyke & Palik 1985) and
cel800 with volume fractions 15:85 resemble the observed band
(Fig. 3). Shape effects in the CDE approximation for such
grains do not work so well in explaining the 11.3
m profile.
We conclude that the [SiC,C] conglomerates with 80-90% of
volume in carbon, not pure SiC grains, provide the best match for
the 11.3
m band in IRC
+10216 and other carbon stars. Moreover, as we
show in the next sections, the composite [SiC,C] grains even become
consistent with both features observed in IRC
+10216, provided that
they are covered by mantles of [Mg,Fe] sulfides.
The originally proposed carrier of the feature, MgS
(Nuth et al. 1985), shows a very broad band at 36
m,
almost 10
m away from the observed peak, which is obviously
unacceptable. A sample of [Mg0.9Fe0.1]S, the closest
laboratory analog of MgS measured by Begemann et al. (1994),
displays a sharper peak at 28.2
m. When used in radiative
transfer calculations, however, this material produces an emission
feature centered at 30
m, almost 4
m away from the peak
position in IRC
+10216. We have to conclude that the identification of the
band carrier with MgS should be reconsidered.
![]() |
Figure 4:
Magnesium-iron sulfide dust features and the 27 |
| Open with DEXTER | |
In order to resolve the problem, we tried many combinations of
[MgxFe1-x]S with different samples of carbon (volume fractions
0.01-0.99). We explored effects of the core-mantle grains, the
Maxwell-Garnett and Bruggeman effective media, and the shape
effects in the CDE approximation. The latter failed to agree with the
observations of IRC
+10216, in most cases producing much too broad the
emission feature (25-45
m) centered at
30
m.
Moreover, the optical constants of all the
[MgxFe1-x]S sulfides, alone or in a combination with different
types of amorphous carbon (Sect. 3.3.3), failed to produce
any dust materials having an emission peak between 26 and 27
m.
In some cases, when the amorphous carbon cores were covered by
the [Mg0.9Fe0.1]S mantles, the outcome was a minimum at
30
m, between two peaks at 24
m and 37
m. Such
behavior of the core-mantle grains has already been noticed
(e.g., Szczerba et al. 1997). Selected results of our effective
medium calculations displayed in Fig. 4 show the absorption
efficiencies of relatively thin (15% in radius) [MgxFe1-x]S
mantles (x=0.9,0.5) on small carbon grains made of AC1, cel400,
cel600, cel800, cel1000, and graphite. The sequence of four laboratory
carbon samples, from cel400 to cel1000, is characterized by an
increasing amount of ordered graphitic structures
(Jaeger et al. 1998). To reproduce the observed band
characteristics, the [Mg0.5Fe0.5]S sulfides should be mixed with (or added
as a mantle to) either graphite or incompletely amorphous carbon
material. Due to changes of the optical properties of the inhomogeneous
materials, the 35
m maximum of the double-peak feature becomes
heavily suppressed (Fig. 4) with only one peak remaining,
centered at 27
m.
We conclude, therefore, that such carbon grains covered by [Mg0.5Fe0.5]S
mantles explain the 27
m band observed in IRC
+10216, provided that
the carbon material contains a large fraction of graphitic structures.
Note also (see Fig. 4) that the same set of solid
materials can be used to explain a family of broad emission
bands observed in carbon stars, with peaks between 25 and 37
m.
An interesting outcome of our modeling is that a single population of
core-mantle grains can reproduce both features in IRC
+10216,
provided that it is the [SiC,C] aggregates (Sect. 3.3.4)
that are covered by the [Mg0.5Fe0.5]S mantles (Sect. 3.3.5);
hereafter we refer to such composite grains as to the [SiC,C]+[Mg,Fe]S dust.
Extinction efficiencies of such grains for different thicknesses of
mantles are compared with the ISO data for IRC
+10216 in
Fig. 5.
The shapes produced by moderately thin mantles
(
0.1) of [Mg0.5Fe0.5]S around the [SiC,C] cores
(SiC:C
1:9 by volume) best resemble the observed flux
distribution. Close similarities between their total extinction and the
SED, including all essential characteristics of the two bands (peak
positions and widths, as well as the continuum levels), suggests that
our identification of the materials is indeed a good approximation to
the reality. This is further demonstrated by the results of our
self-consistent radiative transfer calculations in
Sect. 4.
![]() |
Figure 5:
Inhomogeneous dust grains made of silicon carbide, carbon, and
magnesium-iron sulfides explain both the 11.3 |
| Open with DEXTER | |
| r (AU) | 3-30 | 30-45 | 45-100 | 100-6 105 |
| SiC | ||||
|
|
0.00042 | 6 10-5 |
|
|
|
|
3.3 |
|
|
|
|
|
0.005 |
|
|
|
|
|
1.0 |
|
|
|
| -3 |
|
|
|
|
| [SiC,C] | ||||
|
|
- | 0.00165 | 3 10-5 |
|
|
|
- | 2.2 |
|
|
|
|
- | 0.01 |
|
|
|
|
- | 1.0 |
|
|
| - | -4 |
|
|
|
| [SiC,C]+[Mg,Fe]S | ||||
|
|
- | - | 0.0039 |
|
|
|
- | - | 3.5 |
|
|
|
- | - | 0.015 | 0.05 |
|
|
- | - | 1.15 | 3.0 |
| - | - | -6 | -3 | |
As is shown by the upper set of curves in Fig. 5, a
mixture of carbon, [SiC,C], and core-mantle [Mg0.5Fe0.5]S grains can match
the observed shape as well as does the single population of composite
grains. It is clear that all the three major dust components are
present in the envelope of IRC
+10216. There are, however, no observational
constraints on the relative radial distributions of the components'
abundances. We had, therefore, no choice but to reduce the free parameter
space by assuming that there are only three dust components:
The overall physical picture implied by the model is quite natural, as
expected (cf. Sect. 3.3.2). The SiC grains first
condense in the wind very close to stellar surface, at
2000K. The most abundant carbon materials
begin to nucleate in the wind when it reaches greater distances and lower
temperatures (
1000K), leading eventually to
the formation of [SiC,C] aggregates. When they enter the condensation
zone of the [Mg,Fe] sulfides (
600K),
the latter form mantles on the existing inhomogeneous particles.
In Fig. 6, we plotted optical depths toward the star as a
function of wavelength and opacities of all dust components for only
the smallest grains.
![]() |
Figure 6:
Properties of dust in our model of IRC |
| Open with DEXTER | |
Note that one should be extremely cautious in making direct comparisons of dust absorption efficiencies to observed SEDs for a wide wavelength range, where radiation transfer effects are clearly important. Any sensible quantitative analysis should be done only in the frame of accurate, self-consistent radiative transfer modeling. We would also like to emphasize here again (as did also Kozasa et al. 1996) dangers of the widely used method of drawing a continuum and subtracting it to analyze the observed shapes. The actual continuum levels are essentially unknown and the contribution of different materials may well not be additive. Moreover, a wavelength-dependent effect of finite apertures used in observations modifies shapes of the wide dust features and needs to be properly taken into account (see Sect. 4.2).
Our exploration of the dust grains' parameter space presented in this
and two previous sections included many runs of the radiative
transfer code to verify our conclusions drawn on the basis of
curves alone. It is essential that experience accumulated from
model calculations directs the simplified analysis described above.
Without such a guidance, the comparisons of
to SEDs may
easily be misleading.
In this section we discuss the remaining basic parameters of our model
of IRC
+10216: distance D, bolometric luminosity
,
effective
temperature
,
and location R2 of the outer boundary.
Estimates of the distance to IRC
+10216 range from a lower limit of
100pc to 290pc. As is evident from Table 3,
a number of recent detailed studies point toward the lower end of the
range.
| D(pc) | Reference |
| 290 | Herbig & Zappala (1970) |
| 150 | Kastner (1992) |
| 150 | Crosas & Menten (1997) |
| 100-150 | Zuckerman et al. (1986) |
| 110-135 | Groenewegen et al. (1998) |
| Becklin et al. (1969) |
Since deviations from spherical symmetry in IRC
+10216 are moderate,
luminosity of the central star obtained from the observed SED will
depend weakly on the (unknown a priori) optical depth and viewing
direction. Our model yields 13000 and 5200
for the phases of
maximum and minimum luminosity, respectively, with uncertainties of
about
20%. These luminosities are based upon the assumption of
a sinusoidal periodic variation of fluxes from IRC
+10216 and on our model
fits of the observed SEDs at phases
=0.24 and
=0.56 (see Sect. 4.2). Specifically, the following
formula was used to describe the variations of stellar luminosity with
phase:
![]() |
(1) |
Significant changes in the object occurred during the first 15 years of
observations, when an average K brightness declined by about 1
to the present level. An extrapolation back in time (to the late 1970s)
using our sinusoidal fit starts to give phases deviating by
0.2 from the old papers' estimates.
The intrinsic stellar energy distribution of IRC
+10216 is reprocessed by
dust grains having wavelength-dependent absorption and scattering
properties, and as such is uncertain. According to the spectral
classification C9,5 by Cohen (1979), the opaque dusty envelope
obscures a star with
2200K. A number of other
indirect estimates from model fits to the observed flux distribution
are collected in Table 4.
|
|
Reference |
| 2460 | Sloan & Egan (1995) |
| 2330(15%) | Ridgway & Keady (1988) |
| 2330(15%) | Griffin (1990) |
| 2326 | Ridgway & Keady (1993) |
| 2300 | Keady et al. (1988) |
| 2230 | Cohen (1979) |
| 2200(7%) | Ivezic & Elitzur (1996) |
| 2100 | Lorenz-Martins & Lefèvre (1993) |
| 2010 | Winters et al. (1994) |
| 2010 | Skinner et al. (1999) |
| 2000(5%) | Groenewegen (1997) |
| 2000 | Crabtree & Martin (1979) |
| 2000 | Mitchell & Robinson (1980) |
| 2000 | Rowan-Robinson & Harris (1983) |
| 2000 | Martin & Rogers (1987) |
| 2000-2500 | Lucy (1976) |
| 1800 | Phillips et al. (1982) |
| 1800 | Sopka et al. (1985) |
| 1800 | Sahai et al. (1989) |
| 1500-2700 | Danchi et al. (1994) |
| 1600-2100 | Witteborn et al. (1980) |
| 1100-1400 | Orofino et al. (1990) |
One major problem with the estimates is that they are all based on the
assumption that the central star in IRC
+10216 radiates as a blackbody.
The latter has been known, however, as a poor approximation for the
cool, extended molecular atmospheres of AGB stars; thus, the accuracy
some estimates appear to claim may be misleading.
The absorption-line
spectra of stellar atmospheres strongly deviate from a blackbody in the
optical to mid-IR range, for the extremely low effective temperatures
3000K.
Realistic spectra of stellar atmospheres have not been incorporated in
previous radiative transfer models of IRC
+10216. This may have been justified
by the apparent smoothness of the observed SED, which sharply contrasts
with the absorption spectra of the model atmospheres (see Fig. 7).
Our modeling has shown that, indeed, a blackbody central source with
2000K could give a very good fit to the observed
short-wavelength SED. Note, however, that such low effective temperatures
are not in line with stellar evolution calculations predicting
2500-3000K as a typical range of
for AGB stars. We would
like to stress that the opaque dusty envelope of IRC
+10216 makes it
impossible to derive
with any acceptable accuracy from the
dust continuum radiative transfer calculations alone. Stellar spectrum
is reprocessed by dust grains with poorly known properties.
It has been suggested by studies of stellar pulsations
(Bessell et al. 1996; Hofmann et al. 1998) that stellar radius varies
in a relatively narrow range, by
20%, between the phases
of maximum and minimum luminosity. We assumed in the final model that
the effective temperature of IRC
+10216 varies between 2800K and 2500K
at those phases. More specifically, we used the following formula to
describe phase variations of effective temperature:
![]() |
(2) |
The outer boundary radius of the envelope of IRC
+10216 is certainly larger
than the maximum distance of 600
to which the far-IR emission
of the object has been traced by Infrared Astronomical Satellite (IRAS)
(Young et al. 1993). The observed size does not give any information
about the physical boundary, as it is a lower limit set by IRAS
sensitivity. Molecules that have been traced up to radial distances of
only 240
(Groenewegen et al. 1998) also provide no useful
constraints on the real extent of the envelope. They set a lower limit
because of either a detector sensitivity, or too low a number density
of molecules for collisional excitation, or a photodissociation by the
interstellar radiation field.
|
|
R2 |
|
Reference |
|
Dust continuum (
|
|||
| 6.1 | 0.9 | Winters et al. (1994) | |
| 3.8 | 3.1 | 0.0045 | Skinner et al. (1999) |
| 2.9 | 0.0036 | Danchi et al. (1994) | |
| 2.7 | 3.5 | 0.0016 | Ivezic & Elitzur (1996) |
| 2.6 | 0.0030 | Sopka et al. (1985) | |
| 2.1 | 3.2 | 0.0040 | Bagnulo et al. (1995) |
| 2.1(10%) | 14 | 0.0050 | Groenewegen (1997) |
| 2.0 | 2.6 | 0.0030 | Griffin (1990) |
| 1.1 | 19 | Le Bertre (1997) | |
|
Molecular lines (
|
|||
| 2.4 | Crosas & Menten (1997) | ||
| 1.7 | Kwan & Linke (1982) | ||
| 1.7 | Truong-Bach et al. (1991) | ||
| 1.5 | 0.0049 | Kastner (1992) | |
| 1.4(20%) | 0.0014 | Groenewegen et al. (1998) | |
| 1.2 | Knapp & Morris (1985) | ||
| 0.9 | Sahai (1987) | ||
| 0.8 | 0.0058 | Keady & Ridgway (1993) | |
| 0.8 | Kwan & Hill (1977) | ||
In contrast to previous radiative transfer models that used more or
less arbitrary R2, we derive it by adopting an observationally
determined value for the mass-loss rate
in IRC
+10216
(Table 5). Considering the mass conservation
equation for a stationary, spherically-symmetric outflow,
,
and assuming that
and
15kms-1, we readily
obtain the location of the physical outer boundary:
![]() |
(3) |
The resulting outer boundary of IRC
+10216 is located at
AU, which corresponds to an angular
radius of 4615
(=77
=1.3 108
=3pc
3 105
).
The outermost material at R2 implies a kinematic age of
2 105 years, a reasonable time for an evolved AGB star with
an initial mass of
4
that has experienced
several thermal pulses (Bloecker 1999; Bloecker et al. 2000).
It is clear that there remains some uncertainty in our determination of
R2, arising from possible changes of the outflow velocity v or the
mass-loss time scale
in the past, during the long evolution
of the central star. A similar uncertainty would be present, however,
in any other model adopting the commonly used
density distribution in the outer parts of the envelope.
The model parameters, their uncertainties, and the region of the model
parameter space which we have explored are summarized in
Table 6.
| Parameter | Symbol | Units | Range | Value | Error | Comment |
| Distance | D | pc | -- | 130 | -- | assumed (see Sect. 3.4.1) |
| Maximum luminosity | 1...2 104 | 13000 | model (from SED at |
|||
| Minimum luminosity | 3...6 103 | 5200 | model (from SED at |
|||
| Eff. temperature (max) | K | 1200...3000 | 2800 | model (see Sect. 3.4.2) | ||
| Eff. temperature (min) | K | 1200...3000 | 2500 | model (see Sect. 3.4.2) | ||
| Stellar radius (max) | -- | 500 | -- | derived (
|
||
| Stellar radius (min) | -- | 390 | -- | derived (
|
||
| Inner boundary | R1 | AU | -- | 3.3 | -- | derived (
|
| Outer boundary | R2 | AU | -- | 6 105 | -- | derived (
|
| Envelope's total mass | M | -- | 3 | -- | assumed (see Sect. 4.3) | |
| Early mass-loss rate | -- | 1.6 10-5 | -- | assumed (see Sect. 3.4.3) | ||
| Outflow velocity | v | kms-1 | -- | 15 | -- | assumed (see Sect. 3.2, Appendix A) |
| Density exponent |
|
-- | -9...+9 | +1 | -- | model (3.3-30AU, see Sect. 4.3) |
| Density exponent |
|
-- | -9...-1 | -2 | -- | model (30-45AU, see Sect. 4.3) |
| Density exponent |
|
-- | -9...-1 | -5 | -- | model (45-70AU, see Sect. 4.3) |
| Density exponent |
|
-- | -9...-1 | -3 | model (70-176AU, see Sect. 4.3) | |
| Density exponent |
|
-- | -2...-1 | -1.3 | model (176-3000AU, see Sect. 4.3) | |
| Density exponent |
|
-- | -6...-2 | -4 | -- | model (3000-5700AU, see Sect. 4.3) |
| Density exponent |
|
-- | -2...-2 | -2 | -- | model (5700- 6 105AU, see Sect. 4.3) |
| Cavity opening angle | 10-80 | 36 | model (see Sects. 4.2, 4.5.2) | |||
| Viewing angle |
|
0-90 | 40 | model (see Sects. 4.2, 4.5.2) |
The strategy of our exploration of the model parameter space was the
following. In the first step, we used a single dust component in the
model to get an idea of the approximate density structure and
parameters that are necessary to come close to the observed SEDs and
intensity maps. Very soon we found the general geometry of the dense
core and cavity used in our final model. In the second step, we
explored the dust grain model based mainly on the approximate
comparisons of
with the SED; many full radiative transfer
calculations were also necessary to test different possibilities.
In the third step, we refined the envelope's model by plugging the dust
model into the radiative transfer code and comparing the model results
with all observational constraints. This was the most time-consuming
part of the modeling that required many hundreds of runs to converge to
the final model.
We would like to emphasize that not all of the parameters in
Tables 2 and 6 are independent free
parameters and that all of those that are independent and free are
constrained by the model fits to available observations.
The most extensively varied parameters in our modeling of the envelope
are
(i=1, 2,.., 5),
,
,
,
and
(j=1, 2, 3). Less
extensively varied parameters are
,
,
(i=6, 7), and
.
The least extensively
varied parameters are
,
dust model, and numerical resolution
in terms of the distributions and numbers of intervals over radii,
wavelengths, and grain sizes (176, 220, and 19, respectively, in the
final model).
To give the reader an idea of how "unique'' the model is, we can say that it was very difficult to find the model that quantitatively fits all observational constraints. It was much easier to find a model that fits only a slightly smaller number of observations. The unprecedented number of constraints used in a self-consistent modeling does make a real difference with other much simpler models. This gives us a strong feeling of confidence in the results described below.
It may be useful to remind here that results of our radiative transfer
modeling are fully invariant with respect to the distance D, except
for several parameters which are scaled in the following simple way:
![]() |
(4) |
Figures 7-9 compare model energy distributions
with the observed SEDs of IRC
+10216 at two reference phases
=0.24 and
=0.56.
![]() |
Figure 7:
Observed SED of IRC |
| Open with DEXTER | |
![]() |
Figure 8:
Observed SED of IRC |
| Open with DEXTER | |
![]() |
Figure 9:
More detailed comparison of our model to the observed SED of IRC |
| Open with DEXTER | |
In Fig. 7, we compare the model SED at
=0.24
to the observed spectrophotometry and broad-band flux distribution of
IRC
+10216 in the entire range from optical to radio wavelengths. For
reference, the SED of an equivalent spherical envelope is also shown.
The latter differs from the model only in that the polar outflow
cavities are closed, i.e.
=180
(Fig. 1).
The effect of beam sizes is shown in Fig. 7 at all wavelengths
where fluxes were measured; it is visible mainly at the far-IR and
millimeter wavelengths. The beam-matched fluxes are by a factor
of 3-4 lower than the total model fluxes, emphasizing the very
large extent of the envelope that is much larger than any photometric
apertures. Note that care must be taken to compare our model with only
those (few) measurements, which were obtained close to the luminosity
phase considered. At
100
m, the dust radiation
is compact enough compared to the beam sizes of the observations.
The fit is almost perfect at all wavelengths, except for two fluxes (at
3.6cm and 6cm), where some other sources of radio emission may be
necessary to invoke to explain the observed fluxes which are by a factor
of
2 in excess of the model predictions. Sahai et al. (1989)
found that the contribution from molecular lines to the radio fluxes
is negligible. Knapp et al. (1995) estimated that the radio flux at
3.6cm is too low to be from an HII region, yet too high to originate
in a stellar photosphere, concluding that an extended chromosphere was
most likely source of the excess. Griffin (1990) also found in his
radiative transfer model that there must be additional free-free radiation
of the stellar chromosphere at these wavelengths.
The model fits the observations at phases of both high and
low stellar luminosity. In Fig. 8 we present the same
model with
![]()
(
=0.56),
close to the minimum luminosity.
Comparison of the model SED with
the flux distribution of an equivalent spherical model emphasizes the
influence of the bipolar geometry on subarcsecond scales
(Fig. 1). The spherical model produces fluxes by orders
of magnitude lower than those observed at
2
m
(Figs. 7,8). Ivezic & Elitzur (1996)
proposed that larger dust grains (
0.2
m) alone can
explain excess short-wavelength fluxes in a spherical model.
Although it is easy to construct an optically thinner spherical
model that perfectly fits the observed shape, such a model is unable
to explain the entire set of observational constraints considered
in the present study. Our model demonstrates that it is the
radiation escaping through the optically thinner bipolar cavities,
which produces the excess fluxes over the spherical SED at
2
m.
It is true, however, that a fairly wide distribution of grain sizes
(from
m to
1
m) is essential for successful fits of all the
data in our model of IRC
+10216. Although one can reasonably expect plenty
of small grains in the dust formation zone, being poor scatterers they
cannot reproduce the short-wavelength excess of the SED. On the other
hand, large grains alone scatter too much to fit both the shapes of the
broad emission features and our near-IR speckle images
(Sect. 4.5). We are left with a physically quite natural
choice of a wide distribution of grain sizes, consistently with what
has been deduced from observations on the basis of other considerations
(Sect. 2.2).
In Fig. 9, we compare to observations only those
portions of the model SEDs (at
=0.24 and
=0.56)
which include two broad dust emission features at 11.3
m and
27
m, as well as the 3.1
m absorption feature
(Sect. 3.3). Being a superposition of many molecular
absorption lines in stellar photosphere, the 3.1
m band
is present in the intrinsic stellar spectra at both phases.
It is also clearly visible in the model SED (Fig. 9)
at phases around the luminosity minimum, due to scattered light.
Increasing luminosity enhances hot dust continuum emission, veiling
the absorption feature. In fact, it almost disappears in both
observed and model SEDs already at
=0.24.
|
Wavelength |
1.24 | 1.63 | 2.19 | 3.79 | 4.64 | 8.4 | 9.7 | 12.9 | 18.1 | Comment |
| Observed amplitude (mag) | 2.20 | 2.14 | 2.03 | 1.65 | 1.47 | 0.84 | 0.94 | 0.63 | 0.70 | from Le Bertre (1992) |
| Model amplitude (mag) | 1.06 | 1.26 | 2.00 | 1.63 | 1.42 | 0.91 | 0.86 | 0.76 | 0.70 |
|
Shapes of the broad dust emission features are also reproduced
remarkably well in Fig. 9. Note that the emission bands are
fitted by the beam-matched model fluxes (a 25
circular
beam was used in the model). Moreover, both the continuum level and
shape significantly change in the 20-50
m range when the effect of
finite beams is taken into account. Differences between the total and
beam-matched fluxes emphasize the fact that the spatial distribution of
intensity is strongly wavelength-dependent. Fits to such wide emission
or absorption features should be carried out using accurate radiative
transfer calculations (see also Sects. 3.3.4,
3.3.5).
![]() |
Figure 10:
Temperatures and densities of dust grains in the envelope of IRC |
| Open with DEXTER | |
In Table 7, we compare wavelength-dependent amplitudes of
photometric variations of IRC
+10216 obtained by Le Bertre (1992) to the
predictions of our model.
The latter is obviously in a very good agreement
with the observations, except for only two near-IR bands, J and H.
An inspection of Figs. 7 and 8 shows that the
deviations are related to a "bump'' on the model SED between 1
m
and 2.2
m, which is also clearly visible in the spectrum of the
central star. The bump is the light from the star scattered by dust
grains. The deviation is, therefore, a consequence of the adopted model
atmosphere; it may suggest that the real atmosphere of IRC
+10216 differs
from the model adopted in this study.
In Figs. 10 and 11, we display density and
temperature distributions in the model of IRC
+10216 for only the smallest
grains with a radius a=0.01
m.
The density distribution
is rather well constrained by available spatially-resolved
observations, except for both the innermost and outermost regions. In
the immediate vicinity of the star (
0.1
), we
assumed a
gradient of the dust density.
As there are no observational constraints on the radial dependence
of the dust-to-gas mass ratio, we have no other choice but to assume
that
is constant there. This assumption implies that the
gas density
is also proportional to r (Fig. 10).
We should emphasize that the gas density distribution close to the star
is neither observationally constrained nor predicted by the model. The
situation in the innermost parts of the envelope is very complicated
due to both stellar pulsations and unknown details of the temporal and
radial dependences of the dust condensation process there. It is fairly
clear that in reality,
is a function of r and it may
change a lot due to condensation of new dust components out of the gas
phase. This means that the gas density may also increase toward
the stellar surface; both our model and observations do not "resolve''
the innermost parts of the envelope with
5
.
Our
model requires, however, that this transition zone must be relatively
transparent in the optical and near-IR wavelengths.
In the outer envelope (
40
), we adopted the
standard
profile implying a spherical outflow
with a constant velocity and mass-loss rate. Gas density at R2 in
our model is very low (
0.5cm-3), of the
order of the average density of interstellar medium. Both the SED and
1.3mm intensity profile (Sects. 4.2, 4.5.3)
require that the dust density distribution is noticeably flatter
(
)
at distances
200AU
AU
(1
5
23
). Our model confirms
the presence of a large density enhancement at
3000AU
(cf. Sect. 2.1).
Assuming that the gas and dust density
distributions are similar, such a density bump implies an episode of
higher mass loss (by a factor of 4, see Fig. 11) approximately
1000 years ago.
Our model predicts that there is a pronounced density enhancement at
45AU from the star, most likely caused by a temporal
variation of the mass-loss rate during the last decades (see
Sect. 4.4). The wave extending over the distances
10-150AU is best visible in the total density distribution
(Fig. 10, middle) and the midplane mass-loss rate
(Fig. 11). It is possible that dust acceleration has also
played a role in the formation of the steep density gradient
in the innermost, subarcsecond environment of
IRC
+10216. If we assume that the density wave is moving outward at the
observed expansion velocity (
15kms-1, see
Sects. 2.1, 3.2), we would conclude that the
mass-loss increase began
30 years before our observations. We
believe that it is more than a mere coincidence that, at the same time
(in the early 1970s), the mean K-band brightness of the object
started to gradually decline by 1
2 to its minimum in 1977,
slowly recovering by
0
2 afterwards
(Dyck et al. 1991). Near-IR colors also became redder in the years
of the minimum, corroborating this picture.
In our model, there are SiC grains all the way down to the stellar
photoshere, where they are assumed to condense at temperatures
2000K. Although we had to separate the inner boundary of
the dusty envelope from the stellar surface for numerical reasons, it may
well be that in reality the most refractive dust components nucleate
even inside the stellar photosphere (Sect. 3.3.2).
Depending
on the unknown actual properties and amounts of the grains, structure
and effective temperature of such a dusty stellar photosphere
may be different from what has been assumed in this work and from what
the current model atmospheres predict.
The profiles in Figs. 10 and 11 reflect different
temperatures of the components, according to the optical properties of
the dust materials (Fig. 6). In particular, the SiC dust with
its strong absorption feature at 10.75
m is significantly cooler
than the other components in the innermost parts of the envelope,
producing a 30% jump between their temperature profiles at
30AU. Note that the same SiC grains are by a factor of 3
warmer than the other components in the outermost regions of the
envelope of IRC
+10216, due to a reprocessed (cooler) radiation field
there.
Two vertical jumps in the density profiles of individual dust
components at 30 and 45AU, appearing in Fig. 10 on
top of the broad expanding density wave described above, are due to the
condensation of C and [Mg0.5Fe0.5]S, correspondingly, from the gas phase.
Our model assumes
that almost all SiC grains are incorporated into the [SiC,C] aggregates
at
30AU, which in turn are almost all incorporated
into the [SiC,C]+[Mg,Fe]S grains at
45AU (see
Table 2).
The dust density in the polar outflow cavities
is by a factor of 30 lower than that in other parts of the dense core.
Such an axially-symmetric density distribution causes the well-known
bipolar appearance of IRC
+10216 on subarcsecond scales (see
Sect. 4.5).
The model implies that the dust condensation radii do not change
with stellar luminosity (Figs. 10,11). Our
high-resolution speckle images obtained at different phases over a
period of 3 years do not show any structural changes that can be
attributed to the period of stellar pulsations, either
(Osterbart et al. 2000). In contrast, previous radiative transfer
models and some observational works adopted the view that the dust
formation radius (the inner boundary) moves back and forth (by
40%) over half of the stellar luminosity period
(Sect. 2.2). Our model is very sensitive to the location of
the dust formation zones. Changes of the optical depths associated with
the oscillations of the condensation radii lead to significant changes
of the model SEDs, images, and visibilities (Sects. 4.2,
4.5, 4.6). We could not find any oscillating model
that would be consistent with all observational constraints at
different photometric phases. On the other hand, our final model with
fixed condensation radii at 30 and 45AU explains all the
observations very well.
We believe that both our images and radiative transfer models strongly
suggest that the dust formation radii do not oscillate during stellar
pulsations (Winters et al. 1995).
![]() |
Figure 11:
Temperatures of the smallest dust grains at minimum luminosity
( |
| Open with DEXTER | |
A time-dependent quantity of general interest can be readily
reconstructed from our stationary model: the mass-loss history
that is recorded in the density structure of the parsec-sized envelope
over
years. The mass-loss rate
![]() |
(5) |
As it is clearly visible in Fig. 11, the model of IRC
+10216
reveals two epochs of very high mass loss (
15 and 1000 years
ago) up to 9
10-5
yr-1. The mass loss rate
was by an order of magnitude lower just
100 years ago. Over
the earlier AGB evolution of the star, where we have no observational
constraints, the model assumes a constant
![]()
yr-1 and a
density profile (Sect. 3.4.3). The
episode of enhanced mass loss 1000 years ago is "recorded'' in a
1.3mm image (Sect. 4.5.3), if we assume that the
millimeter radiation is not significantly contaminated by molecular
line emission; the peak mass-loss rate would be reduced otherwise.
The recent episode of high mass loss (terminated 15 years ago) is
reconstructed by the present modeling on the basis of our
high-resolution images (Osterbart et al. 2000). The sharp decrease
of
below 30AU (during the last decade) is partly the real
variation of the mass loss, or the density wave (Fig. 10).
In part, especially in the immediate environment of the star
(
5
,
or during the last 3 years), it may be
artificial, a consequence of the unknown radial distribution of the
dust-to-gas mass ratio
,
as discussed in Sect. 4.3.
The innermost parts of the envelope are "unresolved'' by both models
and observations. We found in the modeling, however, that this zone
must be relatively transparent in the optical and near-IR wavelengths.
In Figs. 12 and 13, we compare our model of
IRC
+10216 with the 0.8
m HST image and with our J-band speckle
image.
![]() |
Figure 12:
Comparison of the 0.8 |
| Open with DEXTER | |
![]() |
Figure 13:
Comparison of the J-band model image with a 150mas resolution (
left panel) with our speckle image of IRC |
| Open with DEXTER | |
The star is completely obscured in Figs. 12 and 13 by the optically thick dusty core (Fig. 1). As it is expected, faint scattered light from the northern outflow cavity is visible much better in the HST image than in our J-band speckle image. The characteristic cometary shape of the light from the southern outflow cavity is reminiscent of other bipolar outflow sources. If we applied the real PSF of WFPC2, its wider wings would spread the bright light of the southern cavity to the dark surroundings, thus making the model image even more similar to the observed one. There are some significant density inhomogeneities on subarcsecond scales, seen in the HST image as distortions of the light distribution symmetry, mainly on the right side of both cavities (see also Fig. 16); they can only be reproduced by a full 3D model.
Note that the brightest peak A is shifted by 0
4 away from the
star at 0.8
m compared to the J-band image. Furthermore, the
separation of the peaks A and B in both H and K images
(Sect. 4.5.2) is smaller than that in J band by another
0
3. Such wavelength-dependent shifts are the well-known
behavior observed in many optically thick bipolar outflow sources
(e.g., HL Tau, L1551 IRS5; Men'shchikov et al. 1999; White et al. 2000).
One can easily predict that at even longer wavelengths, where
optical depths for both absorption and scattering are smaller, the
star will become more visible, whereas the cavity and other "clumps''
will become fainter. The latter will completely vanish at some mid-IR
wavelengths leaving only one bright peak at the position of the star -
a mixture of the diluted direct stellar light with the radiation coming
from the hot innermost parts of the dense core.
In Figs. 14 and 15, our H- and K-band speckle
images of IRC
+10216 are compared to the model convolved
with a circular Gaussian PSF of 95mas (FWHM).
![]() |
Figure 14:
Comparison of the H-band model image with a 95mas resolution
( left panel) with our reconstructed speckle image of IRC |
| Open with DEXTER | |
![]() |
Figure 15:
Comparison of the K-band model image with a 95mas resolution
( left panel) with our speckle image of IRC |
| Open with DEXTER | |
![]() |
Figure 16:
Comparison of the model |
| Open with DEXTER | |
![]() |
Figure 17:
Normalized intensity profiles in the H band (through the peaks A and
B) from the model image in Fig. 14 compared to the observed
profiles from our speckle image of IRC |
| Open with DEXTER | |
![]() |
Figure 18:
Normalized intensity profiles in the K band (through the peaks A and
B) from the model image in Fig. 15 compared to the observed
profiles from our speckle image of IRC |
| Open with DEXTER | |
The radiation of the hot, dense dusty core clearly appears in the model
K image as a faint circular halo around the star
(Fig. 15). Note that the same halo is also present in our
speckle image, visible only on the east and north-east sides, although
its intensity level in the model is somewhat higher (Fig. 18).
The shape of the faint emission in the observed image appears
incompletely circular because of a patchy foreground extinction in the
envelope. Obvious asymmetries in the light distribution of the optical
0.8
m HST image and our speckle J-band image
(Figs. 12, 13), with respect to the symmetry
axis of the H, K images (PA
20
), are most
likely caused by the inhomogeneities of the dust density distribution.
In addition to the asymmetries present in the HST and J images of
IRC
+10216, two dark patches of extinction are most clearly visible in our
high-resolution
speckle image (Fig. 16).
Consistently with the observed color image, the model is shown for only
those points of the area, where intensities in both H and K images
are higher than 2% of the peak level. The (irregular) sharp edge of
the observed
image emphasizes the darker areas north and west of
the brightest peak; the same zones of enhanced extinction distort the
observed short-wavelength images.
The
color images in Fig. 16 nicely delineates and
strongly supports the axially-symmetric geometry of the dense core
adopted in our model (Fig. 2). The model displays
essentially the same color distribution as in the observed image. The
redder color is concentrated around the star (component B), whereas the
bright southern outflow cavity appears much bluer, as expected in a
bipolar nebula. If the star were at the position of the brightest peak
A as, e.g., Haniff & Buscher (1998) assumed, the reddest color would
only be located on one side, north of the star. That would be a highly
unusual situation, very difficult to understand.
Our model demonstrates that a bluer color of the brightest peak does not necessarily imply that we observe direct light of the
star. In optically thick, non-spherical (bipolar) environments, this
would more likely be the light coming from their optically thinner
regions or cavities.
![]() |
Figure 19: Model intensity profiles in the K band (as in Fig. 18) at maximum and minimum luminosities illustrate the phase variations in the near-IR images predicted by our model |
| Open with DEXTER | |
In Figs. 17 and 18, our model is compared to the
observations in a more quantitative way.
The model intensity profiles
are plotted in two directions, parallel (PA
20
)
and perpendicular (PA
110
)
to the projected
symmetry axis, as well as the observed intensity profiles extracted
from our H and K speckle images. Unconvolved intensity cuts through
the star and the southern cavity are also plotted to show the "true''
intensity distribution reconstructed by our modeling with a numerical
resolution of 4mas. One can easily recognize the (rectangular)
profile of the star below the fainter peak and the true shapes of the
intensity distributions which are otherwise buried under a much wider
PSF.
There are several characteristics of the observed profiles that are
important to note. First of all, the brighter peak is very compact,
similar to that produced by the direct stellar light. This means that
the cavities are rather narrow, comparable in size to stellar diameter.
Full opening angle
36
in our model produces
somewhat wider profiles at PA
110
,
so that we feel
that the real cavities in IRC
+10216 should be slightly narrower
(
30
). We adopted the wider cavity in the
model because otherwise the brightest peak A would be not as bright as
the observed one relative to the fainter peak B.
This small discrepancy
results most likely from a simplified density distribution in the
compact dense core (Figs. 1, 2), not
depending on the polar direction in the vicinity of the outflow
cavities. Another feature of the observed profiles is that the
separation of the peaks A and B is the same in both H and K images.
This implies that optical depths at the wavelengths must be comparable.
The intensity profiles are very similar to those derived from our
high-resolution speckle images of the Red Rectangle
(Men'shchikov et al. 1998). Bipolar geometry of the latter is
similar to our present model, except for significantly wider outflow
cavities (
70
vs.
36
). The
dense torus of the Red Rectangle is oriented almost edge-on
toward the observer, with a viewing angle
7
(relative to the midplane).
One may be tempted
to extrapolate that model to IRC
+10216 and interpret the bright components
A and B as the light from the southern and northern cavities,
respectively. This would imply that the star is between A and B and
that the viewing direction is also close to edge-on.
![]() |
Figure 20:
Normalized intensity profiles from the model images of IRC |
| Open with DEXTER | |
Although this interpretation might seem plausible, our modeling has
shown that the star cannot be located between the two peaks. The
central star in IRC
+10216 would be too luminous for this model to work.
A dusty core at a twice smaller distance from the star would be too
dense, too hot, and emit too much radiation to reproduce the observed
images. The location of the star between the peaks A and B can
definitely be ruled out.
In Fig. 19, we illustrate phase variations predicted by our
model in the near-IR images.
Plotted are the model intensity profiles
in K band at the phases of maximum and minimum of luminosity.
The effect of higher luminosity is to increase dust temperature
and, therefore, enhance dust emission from the inner parts of the
envelope. The outflow cavity becomes relatively brighter than the
star, whose direct light gets heavily diluted in the hot dust emission.
Another effect is that the distance between the star and the cavity
becomes by
10mas larger. This apparent periodic "motion''
is purely the effect of increased stellar luminosity in a bipolar dust
shell.
![]() |
Figure 21:
Normalized intensity profiles from the model images of IRC |
| Open with DEXTER | |
![]() |
Figure 22:
Normalized intensity profiles from the model images of
IRC |
| Open with DEXTER | |
In Fig. 20, we show the model intensity profiles in
J and K bands, which are compared to the profiles derived from
images of IRC
+10216 by Kastner & Weintraub (1994).
The model is
convolved with a circular Gaussian PSF of 2
(FWHM).
Consistently with what has been observed in the polarimetric imaging,
our model shows a very extended scattering envelope on spatial scales
of
2-20
from the star.
In Fig. 21, we show the model intensity profiles at
50
m and 100
m, which are compared to the slit scans
obtained by Lester et al. (1986).
The model is convolved with
circular Gaussian PSF of 11
5 and 22
9, respectively,
using the slit sizes reported by the observers
(
and
). The profiles along the symmetry axis
are shown (PA
20
), although the images are
essentially circular at long wavelengths.
The model intensity profile at 50
m agrees quite well with the
observations, whereas the 100
m intensity distribution in the
model seems to be more extended. Similar discrepancy has been
noted by Lester etal. (1986) between their measurements of the
almost unresolved source and the observations by Fazio et al. (1980)
of an extended envelope at 60
m. We do not have any definite
explanation of the differences; most likely, they are related
to different observational techniques.
While the unconvolved intensity
profile seems to be dominated by the unresolved peak from the inner
dense parts of the envelope (Fig. 21), low-level emission
from
10
makes significant contribution to
the convolved intensity profile.
In Fig. 22, the model intensity profiles at 10.7
m
and 1.3mm are compared to those obtained by Bloemhof et al. (1988)
and Groenewegen et al. (1997).
Constrained by the 1.3mm image, our
model of IRC
+10216 implies a flatter density profile at
200AU
3000AU than that in the outermost
envelope (Fig. 10). The dust density (and probably
,
too) was enhanced by a factor of
3 approximately
1000 years ago. This result is consistent with the density profiles
reconstructed by Fazio et al. (1980) and Groenewegen et al. (1997).
The 10.7
m model intensity profile agrees very well with the
observed profile when convolved with the empirical PSF of 0
68
given by Bloemhof et al. (1988).
At the same time, the unconvolved (true) intensity profile shows a bright core of
300 mas in radius (Fig. 22), in contrast to
the unconvolved intensity profile predicted by the model of
Ivezic & Elitzur (1996), which is dominated by direct stellar light.
The difference is not surprising if one recalls that their spherical
model is optically thin at 10.5
m, whereas our two-dimensional
model demonstrates that IRC
+10216 is optically thick (Fig. 6).
In Fig. 23, our model is compared to the recent lunar
occultation observations at 10.5
m by Stecklum et al. (1999)
with an estimated resolution of
50mas.
The eastern and
western branches of the observed (reconstructed) intensity profile were
averaged and mirrored in the figure. Comparing the model with the lunar
occultation measurements, one should bear in mind that the profile
published by Stecklum et al. was a preliminary reconstruction. We used
it in our modeling because the authors were confident that its main
characteristics are real and because it supplies additional constraints
to the model.
Intensity profiles deconvolved from lunar occultation observations are
integrated in the direction along the lunar limb. Thus, while the
resolution perpendicular to the limb may be as high as
10mas, all structural information along the limb is
essentially lost.
Therefore, one cannot expect lunar occultation
observations to resolve as fine structural details of an extended
object as by high-resolution observations with a true circular PSF of
10mas.
The concept of a one-dimensional "resolution'' for the integrated intensity profile is different from the standard concept of resolution and it may be quite misleading. Critically depending on the (unknown) real intensity distribution in the object under consideration, the corresponding true resolution of the lunar occultation data may be much lower. Almost all information about the immediate surroundings of the star is buried in the emission coming from more distant regions. This is the main reason why Stecklum et al. (1999) found no trace of the star with an expected angular diameter of 40mas in their lunar occultation data.
Another problem is that the occultation observations were carried out
very close to the strong absorption resonance of SiC dust at
10.75
m which is not very suitable wavelength for resolving the
star and the structure of the innermost parts of its circumstellar
envelope. Our model shows that optical depth of the envelope of IRC
+10216
containing the SiC grains at this wavelength is as high as in the
near-IR J and H bands (
;
Fig. 6). Thus,
the flat-topped intensity distribution is to be expected for the lunar
occultation observations of an extended optically thick envelope
around the carbon star at 10.5
m.
![]() |
Figure 23:
Normalized intensity profiles from the model images of IRC |
| Open with DEXTER | |
Although we have compared our model to observations of IRC
+10216 in terms
of the SEDs, images, and intensity profiles, in this section we are
going to confront the model and observations also in terms of
visibilities. The two-dimensional Fourier transform of an intensity map
gives a much more detailed and sensitive measure of the intensity
distribution over all spatial frequencies than do convolved images
and intensity profiles. This would enable a more precise, quantitative
assessment of the accuracy of our model.
In Figs. 24-27, we compare the model with
available near-IR visibilities obtained by Mariotti et al. (1983),
Dyck et al. (1987), Ridgway & Keady (1988),
Weigelt et al. (1998a), and Osterbart et al. (2000).
The model
visibility is plotted for only two orthogonal directions, parallel
(PA
20
)
and perpendicular
(PA
110
)
to the symmetry axis. To some extent,
comparisons with observations are ambiguous due to the variable nature
of IRC
+10216 that changes on a time scale of one year, due to both the
stellar pulsations and to non-periodic dynamic processes in its
environment.
To avoid the problem, our approach was to mainly fit our recent speckle visibility data (Weigelt et al. 1998a; Osterbart et al. 2000) which are coeval with the reconstructed images we modeled above (Sects. 4.5.1, 4.5.2). To give the reader a measure of differences between the observations obtained in different epochs, we also plotted older visibilities obtained by Dyck et al. (1987) and Ridgway & Keady (1988). Some visibility data show apparent problems in their low-frequency range, where they should never exceed unity. For completeness, we show all the data sets which are useful at higher spatial frequencies and for an assessment of the overall uncertainties of the observational material.
Overall, our model fits the near-IR visibilities reasonably well,
whereas in the L and N bands it deviates noticeably from available
measurements. The short-wavelength J-band visibility
(Fig. 24) is more difficult to fit, because of the large
role of scattering that strongly depends on how realistic the basic
model geometry is and how well we know the spatial distribution and
properties of dust grains.
![]() |
Figure 24:
Model visibilities of IRC |
| Open with DEXTER | |
![]() |
Figure 25:
Model visibilities of IRC |
| Open with DEXTER | |
![]() |
Figure 26:
Model visibilities of IRC |
| Open with DEXTER | |
![]() |
Figure 27:
Model visibilities of IRC |
| Open with DEXTER | |
In general, the model visibilities in H and K bands are in much
better quantitative agreement with our speckle data. There are some
deviations from the measured visibilities, which are directly related
to the departures of the model intensity profiles from the observed
brightness distribution (Figs. 17, 18).
In
particular, we were unable to better reproduce the small width of the
brightest outflow cavity. The model intensity profiles are noticeably
wider at PA
110
,
resulting in lower intensities at
largest spatial frequencies (Figs. 24, 25). Some
of the deviations of the model visibilities from the observed ones are
caused by the presence of peaks C and D in our speckle images
(Osterbart et al. 2000), which do not exist in the model.
Also in L and N bands (Figs. 26, 27), our
model shows some departures from the visibilities measured by
Mariotti et al. (1983) and Ridgway & Keady (1988). Note, however,
that the measurements themselves differ from each other, too. We believe
that the main reason for the discrepancies is that the visibility
data for IRC
+10216 are too old to rely on.
Given the large non-periodic
variations of the object over the last years, it is not surprising that
our recent speckle images are fundamentally incomparable to much
older observations. Thus, our model which has been designed to
reconstruct the present structure and properties of IRC
+10216,
may not match the old data very well.
We would like to emphasize that the mixture of data from different
epochs is a real problem that highly complicates any detailed modeling
and interpretation of IRC
+10216 on subarcsecond scales. Stationary modeling
requires coeval observational data; one cannot get meaningful
constraints on the model if the time scale for the object's changes is
smaller than the time interval over which the observations were obtained.
One solution to the problem would be to explicitly include time into
the models.
Sufficiently detailed and realistic time-dependent modeling
of individual objects is, however, out of question in the foreseeable
future at the present state of the theory, observations, and numerical
modeling.
The star is in a very advanced stage of its AGB evolution, as indicated
by its long pulsational period (650 days), high mass-loss rate, and
carbon-rich chemistry of its dusty envelope. Based on the isotopic
ratios of C, N, and O in the envelope, the star's initial mass
can be estimated to be close to 4
due to moderate
hot bottom burning (Guelin et al. 1995).
This is in line with a mass
estimate based on stellar luminosity that gives
4-4.5
(for
170pc, Weigelt et al. 1998a).
Recently, Kahane et al. (2000) presented observational results on a
chlorine isotopic abundance ratio that is sensitive to the s-process
nucleosynthesis. Combining these observations with evolutionary models
and s-process calculations, the authors derived
3
.
Current stellar evolution models do not
predict hot bottom burning to take place for this mass range
(although the lithium enrichment of Galactic carbon stars of
rather low luminosities seems to indicate that additional mixing
processes may be present, Abia & Isern 1997). Given the observed CNO
isotopic abundance ratios, this suggests that IRC
+10216 had a low-mass
progenitor (
2
). For instance, only then
the 12C/13C ratio appears to be in agreement with C/O
1
see Kahane et al. 2000.
In the model of IRC
+10216 presented in this study, we adopted a total mass
of the envelope of 3.0
.
Assuming a present-day stellar core
mass of 0.7-0.8
,
the model implies an initial mass of
3.7-3.8
.
We would like to stress here
again that the model predicts only the dust mass
of
the envelope, not its total mass M. In contrast to other dust
radiative transfer models adopting a specific dust-to-gas mass ratio
to convert dust mass to gas mass, we prefer to fix
3.0
based on stellar evolution models for IRC
+10216.
Then our model predicts the values of
in
both the outer and inner parts of the envelope
(Table 2).
It is important to note that the model results presented in this paper
are independent of the adopted values of
and M for IRC
+10216,
provided that simple scaling relations are applied to the following
parameters:
Independently of the actual initial masss of this object, the latter
appears to be at a very advanced evolutionary phase. Given the very
high mass-loss rate derived in our modeling, we can expect only a few
thermal pulses to occur until the AGB evolution of IRC
+10216 is terminated.
Recent high-resolution imaging of IRC
+10216 with a resolution better than
100mas revealed its remarkably non-spherical, "clumpy'' appearance
on subarcsecond scales (Weigelt et al. 1998a). In our previous
paper, the observations were interpreted in terms of a bipolar,
dynamically evolving dusty envelope around the carbon star being at the
very end of its AGB evolution (Osterbart et al. 2000).
In this study, we constructed the first two-dimensional radiative
transfer model for IRC
+10216, which describes in detail many aspects of
its present-day structure. Reconstructing the density distribution
throughout the huge, parsec-sized envelope, the model also gives insights
into the past AGB evolution of the star. Quantitatively explaining all
relevant manifestations of circumstellar dust grains in a
self-consistent, extensive exploration of a very large parameter space
(Sect. 4.1), the model gives a reliable, coherent picture of
the object.
STAR'S LOCATION. An important and firm result of the modeling is
that the brightest component A, visible in the HST and our speckle
interferometry images of IRC
+10216 (Sects. 4.5.1,
4.5.2), does not contain direct light from the central
star. In contrast to an intuitive picture adopted in all previous
works, the star is actually located at the projected position of the
fainter component B. The brightest peak is only the light emitted
and scattered by a narrow bipolar outflow cavity which is tilted toward
us by 40
.
Fainter components C and D appear most likely due to
density deviations around the outflow cavities from axial symmetry on
smaller scales (Sect. 3.2).
STELLAR PARAMETERS. For the adopted distance of 130pc,
the stellar luminosity varies from 13000 to 5200
between the maximum and minimum brightness of IRC
+10216
(Sect. 3.4.1). We assumed that the effective temperature of
the central star is changing from 2800 to 2500K between the two
phases (Sect. 3.4.2). Being somewhat higher than the
temperature usually adopted in radiative transfer calculations, it
agrees better with stellar evolution models. The stellar radius varies
in a relatively narrow range, from 500 to 390
.
During the last 1000 years, this star has experienced at least two
episodes of very high mass loss with
![]()
yr-1(Sect. 4.4).
DENSITY DISTRIBUTION. The density distribution of dust cannot be described everywhere by a simple power law
characteristic for a stationary spherical
mass loss. The density profile found in our modeling
(Sect. 4.3) results most likely from a complex interplay
between stellar pulsations, changing mass-loss rate, and radiative
acceleration of dust and gas in the innermost parts of the envelope.
All these processes are changing the structure of the dense
subarcsecond region of the envelope on a time scale of years. Polar
outflow cavities in the axially-symmetric dense shell cause the
observed "clumpy'' appearance of IRC
+10216 in recent highest-resolution
images. The huge envelope of 3pc in radius has a total mass of
3
,
which corresponds to a dust-to-gas mass ratio of 0.0039
(Table 2). The mass is consistent with an initial mass
of the central star of
4
and the present-day core
mass of 0.7
(Sect. 5).
DUST COMPOSITION. In agreement with theoretical expectations, but
in contrast to all previous fits of the object's SED, our model
predicts that both the radial distribution and composition of dust
around IRC
+10216 are strongly inhomogeneous (Sect. 3.3.6).
The inner dust boundary of the envelope, a subject of considerable
debate over decades, is located very close to or even inside stellar
photosphere, where the newly formed SiC grains have temperatures of
2000K. Most of the carbonaceous dust
nucleates further away from the star (at 30AU), whereas the most
volatile components condense at even larger distances (at 45AU).
Abundances and size distribution of dust grains in our model depend
on the radial distance from the star (Table 2).
BROAD EMISSION BANDS. First detailed exploration of a large
parameter space of various grain models enabled us to conclude that it
is inhomogeneous conglomerate particles that are responsible for
the well-known, yet poorly explained 11.3
m and 27
m
(30
m) emission features. Our modeling strongly suggests that the
11.3
m feature is produced by [SiC,C] grains, unorganized
aggregates made of incompletely amorphous carbon with significant
graphitic content and silicon carbide (Sect. 3.3.4). The
27
m emission band, also known as a 30
m feature, is
perfectly reproduced by the core-mantle [SiC,C]+[Mg,Fe]S grains
(Sect. 3.3.5). Although it is absolutely clear that the
real situation in IRC
+10216 is more complex, our dust model
(Sect. 3.3.6) is the simplest approximation that
consistently and quantitatively explains dust emission observed in this
object. The same set of solid materials can be used to successfully
model a family of broad emission bands observed in many other
carbon stars, with peaks in the 10.3-12.6
m and 25-37
m
wavelength regions.
IRC+10216 AND CRL2688. We would like to draw several
parallels between the object studied in this work and the
proto-planetary nebula CRL2688, also known as the
Egg Nebula (e.g., Sahai et al. 1998). Both objects have
distinct dense, optically thick dusty circumstellar cores with
biconical cavities presumably produced by high-velocity collimated
outflows. The opening angle of the holes in CRL2688 is
30
,
almost the same as in our model of
IRC
+10216 (cf. Sect. 4.5.2). Appearances of the two objects
noticeably differ, however, primarily because they are inclined at
different angles toward the observer (almost edge-on for
CRL2688 vs.
40
for
IRC
+10216). In both objects, shell-like density enhancements are observed
in scattered light as incomplete arcs, which correspond to periodic
increases of similarly high mass-loss rates
(
![]()
yr-1) by a factor of 2-3. One can
possibly identify the recent episode of a very high mass loss in
IRC
+10216 (Sect. 4.4) with the formation of one of such shells.
CRL2688 is in a significantly more advanced stage of a rapid
transition into the planetary nebulae phase than IRC
+10216. The above
brief (and incomplete) comparison suggests that similar physical
processes are operating within this evolutionary sequence.
SYMMETRY, CLOUDS, AND CAVITIES. We should stress that the widely used basic assumption of spherical symmetry appears to have a very limited applicability, as we "turn on'' higher and higher angular resolutions. Furthermore, our model demonstrated that one should be very cautious while interpreting asymmetric optically thick dusty environments on the basis of common sense, instead of accurate quantitative modeling. Extending present results to other non-spherical objects, we believe that interpretations of observations in terms of dust clouds around mass-losing stars may be misleading. We expect that in many cases such "clouds'' will turn out to actually be outflow cavities or other types of inhomogeneities in the density distributions of optically thick circumstellar shells.
CONCLUDING REMARKS. IRC
+10216 is the most difficult object we took
for modeling, primarily because of its variability and enormous amounts
of observational material that should be quantitatively explained by a
realistic model. Having constructed the model that fits a wide variety
of observational constraints, we are confident that the general
structure and properties of IRC
+10216 obtained in this study are indeed
good approximations to the extremely complex reality. We should make it
absolutely clear, however, that no model can provide ultimate answers.
No matter how sophisticated, any model would ignore many important
aspects of nature. Having explained all the observations of dust
continuum self-consistently, our detailed model can serve as
just a first step to a more complete and reliable understanding of
IRC
+10216 and evolved AGB stars in general.
Acknowledgements
We would like to thank Rita Loidl for computations of several model atmospheres used in our study and Volker Ossenkopf for discussions on properties of dust grains. The HST image of IRC+10216 has been retrieved from the Hubble Data Archive operated at the STScI, Baltimore, USA. Extensive radiative transfer modeling described in this paper has benefited a lot from the excellent computer network of Stockholm Observatory, in particular of its Infrared Group. Financial support of the latter is highly appreciated. We would like to thank Pawel Artymowicz for permission to use his Hydra cluster of workstations. We are grateful to the referee, Claudine Kahane, whose comments stimulated our work on further improvements of clarity and content of several sections of this paper.
Geometry of our model (Fig. 1) implies that we look deep
into the bright cavity excavated in the dense subarcsecond core of
IRC
+10216. It is the far side of the outflow cavity, which emits and
scatters most of the short-wavelength radiation we receive in the
brightest peak A. Our model does not incorporate the fainter components
C and D, which we believe are optically thinner spots due to column
density fluctuations inside the dense core. We have, therefore, no
specific information on their relevant physical parameters. In this
section, we consider their apparent velocities in the plane of sky
(
14kms-1,
5kms-1), measured
recently by 2000 over 5 epochs. Simple geometrical
estimates below demonstrate that deprojected radial velocities of
all the components A, C, and D are equal to the general expansion
velocity
15kms-1 of the envelope.
From the detailed modeling of IRC
+10216 reported in this paper, we know
the viewing angle
40
.
The radius-vector
from B to A makes an angle
with
the plane of sky, where
36
is
the opening angle of the cavity (radiation of A is emitted on the far
side of the cone). The deprojected radial velocity of the brightest
component is readily available:
![]() |
(A.1) |
From our K-band speckle images
(Figs. 1f-j, Osterbart et al. 2000), the projected distances
,
,
and
between B and each of the
three components can be easily measured. Since the distances to C and D
are very similar, we can average them and denote as
.
Averaging also over the images, we find a ratio of
1.56.
Considering the line of sight passing through component A
(Fig. 1), one can write
We used all published broad-band fluxes in the modeling, taking into account beam sizes of the corresponding instruments (Becklin et al. 1969; Strecker & Ney 1974; Campbell et al. 1976; Schwartz & Spencer 1977; Shivanandan et al. 1977; Elias et al. 1978; Fazio et al. 1980; Phillips et al. 1982; Spergel et al. 1983; Sopka et al. 1985; Rengarajan et al. 1985; Goebel & Moseley 1985; Le Bertre 1987,1988; Sahai et al. 1989; Woody et al. 1989; Drake et al. 1991; Harvey et al. 1991; Walmsley et al. 1991; Le Bertre 1992; Altenhoff et al. 1994; Knapp et al. 1995; van der Veen et al. 1995; Groenewegen et al. 1997; Osterbart et al. 2000).
Whenever possible, we preferred to rely on existing spectrometry or spectrophotometry data (Becklin et al. 1969; Miller 1970; Merrill & Stein 1976; Witteborn et al. 1980; Forrest et al. 1981; Herter et al. 1982; Goebel & Moseley 1985; Olnon et al. 1986; Le Bertre 1988; Speck et al. 1997; Yamamura et al. 1998), rather than on the broad-band fluxes, because the spectra are coeval and they consistently cover much wider wavelength intervals. Calibration of the IRAS low-resolution spectrum (see Olnon et al. 1986) was corrected as prescribed by Cohen et al. (1992).
Unfortunately, there are only a few near-IR fluxes measured at phases
close to
=0.56. In order to fill the gap and better
visualize the SED (Figs. 7-9),
we chose to scale down intermediate-phase spectrophotometry in the
intervals 1.8-8.4
m
(
0.38, Witteborn et al. 1980) and
16-36
m (
0.12, Forrest et al. 1981).
The scaling factors of 0.74 and 0.53, respectively, fitted these two
segments to the only available spectrum of IRC
+10216 at
=0.56
published by Speck et al. (1997) and to several broad-band fluxes in
the 2-12
m wavelength range (
=0.5) measured by
Le Bertre (1992). To better define the SED shape at
=0.24, we also scaled (by a factor of 0.575) spectra in the
1.5-2.4
m range from Beckli et al. (1969) and
Merrill & Stein (1976), which were obtained close to the phase of
maximum luminosity.
Important constraints for our modeling of IRC
+10216 are given by
high-resolution optical and near-IR images (Weigelt et al. 1998a; Haniff & Buscher 1998; Osterbart et al. 2000), as well as by
longer-wavelengths scans and images (Lester et al. 1986; Bloemhof et al. 1988; Groenewegen et al. 1997; Stecklum et al. 1999). Valuable
spatial information has been provided by near-IR visibilities
(Mariotti et al. 1983; Dyck et al. 1987; Ridgway & Keady 1988; Weigelt et al. 1998a; Osterbart et al. 2000).