A&A 392, 1025-1029 (2002)
DOI: 10.1051/0004-6361:20020992
B. Stecklum1 - B. Brandl2 - Th. Henning3 - I. Pascucci3 - T. L. Hayward4 - J. C. Wilson2
1 - Thüringer Landessternwarte Tautenburg, Sternwarte 5,
07778 Tautenburg, Germany
2 -
Center for Radiophysics & Space Research, Cornell University, Ithaca, NY 14853, USA
3 -
Max-Planck-Institut für Astronomie, Königstuhl 17, 69117 Heidelberg, Germany
4 -
Gemini Observatory, 670 N. A'ohoku Place, Hilo, HI 96720, USA
Received 29 April 2002 / Accepted 3 July 2002
Abstract
We present results of our diffraction-limited mid-infrared imaging of the massive
star-forming
region W3(OH) with SpectroCam-10 on the 5-m Hale telescope at wavelengths of 8.8,
11.7, and 17.9
m. The thermal emission from heated dust grains associated
with the ultracompact H II region W3(OH) is resolved and has a spatial extent
of
2
in the N band. We did not detect the hot core source W3(H2O)
which implies the presence of at least 12 mag of
extinction at 11.7
m towards this source. These results together with
other data were used to constrain the properties of W3(OH)
and W3(H2O) and their envelopes by modelling the thermal dust emission.
Key words: stars: formation, circumstellar matter - ISM: dust, extinction - infrared: stars
Conclusions concerning the heating and the stellar content of hot cores have to be based on the knowledge of their luminosity. This quantity is difficult to estimate since the immediate neighbourhood of UCH IIs often leads to source confusion, especially in the far-infrared (FIR) range where these objects emit most of their energy and the angular resolution of spaceborn observations is as yet poor. Radio interferometry at mm/submm wavelengths allows to separate the dust continuum emission of the hot core from the free-free radiation of the adjacent UCH II. Such measurements were used to constrain models of hot cores (Osorio et al. 1999). High-resolution ground-based MIR observations, on the other hand, provide information on the spectral energy distribution (SED) shortward of the peak flux. A corresponding study of the IRc2 source in the Orion BN/KL complex (Gezari et al. 1998) illustrates their importance. More recently, De Buizer et al. (2002) were able to detect MIR emission from the hot core G29.96-0.02 with a morphology similar to that of the warm ammonia. We performed high resolution MIR imaging of hot cores, including W3(H2O) and the neighbouring UCH II W3(OH), in order to measure their flux densities or to provide at least upper limits. While results for G10.47+0.03 will be the subject of a forthcoming paper (Pascucci et al., in prep.), we present here our findings for W3(H2O) and the UCH II W3(OH).
The UCH II W3(OH) is very well-studied in the radio domain by continuum and molecular line
observations. It is located at the distance of
2.2 kpc (Humphreys 1978) and harbours numerous OH masers.
The hot core W3(H2O), also known
as Turner-Welch object (TW, Turner & Welch 1984), is situated
6
east
of W3(OH).
This enigmatic source shows an outflow traced by the
proper motion of H2O masers (Alcolea et al. 1992)
and is associated with a double-sided radio continuum jet, presumably of synchrotron nature
(Reid et al. 1995). Recent interferometric imaging at 220 GHz by Wyrowski et al. (1999) revealed
another
source in the immediate neighbourhood of W3(H2O), suggesting that the
region harbours a cluster of protostars.
The thermal infrared emission from W3(OH) has been studied by Keto et al. (1992)
using one of the first MIR array cameras (Arens et al. 1987).
Keto et al. claimed the detection of W3(H2O) at the wavelength of 12.2
m
with a flux density of
mJy.
W3(H2O) and W3(OH) were the subject of a continuum and molecular line study of
van der Tak et al. (2000). Since their results are based on single-dish
data which do not resolve the two objects, they cannot be directly compared to
our model presented below.
The observations were performed using SpectroCam-10, the Cornell-built 8-13
m
spectrograph/camera (Hayward et al. 1993) on the 5-m Hale
telescope
. SpectroCam's detector is a
Rockwell 128
128 Si:As BIB array. In camera mode, the pixel scale is
0
25 with a circular field of view of 16
.
We applied filters with central wavelengths and bandwidths (in parentheses) of
8.8 (1.0), 11.7 (1.0), and 17.9 (0.5)
m.
The imaging observations
were performed on 1998 December 27th using the common chopping/nodding technique
with a chopper throw of 20
in north-south direction. The wavelet filtering
algorithm of Pantin & Starck (1996) was applied to the images. This
algorithm is useful for recovering faint extended emission otherwise hidden in the noise.
The high dynamic range of the individual frames allowed the application of a
shift-and-add procedure which includes resampling,
yielding a final pixel scale of 0
125. To enlarge our field of view, we observed
two positions at 11.7
m, the first centered on W3(OH) and the second offset to the
east by 10
.
Lastly, the frames were mosaicked.
The astrometry is based on the radio position of W3(OH) which is assumed to coincide with the peak of the infrared emission.
The flux calibration was performed using
Tau as reference which was measured
at about the same airmass (1.2) as the target. For this purpose, the photometric
zero points from Cohen et al. (1992) and the photometry from Cohen et al.
(1995) for
Tau were used. The observations were performed during
photometric conditions, with an internal photometric error of less than 2% as estimated
from the flux variation of the standard star. The 3
sensitivities (mJy/beam)
for the detection of point sources
in the final
images are as follows: 4 (8.8
m), 6 (11.7
m), and 93 (17.9
m).
The prime results of our observations are contained in Fig. 1 which shows
the 11.7
m image together with the 8.4 GHz radio continuum contours from Wilner at al.
(1999, beam size 0
2).
The two infrared sources in Fig. 1 correspond to W3(OH) and the cometary
UCH II situated north-east of it.
A comparison with
Tau
(Fig. 1 insert) shows that W3(OH) is spatially well resolved in our diffraction-limited
11.7
m image (beam size 0
6).
The lowest contour line of the infrared emission
represents the 3
detection limit. Clearly, the flux from W3(H2O)
is below our sensitivity limit. This result is in contradiction to the infrared
detection of W3(H2O) claimed by Keto et al. (1992).
We note that their conclusion is doubtful since the emission
they associate with W3(H2O) peaks only 4
instead of 6
east of W3(OH)
(see their Fig. 1). Furthermore, their total flux of 45
10 mJy
contradicts with the fact that the emission well exceeds their lowest contour
level of 100 mJy/
.
Thus, we conclude that they did not detect W3(H2O)
as well, and were confused by the north-eastern cometary UCH II.
From Fig. 1 it is obvious that there is a good overall correspondence between the MIR and the 8.4 GHz radio continuum emission. However, there are certain features which are different in both maps. The north-eastern trail from W3(OH) is more confined in the radio continuum and only marginally indicated by the infrared contours. The peak of the radio emission from the north-eastern UCH II is closer towards W3(OH) than its infrared maximum. This is presumably caused by the extinction of a dust lane stretching from W3(H2O) to the north-west which can be seen in the C17O(1-0) map of Wyrowski et al. (1997).
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Figure 1:
11.7 |
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For the northeastern UCH II the following fluxes (within a 3
aperture) were derived at the three wavelengths: 0.3, 0.6, and 6.1 Jy,
respectively.
| Wavelength | Peak flux | Total flux | FWHM |
| [ |
[Jy]/ |
[Jy] | [
|
| 8.8 | 2.6 | 6.5 | 1.96 |
| 11.7 | 7.7 | 22.4 | 2.08 |
| 17.9 | 19.5 | 93.0 | 2.88 |
| IRAS-LRS | Total flux | MSX | Total flux |
| [ |
[Jy] | [ |
[Jy] |
| 8.8 | 24.9 | 8.28 | 11.1 |
| 11.7 | 24.1 | 12.13 | 36.7 |
| 17.9 | 89.1 | 14.65 | 77.1 |
| 21.41 | 332.6 |
The FWHM of the MIR emission from W3(OH) was derived from Gaussian fits, taking the
size of the diffraction-limited beam into account. The sizes and flux densities
of W3(OH) are listed in Table 1. The fluxes are based on an
aperture of 4
diameter.
The extent of the MIR emission originating from the thermal emission of heated dust
grains exceeds that of the
8.4 GHz radio continuum (FWHM 1
52), indicating that
the warm dust is more extended than the ionized gas. The variation
of the angular size in dependence on wavelength can be approximated as
FWHM(
)
and results from the decline
of the temperature with increasing distance from the heating star(s).
The comparison of our flux densities of W3(OH) with other estimates allows conclusions on the influence of different beam sizes. For this purpose, we retrieved the IRAS-LRS spectrum, identified W3(OH) in the MSX point source catalog (Egan et al. 1999), and retrieved an ISO-LWS spectrum from the data archive.
The LRS spectrum was integrated according to the applied passbands. It is obvious
that the 8.8
m fluxes given in Table 1 considerably exceed our value. This
can be explained by ubiquitous emission attributed to Polycyclic Aromatic Hydrocarbons
(PAHs) surrounding the UCH II which strongly contributes to the flux in the large
apertures of IRAS and MSX. Pronounced 7.7 and 8.6
m PAH bands can be
misleading in ground-based derivations of the optical
depth of the 9.7
m silicate feature (e.g., Roelfsema et al. 1996).
Our attempt to detect W3(H2O) in the IR was stimulated by the presence of an outflow. Generally, IR emission can escape in outflow lobes primarily due to scattering (e.g., Fischer et al. 1996). An example is NGC6334 I(N), a presumed high-mass Class 0 object, for which Sandell (Sandell 2001) rendered the detection of IR emission impossible because of the extremely high extinction derived from mm/submm maps. However, this source is associated with NIR emission (Tapia et al. 1996; Megeath & Tieftrunk 1999) obviously originating from the blue-shifted lobe of its outflow.
The flux densities from W3(H2O) in the absence of any intervening absorbing matter
can be estimated from the temperature map
given by Wyrowski et al. (1997). The expected peak surface
brightness amounts to 2170 Jy/
at 11.7
m. Together with
our 3
sensitivity, this yields a lower limit to the extinction at this
wavelength of 12 mag. Our failure to detect this source is consistent with the
high molecular hydrogen column densities of 1...
cm-2inferred from molecular line and continuum investigations (Turner & Welch 1984;
Wyrowski et al. 1997). It suggests that the molecular outflow of
W3(H2O) is very young, i.e. did not fully penetrate the hot core yet, and,
in addition, might be in the plane of the sky. In fact,
Fig. 1 from Wyrowski et al. (1999) shows that the jet is confined
to the region of the hot core. The moderate expansion velocity of the H2O masers
of 20 km s-1 (Alcolea et al. 1992) implies
a dynamical timescale of only 500 yr which is consistent with the upper limit
on proper motions of the radio jet of 150 km s-1 (Wilner et al. 1999).
These velocities are low compared to those of thermal radio jets (Anglada 1996)
and indicate that the outflow is presumably slowed-down by the high-density environment.
One of the questions concerning W3(OH) and W3(H2O) is related to their individual luminosities which directly translates to the nature of the internal heating sources. Although it is reasonable to assume that the internal heating is due to stars of intermediate or high mass, no direct confirmation of their presence exists. The luminosity might also, at least partly, result from accretion. The high column densities toward W3(H2O) render it very difficult to figure out whether the mass accretion is due to infall from a circumstellar disk or stellar mergers like in the scenario of Bonnell et al. (1998). The high optical depths will lead to a thermalization of the released energy irrespective of the accretion mechanism.
The derivation of the individual luminosities has to be based
on the decomposition of the SED. While our measurements provide
constraints for the MIR, the lack of spatial resolution
in the FIR does not permit to separate both components.
An upper limit of
1800 Jy on the 50
m flux of W3(H2O) has
been established by Campbell et al. (1989) from KAO scans.
In the mm/submm range, aperture
synthesis measurements
show that the 1.3 mm emission from W3(H2O) is due to dust radiation while
free-free emission dominates the flux of W3(OH) at this wavelength (Wyrowski et al.
1999). The ISO-LWS spectrum
between 42 and 140
m
can well be fitted by a modified black-body (35 K and
).
The association of W3(H2O) with cold dust suggests that the MIR/FIR excess
in the ISO spectrum for
is presumably due to the hot core.
We modelled the thermal dust radiation from W3(OH) and W3(H2O) in order to figure
out how much the hot core contributes to the FIR excess seen in the ISO-LWS spectrum and
which sensitivities are required for its detection in the MIR.
The input SED is based on fluxes coming from this work, from the
MSX point source catalogue at 21.4
m (see Table 1), from the IRAS-LSR
and ISO-LWS spectra, and from
Wyrowski et al. (1997) as well as Wilner et al. (1995) for the mm
wavelengths.
To solve the radiative transfer problem we used the 1D-code of Manske & Henning
(1998)
assuming spherically symmetric shells like in previous works.
As for the dust composition, we use graphite, silicate, and iron with optical
constants taken from Dorschner et al. (1995) and Draine & Lee (1984)
together with a
MRN-type size distribution (Mathis et al. 1977).
The model parameters and the related references are given in Table 2: here
L* is the stellar luminosity,
and
are
the inner and the outer radius of the envelope, and
is the dust mass.
We underline that the inner radius of the dust shell of W3(OH) coincides with the outer
radius of the UCH II while for the hot core,
is derived from the dust
sublimation temperature (
1000 K).
To model the W3(H2O) SED we follow Osorio et al. (1999) in
adding an accretion luminosity of
to the stellar luminosity
and a free-fall density shell.
For W3(OH) the density profile that better fits our observations is Gaussian
and yields an almost constant density distribution till
20 000 AU. The resulting opacities at the mm wavelengths vary as
.
Figure 2 shows the individual SEDs as well as their superposition.
Our model produces the following FWHMs at the observed wavelengths: 1
6 at 8.8
m,
2
0 at 11.7
m and 3
1 at 17.9
m. They are
quite in agreement with those given in Table 1 which supports the view that
the parameters of the radiative transfer model are representative for the actual
conditions.
From the SED of W3(H2O) we conclude that deep observations in the Q band might be
able to detect the MIR emission from the hot core.
| Source | L* |
|
|
|
| [
|
[AU] | [AU] | [ |
|
| W3(OH) | 81 | 22702,3 | 57 0004 | 5.0 |
| W3(H2O) | 2.45,6 | 190 | 24 0005 | 3.07 |
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Figure 2: SEDs of the individual sources (W3(OH) - dotted line, W3(H2O) - dashed line) and of their sum (solid line). Asterisks with error bars indicate the measured flux densities. Diamonds represent the model fluxes for the observational beam sizes. Arrows mark the detection limits for W3(H2O). |
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Acknowledgements
We thank S. Rinehart for assistance during the observations and D. Wilner for providing the 8.4 GHz VLA map. This work was supported by the Deutsche Forschungsgemeinschaft grant Ste 605/18-1.