Issue |
A&A
Volume 520, September-October 2010
|
|
---|---|---|
Article Number | A50 | |
Number of page(s) | 23 | |
Section | Interstellar and circumstellar matter | |
DOI | https://doi.org/10.1051/0004-6361/201014177 | |
Published online | 30 September 2010 |
The molecular environment of the Galactic star forming region G19.61-0.23
,![[*]](/icons/foot_motif.png)
G. Santangelo1,2,3,4 - L. Testi1,4 - S. Leurini1,6 - C. M. Walmsley4 - R. Cesaroni4 - L. Bronfman7 - S. Carey9 - L. Gregorini2,3 - K. M. Menten6 - S. Molinari8 - A. Noriega-Crespo9 - L. Olmi4,5 - F. Schuller6
1 - European Southern Observatory, Karl Schwarzschild str.2, 85748 Garching bei Muenchen, Germany
2 - INAF - Istituto di Radioastronomia, via Gobetti 101,
40129 Bologna, Italy
3 - Dipartimento di Astronomia, Università di Bologna,
via Ranzani 1, 40127 Bologna, Italy
4 - INAF - Osservatorio Astrofisico di Arcetri, Largo E. Fermi 5,
50125 Firenze, Italy
5 - University of Puerto Rico, Rio Piedras Campus, Physics Department,
Box 23343, UPR Station, San Juan, Puerto Rico
6 - Max-Planck-Institut für Radioastronomie, Auf dem Hügel 69, 53121 Bonn, Germany
7 - Departamento de Astronomía, Universidad de Chile, Casilla 36-D, Santiago, Chile
8 - Istituto Nazionale di Astrofisica - Istituto Fisica spazio interplanetario, via Fosso del Cavaliere 100, 00133 Rome, Italy
9 - Spitzer Science Center, California Institute of Technology,
Pasadena, CA 91125, USA
Received 1 February 2010 / Accepted 3 June 2010
Abstract
Context. Although current facilities allow the study of
Galactic star formation at high angular resolution, our current
understanding of the high-mass star-formation process is still very
poor. In particular, we still need to characterize the properties of
clouds giving birth to high-mass stars in our own Galaxy and use them
as templates for our understanding of extragalactic star formation.
Aims. We present single-dish (sub)millimeter observations of gas
and dust in the Galactic high-mass star-forming region G19.61-0.23,
with the aim of studying the large-scale properties and physical
conditions of the molecular gas across the region. The final aim is to
compare the large-scale (about 100 pc) properties with the
small-scale (about 3 pc) properties and to consider possible
implications for extragalactic studies.
Methods. We have mapped CO isotopologues in the J=1-0 transition using the FCRAO-14m telescope and the J=2-1 transition using the IRAM-30m telescope. We have also used APEX 870 m continuum data from the ATLASGAL survey and FCRAO supplementary observations of the 13CO J=1-0 line from the BU-FCRAO Galactic Ring Survey, as well as the Spitzer infrared Galactic plane surveys GLIMPSE and MIPSGAL to characterize the star-formation activity within the molecular clouds.
Results. We reveal a population of molecular clumps in the 13CO(1-0) emission, for which we derived the physical parameters, including sizes and masses. Our analysis of the 13CO
suggests that the virial parameter (ratio of kinetic to gravitational
energy) varies over an order of magnitude between clumps that are
unbound and some that are apparently ``unstable''. This conclusion is
independent of whether they show evidence of ongoing star formation. We
find that the majority of ATLASGAL sources have MIPSGAL counterparts
with luminosities in the range 104-
and are presumably forming relatively massive stars. We compare our
results with previous extragalactic studies of the nearby spiral
galaxies M 31 and M 33; and the blue compact dwarf galaxy
Henize 2-10. We find that the main giant molecular cloud
surrounding G19.61-0.23 has physical properties typical for Galactic
GMCs and which are comparable to the GMCs in M 31 and M 33.
However, the GMC studied here shows smaller surface densities and
masses than the clouds identified in Henize 2-10 and associated
with super star cluster formation.
Key words: ISM: molecules - ISM: individual objects: G19.61-0.23 - radio continuum: ISM - stars: formation
1 Introduction
High-mass stars (OB spectral type,
and
),
although few in number, play a major role in the energy budget of
galaxies, through their radiation, wind and the supernovae. They are
believed to form by accretion in dense cores within molecular cloud
complexes
(Yorke & Sonnhalter 2002; McKee & Tan 2003; Keto 2003,2005) and/or coalescence (e.g. Bonnell et al. 2001). The intense
radiation field emitted by a newly-formed central star heats and ionizes its
parental molecular cloud, leading to the formation of a hot
core (HC, e.g. Helmich & van Dishoeck 1997)
and afterwards an HII region.
Our current understanding of their formation remains poor, especially
concerning the earliest phases of the process. The main observational
difficulty is that high-mass stars are fewer in number than low-mass
stars
and the molecular clouds that are able to form high-mass stars are
statistically more distant than those forming low-mass stars.
Therefore, current observational studies of high-mass star formation
suffer both from the lack of spatial resolution and, consequently,
from a lack of theoretical understanding.
The high-mass star-forming region G19.61-0.23 is an interesting
target for the study of star cluster formation given its richness in
terms of young
stellar objects (YSOs), as indicated by studies at centimeter
(e.g.
Garay et al. 1998; Forster & Caswell 2000), millimeter (e.g.
Furuya et al. 2005) and mid-infrared (MIR; De Buizer et al. 2003) wavelengths. G19.61-0.23 is located at a distance of 12.6 kpc (see Kolpak et al. 2003), based on the 21 cm HI absorption spectrum toward the source. The total bolometric luminosity (Walsh et al. 1997) is about
.
The region contains OH (Caswell & Haynes 1983; Forster & Caswell 1989), water
(Hofner & Churchwell 1996) and methanol (Caswell et al. 1995;
Val'tts et al. 2000; Szymczak et al. 2000)
masers, and a grouping of UC HII regions and extended radio
continuum, indicating that it is an active region of massive star
formation. The radio continuum emission from this region comes from
five main sources, all of which are discussed in detail in Garay et al. (1998). The region has been mapped in CS, NH3 and CO
(Larionov et al. 1999; Plume et al. 1992; Garay et al. 1998). Extended mid-infrared emission associated with the region is also detected by the MSX satellite (Crowther & Conti 2003).
Single-dish observations of molecular lines with high critical
densities show the presence of dense molecular gas over a broad range
in velocity (Plume et al. 1992).
In this paper we present a spectroscopic study of the region surrounding
G19.61-0.23 in several transitions of CO isotopologues at an angular resolution of
(about 2.8 pc at the distance of 12.6 kpc), on a large region of about
(roughly 85 pc) centered on G19.61-0.23. Millimeter observations
of carbon monoxide provide useful information on the physical
properties of dense interstellar clouds as well as on their dynamical
state. Moreover, supplementary measurements of continuum emission in
the sub-millimeter range with APEX, based on ATLASGAL data, and in the
mid-infrared with
Spitzer, based on GLIMPSE and MIPSGAL data, are presented. The aim is to study the global large-scale physical
properties and their relation with the small-scale characteristics. We
analyzed the physical conditions and the velocity structure of the molecular
components across the region. We finally consider the possible implications
for extragalactic observations of well-studied nearby starburst galaxies at the same linear resolution.
![]() |
Figure 1:
FCRAO velocity-integrated 13CO(1-0) emission in white contours from our data, overlaid on the 13CO(1-0) emission from the BU-FCRAO GRS (color). Both maps are integrated between 25 and 77 km s-1. The contour levels range from 10 |
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In Sect. 2 we describe the dataset of observations used in this paper; in Sect. 3 we present the large-scale morphology of the emission; in Sect. 4 we describe the identification of the clumps: from the molecular line emission and from the sub-mm continuum emission; in Sect. 5 we discuss the association of the clumps with star-formation tracers; in Sects. 6 and 7 we derive the physical parameters of the clumps, from the molecular line emission and from the continuum emission, and we discuss the implications of the results for the structure of the clumps; in Sect. 8 we discuss the spectral energy distributions of the IR sources associated with the APEX continuum sources; in Sect. 9 we compare our results with studies of nearby galaxies; Sect. 10 contains our summary and conclusions.
2 Observational dataset
2.1 FCRAO
CO(1-0), C
O(1-0) and C
O(1-0) data
The data were obtained in the period from 2000 28th October to 7th November and in 2001 May, using the 14-m Five College Radio Astronomy Observatory (FCRAO) telescope, located near New Salem (Massachusetts, USA). The observations were performed with the SEQUOIA (Second Quabbin Observatory Imaging Array) 16 beam array receiver.
An area of about
was mapped in the 13CO(1-0) line. The system temperature was between 294 K and
680 K. The telescope beam size is approximately 46
at the
frequency of the observations, according to Ladd & Heyer (1996).
The C18O(1-0) and C17O(1-0) emission lines were observed over smaller regions: the C18O(1-0) line in three regions of about
(with 22
sampling, i.e. Nyquist),
in a diagonal direction through the center of the
13CO map (see Fig. 1) from North-East to South-West; the
C17O(1-0) line in the central region of about
,
on a 45
sampled grid (i.e. undersampled). The observations were performed in frequency switching mode.
The system temperature and beam sizes at these frequencies are reported in
Table 1.
In each molecular line, the same area was covered several times to
obtain
complete but independent maps of the whole region. Observations related
to the same pointing were first added together. The final maps are thus
the weighted average of all the data. The line intensities of all the
spectra were converted into main beam
temperature units, using the main beam efficiency values given in Table 1.
The original velocity resolution for the three lines was 0.2 km s-1, but the data were smoothed to a velocity resolution of 1 km s-1, to increase the signal to noise ratio. The final rms noise is 0.2 K per channel for the 13CO(1-0) line, 0.05 K per channel for the C18O(1-0) line and 0.02 K per channel for the C17O(1-0) line. However, part of the analysis was made at a velocity resolution of 0.5 km s-1, as explained below (see Sects. 3.2 and 4.1), to clearly distinguish and derive the parameters of some narrow features in the emission.
2.2 IRAM
CO(2-1), C
O(2-1) and C
O(2-1)
The data were obtained using the IRAM-30m telescope on Pico Veleta in its On-The-Fly (OTF) observing mode. The 13CO(2-1) and C18O(2-1) observations are described in López-Sepulcre et al. (2009). The C17O(2-1) line was observed in 2004 February, in frequency switching mode, on the same region. The system temperature was between 383 K and 517 K.
The rms noise is 0.8 K per 1 km s-1 channel for the 13CO(2-1) line, 0.9 K per channel for
the C18O(2-1) line and 0.3 K per channel for the C17O(2-1) line. The
telescope beam size at the frequencies of the observations is
11
. A summary of all the observational parameters is given in Table 1.
The data reduction was performed with the standard data analysis program
GILDAS, developed at IRAM and Observatoire de Grenoble.
2.3 APEX 870
m continuum data
Observations of the 870 m continuum emission
were made using the Atacama Pathfinder Experiment (APEX)
12 m telescope on July 2007. The data are part of the APEX Telescope Large Area
Survey of the Galaxy (ATLASGAL, Schuller et al. 2009), performed with the
Large APEX Bolometer Camera (LABOCA, Siringo et al. 2007, 2009). The rms
noise of the map is 40 mJy beam-1. The beam size at this wavelength is
.
The survey is optimized for recovering compact sources
and extended uniform emission on scales
larger than
is filtered out (Schuller et al. 2009).
2.4 BU-FCRAO Galactic ring survey
We retrieved FCRAO 13CO(1-0) observations of a slightly larger area (about
)
than the one sampled with our FCRAO
observations, from the Boston University-Five College Radio Astronomy
Observatory Galactic Ring Survey (hereafter BU-FCRAO
GRS
), a survey of the Galactic 13CO J=1-0 emission (see Jackson et al. 2006).
Table 1: Summary of the parameters of the spectral line observations.
The velocity coverage of the survey is -5 to 135 km s-1 for Galactic
longitudes
.
At the velocity resolution of
0.21 km s-1, the typical rms sensitivity is
K, which corresponds to the rms noise of our 13CO(1-0) observations, for a main-beam efficiency
of 0.48. The intensities of
the BU-FCRAO GRS data are in agreement with our data within
10%. We
used the BU-FCRAO GRS as a comparison with our data of the same line in the
regions covered by both observations and to cover the regions which have not
been sampled by our observations.
2.5 Spitzer data
Mid infrared observations of a large region around G19.61-0.23 were extracted
from the Spitzer Galactic plane surveys GLIMPSE (Benjamin et al. 2003) and
MIPSGAL (Carey et al. 2005). Data from 3.6 m through 24
m were
extracted directly from the Spitzer science archive, while for the 70
m
maps we used the latest processing from the MIPSGAL team which substantially
improved the quality of the maps as compared with the standard pipeline results (Carey et al. 2009).
All the data were analyzed with the KVIS tool, which is part of the KARMA suite of image visualization tools (Gooch 1996).
3 Morphology of the large-scale molecular line emission
Figure 1 shows the FCRAO 13CO(1-0) integrated intensity map overlaid over a larger area map of the 13CO(1-0) emission from the
BU-FCRAO GRS. The two maps are integrated over the same velocity range
(25-77 km s-1). The figure, at the angular resolution of
46
,
highlights the complex structure of the molecular gas.
The colored symbols in the figure indicate the positions of the known
sources
in the molecular complex associated with G19.61-0.23. A summary of all
these observations with associated references is given in Table A.1 (only available in electronic form).
The large scale morphology and extent of the molecular gas can be seen. The
main cloud of the complex (defined as cloud 2 in Sect. 3.2 and
highlighted by the larger magenta ellipse in Fig. 1) contains
G19.61-0.23, which is identified in the center of the field, around RA(J2000) = 1827
38
and Dec(J2000) =
-11
56
17
.
This main cloud is also seen in the central region of the C18O(1-0)
velocity-integrated map (Fig. A.1 available in electronic form),
as well as in all other tracers of star formation, such as
masers, HII regions and IR emission (see Table A.1). A good
correlation between the 13CO(1-0) and C18O(1-0) emission is seen also in the other two regions sampled in the C18O(1-0) line, which present the same morphology as the 13CO(1-0) emission.
3.1 A closer view of the molecular line emission
Observations of both transitions of all three CO isotopologues were performed only in the central region of about
(17 pc
13 pc), containing the main complex of the molecular emission.
Figure 2 shows in the top panel the FCRAO 13CO(1-0),
C18O(1-0) and C17O(1-0) maps, integrated between 32 and 50 km s-1, in the central region covering the main cloud of the complex. The bottom panels of Fig. 2 give the IRAM-30m 13CO(2-1), C18O(2-1) and C17O(2-1) maps, integrated over the same velocity range.
![]() |
Figure 2:
Top: FCRAO emission maps, integrated between 32 and 50 km s-1, of the central
|
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In the 13CO(1-0) and C18O(1-0) emission maps, the molecular gas is concentrated within two main clumps (clump co1 and clump co2, see Sect. 4.1). This is not confirmed in the C17O(1-0) emission map, where the two peaks are not clearly distinguished. This is maybe affected by the low sampling of the region in the C17O(1-0) line. The same morphological characteristics are confirmed in the 13CO(2-1) line, where the two clumps can be clearly distinguished, and partially in the C18O(2-1) line, where clump co2 is still visible, although very faint. In the C17O(2-1) emission, clump co2 is even fainter and, due to the lower signal to noise radio, it is hard to be distinguished.
3.2 Kinematics of the emission and cloud definition
Figure A.2 (available in electronic form),
shows the
large-scale channel maps of the 13CO(1-0) emission (i.e., the emission in 2 km s-1 wide velocity intervals), which reveals the
complex spatial and velocity structure of the molecular gas. The contours of the emission are from 10
(
K per channel) in steps of 5
.
The numbered crosses represent the molecular features (clumps), which we identified in the emission (see Sect. 4.1).
Throughout this paper we will use the word ``cloud'' for the four main molecular complexes described below and identified in the 13CO(1-0) emission and ``clump'' for the smaller scale structures resolved within the four main clouds (see Sect. 4.1).
We distinguish four velocity intervals, corresponding to the main features (clouds) that can be identified in the molecular gas. These are four molecular clouds, well separated in velocity and/or spatial distribution. The main parameters of these four molecular clouds are given in Table 2 and Fig. 3 shows the integrated emission from each of them.
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Figure 3: Maps of the four molecular clouds identified in 13CO(1-0) emission, integrated over the velocity channels of emission of each cloud (see Col. 2 of Table 2). The FCRAO 13CO(1-0) emission from our data is represented by the white contours and is overlaid on the 13CO(1-0) emission from the BU-FCRAO GRS. |
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- Cloud 1
- (28-32 km s-1): the lowest velocity channels show no
significant emission, with the exception of one narrow feature (clump co4, see Table 3), which
is clearly visible above the 10
level in the 29 km s-1 velocity channel. In order to analyze this feature, we created a 13CO(1-0) data cube with a velocity resolution of 0.5 km s-1.
- Cloud 2
- (32-50 km s-1): this is the velocity range of the main complex of the emission, which is the GMC surrounding G19.61-0.23. It is represented by the larger magenta ellipse in Fig. 1, with linear semi-axes of 49 pc and 15 pc. All the emission is spatially concentrated in the same area, with an elliptical shape. This suggests that the emission is all at the same distance, i.e. at the distance of the main central region at 12.6 kpc. Several molecular features can be distinguished in the emission, both in the spatial and velocity distributions. The identification of the single clumps is discussed in Sect. 4; in particular, one of them, clump co5 (see Table 3) has been identified using the BU-FCRAO GRS, because it is at the edge of our observed region.
- Cloud 3
- (54-63 km s-1): these velocity channels show several features in the emission as well, spread over 10 km s-1. Also, in this case the emission is all concentrated in the same area, in the north-west of the sampled area, which suggests that it is all at the same distance. The smaller ellipse in Fig. 1 delineates the approximate outline of this GMC. It is worth noting that the narrow feature, seen only in the 60 km s-1 velocity channel (clump co19, see Table 3), has been analyzed with the higher velocity resolution of 0.5 km s-1.
- Cloud 4
- (64-73 km s-1): the highest velocity channels show four main features in the emission and two of them (clump co14 and clump co17) have been identified using the BU-FCRAO GRS. The emission at the east edge of the map has not been included in the further analysis.

Table 2: Summary of the parameters of the four molecular clouds identified in the FCRAO 13CO(1-0) emission.
Finally, we point out that the association of the emission, which is close in velocity and position, as part of the same GMC is fairly arbitrary and has consequences for the distance estimates of the different clouds.
4 Identification of the clumps
4.1 The
CO emission
Source identification was based on the visual inspection of all velocity channels of the FCRAO 13CO(1-0) map of the large-scale emission and of the BU-FCRAO GRS.
The detection threshold used for the identification of the different clumps in the 13CO(1-0) emission was set to 10
(
K).
We identified 19 clumps in the FCRAO 13CO(1-0) emission, which are
indicated in Fig. A.2,
in the channel corresponding to
their peak emission (see also Table 3).
The clumps co5, co10, co12, co11, co14 and co17, as shown in Fig. A.2, are at the edges of the sampled region
and we thus used the BU-FCRAO GRS data to derive their physical parameters for the analysis.
The angular extent of each identified clump was determined by finding the area, A1/2, within the
50% intensity contour in the FCRAO 13CO(1-0) maps, integrated
over the channels of the emission,
and computing the equivalent radius of a circle with the same area.
The angular diameter of each clump was derived
by deconvolving the diameter, assuming source and
beam to be Gaussian: thus
.
The derived angular sizes are given in Table 3.
All the identified clumps have deconvolved sizes which are larger than
the beam size of the observations, indicating that they are well
resolved.
Table 3: Physical parameters of the clumps identified in the FCRAO 13CO(1-0) emission.
As explained above, we computed both the near and far distances for each of the four velocity intervals of the emission, corresponding to the four main molecular clouds in the whole region. Therefore, assuming that each of the four molecular clouds is made from material at the same distance, which is reasonable given the localized morphology of the emission, each clump is assumed to be at the same distance as the cloud it belongs to (see Table 3). This leaves the question of the ``near-far ambiguity'', which we discuss in Sect. 5.
The spectrum of the emission of each identified clump was obtained by
integrating the 13CO(1-0) data cube in the channels of the emission of the clump, over the area
enclosed by the deconvolved 50% contour level of the
13CO(1-0) emission. The spectra of clump co4 and
clump co19 have been derived from the higher velocity resolution
(0.5 km s-1) data-cube, as discussed
in the previous section. The parameters of each clump were determined
by
fitting a Gaussian profile to each produced spectrum. Line profiles
showing more than one velocity component were analyzed by fitting more
than one Gaussian component, in order to remove the contribution to the
emission by other clumps along the line of sight from the emission
coming from the
clump of interest. The results of this analysis are reported in
Table 3.
4.2 The continuum emission
Figure 4 shows the APEX 870 
![]() |
Figure 4:
APEX 870 |
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Most of the APEX continuum sources have counterparts in one of the FCRAO 13CO(1-0) clumps (see also Fig. A.3 available in electronic form), with the exception of sources C8 and C9. Source C8 is associated with significant emission in the 13CO(1-0) line, but over a region slightly to the south of C8 (see Fig. A.3). The 13CO(1-0) emission in this case corresponds to 13CO clump co7, which ``contains'' the APEX sources C8 and C7. We thus assume for both C8 and C7 the distance corresponding to 13CO 8. C9 is associated with 13CO emission at 62 km s-1 and hence probably to cloud 3.
Table 4:
Physical parameters of the sources identified in the APEX 870 m continuum emission.
Moreover, given the lower resolution of the 13CO data, the continuum sources C3 and C4 correspond both to clump co3 in the FCRAO 13CO(1-0) emission.
Column 8 of Table 4 indicates the counterpart, if any, of each APEX continuum source,
as identified from the comparison between the 13CO emission and the APEX continuum emission.
It is worth noting that the two maps (13CO map and APEX continuum maps)
have significantly different resolutions, with the APEX resolution
being
at 870
m and the FCRAO resolution being 46
at the
frequency of the 13CO(1-0) line.
Therefore it is not surprising that the sources identified in the APEX continuum emission are more compact
than the 13CO clumps (as seen also in Fig. A.3).
Moreover, the 870
m continuum emission
probably traces dense cores embedded in the 13CO(1-0) clumps.
For the APEX continuum sources that have a counterpart in the FCRAO 13CO(1-0) emission, we assume as distance the one of the corresponding 13CO(1-0) clump. The obtained distances are reported in Cols. 9-10 of Table 4 (see Sect. 4.1 and Table 3).
5 Association with infrared emission
One of our aims is to compare the properties of the molecular
clumps with and without star formation within them. With this in mind, we have compared images from the GLIMPSE (Benjamin et al. 2003) and MIPSGAL mid
infrared surveys (Carey et al. 2005) with both ATLASGAL maps and our FCRAO
13CO data (supplemented by the BU-FCRAO GRS). It is worth recalling that
the MIPSGAL 70 m survey has a ``beam'' of
,
which is comparable to that of ATLASGAL. Moreover, the GLIMPSE 8
m data
traces PAH emission excited by UV from OB stars close to GMCs whereas the 24
m MIPSGAL radiation often traces dust heated by embedded
proto-stellar objects. Also, the
4.5
m GLIMPSE data has been found often to trace molecular hydrogen
emission associated with outflows. In Fig. A.3,
we superpose FCRAO 13CO and ATLASGAL maps to Spitzer images at 3.6, 8 and 24
m.
One sees here that there are several ATLASGAL sources associated with strong continuum emission in the Spitzer bands. Table 5 summarizes these associations (within 1)
as well as the information about maser emission and HII regions close to the positions of continuum emission.
Table 5:
Association (within 1)
of the APEX 870
m sources with active star-formation tracers, such as Spitzer 3.6
m, 8
m and 24
m; water, methanol and OH masers; HII regions; and IRAS sources.
Not surprisingly, there is strong mid infrared
emission from the vicinity of clumps C1 and C2 which are associated
with the HII region complex G19.61-0.23 but one also notes strong
emission associated with the C7/C8 complex and with C12. In all of
these cases, it is reasonable to assume that there is an embedded
cluster of young stars producing ultra-violet radiation responsible for
exciting the PAH and small grain emission observed at 8 and
24 m. Less obvious in Fig. A.3 is the fact that in many cases there are point-like (<6 arcsec.) continuum sources at 24
m close to the
ATLASGAL 870 micron peaks. It is noticeable that there are 3 ATLASGAL
sources without clear 24
m counterparts and we presume this implies a
relatively low dust temperature (below 25 K). These are perhaps similar to the
infrared dark clouds (IRDCs) observed associated with star-forming regions
closer to the sun but lacking a strong infrared background. We note also that
we have searched without success for extended emission in the 4.5
m IRAC
band of the type often found associated with outflows in nearby star-forming
regions. Finally, all the ATLASGAL sources show association with extended
Spitzer 8
m emission, except source C14, which corresponds to the
13CO clump co14, and the 13CO clump co17 (see Table 3). Both clumps correspond to IRDCs seen against the 8
m emission and identified by Simon et al. (2006a,b).
The above information suggests to us that all the ATLASGAL clumps but C14 are at the ``far'' (around 12 kpc) distance rather than the near (around 4 kpc). This is likely to be true for the clumps with velocity around 42 km s-1 (cloud 2 in the nomenclature of Table 2), as shown by Kolpak et al. (2003) and confirmed by Anderson & Bania (2009). We therefore use the far distance as a working hypothesis in what follows for all clumps, with the exception of continuum emission clump C14 and clumps co14 and co17, seen in 13CO(1-0) emission, for which we used the near distance.
We demonstrate the association between ATLASGAL sources and
24 m MIPSGAL sources in Fig. 5 where we plot a histogram
(upper panel) of the angular separations between the 870
m
peak and the nearest 24
m source.
![]() |
Figure 5:
Top: histogram of the distances of the APEX 870 |
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To estimate the reliability of the associations of the infrared
sources with the millimeter continuum cores, we have simulated randomly
located samples of 14 cores and associated them with the closest infrared
source. The bottom panel of Fig. 5 shows the
distribution of the average separation between the infrared sources and the
random sample of millimeter cores.
One sees that the histogram for the real millimeter cores has
a strong peak for separations of less than 10
(roughly half the APEX beam) which is not present for the random samples.
A statistical test on the two histograms shows that there is only a
0.1% probability that they are drawn from the same parent
distribution. Indeed, the simulation shows that one roughly expects 2 chance coincidence within
15
whereas there are 11 APEX sources within
15
of the nearest Spitzer 24
m source.
We thus conclude that, with the exception of the three sources with separations larger than 30
,
the associations of the ATLASGAL 870
m cores with their neighboring Spitzer 24
m sources are real.
6 Physical parameters of the clumps
6.1 The
CO(1-0) emission
The central
is the only
region where we have observations of the J=1-0 and the J=2-1 transitions of
the three isotopologues and therefore the only region where we can derive the
optical depth of the 13CO(1-0) line. The optical depth,
,
of the 13CO(1-0) transition can be estimated from the line
ratio of the two isotopes, 13CO(1-0) and C18O(1-0). We derive
values for the mean line optical depth of
0.5 suggesting
that while the line peak may be moderately optically thick
(
at most),
the integrated 13CO(1-0) emission is optically thin over the
central region. This is also consistent with the observed lack of variation
of the integrated (2-1)/(1-0) line ratios,
as a function of the integrated line intensities (Fig. 6).
The points in the plots correspond to the values of the line ratios taken over 46
beams.
![]() |
Figure 6:
Integrated (2-1)/(1-0) line ratios over the central
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Given that the 13CO emission at the peak of the line is close to be optically thick, as an estimate of the excitation temperature of the molecular gas we assumed 20 K, the peak line brightness temperature as measured in the clump with the highest optical depth. In the following we have assumed this excitation temperature for all the clumps.
The total column density of the 13CO molecule for each identified clump
was derived using the J=1-0 transition, under the assumption of local
thermodynamic equilibrium (LTE) at an excitation temperature
.
The column density of this molecule, in the optically thin limit, is given by
where:
![]() |
(2) |
(see Eqs. (A1) and (A4) of Scoville et al. 1986).





The total LTE mass of gas in the identified clumps,
,
can be computed from the 13CO column density as follows:
(Scoville et al. 1986), where [H2]/[13CO] is the abundance ratio of molecular hydrogen to 13CO,




Table 6: Masses and surface densities of the clumps identified in the FCRAO 13CO(1-0) emission.
The estimated gas masses can be compared with the masses computed under
the assumption of virial equilibrium for an homogeneous sphere,
neglecting contributions from the magnetic field and surface pressure:
![]() |
(4) |
(e.g. MacLaren et al. 1988), where


We also computed the surface density,
), of each clump,
using both the LTE masses and the virial masses and they are given in Cols. 4
and 7 of Table 6, respectively. The surface density is a measure of pressure for virialized clouds, since
the gas pressure needed to support a virialized cloud
against gravity in the absence of other forces is of the order G
,
independent of the shape of the cloud (e.g. McKee et al. 1993; Bertoldi & McKee 1992).
From Table 6, one sees that the surface densities derived from
13CO (
), which are essentially distance independent, vary in the range 0.01 to 0.1 g cm-2,
which is roughly equivalent to a range of visual extinction 2.5 to
25 mag for a local ISM dust-to-gas ratio. This is comparable to
the surface density averaged over the whole cloud 2 GMC (see
Table 8 and Sect. 9) and so
these clumps are mostly at pressures of the order typically experienced in the GMC. The masses range from
to
and thus overlap with the range studied by Williams & Blitz (1998) in the Rosette cloud and in G216-2.5.
For each clump we also
derived an average density, using the deconvolved half power sizes we
determined from the 13CO(1-0) emission (see Col. 5 of Table 3). The values we obtained are reported in Cols. 5 and 8 of Table 6, respectively from the LTE masses and the virial masses, and are in the
range 102-104 cm-3.
These values can be compared with the results from LVG models,
based on the approach of de Jong et al. (1975, spherically symmetric
homogeneous model with linear dependence of v upon r, collisional
rates from Flower & Launay 1985#.
Trapping has been accounted for
using
as an independent variable where
can stand for any of the CO isotopologues of interest and we
scale between them using the ratios given in Table 3
(line-width assumed to be the observed value of 5 km s-1). In practice,
trapping corrections are only of importance for 13CO and we
find that the observed excitation, from the integrated (2-1)/(1-0) line
ratios (see Fig. 6), is compatible with T=30-40 K and
n(H
cm-3 for the C18O and C17O lines and with T=25-30 K and n(H
cm-3
for the 13CO line. The expected densities from LVG models are thus slightly larger than the average densities reported in Table 6.
However, this can be explained with a moderate amount of clumping in the region.
6.1.1 The [
O]/[
O] ratio in G19.61-0.23
Using the FCRAO J=1-0 and IRAM J=2-1 data of C18O and
C17O, we can derive the 18O/17O isotopic ratio in the central
region centered on G19.61-0.23.
Assuming that the two isotopologues have the same excitation temperature and
that C18O is optically thin, we derive an average 18O/17O
isotopic ratio of
for clump co1 and
for clump co2, from the line integrated intensity ratio between the FCRAO J=1-0 transitions of C18O and C17O,
and of
for clump co1 and
for clump co2, from the line ratio between the IRAM J=2-1 transitions of C18O and C17O.
The values that we find are marginally consistent with the value discussed by Wilson & Rood (1994), .
Moreover, we find a quite constant isotope ratio over the central
region, including clump co1 and clump co2, in both
transitions.
6.1.2 CO selective photodissociation
Figure 7 shows the line ratios for the CO isotopes for the central region of our map, as a function of the inferred H2 column density. The points in the plots correspond to the values of the line ratios taken over every beam. At high values of line intensity (high column density), we do not see a variation of the line ratios. This is consistent with the fact that the integrated line intensities are mostly optically thin. At low column densities, there is a tendency of an increase of the 13CO(1-0)/C18O(1-0) ratio, which is also seen in the ratio of the (2-1) lines. This trend is consistent with the expectations for selective photodissociation at the edges of the clouds (see e.g. van Dishoeck & Black 1988).
![]() |
Figure 7: The points in the plots correspond to the values of the line ratios taken over every beam, in regions of the map with high enough S/N ratio (larger than 5). Top left: ratio between FCRAO 13CO(1-0) emission and C18O(1-0) against H2 column density derived from the C18O(1-0) line intensity. Top right: ratio between IRAM 13CO(2-1) emission and C18O(2-1) against H2 column density derived from the C18O(2-1) line. Bottom left: ratio between FCRAO C18O(1-0) emission and C17O(1-0), against H2 column density derived from the C18O(1-0) line intensity. Bottom right: ratio between IRAM C18O(2-1) emission and C17O(2-1) against H2 column density derived from the C18O(2-1) line. |
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6.2 The continuum emission
To derive the angular extent of each identified source, we used the same method
as described in Sect. 4.1 for the FCRAO 13CO(1-0) emission.
The derived angular sizes,
,
are shown in Table 4 (Col. 4).
As already pointed out in Sect. 4.2,
all the continuum sources that have a 13CO
counterpart (see Col. 8 of Table 4) have smaller sizes than
the respective 13CO
clumps. This is possibly indicating that the continuum sources trace
the densest cores within the CO clumps. The integrated flux densities
of the continuum sources are given in Col. 7 of Table 4.
Dust emission is generally optically thin in the sub-millimeter continuum.
Therefore, following Hildebrand (1983)
and assuming constant gas-to-dust mass ratio equal to 100,
optically thin emission and isothermal conditions, the total gas+dust
mass of each source is directly proportional to the continuum flux
density integrated over the source:
where











7 Stability of the clumps
Figure 8 shows the ratio between the virial mass and the 13CO LTE mass for each of the 19 clumps identified in the FCRAO 13CO(1-0) emission, assuming the far distance for all clumps but clump co14. The filled triangles indicate the clumps associated with active star-formation tracers (see Table 5) and the empty squares represent the clumps without star-formation tracers. The ratio is larger than 1 for all the sources but 3 (clumps co4, co5 and co16), which indicates that the clumps range from gravitational unbound to unstable in few cases, with an average value for the ratio of about 3. Most of the clumps thus seem to be transient molecular structures, as highlighted from the 13CO(1-0) analysis. This result does not seem to depend on whether the clumps are associated with star formation (see however Williams & Blitz 1998; Williams et al. 1995).
We can compare this result with the study of Fontani et al. (2002), who observed the molecular clumps associated with 12 ultracompact (UC) HII regions in CH3C2H and found that the clumps are unstable against gravitational collapse (see also Cesaroni et al. 1991; Hofner et al. 2000 for the C34S and the C17O lines).
However, G19.61-0.23, also studied by Fontani et al. (2002), is one of only two sources with
ratio very close to one.
Therefore, in order to investigate the discrepancy between Fontani et al. (2002) and us,
we repeated the analysis using the C17O(2-1) from our IRAM-30m observations, for the two central clumps co1 and co2.
We find for both clumps a much smaller
ratio, which is <1 for clump co2. We thus find evidence that the
ratio changes with the tracer: the gas traced by the 13CO seems to be more virialized than the gas traced by the C17O.
Since C17O (as well as C34S and CH3C2H) traces higher density gas than 13CO, our result seems to indicate that the clumps are globally in equilibrium but locally unstable.
New observations of all the identified clumps in high density tracers are needed to further investigate this point.
![]() |
Figure 8:
Plot of the ratio between the mass derived assuming virial equilibrium (
|
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It is worth to further discuss clump co5, which corresponds to continuum
emission source C5, an interesting case
because of its small virial mass compared with its LTE mass.
From Fig. 8,
the clump seems not to be in virial equilibrium against gravitational
collapse. Moreover, it appears also to be associated with active star
formation (see
Fig. A.3 and Table 5), which excludes the possibility that we overestimated the temperature in computing the LTE mass of the clump, from Eq. (3). A possible explanation for the small ratio
of clump co5 is that the magnetic field might be playing an important role in stabilizing the clump.
It is also interesting to compare the continuum masses (Col. 10 of
Table 4) of all the continuum sources that have a 13CO
counterpart with the LTE masses of the respective 13CO clumps (Col. 4 of Table 6). All the continuum sources with a 13CO counterpart have
,
which is probably due to the fact that the 13CO
clumps have larger sizes than the respective continuum counterparts.
However, there are three exceptions: the continuum source C1, which is
associated with 13CO clump co1; the continuum source C7, which is
associated with 13CO clump co7; and the continuum source C12, which is associated with
13CO clump co12. A possible explanation might be that we underestimated the
temperature for these three sources, therefore we overestimated the continuum
mass and we underestimated the LTE mass. This explanation is consistent with
the association of the three sources with active star-formation tracers, in
particular with Spitzer emission at 3.6
m, 8
m and 24
m.
Therefore we obtain the same result on the gravitational stability of the clumps also from the continuum masses.
8 SED and luminosities
In Sect. 5 we demonstrated that associations
between the ATLASGAL sources and the 24 m MIPSGAL emission exist.
In the following we assume that these associations indeed
are real and combine the Spitzer and
APEX results in order to derive crude spectral energy distributions from the
24 and 70
m MIPSGAL data and ATLASGAL 870
m observations.
We have integrated the MIPSGAL 24 and 70 m images over the area of
ATLASGAL sub-mm continuum emission in order to derive the spectral energy distributions shown in Fig. 9.
![]() |
Figure 9:
Spectral energy distributions (SEDs) of the APEX 870 |
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Table 7:
Properties of the ATLASGAL sources with a counterpart in the mid-infrared emission, derived by fitting the 870 and 70 m points with a modified black body.


One useful application of these results is to consider the inferred
luminosity to gas mass ratio, L/M, for the
ATLASGAL sources. This is a distance independent parameter and hence
useful for comparison with extragalactic star-formation indicators
(see Plume et al. 1992,1997). Since bolometric luminosity is a rough measure of star formation rate (for a given initial mass function, IMF),
L/M is a measure of the gas exhaustion timescale of the clumps, which is typically much larger than the
free fall time (see Krumholz & McKee 2005); hence, an indicator of the
clump evolutionary timescale.
One might expect L/M to correlate with the surface density
(also a distance
independent quantity roughly speaking and a measure of pressure for
virialized clumps) and we thus show in Fig. 10 a plot of
L/M against
for our sample.
One expects L/M to increase with time as molecular gas is converted
into stars as star formation proceeds. One might
also expect star formation rates to increase in regions of high pressure or
surface density.
It is interesting in this context that Sridharan et al. (2002)
find evidence of an increase of L/M going from regions without
3.6 cm radio emission (at the mJy level with the VLA) and clumps
associated with UC HII regions. It would be useful to test this
result for more homogeneous samples similar to the present one.
We note, however, that Faúndez et al. (2004) find such result marginal and offer
an alternative interpretation of L/M as an indicator of the luminosity
of the most massive star embedded within the clump. However, these results
are based on much less sensitive radio continuum measurements, using a
highly inhomogeneous sample of objects
with distances varying over an order of magnitude.
It is clear that larger samples
with both high angular resolution far-infrared measurements and
sensitive radio observations are needed to make further progress in
this area.
A surprising feature of our results (see Fig. 10) is that low column density sources (below 0.5 g cm-2) appear to have higher L/M than high column density sources, which is hard to understand theoretically. However, this finding is marginal given the poor statistics.
![]() |
Figure 10:
Luminosity to mass ratio, L/M, for the 870 |
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These estimates for L/M can be compared with the results of Wu et al. (2005)
who used HCN as a dense gas tracer in order to estimate the star forming
efficiency both in Galactic cores and extragalactic star-forming
regions. From a survey of 31 Galactic cores, one can derive a median
L/M ratio of 63 /
for regions with luminosities above
;
the ratio for extragalactic star-forming regions is similar. Below
,
the ratio drops rapidly. Our
median value of L/M from the black body fit is roughly a factor of 4 lower but our sample is small and straddles the
limiting value for the Wu et al. (2005) relation. However, given both
the dispersion in the Wu et al. (2005) result and the uncertainties in our
determinations of both L and M, we conclude that one needs both more
complete SEDs and more reliable mass determinations to make further progress.
The former will be undertaken by future surveys with HERSCHEL (such as
HI-GAL; Molinari et al. 2010)
but the latter will require careful calibration and intercomparison of
the various approaches to determining clump masses.
9 Comparison with extragalactic observations
G19.61-0.23 is one of the most luminous (
,
see Sect. 1) known Galactic massive star-forming regions and therefore
one of the best templates to study locally the
starburst phenomenon.
Several high resolution studies have been carried out in this region as well as
in other well known Galactic high mass star-forming regions.
However, the aim of this work is to analyze the
large-scale properties and physical conditions of the molecular gas in the region
and the implications for extragalactic studies of nearby starburst galaxies.
Of particular interest are the youngest extragalactic embedded super star clusters (SSCs), which have been seen in merging systems (e.g. Whitmore 2002) and in some dwarf irregular galaxies (e.g. Elmegreen 2002; Johnson & Kobulnicky 2003) and have been identified by the free-free radio emission from their associated HII regions (e.g. Johnson & Kobulnicky 2003). One can see that the molecular clouds associated with the SSCs show lower surface densities than their end product (the star clusters). Since extragalactic studies are mostly done with single-dish telescopes and in low J transitions of CO, this result may be due to: (1) the limited linear resolution reached with current facilities; and/or (2) the molecular tracers used in the extragalactic studies, which are not tracing the real active sites of cluster formation, but rather lower density associated material.
In order to analyze the effect of low angular resolution in extragalactic studies, we compared the results from our 13CO
low resolution observations of the Galactic region G19.61-0.23 with the
physical parameters that have been found for some nearby extragalactic
starbursts, in particular with CO(2-1) high angular resolution
observations of Henize 2-10, a dwarf irregular starburst galaxy at
the distance of 9 Mpc (H0 = 75 km s-1 Mpc-1, Vacca & Conti 1992; Kobulnicky & Johnson 1999). We observed Henize 2-10 (Santangelo et al. 2009) at high angular resolution (
,
which corresponds to a linear resolution of
pc at the distance of Henize 2-10),
revealing a rich population of molecular clouds with estimated masses and surface densities
systematically larger than those measured in our Galaxy and we found possible evidence that the super
star clusters are associated with very massive and dense molecular cores.
We also compared our results with studies of M 31 and M 33 from
Sheth et al. (2008) and Rosolowsky et al. (2003). They present CO(1-0) observations of the two spiral galaxies made with the BIMA array at a linear resolution of
20 pc.
9.1 The total
CO(1-0) emission
The total region of G19.61-0.23 that we sampled in 13CO(1-0) with FCRAO is about
large (using the data from the BU-FCRAO GRS to cover the
regions which were not sampled by our observations),
which corresponds approximately to a size of 98 pc at the distance of the main complex of G19.61-0.23 (12.6 kpc).
This value corresponds approximately to the size of each cloud identified in the SMA CO(2-1)
emission of Henize 2-10 (see Tables 8 and 3 of Santangelo et al. 2009).
We can thus compare the properties of the total FCRAO 13CO(1-0) emission from the main cloud of the complex, containing G19.61-0.23 (cloud 2; see Sect. 3.2 and Table 2),
with the physical parameters of the 14 clouds resolved in the SMA CO(2-1) emission from Henize 2-10.
With this aim,
we analyzed the total FCRAO 13CO(1-0) emission from cloud 2
as if we were observing a single molecular cloud
at the same linear resolution with which we observed Henize 2-10 (
pc).
In particular, we integrated all the 13CO(1-0) emission from the BU-FCRAO GRS data of cloud 2,
between 32 and 50 km s-1
and smoothed the derived spectrum to the same velocity resolution
obtained in the SMA observations of Henize 2-10 (5 km s-1).
The physical parameters of cloud 2 ``observed'' in this fashion are given in Table 8, where
the FWHM line width is listed in Col. 1.
We list, for comparison, in Table 8 also the parameters of one of the clouds resolved in the SMA emission from Henize 2-10.
Table 8: Summary of the parameters of the total integrated 13CO(1-0) emission of the GMC surrounding G19.61-0.23 and of a typical cloud in Henize 2-10, from SMA observations.
We note that the line-widths (Col. 1) are computed from the original total integrated 13CO(1-0) spectrum, before smoothing to the resolution of 5 km s-1, and that the total emission is computed by integrating the emission from the channels relative to the emission from cloud 2 (between 32 and 50 km s-1). From the comparison with the typical line widths of the clouds identified in Henize 2-10 (see Table 8), cloud 2 has a line width a factor of 2-3 smaller than the extragalactic clouds.Following the same approach described in Sect. 6.1, we computed the virial mass and the LTE mass of
cloud 2, assuming that: (1) the 13CO(1-0) emission is optically thin, as for the extragalactic clouds; (2) the cloud
is at a distance of 12.6 kpc; and (3)
K.
We also computed the surface density
of the cloud, using both the virial mass and the LTE mass.
A summary of the derived masses and surface densities of cloud 2
is given in Table 8.
The derived masses are smaller than the masses derived for the CO clouds in Henize 2-10, which are of the order of a few 10
.
In Fig. 11 we show our results from Tables 6 and 8 on a mass-surface density plot similar to that discussed by Tan (2007).
![]() |
Figure 11:
Surface density,
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The blue and cyan squares are the values for the clouds in Henize 2-10,
respectively, from the molecular and virial masses, which are
in the same general area of the diagram as Galactic GMCs, though with somewhat higher masses and surface densities.
Moreover, due to our limited
angular resolution, the surface density may well be considerably
underestimated.
The black star represents the position of cloud 2
from the LTE mass (see Table 8).
This cloud appears in the same area as the Galactic GMCs and the GMCs in M 31 and M 33, which
confirms that there are no significant differences in the cloud properties of the two
nearby spiral galaxies and the Milky Way (e.g. Rosolowsky et al. 2003; Sheth et al. 2008).
However, cloud 2 shows lower surface density than the clouds in
Henize 2-10, which
suggests that the clouds in Henize 2-10 might be different from
the GMCs in the Galaxy as well as from those in M 31 and
M 33. Finally, the black circles represent the position in the
plot for the clumps resolved in cloud 2 (clumps co1, co2,
co3, co6, co8, co9 and co5), from the LTE masses. It is evident from
the plot that the clumps resolved in cloud 2 have higher pressure
than the whole molecular cloud 2, seen at low angular resolution.
In particular, from the whole mass and surface of cloud 2 and the
masses and surface of the clumps resolved in the 13CO(1-0)
emission from cloud 2, we can derive a filling factor in area and
in mass for the dense molecular gas in the GMC of G19.61-0.23, computed
respectively as:
and
,
where Ai and Mi are the area and mass of every clump resolved in cloud 2 (i.e. clumps co1, co2, co3, co6, co8, co9 and co5;
see Table 6) and
and
are the area and mass of cloud 2 (see Table 8).
We find that the fraction of dense molecular gas in cloud 2 is
about 10-20% (respectively from the LTE and the virial masses).
Extrapolating those results to the extragalactic context, assuming that
the fraction of the area and the mass of a GMC which is in the form of
dense gas is the same as in the Galactic context, we would expect each
cloud identified in Henize 2-10 to be resolved in several
molecular clumps which account for a total dense molecular gas mass up
to 10
,
each having a surface density up to 1.5 g cm-2. It seems thus reasonable to assume that the clusters in Henize 2-10 form from small parsec sized clumps at much higher
surface density and pressure than the rest of the GMC and than the typical Galactic clumps.
Therefore, we suggest that finding molecular clouds in Henize 2-10 with lower surface densities than their end product, the SSCs, might be due to the low linear resolution which is currently available. High sensitivity observations at higher resolution are needed to confirm this scenario, as well as observations of higher density tracers.
10 Summary and conclusions
In this paper we have presented single dish observations of the
molecular gas and the sub-mm continuum of the high-mass star-forming
region G19.61-0.23. Our observations, with a spatial resolution of
about 2.8 pc at the adopted distance of 12.6 kpc, reveal a
population of molecular clumps. The physical parameters of the
identified clumps show a spread of virial parameters
,
ranging from gravitationally unstable
to unbound. These results seem to be independent of the presence or otherwise of
star-formation indicators in the cloud, which is in slight contrast to results for less distant GMCs (e.g. Williams et al. 1995; Williams & Blitz 1998).
One needs however more precise mass determinations for the clumps in
G19.61-0.23, using high density molecular tracers, such as CS.
Analogously, it would be very useful to obtain molecular line data for
the ATLASGAL continuum sources.
Towards the ATLASGAL continuum sources, we have studied the
association with mid-infrared emission and found that most ATLASGAL
sources have counterparts in the mid-infrared emission at the peaks of
the sub-millimeter continuum emission.
For those sources we derived crude spectral energy distributions and
estimated the luminosities and dust temperatures. We find that the
majority of the continuum sources are associated with star-forming
regions of luminosity 1-
and gas masses 400-6000
.
The luminosity to gas mass ratio, L/M, is in the range 10-100
with some evidence for a fall off for high mass clumps. The ATLASGAL sources are clearly good tracers of star formation.
We compared our results for the Galactic luminous high-mass star-forming region G19.61-0.23 with a previous extragalactic study of a dwarf starburst galaxy Henize 2-10. We find that the main cloud in G19.61-0.23 has physical properties comparable with the typical galactic GMCs and with the GMCs in M 31 and M 33. However this cloud shows less extreme properties than the clouds identified in Henize 2-10, in particular smaller surface densities and masses.
The new generation of telescopes is needed to address these questions. They will also allow to observe with higher sensitivity higher density tracers, to see the real sites of active star formation.
AcknowledgementsWe thank the APEX support astronomers for performing excellent service mode observations at APEX. The FCRAO observations were partially acquired by Carla Maxia. This work was partially supported by ASI-INAF contracts. Leonardo Bronfman acknowledges support from Center of Excellence in Astrophysics and Associated Technologies (PFB 06) and by FONDAP Center for Astrophysics 15010003.
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Online Material
Appendix A: Online Material
In this appendix we present additional material, which may be useful. In particular, we show the list of all the sources in the sampled field, from the SIMBAD Astronomical Database (Table A.1); the integrated intensity map of the C18O(1-0) emission from our FCRAO observations (Fig. A.1); the channel map of our FCRAO 13CO(1-0) data (Fig. A.2); and finally the overlay between the 13CO(1-0) clumps and the APEX continuum clumps with the Spitzer emission at 3.6, 8 and 24

Table A.1: List of the sources in the sampled field, from the SIMBAD Astronomical Database. Columns (1)-(2): coordinates (J2000.0); Col. (3): distance from the peak emission of the associated clump (see Sect. 4.1); Col. (4): References.
![]() |
Figure A.1:
FCRAO intensity map of the C18O(1-0) emission, integrated between 25 and 57 km s-1. The contour levels are from 10 |
Open with DEXTER |
![]() |
Figure A.2:
Channel map of the BU-FCRAO GRS 13CO(1-0) data in grey scale and our FCRAO 13CO(1-0) emission in black contours.
Center velocities of the channels are indicated in the bottom left
corner of each panel and increase in steps of 2 km s-1. Contour levels are drawn from 10 |
Open with DEXTER |
![]() |
Figure A.3:
Composite image of the 24 |
Open with DEXTER |
![]() |
Figure A.3: continued. |
Open with DEXTER |
![]() |
Figure A.3: continued. |
Open with DEXTER |
Footnotes
- ... G19.61-0.23
- Based on observations made with the 14 m FCRAO telescope, the Spitzer satellite, and the Atacama Pathfinder Experiment (APEX), ESO project: 181.C-0885. APEX is a collaboration between the Max-Planck-Institut fur Radioastronomie, the European Southern Observatory, and the Onsala Space Observatory.
- ...
- Appendix A is only available in electronic form at http://www.aanda.org
- ... values
- http://www.astro.umass.edu/ fcrao/observer/status14m.html#ANTENNA
- ...
- http://www.iram.es/IRAMES/telescope/telescopeSummary/telescope_summary.html
- ...
GILDAS
- http://iram.fr/IRAMFR/GILDAS/
- ...
GRS
- http://www.bu.edu/galacticring/new_data.html
- ...
sources
- Retrieved from the SIMBAD Astronomical Database, http://simbad.u-strasbg.fr/simbad/
All Tables
Table 1: Summary of the parameters of the spectral line observations.
Table 2: Summary of the parameters of the four molecular clouds identified in the FCRAO 13CO(1-0) emission.
Table 3: Physical parameters of the clumps identified in the FCRAO 13CO(1-0) emission.
Table 4:
Physical parameters of the sources identified in the APEX 870 m continuum emission.
Table 5:
Association (within 1)
of the APEX 870
m sources with active star-formation tracers, such as Spitzer 3.6
m, 8
m and 24
m; water, methanol and OH masers; HII regions; and IRAS sources.
Table 6: Masses and surface densities of the clumps identified in the FCRAO 13CO(1-0) emission.
Table 7:
Properties of the ATLASGAL sources with a counterpart in the mid-infrared emission, derived by fitting the 870 and 70 m points with a modified black body.
Table 8: Summary of the parameters of the total integrated 13CO(1-0) emission of the GMC surrounding G19.61-0.23 and of a typical cloud in Henize 2-10, from SMA observations.
Table A.1: List of the sources in the sampled field, from the SIMBAD Astronomical Database. Columns (1)-(2): coordinates (J2000.0); Col. (3): distance from the peak emission of the associated clump (see Sect. 4.1); Col. (4): References.
All Figures
![]() |
Figure 1:
FCRAO velocity-integrated 13CO(1-0) emission in white contours from our data, overlaid on the 13CO(1-0) emission from the BU-FCRAO GRS (color). Both maps are integrated between 25 and 77 km s-1. The contour levels range from 10 |
Open with DEXTER | |
In the text |
![]() |
Figure 2:
Top: FCRAO emission maps, integrated between 32 and 50 km s-1, of the central
|
Open with DEXTER | |
In the text |
![]() |
Figure 3: Maps of the four molecular clouds identified in 13CO(1-0) emission, integrated over the velocity channels of emission of each cloud (see Col. 2 of Table 2). The FCRAO 13CO(1-0) emission from our data is represented by the white contours and is overlaid on the 13CO(1-0) emission from the BU-FCRAO GRS. |
Open with DEXTER | |
In the text |
![]() |
Figure 4:
APEX 870 |
Open with DEXTER | |
In the text |
![]() |
Figure 5:
Top: histogram of the distances of the APEX 870 |
Open with DEXTER | |
In the text |
![]() |
Figure 6:
Integrated (2-1)/(1-0) line ratios over the central
|
Open with DEXTER | |
In the text |
![]() |
Figure 7: The points in the plots correspond to the values of the line ratios taken over every beam, in regions of the map with high enough S/N ratio (larger than 5). Top left: ratio between FCRAO 13CO(1-0) emission and C18O(1-0) against H2 column density derived from the C18O(1-0) line intensity. Top right: ratio between IRAM 13CO(2-1) emission and C18O(2-1) against H2 column density derived from the C18O(2-1) line. Bottom left: ratio between FCRAO C18O(1-0) emission and C17O(1-0), against H2 column density derived from the C18O(1-0) line intensity. Bottom right: ratio between IRAM C18O(2-1) emission and C17O(2-1) against H2 column density derived from the C18O(2-1) line. |
Open with DEXTER | |
In the text |
![]() |
Figure 8:
Plot of the ratio between the mass derived assuming virial equilibrium (
|
Open with DEXTER | |
In the text |
![]() |
Figure 9:
Spectral energy distributions (SEDs) of the APEX 870 |
Open with DEXTER | |
In the text |
![]() |
Figure 10:
Luminosity to mass ratio, L/M, for the 870 |
Open with DEXTER | |
In the text |
![]() |
Figure 11:
Surface density,
|
Open with DEXTER | |
In the text |
![]() |
Figure A.1:
FCRAO intensity map of the C18O(1-0) emission, integrated between 25 and 57 km s-1. The contour levels are from 10 |
Open with DEXTER | |
In the text |
![]() |
Figure A.2:
Channel map of the BU-FCRAO GRS 13CO(1-0) data in grey scale and our FCRAO 13CO(1-0) emission in black contours.
Center velocities of the channels are indicated in the bottom left
corner of each panel and increase in steps of 2 km s-1. Contour levels are drawn from 10 |
Open with DEXTER | |
In the text |
![]() |
Figure A.3:
Composite image of the 24 |
Open with DEXTER | |
In the text |
![]() |
Figure A.3: continued. |
Open with DEXTER | |
In the text |
![]() |
Figure A.3: continued. |
Open with DEXTER | |
In the text |
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