A&A 414, 299-315 (2004)
DOI: 10.1051/0004-6361:20031623
F. Fontani 1 - R. Cesaroni 2 - L. Testi 2 - C. M. Walmsley 2 - S. Molinari 3 - R. Neri 4 - D. Shepherd 5 - J. Brand 6 - F. Palla 2 - Q. Zhang 7
1 - Dipartimento di Astronomia e Fisica dello spazio, Largo E. Fermi 2,
50125 Firenze, Italy
2 -
INAF, Osservatorio Astrofisico di Arcetri, Largo E. Fermi 5,
50125 Firenze, Italy
3 -
IFSI, CNR, via Fosso del Cavaliere, 00133 Roma, Italy
4 -
Institut de Radio Astronomie Millimétrique, 300 rue de la Piscine,
38406 St. Martin d'Hères, France
5 -
National Radio Astronomy Observatory, PO Box O, Socorro, NM 87801, USA
6 -
Istituto di Radioastronomia, CNR, via Gobetti 101, 40129 Bologna,
Italy
7 -
Harvard Smithsonian Center for Astrophysics, 60 Garden Street,
Cambridge, MA 02138, USA
Received 11 June 2003 / Accepted 14 October 2003
Abstract
We present the results of a multi-line and continuum study
towards the source IRAS 23385+6053 performed with the IRAM-30 m telescope, the Plateau de Bure
Interferometer, the Very Large Array Interferometer and the James Clerk
Maxwell Telescope. We have obtained single-dish maps in the C18O (1-0),
C17O (1-0) and (2-1) rotational lines, interferometric maps in the
CH3C2H (13-12) line, NH3(1,1) and (2,2) inversion transitions, and single-pointing observations of the CH3C2H (6-5), (8-7) and (13-12) rotational
lines.
The new results confirm our earlier findings, namely that IRAS 23385+6053 is a good candidate high-mass protostellar object, precursor
of an ultracompact H II region.
The source is roughly composed of two regions: a
molecular core
pc in size, with a temperature of
40 K and
an H2 volume density of the order of 107 cm-3, and an extended halo
of diameter
0.4 pc, with an average kinetic temperature of
15 K and H2 volume density of the order of 105 cm-3. The
core temperature is much smaller than what is typically found in molecular
cores of the same diameter surrounding massive ZAMS stars.
From the continuum spectrum we deduce that the core luminosity is
between 150 and 1.6
,
and we believe that the upper
limit is near the "true'' source luminosity.
Moreover, by comparing the H2 volume density
obtained at different radii from the IRAS source, we find that the halo
has a density profile of the type
.
This suggests that the source is
gravitationally unstable. The latter hypothesis is also supported by
a low virial-to-gas mass ratio (
0.3).
Finally, we demonstrate that the temperature at the core surface
is consistent with a core luminosity of
and conclude
that we might be observing a protostar still accreting material
from its parental cloud, the mass of which is at present
.
Key words: stars: formation - radio lines: ISM - ISM: molecules - ISM: individual objects: IRAS 23385+6053
The study of massive stars (
)
and their formation
is important for a better understanding of the evolution and
morphology of the Galaxy. However, up to now most progress has been done in the
study of the formation of low-mass
stars (
). This is a consequence of the many observational
problems which
hinder the study of the high-mass star formation process: massive stars
are more distant than low-mass ones, interact more strongly with their
environment, have shorter evolutionary timescales and mainly form in
clusters. Neverthless, recently a major observational
effort has been made to identify the very earliest stages of their
evolution. Successful results have been obtained searching for high-density and
high-temperature tracers (e.g. NH3 or CH3CN) towards selected
targets associated with regions of massive star formation, such as
ultracompact H II regions (Cesaroni et al. 1994; Olmi et al. 1996; Cesaroni et al. 1998),
H2O masers (Codella et al. 1997; Plume et al. 1997; Beuther et al. 2002b),
and IRAS sources (Molinari et al. 1996; Beuther et al. 2002a).
Probably the most relevant finding of these studies is the detection of
hot (
100 K), dense (
107 cm-3), molecular cores where high-mass
stars have recently formed. It is believed that such "hot cores''
(HCs, hereafter) represent the natal environment of O-B stars.
The next step in the search for very young massive stars is the detection of a genuine example of massive protostar. Molinari et al. (1998b) suggested that the source IRAS 23385+6053 might be such an object.
IRAS 23385+6053 is one of a sample of IRAS sources selected in a long-standing project as a likely candidate massive protostar. The selection criteria used in this project are based on the IRAS colours (Palla et al. 1991) and are aimed at identifying luminous (and hence likely massive) stellar objects in the earliest stages of their evolution. Observations of molecular tracers such as H2O (Palla et al. 1991) and NH3 (Molinari et al. 1996) have proven these objects to be associated with dense molecular gas. Additional observations in the continuum with the James Clerk Maxwell Telescope (JCMT, Molinari et al. 2000) and the Very Large Array (VLA) (Molinari et al. 1998a) have confirmed that a well defined sub-sample of these sources is embedded in dense dusty clumps (detected at mm and sub-mm wavelengths), and do not present any free-free emission, i.e. are undetected at centimeter wavelengths down to levels below that expected on the basis of their luminosity. The latter finding suggests that, although luminous (i.e. massive), the objects embedded in the clumps are still too young to develop an H II region. Such a sample contains excellent targets to search for massive protostars.
Recently, Brand et al. (2001) have performed a single-dish multi-line study mapping a small number of these candidates in various molecular transitions, finding that they are associated with clumps that are larger, cooler, more massive and less turbulent than those associated with ultracompact H II regions.
One of these sources, IRAS 23385+6053 (at a kinematic distance of 4.9 kpc), was
observed in more detail at different angular resolutions
with the OVRO interferometer (Molinari et al. 1998b, 2002)
and the VLA (Molinari et al. 2002).
This object has also been observed with ISOCAM at 7 and 15
m.
The main findings of these first studies are the following:
Also, Molinari et al. (2002) discovered two extended H II regions with the VLA at 3.6 cm which, however, do not coincide with I23385; rather they seem to overlap with a cluster of infrared sources detected with ISOCAM that surrounds the molecular peak. The infrared emission is coincident with a cluster of stars in near-infrared images (Molinari, priv. comm.). In this work, we discuss whether I23385 is a newly-born B0 star just arrived on the ZAMS or if it is a massive protostar still in the main accretion phase. For this purpose, the question we must answer is whether I23385 derives its luminosity primarly from hydrogen burning or from accretion. We believe that understanding the nature of I23385 can be improved by examining the physical parameters of the core, in particular by measuring the temperature of the associated core. In fact, in low-mass objects the temperature seems to be lower in the earlier evolutionary stages (Myers & Ladd 1993). By analogy, if high-mass ZAMS stars are found in "hot cores'', then high-mass protostars might lie inside colder cores. Furthermore, a detailed picture of the source, from small to large spatial scales, should be very useful to our purposes. We present here the results obtained from observations of the C18O and C17O (1-0), the C17O (2-1) and the CH3C2H (6-5), (8-7) and (13-12) lines using the IRAM-30 m telescope and the Plateau de Bure Interferometer (PdBI). We also mapped the NH3(1,1) and (2,2) inversion lines with the VLA. In Sect. 2 we will describe the observations; in Sects. 3 and 4 we will present the observational results and derive the physical parameters of the source, respectively; in Sect. 5 we will discuss these results, and finally we will draw our conclusions in Sect. 6.
The molecular transitions observed with the IRAM-30 m telescope
are listed in Table 1: here, we also give the frequencies, the half power
beam width of the telescope, the total bandwidth used and the spectral
resolution. The main beam brightness temperature,
,
and the flux density,
,
are related by the expression
.
Table 1: Transitions observed with the IRAM-30 m telescope and the Plateau de Bure interferometer.
C18O and C17O data were obtained on September 5, 2000. We simultaneously
used
two 3 mm receivers centered at the frequencies of the C18O (1-0) and C17O (1-0), and two 1.3 mm receiver both centered at the frequency of the C17O (2-1) line to optimize the signal-to-noise ratio. For every
line, three 3
3 maps with grid spacings 6, 8 and 10
and three
5
5 point maps with the same grid spacing were made. All maps are
centered at
54
5,
28
10: this position corresponds to
the sub-mm
peak detected by Molinari et al. (2000). Map sampling allows us to
cover a region
40
in size. Pointing and receiver
alignment were regularly checked, and they were found to be
accurate to within 2
.
The data were calibrated with the "chopper wheel''
technique (see Kutner & Ulich 1981).
The integration time was 2 min per point in "wobbler-switching''
mode, namely a nutating secondary reflector with a beam-throw
of 240
in azimuth and a phase duration of 2 s.
The system temperature was 250 K at the frequency of the C17O (1-0)
and C18O (1-0) lines, and it was
1000 K in the C17O (2-1) line.
CH3C2H data were obtained on August 12, 1999. We simultaneously
observed the (6-5), (8-7) and (13-12) rotational transitions in the
3 mm, 2 mm and 1.3 mm bands respectively. Only single-pointing observations
were made.
The data have been calibrated using the "chopper wheel'' technique, and the
observations were performed using the "wobbler-switching'' mode.
The system temperature was 120 K at 3 mm,
260 K at 2 mm and
350 K at 1.3 mm.
An 850 m continuum image was taken on October 16 1998 with SCUBA at the
JCMT (Holland et al. 1998) towards the postion of the core
I23385. The standard
64-points jiggle map observing mode was used, with a chop
throw of 2 arcmin in the SE direction. Atmospheric conditions were not
excellent, with
0.15. Telescope focus and pointing
were checked using Uranus and the data were calibrated following standard
recipes as in the SCUBA User Manual (SURF).
All transitions observed with the IRAM-30 m telescope except for CH3C2H (6-5) and (8-7) have been observed also with the IRAM 5-element array at Plateau de Bure. The observations were carried out in November 1998 and April 1999 in the B and C configurations of the array. The antennae were equipped with 82-116 GHz and 210-245 GHz receivers operating simultaneously. These were tuned single side-band at 3 mm and double side-band at 1.3 mm resulting in typical system temperatures of 200 K (in the USB) and 1000 K (in the LSB) at 3 mm and 250 K (DSB) at 1.3 mm. The facility correlator was centred at 112.581 GHz in the USB at 3 mm and at 221.921 GHz in the LSB at 1.3 mm. The C18O(1-0) and C17O(1-0) lines were covered using two correlator units of 20 MHz bandwidth (with 256 channels); two 160 MHz units were suitably placed to obtain a continuum measurement at 3 mm. The C17O(2-1) and CH3C2H(13-12) K= 0, 1, 2 transitions were observed with a 40 MHz bandwidth (256 channels), while the other K lines were covered with 160 MHz bandwidths (64 channels), which were also used to obtain a continuum measurement at 1.3 mm. The effective spectral resolution is about twice the channel spacing (see "The New Correlator Description of the PdBI'', http://www.iram.fr).
Phase and amplitude calibration were obtained by regular observations (every 20 min) of nearby point sources (2200+420 and 0059+5808). The bandpass calibration was carried out on 3C454.3, while the absolute flux density scale was derived from MWC349, regulary monitored at IRAM. Continuum images were produced after averaging line-free channels and then subtracted from the line. The resulting maps were then cleaned and channel maps for the lines were produced. The synthesized beam sizes are listed in Table 1.
The NRAO Very Large Array (VLA) ammonia observations were performed on August
8, 2000. The NH3(1,1) and NH3(2,2) inversion lines at
23.694496 and 23.722633 GHz, respectively, were simultaneously observed
with spectral resolutions of
1.2 and 4.9 km s-1 respectively. The array was used in its most
compact configuration (D), offering baselines from 35 m to 1 km.
The flux density scale was established by observing 3C286 and 3C147;
the uncertainty is expected to be less than 15%. Gain calibration
was ensured by frequent observations of the point source J0102+584,
with a measured flux density at the time of the observations of 3.4 Jy.
The same calibrator was also used for bandpass correction.
The data were edited and calibrated using the Astronomical Image Processing
System (AIPS) following standard procedures.
Imaging and deconvolution was performed using the IMAGR task and
naturally weighting the visibilities. The resulting synthesised beam
FWHM is 4.0
with position angle
,
and the noise level in each channel is 4 mJy beam-1 and
3 mJy beam-1 for the NH3(1,1) and NH3(2,2) data respectively.
The reduction of the IRAM-30 m telescope and PdBI data has been carried out with the GAG-software developed at IRAM and the Observatoire de Grenoble. In the next subsections we briefly outline the fitting procedures adopted to analyze the CH3C2H and NH3 spectra.
CH3C2H is a symmetric-top molecule with small dipole moment ( Debye).
Its rotational levels are described by two quantum numbers: J,
associated with the total angular momentum, and K, its projection on
the symmetry axis. Such a structure entails that for each
radiative transition, J+1 lines with
can be seen (for a detailed
description see Townes & Schawlow 1975). In our observations the
bandwidth covers all components for the (6-5) and (8-7) transitions, and
up to the K=10 component for the (13-12) line. However, we detected only
lines up to K=3.
In order to compute the line parameters, we have performed Gaussian fits to the observed spectra
assuming that all the K components of each
transition
arise from the same gas. Hence, they have the same LSR velocity
and line width. Then, in the fit procedure we fixed the line separation
in each spectrum to the laboratory value and we assumed the line widths
to be identical. In Sect. 4
we will use the line intensities derived from this procedure to estimate the
kinetic temperature of the emitting gas.
The NH3(1,1) and (2,2) inversion lines show hyperfine structure (see i.e. Townes & Schawlow 1975). To take into account this structure, we fitted the lines using METHOD NH3(1,1) and METHOD NH3(2,2) of the CLASS program. In this case the fit to the NH3 lines is performed assuming that all components have equal excitation temperatures, that the line separation is fixed at the laboratory value and that the linewidths are identical. This method also gives an estimate of the total optical depth of the lines using the intensity ratio between the different hyperfine components.
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Figure 1: C18O and C17O spectra towards the central position in the maps, which is the peak of the sub-mm emission (Molinari et al. 2000). The dashed line indicates the main component arising from the source. The dotted line with red-shifted velocity shows the second component. In the C17O (1-0), the vertical lines under the spectrum indicate the position of the hyperfine components. |
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Figure 2:
From top to bottom: CH3C2H (6-5), (8-7) and (13-12) IRAM-30 m
spectra towards the peak of the sub-mm emission (Molinari et al. 2000). The
numbers under the spectra indicate the position
of the different K components. The
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Table 2: Line parameters of CO isotopomers at the peak position (IRAM-30 m observations). All line parameters have been obtained from a two-Gaussian fit, except for the C17O (1-0) line, for which we have used METHOD HFS of the CLASS program to take into account the hyperfine structure (see text).
Table 3: CH3C2H line parameters (IRAM-30 m observations).
In Fig. 1 we show the C18O and C17O spectra taken at the central position in
the maps, corresponding to the peak of the sub-mm emission detected by
Molinari et al. (2000). Single-pointing spectra of the CH3C2H (6-5),
(8-7) and (13-12) lines are shown in Fig. 2. The C18O (1-0) and
C17O (1-0) spectra towards the central position clearly indicate the
presence of two velocity components, centered at -50.5 km s-1and at
-47.8 km s-1, respectively (see Fig. 1).
The component with higher velocity appears very strong especially in the
C18O (1-0) spectrum. We have fitted the two components with Gaussians.
In particular, the C17O (1-0) line has hyperfine structure: thus, we have
performed Gaussian fits taking into account this structure by using
METHOD HFS of the CLASS program. This procedure also gives an estimate
of the line optical depth: we will discuss this point in Sect. 3.1.3.
The line parameters of the two components at the peak position are given in
Table 2.
Peak velocity (
), full width half maximum (
)
and
integrated intensity of the line (
)
are given in
Cols. 3-5, respectively. In Col. 2 we
also give the 1
rms of the spectra. In the CH3C2H observations only
the lower velocity component is seen.
For these lines, we have performed Gaussian fits as explained in
Sect. 2.5. The results are given in Table 3.
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Figure 3:
Top panel: IRAM-30 m map of the main component of the C18O (1-0)
line obtained integrating
between -52.5 and -49.0 km s-1. Contour levels go from
![]() ![]() ![]() ![]() ![]() ![]() ![]() ![]() ![]() ![]() |
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Maps of the spectral component at -47.8 km s-1 show that the C18O (1-0)
(Fig. 3) and the C17O (2-1) lines peak at (0
, -15
)
from the central position of I23385, suggesting that this emission is unrelated
to this source. The presence of a
secondary source to the South was already found by
Molinari et al. (1998b) in the HCO+(1-0) line.
Only the component centered at -50.5 km s-1 represents the
emission arising from I23385: hereafter we shall refer to this as the "main''
component. The secondary
component, centered at -47.8 km s-1, will not be discussed further.
The integrated intensity maps of the main component are shown in
Figs. 3 and 4.
We do not show the C17O (1-0) integrated map because the line is faint
over the whole map (
in many points).
The first clear result is that the emission looks quite flat and without
an obvious peak towards I23385. This is especially evident in the
C17O map.
Also, in the C18O (1-0) and C17O (2-1) maps, the half maximum power
contour is elongated in the N-S direction: this could
be due to the presence of the secondary component in the spectra. In fact, it
is difficult to separate the two components, especially
in the southern part of the map
where the overlap of the two lines is more pronounced. In an attempt
to derive the size of the emtting region in each line, we
have estimated the angular diameter considering only the northern
part of the maps (that with positive offset in
), which is less
affected by the secondary component:
we find an average diameter of the emitting region
22
for
the C18O (1-0) line, and
18
for the C17O (2-1) line. After
correcting for the beam size (see Table 1), one finds a
deconvolved angular diameter of
18
(corresponding to
0.45 pc) for the C18O (1-0) line and of
15
(
0.30 pc) for
the C17O (2-1) line.
In conclusion, from the 30-m maps of I23385 in the C18O and C17O lines, one cannot see an intensity peak towards the nominal position of the core, which instead is clearly seen by Molinari et al. (1998b) in different molecular transitions, as well as in our PdBI maps in the same lines, as shown in Sect. 3.3. We will further discuss this point in Sect. 5.2.
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Figure 4:
Same as Fig. 3 for the main component of the C17O (2-1) line, integrated between -52.5 and -49.0 km s-1. Contour levels
go from ![]() ![]() ![]() ![]() |
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The availability of two rotational transitions of
the same molecular species (namely C17O (1-0) and (2-1)) allows us to
derive a map of the kinetic temperature, as we will explain in
Sect. 4.3.
However, this requires knowledge of the optical depth of such lines.
Since we have also observed the C18O (1-0) line, it is possible to
estimate the opacity of the C17O (1-0) line from the ratio of two spectra,
assuming equal temperatures and beam
filling factors, and an abundance ratio of 3.7 for 18O/17O (see
Penzias 1981; Wilson & Rood 1994).
We find an intensity ratio typically between 3
and 4, with a mean value of 3.5, which implies that the
C17O (1-0) line is optically thin.
For C17O, it is possible to derive the optical depth from the measure of
the relative intensities of the hyperfine components.
Unfortunately, in our spectra we are not able to resolve the
hyperfine structure, hence the optical depth derived in this way is not
reliable. Concerning the
C17O (2-1) line, we cannot measure the optical
depth directly from our observations. However, in LTE conditions, one
can demonstrate that up to
temperatures as high as 40 K, the optical depth of the (2-1) line is
3 times that of the (1-0) line. Since the maximum value
of the opacity of the (1-0) line derived from the line ratio is
,
the (2-1) line must have an
optical depth less than
0.5. Thus, when in Sect. 4.3
we will derive the kinetic temperature from the ratio between the C17O (2-1) and (1-0) lines, we
will assume that the lines are optically thin.
I23385 has been mapped in the sub-mm continuum at 850 m with SCUBA, with an
angular resolution of 15
(Fig. 5). The intensity
profile presents an unresolved compact central peak, and an extended halo
which surrounds the peak up to
100
.
The figure also
shows the integrated emission of the main component of the C18O (1-0)
line (upper panel of Fig. 3).
We can see that there is a reasonable match between the 850
m
emitting region and that traced by the C18O (1-0) line, although the
corresponding peaks are not coincident.
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Figure 5:
SCUBA map of IRAS 23385+6053 at 850 ![]() ![]() |
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We present here the results of molecular line and millimeter continuum observations carried out with the Plateau de Bure interferometer.
All molecular transitions observed with the IRAM-30 m telescope have been also imaged with the PdBI, with the exception of the CH3C2H (6-5) and (8-7) lines. In Fig. 6 we show the maps obtained integrating the emission under the C18O (1-0), C17O (2-1) and CH3C2H (13-12) lines. The secondary component is not detected, except perhaps in C18O (1-0), in which the shape of the red wing of the line might be affected by the secondary component. This is likely due to the fact that the secondary component is more extended, thus its emission has been resolved out.
We do not show the C17O (1-0) map
because this is very noisy, and the signal is undetected up to a
level of
36 mJy beam-1.
The C18O (1-0), C17O (2-1) and CH3C2H (13-12) emission is detected with
a good signal-to-noise ratio. We can clearly see the presence of a
central compact core coincident with I23385. In the C17O (2-1) and CH3C2H
(13-12) lines, the source
shows a complex morphology, while it looks more simple in the
C18O (1-0) line. This is consistent with the different angular
resolution: at 1.3 mm the beam size is
2 times smaller, allowing us to
better resolve the core structure.
In particular, it can be noted that the C17O (2-1) emission is
marginally depressed at the peak position of the continuum and the CH3C2H (13-12) line. This might be suggestive of CO depletion in the inner region
of the core (see discussion in Sect. 5.2).
We have estimated the diameters of the emitting regions from the half maximum power contours shown in Fig. 6: if we assume the source to be Gaussian, we can derive the angular diameter after beam deconvolution, as given in Col. 2 of Table 5.
In Fig. 7 spectra of the C18O (1-0), C17O (1-0) and (2-1)
and CH3C2H (13-12) lines are shown, that have been obtained integrating
the emission
arising within the
level inferred from the maps of
Fig. 6.
The availability of IRAM-30 m spectra allows a comparison between
interferometric and single-dish data. This comparison is also shown in
Fig. 7, where the single-dish spectra have been resampled with
the same resolution in velocity as the PdBI spectra, namely
0.4 km s-1.
The superimposition of the spectra clearly demonstrates that a large
fraction of the extended emission is filtered out by the interferometer.
This is especially evident in the C18O (1-0) line, for which the flux
measured
with the PdBI is
11 times less than those obtained with the IRAM-30 m
telescope. This is also true
for the C17O (2-1) line, for which the intensity ratio is
10.
In the CH3C2H (13-12) transition this effect is smaller as the single-dish
flux is
3 times larger. As noted earlier, the secondary
component is resolved out in the PdBI spectra.
Looking at the C17O (2-1) spectrum
of Fig. 7, the line profile seen by the interferometer seems
to peak at a slightly blue-shifted velocity with respect to the 30-m
spectrum. We believe that this is due to the fact
that the S/N ratio is poor in the PdBI spectrum, hence the peak velocity,
and the other line parameters, are affected by large uncertainties.
In fact, the offest observed (0.5 km s-1) lies within the
uncertainty on the line peak velocity (
0.45 km s-1)
obtained from a Gaussian fit.
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Figure 6:
Maps obtained with the PdBI.
a) C18O(1-0) map integrated over the velocity range
(-49, -52) km s-1. Contour levels range from 0.05 (![]() ![]() ![]() ![]() ![]() ![]() ![]() ![]() |
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Figure 7: Flux density comparison between IRAM single-dish (dashed line) spectra and Plateau-de-Bure interferometric spectra (solid line). The interferometric flux densities have been multiplied by a factor of 10 for the CO isotopomers, and by a factor of 3 for the CH3C2H lines. The velocity of the CH3C2H spectrum is computed with respect to the frequency of the line with K=0. |
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Figure 8:
Top panel: map of the 3 mm continuum emission. The rms level is ![]() ![]() ![]() ![]() |
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With the PdBI we detect a compact central core, as can be seen from
Fig. 8, where we show the 3 mm and 1.3 mm
continuum maps. The 3 mm map shows a compact core with an
elongated shape along the E-W direction. This shape is better resolved at
1.3 mm, revealing a
secondary faint peak of emission offset by +2
in RA from the
main peak. This secondary peak is not detected in any of the molecular tracers.
The angular diameters are 1.5
and 1.1
at 3 mm and 1.3 mm,
respectively.
Measured flux densities
are 0.0124 and
0.148 Jy at 3 and 1.3 mm, respectively, obtained by
integrating over the solid angle down to the 3
level.
The flux density of the secondary source at 1.3 mm is
5% of
the total, namely 0.008 Jy.
We can compare the continuum flux density measured with the PdBI and with SCUBA, to estimate the
amount of the flux density filtered out by the interferometer. Using a
spectral
index for the dust emissivity of 4 (see Sect. 4.1), we have
extrapolated the flux density observed at 850 m with
SCUBA, to 1.3 mm. This has been
smoothed to an angular resolution of
22
,
corresponding
to the primary beam of the PdBI at 1.3 mm. The flux density measured in this
map towards the core I23385 is
0.28 Jy. We estimate in
0.11 Jy
the flux density to arise from the halo: this is filtered out by the
interferometer, and thus the flux density that we should observe with the PdBI
is
0.17 Jy. Taking into account the uncertainties
that affect our measurements
(in particular the combined calibration errors of both SCUBA and PdBI,
which are at least of the order of 30%), the
0.15 Jy observed at 1.3 mm with PdBI is consistent with
what is expected.
Thus, within the errors, it is plausible that with the PdBI we observe all
the continuum flux arising from the core I23385.
With the VLA, we have mapped the NH3(1,1) and (2,2)
inversion transitions. The corresponding maps and integrated spectra are
shown in Fig. 9. In both maps, the NH3 emission is
superimposed on the C18O (1-0) map. As for the CO isotopomers
observed with the IRAM-30 m telescope, the emission does not peak towards
the position of the core detected at 3 mm and 1.3 mm with the PdBI.
Although the signal-to-noise ratio is
poor in both maps (see Fig. 9), one can see that the
emission arises from a "clumpy'' structure, and it peaks at 5
(
0.12 pc) from the core position.
In Sect. 5.2 we will discuss
this result by comparing the NH3 maps with those obtained in the other
tracers. Comparison between Effelsberg-100 m (Molinari et al. 1996)
and VLA observations are shown
in Fig. 10. For the main component (centered at -50.5 km s-1),
with the VLA we lose about the 50% of the total flux density seen with the
single-dish telescope; for the NH3(1,1) line, this occurs for all the
hyperfine lines. Finally, we completely resolve out the secondary
component (centered at -47.8 km s-1) as in the other molecular tracers observed
with the PdBI .
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Figure 9:
Left panel: NH3(1,1) integrated map over the velocity range (-48,
-52) km s-1. Contour levels range from 0.012 (![]() ![]() ![]() ![]() |
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![]() |
Figure 10: Flux density comparison between Effelsberg-100 m (dashed line) and VLA (solid line) spectra of the NH3(1,1) and (2,2) lines. VLA fluxes have been multiplied by a factor of 2. The thick vertical lines under the NH3(1,1) spectrum indicate the position of the two components. The Effelsberg spectra have been resampled to the channel spacing of the VLA spectra. |
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Our goal is to investigate the hypothesis of Molinari et al. (1998b), namely that I23385 is a high-mass protostellar object, by examining the physical parameters of the core. First, we will analyze the continuum spectral energy distribution (SED). Then, from the PdBI map of the CH3C2H (13-12) line, we will compute the core temperature; finally, from continuum and line emission we will obtain the mass and the H2 volume density of the core.
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Figure 11:
Image: IRAS 23385+6053 observed at 2 ![]() |
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Figure 12:
Image of IRAS 23385+6053 at 15 ![]() ![]() |
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![]() |
Figure 13:
Continuum SED of I23385. Open
hexagons and stars indicate MSX and ISOCAM
flux densities respectively measured integrating over the "ring'' region
of Fig. 12. The filled triangle represents the SCUBA measurement.
Filled squares, open squares, filled circles and open
circles indicate respectively IRAS, JCMT, PdBI and OVRO data (see also
Fig. 2 of Molinari et al. 1998b). The arrows on the bottom left
and bottom right respectively indicate the ISOCAM and VLA upper limits
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In discussing the continuum SED, it is important to distinguish between two "sub-regions'':
In Fig. 13 the continuum SED of I23385 is shown. With respect to
Fig. 2 of Molinari et al. (1998b), Fig. 13 contains more
data, namely PdBI, IRAS, JCMT, OVRO, ISOCAM and MSX. Since no 7 and 15
m emission is detected with ISOCAM towards the source, we take the
level as an
upper limit at these wavelengths. The same was done for the VLA measurements
at centimeter wavelengths.
We performed a grey-body fit to the continuum SED of Fig. 13
(solid line).
The resulting bolometric luminosity is the same as in Molinari et al.
(1998b), namely
.
The slope of
the millimetric part of the spectrum is fitted assuming a dust
opacity
,
where
,
which
assumes a gas-to-dust mass ratio of 100 (see
Preibisch et al. 1993).
The best fit is obtained for
.
Therefore, the
best fit opacity index is
.
The other best fit parameters
are: source temperature of 40 K, diameter of 8
and a mass of
.
Since most of the luminosity is due to the IRAS 60 and 100
m
flux densities, it is
important to assertain the origin of the IRAS flux densities. In fact,
the IRAS beam is much larger than the source diameter (
2 arcmin at 100
m), thus the IRAS flux densities may arise both from I23385 and
from the
cluster of stars surrounding it (the "ring'' in the 15
m ISOCAM map of
Fig. 12). Hence, the source
luminosity estimated before (
)
is to be
regarded as an upper limit for the luminosity of I23385. However, we know
from the JCMT and interferometric maps
that the flux densities at 850
m and at longer wavelenghts certainly
come from I23385. Thus, we performed a grey-body fit using only these data (dotted line
of Fig. 13): the corresponding grey-body fit gives a luminosity of
which represents a lower limit.
The two limits thus obtained are very different, but we believe that the source
luminosity is closer to the upper limit.
In fact, the MSX image at 21
m shows that the emission at this
wavelength arises from the "ring'', hence very likely this region is
also responsible for the 25
m emission. However, as already
discussed by Molinari et al. (1998b), it is unlikely that the "ring''
contributes significantly to the IRAS flux densities at 60 and 100
m,
because
even a power-law extrapolation of the spectrum of the extended region
(dashed line in Fig. 13) gives flux densities at 60 and 100
m much
lower (a factor of
10) than the values observed.
We conclude that most of the emission at 60 and 100
m is due to I23385, and therefore a luminosity of
is not very
far from the real value. We will further discuss this point in
Sect. 5.3, on the basis of our CH3C2H observations.
It is also worth noting that the 1.3 mm flux density measured with the PdBI
is 3 times less than the value measured with the JCMT at the same wavelength.
In fact, as explained in Sect. 3.3.2, with the interferometer we
observe approximately all the flux density arising from the compact core, but
we miss that coming from the extended halo, which we do detect with the JCMT.
Finally, it is unlikely that the source associated with the
secondary peak detected in the 1.3 mm map contributes significantly to the
total observed luminosity, because its
1.3 mm flux density is only 5% of that from the main core.
From the CH3C2H (13-12) spectra of Figs. 2 and 7 we derive the kinetic temperature and the total column density of the molecule by means of the Boltzmann diagrams method (see e.g. Fontani et al. 2002). The fundamental assumption of the method is the local thermodynamic equilibrium (LTE) condition of the gas. Such an assumption is believed to work very well for CH3C2H because of its low dipole moment (see Bergin et al. 1994). Under the further assumption of optically thin emission, the column density Ni of the upper level i of each transition is proportional to the integrated intensity of the line.
In Fig. 14 Boltzmann diagrams are shown: the straight
lines represent least square fits to the data, and the kinetic temperature and
the column density are related to the slope and the intercepta, respectively.
The interferometric data
yield
K and
cm-2 for the
core. It is evident that such temperature is well below that of a HC.
In a recent paper, Thompson & Macdonald (2003) have observed
rotational transitions of the CH3OH molecule towards IRAS 23385+6053, from which
they derive that the kinetic temperature is likely to be smaller than
50 K, and therefore it is unlikely that IRAS 23385+6053 might contain a HC. Our study
strongly supports this idea and give a much more accurate
temperature estimate of the core.
With the IRAM-30 m data we obtain
K and
cm-2. In this case, the column densities Ni have been corrected for the beam filling
factor. For this purpose, an estimate of the CH3C2H emitting region is
needed. Unfortunately, we have no direct estimate because no CH3C2H single-dish
maps are available. However, we can use the source size estimated from
the SCUBA map, given in Sect. 4.5.
The previous results are summarised
in Table 4. The errors on
and
have
been computed in two different ways: for the single-dish data we must
take into
account the calibration error. This error affects simultaneously each line in
the same bandwidth. Hence, in the diagrams, the effect of this
error is to shift the points in the same bandwidth (e.g. the (6-5) lines)
by the same quantity. This error is
10% for the (6-5) lines
and
20% for the (8-7) and (13-12). Hence, in order to compute the
uncertainties on
and
,
we have varied the values
of Ni by 10% simultaneously for all the (6-5) K components, and
by 20% for the (8-7) and (13-12). These variations have been made in
different directions.
The uncertainties in Table 4 are the maximum difference between
the values thus obtained and the nominal ones.
For the PdBI estimates, we have data of a single band, and the
calibration error does not affect
but only
.
Let us now discuss the two basic assumptions of the method, i.e.
optically thin emission and LTE conditions of the gas.
The LTE assumption holds very well when the H2 density is greater than
a critical value (see e.g. Spitzer 1978). For the observed
transitions the maximum critical density is 105 cm-3, and
we shall see in Sect. 4.5 that the inferred H2 density is
above this value, justifying the assumption of LTE conditions.
Concerning the optical depth of the lines, the excellent agreement between
the data and the linear fit of Fig. 14 strongly supports the
assumption of optically thin lines. In fact, large optical
depths are expected to affect mainly the transitions with lower excitation.
Hence we should have a flattening of the Boltzmann diagram at lower energies,
which is not seen in Fig. 14.
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Figure 14:
Top panel: rotation diagram inferred from CH3C2H lines observed
with the IRAM-30 m telescope. Filled circles, filled triangles and open circles
indicate respectively the (6-5), (8-7) and (13-12) transitions. The straight
line represents a least square fit to the data. Column densities are
source-averaged values using a source diameter of 15
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Table 4:
Temperature and column density estimates.
and
D are the angular and linear source diameter, respectively.
is the
kinetic temperature, and
the total column density of the
corresponding molecular species.
In the previous section we have computed the kinetic temperature of the source
from the CH3C2H lines. We can also estimate the temperature by means of
the C17O lines observed with the IRAM-30 m telescope. Using a source size of 15
,
found in Sect. 3.1.2 from the C17O (2-1) map, we have derived
the beam-averaged brightness temperatures for the C17O (1-0) and (2-1)
lines. Then, from the integrated line intensities, and assuming optically thin
lines and LTE conditions, we find a "Boltzmann relationship'' between the
total column density of the upper level of each transition and the
corresponding rotational energy, as
discussed above for the CH3C2H lines. We have done this
for each point of the C17O maps in which the C17O (1-0) line
is stronger than the
level. The resulting average kinetic
temperature is
15 K.
It is important to stress that in deriving the kinetic temperature from
C17O line ratios we have assumed LTE conditions. Statistical
equilibrium calculations (see Wyrowski 1997) show that this
assumption holds if
cm-3. Otherwise, the
temperature estimated in this way is to be regarded as a lower limit. Since
we obtain
cm-3 over the whole map, we conclude that the
LTE assumption is satisfied in our case.
We obtain a total column density ranging from
to 7
1015 cm-2: the C17O total column
density given in Table 4, namely
cm-2, is the mean
value over the map.
Table 5:
Mass and H2 column- and volume-density estimates from
lines. Molecular
abundances relative to
have been assumed equal to 1.2
10-7, 3.4
10-8 and
for C18O, C17O and CH3C2H, respectively.
and
are the
column density and the FWHM of the lines,
respectively.
Table 6:
Mass and
column- and volume-density estimated from
continuum observations.
The NH3 emission seen with the VLA arises from a region
whose diameter is "intermediate'' between that of the core I23385 and that of
the C17O and C18O total emitting region seen with the IRAM-30 m telescope.
The emission peak does not coincide with the continuum nor with
the C18O (1-0) line.
The NH3(1,1) hyperfine structure allows us to estimate the optical depth
as explained in Sect. 2.5: we obtain
for this line. For the (2, 2), we have no direct estimates, but
we can reasonably assume that for temperatures between
10 and
40 K, under LTE conditions, the (2, 2) line is also optically thin.
The temperature
and column density can be derived following the method by Ungerechts et al.
(1986). We obtain a temperature of
26 K and a total column
density of 6
1015 cm-2. We have
assumed equal linewidth and beam filling factor for both transitions. The
results are given in Table 4.
The grey-body fit to the spectrum of Fig. 13 is obtained for a dust
temperature of 40 K, a dust
opacity
,
an average source diameter of 8
,
(
0.2 pc), and a mass of
400
.
It is also useful to derive the mass of the core seen with the PdBI. From
the 3 mm continuum flux density, using the core temperature
deduced from the CH3C2H lines (namely T=42 K),
,
and assuming optically thin dust emission,
we find that the mass contained inside
1.
5 is
.
Note that we have used the 3 mm flux density,
rather than that at 1.3 mm, because we expect to miss less flux
at this wavelength.
To compute the mass from the molecular line emission, we use the expression:
From the line-widths of the observed transitions and the
corresponding angular diameters in Table 5,
we can also derive the mass required for virial equilibrium:
assuming the source to be spherical and homogeneous, neglecting contributions
from magnetic field and surface pressure, the virial mass is given by
(MacLaren et al. 1988):
Finally, from
we derive the
volume density,
.
All masses and densities
are given in Tables 5 and 6. It is worth noting that the density
of the central core is
107 cm-3: this value is well above
the maximum critical density of the CH3C2H lines observed, thus supporting
our LTE assumption and our derivation of the kinetic temperature.
As usual, the main errors in estimating the masses are due to
the molecular abundances, the assumed dust opacity and the gas-to-dust
ratio, and it is very difficult to quantify the uncertainties for these
parameters.
One can see clearly that masses and densities derived from different tracers differ very much from one another. This is partly due to the fact that different tracers arise from different regions. However, even for the same region, the mass derived from the continuum emission is a few times that estimated from the line emission. This is likely due to uncertainties in the assumed molecular abundances. We shall come back to this point in Sect. 5.2.
The availability of high and low angular resolution observations of IRAS 23385+6053 allows us to paint a detailed picture of the source, and discuss the nature of the core I23385.
The values of the masses estimated for the same region using dust and line
emission show a systematic difference: from Tables 5
and 6 one can see that the mass estimated from dust (
)
is
2-3 times greater than that deduced from molecular
lines (
).
However,
is affected by several
problems which may lead one to underestimate the mass, as we will discuss
in Sect. 5.2. On the other hand, the dust emission is independent
of molecular abundances, so that the mass estimated
from the mm continuum seems to be more reliable.
Since the source is a candidate massive protostar, it is useful to
discuss its virial equilibrium. In order to do this, we need an estimate
of the virial mass. We have used the diameters deduced from each tracer
to give an estimate of the virial mass. Then, we have compared these
estimates to those deduced from the column density derived from the same tracer,
and with that obtained from the continuum emission arising from the same
region.
The result is shown in Fig. 15. The empty circles indicate the
estimates derived from lines, while the full circles represent the continuum.
In a cloud with a density profile which follows a power law of
the type
,
one can demonstrate that the mass
contained inside a given radius r, M(r), is proportional to r3-m.
Instead, the virial mass depends on the source
diameter and on the linewidth. However, based on the
values in Table 5, we conclude that the linewidth does not change
significantly at different radii. Therefore, the estimate of the ratio
scales approximately as r2-m. For IRAS 23385+6053, as
we shall show later (see Fig. 16), we derive that
m= 2.3
0.2, hence
.
In Fig. 15 we plot the ratio
as a function of D. The curve is in rough agreement with data points obtained from
the continuum measurements. However, the "true'' virial mass, deduced
from the virial theorem, must be computed from the radius of the whole
cloud and the corresponding
.
We do not know
the "total'' dimension of the source, but we can compute at which radius
the ratio
becomes equal to 1.
For a power-law density distribution of the type
,
the virial mass obtained from Eq. (2) must be
multiplied by
a factor
(see MacLaren et al. 1988), which is
0.35 for m= 2.3. This
increases the ratio
by a factor 3, implying that
at a radius of 10
,
and that the
virial mass
equals the gas mass at a radius of
50
,
which is much greater than
the maximum diameter observed by us. Hence, since the real source size
is likely to be smaller than that corresponding to
,
we
believe that I23385 is likely to be gravitationally unstable.
This conclusion is further supported by discussing the density profile.
![]() |
Figure 15:
Ratio between masses deduced from gas (
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In Fig. 16 we plot the density estimated from all tracers observed
against the corresponding linear diameter (densities
and diameters are given in Table 5 and 6). The data
follow the relation
,
hence
.
This
is similar to that predicted by star formation models (Shu et al.
1987), in which star formation occurs in molecular
clouds which are singular isothermal spheres with
density
r-2. This sphere rapidly undergoes inside-out
collapse.
Then, the density profile in Fig. 16 supports the idea that IRAS 23385+6053 is
unstable, as expected for a protostar which is still in the accretion phase.
On the basis of Tables 4-6 and the SCUBA map of Fig. 5, one can identify two regions in I23385: a compact core and a surrounding extended halo. Their physical parameters are:
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Figure 16:
H2 volume density against the linear diameter D for all the
tracers observed. All values have been taken from Table 4. The straight
line is a linear fit to the data, which gives
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Figure 17:
Brightness temperature of the
C17O (1-0) line computed assuming a source as described in the text, and
a C17O relative abundance of
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Figure 18:
Brightness temperature of Fig. 17 convolved
with the IRAM-30 m telescope beam (22
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Let us consider a source consisting of the two regions outlined above:
a core and a surrounding halo. Both are assumed to be spherical, homogeneous
and isothermal.
The expected brightness temperature
of the C17O (1-0) line for
such a source is shown in Fig. 17, where
is plotted against the radial distance R from the source center.
Convolving
with a Gaussian beam, we derive the
corresponding main beam brightness temperature
.
Figure 18 represents
convolved with a
Gaussian beam with HPBW = 22
(that of the IRAM 30 m telescope); one
can see that the emission coming from the core is flattened by beam dilution
effects.
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Figure 19:
Left panel: map of the C17O (1-0) line in the peak channel
(at -50.5 km s-1). The solid contour represents the observed 2![]() ![]() ![]() |
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We now discuss why the central core is not detected in the C17O (1-0) PdBI map. Since the molecular emission is extended, we must determine first how much flux density is filtered out by the interferometer. Starting from the brightness temperature profile of Fig. 17, we have used a modified version of the procedure described in Wilner et al. (2000) and Testi et al. (2003). The program uses the model to create first the source image in the sky; then, it computes the Fourier Transform and resamples the visibility function in the UV points corresponding to those measured in that channel, which finally are used to reproduce the image. In order to compare the PdBI map with what is predicted by the model, we plot in Fig. 19 the channel where the peak is observed (at -50.5 km s-1), superimposed on the map predicted by our model. We have also done the same using a model that reproduces the "halo'' only. It is evident that the model reproduces a central peak which is instead completely lost in the PdBI map; on the other hand, the emission of the halo is quite consistent with what observed if we consider that our model is very simple, and does not consider possible patchy structures inside the halo.
A possible explanation of the discrepancy between the PdBI map and our model can be that in the core the C18O and C17O species are partially depleted because they are frozen onto dust grains. This is suggested by the fact that gas masses deduced from the CO isotopomers given in Table 5 are systematically lower than the dust masses inferred from the continuum measurements. This might be due to a partial freeze-out of the molecules on the dust grains. This situation is possible even at temperatures as high as 40 K if dust grains have ice mantles. In fact, chemical models predict that ice mantles may exist at the densities and temperatures measured by us in the core (van Dishoeck & Blake 1998), and this allows partial depletion of CO and its isotopomers. Furthermore, recently Thompson & Macdonald (2003) have performed a chemical analysis of I23385 using molecular lines with rest frequencies in the range 330-360 GHz, finding that the chemical composition of I23385 is consistent with that of a molecular core in the middle evaporation phase, i.e. when the majority of the molecular species are beginning to be evaporated from dust grains ice mantles.
Also, dust grains with ice mantles might be responsible for the non-detection of NH3 towards the source center: in fact, the same chemical models also predict that the presence of ice mantles allows NH3 depletion up to temperatures of 90 K. Finally, it is worth noting that partial depletion of CO is consistent with detection of CH3C2H emission in the core. In fact, Ruffle et al. (1997) found that in dense cores, when CO depletion occurs, molecular species produced from CH and without oxygen (like CH3C2H) increase their rate of production.
Here we want to find out whether our results may be used to establish the nature and the evolutionary stage of the embedded YSO.
In cores where the gas is heated by an embedded star, the gas temperature
at a radial distance
from the central star is expected to
scale as (see e.g. Plume et al. 1997):
The drawn line indicates the steepest power
law,
.
It is evident that it is not possible
to match our temperature estimate with that expected for such a power law.
To solve this problem we examine three possibilities:
1) We might be overestimating the source luminosity.
In Sect. 4.1 we discussed that
the luminosity of the embedded source is of the order of 104 solar
luminosities. This was based on the hypothesis that the bulk of the IRAS
fluxes at 60 and 100 m is due to I23385. Unfortunately, the IRAS angular
resolution is not sufficient to confirm this hypothesis.
Hence, the "bright ring'' surrounding I23385 might emit a consistent
fraction of the flux at 60 and 100
m. In that case, the luminosity of I23385
might be lower. A temperature of 42 K at 0.017 pc in an optically thick core
implies a central source of
.
Altough well below
the value predicted in Sect. 3.3.2, this luminosity is
consistent with an intermediate-mass protostar deriving its luminosity from
accretion, as shown by Behrend & Maeder (2001).
In fact, the authors performed
calculations of the evolution of protostars with mass from 1 to 85
,
assuming growing accretion rates. For an accretion luminosity of
,
the protostar mass is
.
2) Another possibility is that we have underestimated the core diameter.
This is possible if the
source is not Gaussian: in fact, if the core is spherical, the diameter
estimated in Table 5 requires a correction (see Panagia & Walmsley
1978). In our case one obtains 2
(0.047 pc), for the
diameter of the core. This brings the luminosity
to
,
still much less than the value obtained in
Sect. 4.1 from the continuum spectrum.
3) Finally, it is possible that the temperature profile,
is steeper in case of a non-spherical geometry, as in the presence of
a disk. Cesaroni et al. (1998) have found that HCs are likely to
be disk-like structures, in which the temperature profile is
.
With this power-law it is possible to obtain a lower temperature
at 0.017 pc with a luminosity of 1.6
.
Which solution is correct? Concerning the second hypothesis
(underestimate of the core radius),
we have already seen that it is very unlikely.
This is also valid for the third one (disk-like structures): in fact, to
measure such a low temperature, the disk should
lie along the line of sight, but unfortunately this is more likely
"face-on'', because the outflow detected by Molinari et al. (1998b)
lie approximately along the line of sight. The first hypothesis
(overestimate of the core luminosity) is the most likely, but
presently it is impossible to give a reliable answer,
because the correct source luminosity can be derived only by means of a map
at 100
m at high angular resolution, which is not available.
However, as already discussed, a luminosity
as low as
is consistent with a protostar in the accretion
phase, whose mass, at present, is
.
![]() |
Figure 20:
Kinetic temperature measured at the surface of molecular cores
plotted against the distance-independent ratio
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We have used the IRAM-30 m telescope, the Plateau de Bure Interferometer and the Very Large Array to observe the massive protostar candidate IRAS 23385+6053 in the C18O (1-0), C17O (1-0) and (2-1), CH3C2H (6-5), (8-7) and (13-12), NH3(1,1) and (2,2) lines. The following results have been obtained:
The first hypothesis seems the most likely, although the real source luminosity can be derived only with high resolution maps at FIR wavelengths, which will become feasible only with the HERSCHEL satellite.
Acknowledgements
We would like to thank the referee, Dr. H. Beuther, for his very useful comments. We also thank Paola Caselli for stimulating discussion about the main topic of Sect. 5.2.