A&A 369, 155-169 (2001)
DOI: 10.1051/0004-6361:20010097
R. Chini1 - D. Ward-Thompson2 - J. M. Kirk2 - M. Nielbock1 - B. Reipurth3 - A. Sievers4
1 - Astronomisches Institut der Ruhr-Universität Bochum,
Universitätsstr. 150/NA 7, 44780 Bochum, Germany
2 - Department of Physics and Astronomy,
Cardiff University, PO Box 913, Cardiff, UK
3 - CASA, University of Colorado, CB 389, Boulder, CO 80309, USA
4 - IRAM, Avda. Divina Pastora 7, Nucleo Central,
18012 Granada, Spain
Received 19 September 2000 / Accepted 11 January 2001
Abstract
We present 450, 850 m and 1300
m images of regions with
embedded candidate protostars. Some of them are associated with HH
objects (HH 7-11, HH 1-2, HH 147,
HH 111, HH 108) and
have been previously identified in the course of a 1300
m
survey. Other regions were taken from the IRAS PSC (04239+2436,
04368+2557, 20050+2720, 20386+6751, 22134+5834, 23011+6126). The new
mm/submm images show the detailed structure of the regions some of
which contain new compact sources as well as extended emission features.
The inferred mm/submm fluxes are combined with IRAS data in order to
derive the temperature of the associated dust, its mass and the
re-radiated luminosity. Taking the ratio of FIR-to-submm luminosity
as an indicator for the evolutionary stage, we find that 15 out of 17
sources have
,
indicating that most
objects are probably genuine protostars. For the first time, we detect dust
emission associated with HH objects themselves, H2 and CO flows which
we interpret as density enhancements swept up by the ejected material.
Key words: interstellar medium: dust - stars: circumstellar matter - formation
Regions of star formation contain many tell-tale signs which indicate recent or ongoing formation of new stars. Among the most ubiquitous of such indicators are Herbig-Haro (HH) objects. These are shocks which trace the bipolar outflows that all young stellar objects (YSOs) appear to produce shortly after their birth. We have been carrying out a survey of the environments of HH objects for a number of years at mm and submm wavelengths (e.g. Chini et al. 1993, 1997; Reipurth et al. 1993, 1996). In the course of this work, we have studied the detailed circumstellar dust structures around the YSOs responsible for driving the outflows associated with the HH objects (e.g. Chini et al. 1997). In addition, we have also discovered new sources in the vicinity of these YSOs that were not detected by any other means. The best known of these sources is HH 24 MMS (Chini et al. 1993; Ward-Thompson et al. 1995), which appears to be a protostellar object.
Our mm catalogue of new and previously known sources (Chini et al.
1997) can be augmented by IRAS Point Source Catalogue
(PSC) data (Beichman et al. 1988; Reipurth et al.
1993) to increase the spectral energy coverage, and to
obtain the temperature of the emitting dust, which we find to be
typically
30-40 K (Reipurth et al. 1993; Bontemps
et al. 1996; Dent et al. 1998). The temperature can
then be used in conjunction with the mm/submm fluxes to calculate
masses, and hence densities according to Eq. (1) (e.g.
Reipurth et al. 1993) by fitting a modified Planck function
assuming radiation from a grey-body rather than a black-body.
For all calculations, a value for the mass absorption coefficient
of
cm2/g
interstellar matter (ISM) was assumed. However, such a fit and
therefore any related quantity is strongly dependent on the
temperature and also the frequency dependency
of the
mass absorption coefficient
,
which can be
derived from the submm spectral index.
![]() |
![]() |
![]() |
aperture | ||||||
Source |
![]() |
![]() |
peak | int | peak | int | peak | int | radius |
[Jy/beam] | [Jy] | [Jy/beam] | [Jy] | [Jy/beam] | [Jy] | [
![]() |
|||
HH 7-11 MMS 3 |
![]() |
![]() |
4.6 | 10.1 | 1.7 | 0.6 | 0.4 | 0.3 | 10 |
HH 7-11 MMS 5 |
![]() |
![]() |
2.3 | - | 0.8 | - | 0.2 | - | - |
HH 7-11 MMS 2 |
![]() |
![]() |
8.7 | 23.3 | 3.5 | 2.4 | 1.2 | 0.7 | 10 |
HH 7-11 MMS 1 |
![]() |
![]() |
10.7 | 29.8 | 3.4 | 1.8 | 1.3 | 1.0 | 10 |
HH 7-11 MMS 6 |
![]() |
![]() |
1.7 | - | 0.7 | - | 0.1 | - | - |
HH 7-11 MMS 4 |
![]() |
![]() |
1.5 | 17.8 | 0.9 | 2.8 | 0.2 | 0.7 | 25 |
HH 7-11 MMS 7 |
![]() |
![]() |
- | - | 0.9 | - | 0.2 | - | - |
IRAS 04239+2436 |
![]() |
![]() |
0.9 | 1.2 | 0.3 | 0.2 | 0.1 | 0.1 | 15 |
L 1527 |
![]() |
![]() |
6.4 | 106.3 | 1.5 | 10.8 | 0.3 | 2.8 | 50 |
HH 1-2 MMS 3 |
![]() |
![]() |
3.4 | 8.0 | 1.1 | 0.5 | 0.2 | 0.1 | 10 |
HH 1-2 MMS 2 |
![]() |
![]() |
4.9 | 9.3 | 1.2 | 0.4 | 0.3 | 0.1 | 8.5 |
HH 1-2 MMS 1 |
![]() |
![]() |
8.0 | 15.4 | 1.8 | 0.6 | 0.5 | 0.2 | 30 |
HH 147 MMS |
![]() |
![]() |
1.7 | 19.8 | 0.6 | 2.1 | 0.2 | 0.4 | 30 |
HH 111 MMS |
![]() |
![]() |
4.7 | 48.5 | 1.4 | 4.2 | 0.6 | 1.5 | 30 |
HH 108 IRAS |
![]() |
![]() |
4.4 | 24.5 | 0.9 | 2.4 | 0.3 | 0.6 | 25 |
HH 108 MMS |
![]() |
![]() |
2.0 | 9.0 | 0.5 | 1.4 | 0.2 | 0.3 | 25 |
IRAS 20050+2720 MMS 1 |
![]() |
![]() |
13.6 | 37.0 | 2.8 | 3.8 | 0.9 | 1.8 | 20 |
IRAS 20050+2720 (incl. outflow) | 184.2 | 23.9 | 10.5 | 65 | |||||
IRAS 20050+2720 MMS 2 |
![]() |
![]() |
- | - | - | - | 0.3 | 0.3 | 15 |
IRAS 20050+2720 MMS 3 |
![]() |
![]() |
- | - | - | - | 0.2 | 0.3 | 15 |
L 1157 (central source) |
![]() |
![]() |
7.9 | 6.0 | 1.5 | 0.9 | 0.4 | 0.4 | 10 |
L 1157 (source + disk) | 25.3 | 3.8 | 1.3 | 55![]() |
|||||
IRAS 22134+5834 |
![]() |
![]() |
7.4 | 91.5 | 1.8 | 8.5 | 0.3 | 2.7 | 50 |
IRAS 23011+6126 |
![]() |
![]() |
12.6 | 43.7 | 1.8 | 4.1 | 0.4 | 1.0 | 40 |
Submillimetre continuum observations at 450 m and 850
m
were carried out using the Submillimetre Common User Bolometer Array
(SCUBA) camera at the James Clerk Maxwell Telescope
(JCMT)
on Mauna Kea, Hawaii. The observations were carried out
on the evening of 1997 August 6 from 17:30 to 01:30 HST (UT Date: 1997
August 7, 03:30 to 11:30) and the morning of 1997 October 3 from 01:30
to 09:30 HST (UT: 11:30 to 19:30). SCUBA was used in its 64-position
jiggling mode to make a fully sampled image of a 2
3 field
simultaneously at 450
m and 850
m (Holland et al. 1998). On-source integration times were 10 s/point in
each of the 64 positions, which corresponds to 40 s/beam at each
wavelength.
While the observations were carried out, the secondary mirror was used
to chop 150
in azimuth at around 7 Hz to reject sky
emission. The opacity at both 450 and 850
m was monitored by
skydips, and the opacity at 1300
m was monitored by the
radiometer located at the adjacent Caltech Submillimetre
Observatory. During the August observations the atmospheric opacity
was 1.8 at 450
m, 0.3 at 850
m and 0.08 at 1300
m,
typical of average conditions at the site, and corresponding to a
zenith atmospheric transmission at 850
m of around 75%. For the
October observations the atmospheric opacity was 1.5 at 450
m,
0.23 at 850
m and 0.06 at 1300
m, typical of above average
conditions at the site, and corresponding to a zenith atmospheric
transmission at 850
m of around 80%. The transmission remained
stable throughout both sets of observations.
Pointing and focus were checked using bright sources such as the
planet Uranus and the radio source 3C 84, and the
pointing was found to be good to 1
.
Calibration was
performed using the planets Uranus and Mars
(Griffin et al. 1986; Orton et al. 1986; Griffin &
Orton 1993) and the secondary calibration source
CRL 618 (Sandell 1994), and a consistent calibration
was obtained. We estimate the total absolute calibration uncertainty
to be
20% at 450
m, and
10% at 850
m. The
maps of Uranus show that the JCMT error beam at 450
m is only
significant below the 10% level of peak, and above this the beam is
essentially circular. At 850
m the error beam is only
significant below the 3% level. The error beam at 450
m was
taken into consideration when calculating the flux densities of our
target sources, but at 850
m it was found to be insignificant.
Observations at 1300 m were made with the 37-channel bolometer
array at the IRAM 30 m telescope on Pico Veleta during the winters of
1998 and 1999. The atmospheric opacity as determined from skydips
ranged between 0.08 and 0.19. We used the standard mapping and
reduction techniques; for details we refer to one of our earlier
papers (e.g. Chini et al. 1997).
We measured the beam-size at each wavelength using the planet Uranus and
extra-galactic blazar sources. We found the beam-size to be 8
3 at
450
m, 15
0 at 850
m and 10
7 at 1300
m.
Figure 1 shows our maps of each of the individual
regions, which are discussed in detail in Sect. 3 below.
Table 1 gives the flux densities of each of the sources we
have identified in the maps as well as their peak positions.
Table 3 gives the parameters we derived for each of these
sources, the details of which are also discussed in Sect. 3. The
1
sky noise in each of the regions was measured from the maps
shown in the corresponding figures by calculating the pixel to pixel
rms variation of the data. It corresponds to the remaining sky noise
in the images after the data reduction and sky subtraction process
discussed above; the values are listed in Table 2.
The peak flux densities in a single beam at each wavelength are listed
in Table 1. We also measured the integrated flux densities
of each of the objects in different radius apertures and these are
also listed in Table 1. For definition of peak and integrated
flux densities see note to this Table. In confused regions where the
sources are not fully isolated, it was difficult to apply proper apertures
due to the complex structure of the individual fields
(multiple and/or elongated sources, diffuse background emission etc.).
In some cases we had to choose rather small apertures on the order of the
size of the 850 m beam; this may lead to an underestimate of the total
flux from these sources. It was necessary to use this smaller aperture on
the triple source HH 7-11 MMS 1-3 and the double source HH 1-2 MMS 2-3.
All sources were at least marginally resolved except HH 7-11 MMS 1
and 2 at 850
m.
Source |
![]() |
![]() |
![]() |
HH 7-11 MMS 1-6 | 220 | 180 | 33 |
IRAS 04239+2436 | 170 | 23 | 4 |
L 1527 | 400 | 77 | 15 |
HH 1-2 MMS 1-3 | 440 | 74 | 11 |
HH 147 MMS | 440 | 74 | 11 |
HH 111 MMS | 270 | 35 | 24 |
HH 108 IRAS + MMS | 310 | 37 | 10 |
IRAS 20050+2720 MMS 1-3 | 370 | 92 | 15 |
L 1157 | 330 | 28 | 7 |
IRAS 22134+5834 | 310 | 54 | 16 |
IRAS 23011+6126 | 410 | 33 | 8 |
Source |
![]() |
Distance |
![]() |
![]() |
![]() |
![]() |
![]() |
||
[K] | [0mm]![]() |
[pc] |
![]() |
![]() |
![]() |
[0mm]
![]() |
![]() |
![]() |
|
HH 7-11 MMS 1 | 31 | 1.9 | 350 | 2.9 | <69 | 0.4 | <160 | 3.8 106 | 2.0 1023 |
HH 7-11 MMS 2 | 29 | 1.8 | 350 | 3.0 | <58 | 0.4 | <149 | 3.9 106 | 2.0 1023 |
HH 7-11 MMS 3 | 30 | 1.8 | 350 | 1.1 | <23 | 0.1 | <177 | 1.5 106 | 7.7 1022 |
HH 7-11 MMS 4 | 23 | 1.6 | 350 | 4.0 | <19 | 0.3 | < 64 | 3.3 105 | 4.4 1022 |
IRAS 04239+2436 | 51 | 1.0 | 140 | 0.03 | 1.2 | 0.004 | 288 | 2.0 105 | 6.3 1021 |
L 1527 | 23 | 1.2 | 140 | 3.5 | <3 | 0.1 | < 21 | 5.7 105 | 5.9 1022 |
HH 1-2 MMS 1 | 32 | 2.0 | 460 | 1.4 | <61 | 0.2 | <265 | 3.0 104 | 6.2 1021 |
HH 1-2 MMS 2 | 40 | 2.0 | 460 | 0.7 | <29 | 0.2 | <182 | 6.3 105 | 3.7 1022 |
HH 1-2 MMS 3 | 37 | 2.0 | 460 | 0.8 | <26 | 0.2 | <165 | 4.3 105 | 3.0 1022 |
HH 147 MMS | 26 | 2.0 | 460 | 4.2 | <64 | 0.5 | <121 | 9.0 104 | 1.9 1022 |
HH 111 MMS | 20 | 1.8 | 460 | 16.6 | 42 | 1.0 | 41 | 3.6 105 | 7.4 1022 |
HH 108 MMS | 13 | 2.0 | 310 | 3.6 | 1 | 0.1 | 11 | 3.3 105 | 5.1 1022 |
HH 108 IRAS | 18 | 2.0 | 310 | 4.5 | < 8 | 0.3 | < 31 | 5.4 105 | 6.3 1022 |
IRAS 20050+2720 MMS 1 | 34 | 1.4 | 700 | 17.1 | 303 | 1.9 | 164 | 3.5 105 | 7.4 1022 |
IRAS 20050+2720 (incl. outflow) | 28 | 1.0 | 700 | 203 | 375 | 9.2 | 41 | 1.2 105 | 8.3 1022 |
L 1157 (central source) | 29 | 1.2 | 440 | 2.6 | 11 | 0.2 | 63 | 1.7 106 | 1.1 1023 |
L 1157 (source + disk) | 22 | 1.3 | 440 | 14.4 | 15 | 0.6 | 25 | 1.1 105 | 3.8 1022 |
IRAS 22134+5834 | 45 | 1.0 | 900 | 52.4 | 1518 | 5.5 | 278 | 3.2 104 | 2.2 1022 |
IRAS 23011+6126 | 27 | 1.5 | 730 | 25.2 | 120 | 1.8 | 67 | 5.7 104 | 2.5 1022 |
![]() |
Figure 1:
Grey scale and contour plots of the investigated
regions. Table 2 contains the values of ![]() ![]() ![]() ![]() ![]() ![]() ![]() ![]() ![]() ![]() ![]() ![]() ![]() ![]() ![]() ![]() ![]() ![]() ![]() ![]() ![]() ![]() ![]() ![]() ![]() ![]() ![]() ![]() ![]() ![]() ![]() ![]() ![]() ![]() ![]() ![]() ![]() ![]() ![]() ![]() |
Open with DEXTER |
![]() |
Figure 1:
continued.
HH 1-2 / HH 147 region (upper row):
450 ![]() ![]() ![]() ![]() ![]() ![]() ![]() ![]() ![]() ![]() ![]() ![]() ![]() ![]() ![]() ![]() ![]() ![]() ![]() ![]() ![]() ![]() ![]() ![]() ![]() ![]() ![]() ![]() ![]() ![]() ![]() ![]() ![]() ![]() ![]() ![]() ![]() ![]() |
Open with DEXTER |
![]() |
Figure 1:
continued.
IRAS 20050+2720 (upper row):
450 ![]() ![]() ![]() ![]() ![]() ![]() ![]() ![]() ![]() ![]() ![]() ![]() ![]() ![]() ![]() ![]() ![]() ![]() ![]() ![]() ![]() ![]() ![]() ![]() ![]() ![]() ![]() ![]() ![]() ![]() ![]() ![]() ![]() ![]() ![]() ![]() ![]() ![]() ![]() |
Open with DEXTER |
![]() |
Figure 1:
continued.
IRAS 23011+6126:
450 ![]() ![]() ![]() ![]() ![]() ![]() ![]() ![]() ![]() ![]() ![]() ![]() ![]() ![]() ![]() ![]() |
Open with DEXTER |
![]() |
Figure 2:
Spectral energy distributions of the individual sources.
The FIR fluxes are taken from the IRAS PSC. The solid
lines are fitted modified Planck functions (grey-bodies).
We have also labelled the plot with the fitted temperature
and the submm-slope ![]() |
Open with DEXTER |
![]() |
Figure 2: continued |
Open with DEXTER |
We will define the far-infrared luminosity,
,
of each
source as the total luminosity of the source longward of 12
m. We
can measure this by summing the luminosity under the IRAS data
points (or upper limits) as far as 100
m plus the luminosity
observed by us at 450, 850 and 1300
m. The values of
are listed in Table 3. We also define each source's
submm luminosity,
,
to be the integrated luminosity
longward of 350
m. We can then use the ratio of
to attempt to determine the evolutionary status of
each source. André et al. (1993) used the
total bolometric luminosity,
,
and defined the
protostellar Class 0 stage to be any source that has already formed a
central hydrostatic protostar and has
.
The more evolved Class I sources all have higher values for this
ratio. Since we have data shortward of 12
m only for a few
sources, we can generally only use
as a
lower limit to the ratio
.
The exact scaling
between these two ratios for any particular source depends on the
detailed source spectrum. However, the difference between
and
is - even in extreme cases - in the order of 10% and
thus does not influence our classification significantly.
Interestingly, the SCUBA images seem to show four additional potential
sources. We follow our previous nomenclature and number them by their
mm/submm strength. The strongest of them lies east of the ridge just
described. This source is also visible in the 1300 m image of
Chini et al. (1997) but was not recognized as an individual
source there due to its low signal-to-noise ratio. However, the
presence of the source at all three wavebands leads us to conclude
that it is real; we here name it HH 7-11 MMS 4. We note that this
source also appears in the submm data of Chandler & Richer
(2000) although these authors did not remark upon it. Its
position coincides with the Herbig-Haro object HH 8 (see
e.g. Herbig & Jones 1983; Chrysostomou et al. 2000)
and with faint CO emission observed by Grossman et al. (1987).
A further tentative source appears at the eastern edge of the 450 and
850
m maps which also is indicated on our original 1300
m
images. This source - if real - would coincide with the position of HH 7;
we here name this source HH 7-11 MMS 7. Accurate photometry
of this source cannot be established due to its position at the edge of
the maps. Therefore, it has been excluded from Tables 1 and
3. A stellar origin of MMS 4 and MMS 7 can be ruled out, as
Aspin et al. (1994) classified them as nebulous
near-infrared sources ASR 6 and ASR 22, matching 1.1 mm peaks (see
Fig. 7 in their paper) similar to our maps. Additionally, neither source
corresponds to any of the VLA sources found by Rodríguez et al.
(1999). This might be indicating that we are seeing - for the
first time - HH objects directly at mm/submm wavelengths, in which case
the emission would probably originate from density enhancements of the
dusty environment produced by the interacting HH jet. Although it is
generally considered that most of the pre-shock material evaporates
during interaction with the outflow, Mouri & Taniguchi (2000)
recently showed that 70-80% of the grains could escape destruction.
It is noteworthy that Molinari et al. (1999) report on the
detection of crystalline water ice in HH 7 which has formed on dust
grains. Their production can only be explained with grain temperatures
100 K which can be attained in dissociative shocks. This would imply
a large amount of post-shock dust in this area.
Two other new mm sources appear south of the main ridge in the 450 and
850 m images. Again there are weak indications for their
presence in our earlier 1300
m data. Within the positional
uncertainties, the stronger one, HH 7-11 MMS 5, is coincident with
VLA 16, and the fainter one, HH 7-11 MMS 6, with VLA 19. Both of
them are identified as YSOs by Rodríguez et al. (1999).
VLA 16 is a time variable source exhibiting large circular
polarization and coincides with the NIR source ASR 7 (Aspin et al. 1994), which is believed to be a T Tauri star.
VLA 19 exhibits a spectral index at cm wavelengths which also
suggests an association with a young star. Thus, it is very likely
that we have detected the mm/submm counterparts of two further young
objects in the HH 7-11 region.
Figure 2 displays the SEDs of HH 7-11 MMS 1-4. In order
to avoid overlapping apertures the submillimetre fluxes for MMS 1-3
were measured in a radius of 10
.
The remaining source, MMS 4,
was measured in a 25
radius aperture (excluding the segment
containing the source MMS 7). IRAS only detected a single point
source in the area that coincides with the strong mm/submm
ridge. Consequently, we do not know which of the three submm sources
is the IRAS source, or whether all three contribute at some
level. Therefore, we applied the procedure of distributing the IRAS flux density according to the ratio of the submm flux density.
MMS 1-3 all have central protostellar sources, as evinced by the
presence of cm radio continuum emission. The value of the
ratio for each source is listed in
Table 3. By adding the NIR photometry values from Aspin et al. (1994) to our data, we can extend the
spectral coverage for MMS 1 and 4, which are listed there as sources
ASR 1 and ASR 6. This allows us to derive bolometric luminosities of
for MMS 1 and <
for MMS 4. The
resulting
ratios are 189 for MMS 1 and <77 for MMS 4. Obviously all 3 sources MMS 1-3 have values of
less than 200, although being close to the borderline.
The fact that Gregersen et al. (2000) did not find any evidence
for infall of circumstellar matter related to MMS 1 makes a Class I
nature very likely. In summary, in the region of HH 7-11 we have
detected: three young stellar objects (YSOs), MMS 1-3; two HH objects,
MMS 4 and 7; and two T Tauri stars, MMS 5 and 6. If our interpretation
is correct, this corresponds to the first direct mm/submm continuum
detections of HH objects themselves.
Figure 1 shows the 450, 850 and 1300 m images of
the IRAS 04239+2436 region. The 450 and 1300
m data have been
smoothed to the resolution of the 850
m data. All three images
show a very similar structure - basically a single, marginally
resolved source at this resolution. We measured the peak flux density
at each wavelength, and list this in Table 1, as well as
the integrated flux density in a 15
radius circular aperture,
since this encompassed all of the flux above the 3
level (see
Table 2). The fact that the integrated flux densities are
all similar to the peak flux density shows that this is most likely
a point source with some diffuse extended circumstellar matter as
outlined by the
contours.
Figure 2 shows the spectral energy distribution of this
source, wherein we have used the integrated flux densities from
Table 1, combined with the IRAS PSC flux densities,
since even a source with radius 15
would appear as a point
source to IRAS. The 100-1300
m data can all be fitted by a
single temperature modified blackbody function of temperature 51 K and
.
The shorter wavelength IRAS data require
additional hotter dust components to explain their flux densities. NIR
and MIR photometry by Myers et al. (1987) yields a total
luminosity of 1.2
shortward of 100
m. The source is not
visible at optical wavelengths (Tamura et al. 1991).
As
underestimates the total luminosity of this source, we
added the NIR measurements of Myers et al. (1987) to our
calculations. This gives
resulting in a
ratio of 370. Therefore, IRAS 04239+2436 is
definitely the most evolved source in our present sample and has to be
regarded as a Class I source.
Figure 1 shows the 450, 850 and 1300 m images of
the L 1527 region at the full spatial resolution at which they were
observed. The images all show a very similar morphology, consisting of
a compact source at the centre, surrounded by more extended, lower
level emission. We interpret this as an enshrouded central source
surrounded by a dust envelope that is elongated in a SE-NW
direction. Using the above assumed distance it has a semi-major axis
of 5300 AU and a semi-minor axis of 2400 AU at the
level,
and an axial ratio of 2.2:1. The long axis of the object that we see
is in the same orientation as the source extension seen in
interferometric millimetre transitions (Hogerheijde et al.
1997, 1998).
Eiroa et al. (1994) associated HH emission with L 1527 and
concluded that the outflow was driven by a Class 0 source with an
edge-on disk. Later observations of this HH 192 outflow (Gomez et al. 1997) showed an orientation that is roughly
east-west. Hence the outflow is not aligned with either the major or
minor axis of our mm/submm images, nor with the mm interferometer
source extension. Our value for
corroborates the Class 0 nature of this source.
Table 1 shows the peak flux densities, as well as the
integrated flux densities in a 50
radius circular aperture
centred on this source. This was chosen as it encompasses all of the
flux above
in this region. These flux densities were
plotted along with the IRAS PSC flux densities in
Fig. 2. This source can be seen to be significantly
brighter than the previous source at FIR and mm/submm wavelengths,
despite being at roughly the same distance. However, it also contains
a significant amount of colder dust, since its 100-1300
m
emission can be fitted with a single grey-body with
K and
.
There is also less evidence for hotter dust in
this case since the source was not detected by IRAS at 12
m.
The slightly extended source HH 1-2 MMS 1 contains within its
contours two cm radio sources VLA 1 and 2. VLA 1 has been previously
identified as the driving source of the outflow with which HH 1 and 2
are associated (Pravdo et al. 1985; Rodríguez et
al. 1990). Further to the north-west there is an optically
visible T Tauri star (Cohen & Schwartz 1979). An overview of
the region is given by Reipurth et al. (1993). We noted in our
previous paper (Chini et al. 1997) that the elongation of
MMS 1 is roughly perpendicular to the direction of the HH 1-2
outflow, and we see the same elongation here at both 450 and
850 m. We note that this is also parallel to the elongation
observed in H13CO+ (Choi & Lee 1998). HH 1-2 MMS 2
and 3 are also in a slightly confused region, containing VLA cm
sources and masers (see discussion in Chini et al. 1997).
HH 147 MMS is coincident with a T Tauri star, source No. 3 of Strom et
al. (1985), which drives the HH 147 bipolar outflow
(Eislöffel et al. 1994).
Figure 2 displays the SEDs of HH 1-2 MMS 1-3 and
HH 147 MMS. The IRAS point source IRAS 05339-0646 coincides
with our position of HH 147 MMS, while the source IRAS 05338-0647
coincides with the ridge that contains HH 1-2 MMS 2-3. It is
unclear which of the two millimetre sources corresponds to
IRAS 05338-0647, therefore we have divided its flux density according
to the ratio of the submillimetre flux densities of the sources. An
aperture with a radius of 30
was used for HH 147 MMS and
HH 1-2 MMS 1. Due to source confusion it was necessary to use an
aperture of radius 8
5 for MMS 2 and 10
for MMS 3. This
probably leads to an underestimate of the 850
m fluxes. The
calculation of the dust temperature for MMS 1 is limited by the fact
that IRAS PSC values do not exist. The derived upper limits of
the FIR flux densities (see head of Sect. 3) lead to a
temperature of 32 K.
We can also compare the ratios of
for each
source. Treating MMS 1 as a single source it does not satisfy the
Class 0 criterion. However, as it contains more than one VLA source it
is clearly a multiple object and thus this classification
criterion might be problematic. Because MMS 2 and 3 are only partially
resolved in our data and MMS 2 contains at least two known VLA sources,
their appearance as Class 0 objects must also be
treated with caution. Finally, HH 147 MMS exhibits a ratio
of about 120 indicating a Class 0 source. Including
the photometry shortward of 12
m (Strom et al. 1985), the
bolometric luminosity
rises up to
which
shifts the source close to the transition between Class 0 and I with
a ratio
of 189. This result can be explained
by the following two scenarios: either we measure the emission of
circumstellar disk around a T Tauri star, or we are dealing with two
separate sources of which the visible T Tauri star may have been
ejected from the cloud core that we have detected at submm/mm wavelengths.
Figure 2 shows the SEDs of HH 108 MMS and HH 108 IRAS,
which coincides with the IRAS source IRAS 18331-0035. IRAS fluxes are not available for HH 108 MMS, but luckily we can make
use of recent ISOPHOT data (Krusch 1999). The fluxes
were measured in 25
radius apertures and the contribution from
the ridge was removed. As derived from grey-body fits, both sources
seem to be the coldest in our sample yielding 18 K for the IRAS
source and 13 K for HH 108 MMS, which appears to possess at least a
second dust component of 24 K. Due to the fact that the IRAS
flux value for HH 108 IRAS at 12
m is only an upper limit,
should be a good estimate for
.
Therefore,
all our results classify it as a Class 0 source. However, Gregersen
et al. (2000) could not find any evidence for matter infall.
HH 108 MMS does not appear to have been detected other than in the
FIR or mm/submm; its
ratio of 11
suggests that it is potentially another similar source to HH 24 MMS
(Chini et al. 1993; Ward-Thompson et al. 1995),
namely an extremely young protostellar source, either on the verge of
collapse or just beginning the protostellar collapse phase. This
source would bear further investigation at other wavelengths.
Figure 1 shows the 450, 850 and 1300 m images of the
IRAS 20050+2720 region. A bright central object is seen at all
wavelengths, together with an extension to the south. Additional
sources are seen in the somewhat larger 1300
m image, which are
outside of the area mapped by SCUBA. According to our former procedure
we name the bright central object coinciding with IRAS 20050+2720 as
MMS 1. The other two sources to the south, which are probably detected
for the first time, are called MMS 2 and 3 and their 1300
m flux
densities are listed in Table 1 as well as the other
results of the photometry carried out on this object. In order to
derive properties only for MMS 1 we first performed flux density
measurements within an aperture of 20
radius. The results are
shown Table 3, between them
K,
and
.
If we extend the
aperture up to 65
radius covering also the prominent extent
to the south which seems also more comparable to the less resolved
IRAS PSC measurements, we derive
K,
and
.
Together with the obtained
luminosities from Table 3, we think it is safe to conclude
that most of the luminosity is produced in the highly populated star
cluster around MMS 1. Yet, most of the interstellar matter seems to be
located in the southern
20000 AU long extended structure. At
this distance
and within the crowded cluster field, there may be confusion by
several sources in our beam. Taking the results of MMS 1 alone, it is
the second most massive and luminous object in our sample. This is
clearly a young cluster in the process of formation, and we may be seeing
the start of a sequence of rich star formation in this area.
![]() |
Figure 3:
Comparison between CO (1-0) and continuum
emission. The left plot showing an H2 v=1-0 S(1)
image overlaid with CO (1-0) contours is taken from
Zhang et al. (2000). The image on the right displays
an H2 v=1-0 S(1) image taken from Davis
& Eislöffel (1995) overlaid with contours of
our 850 ![]() |
Open with DEXTER |
L 1157 is located in a small isolated cloud in Cepheus, at an adopted
distance of 440 pc (Viotti 1969). The embedded FIR source
IRAS 20386+6751 is a single isolated Class 0 source with a luminosity
of 11
(Umemoto et al. 1992) driving a
molecular outflow with a rich chemistry (Gueth et al. 1996,
1997, 1998; Bachiller & Pérez Gutiérrez
1997a). The source was detected at the VLA by Rodriguez &
Reipurth (1998). An infrared outflow was detected by Davis &
Eislöffel (1995), one knot coinciding with the HH 375
flow while Maradones et al. (1997), Choi et al.
(1999) and Gregersen et al. (2000) find evidence for infall.
Figure 1 shows the 450, 850 and 1300 m images of
the L 1157 region. The maps show a central source with extended
structure in an approximately east-west direction. The 850 and
1300
m data also show low level emission that extends to the
north and south. This low-level emission is aligned with the CO
outflow first observed by Umemoto et al. (1992) and later
confirmed by Zhang et al. (1995). Furthermore, it is the second
case in our sample, where a coincidence between a submillimetre peak and a
Herbig-Haro object (HH 375) is apparent.
Obviously, all three images display a compact central source and a
diffuse, east-west extension which might be due to a circumstellar
disk or envelope perpendicular to the outflow direction. An additional
continuum emission component is aligned with the CO outflow at 850
(see Fig. 3) and
1300 m but not at 450
m. The peak flux densities and
integrated flux densities in a 10
radius aperture are listed
in Table 1 as well as the measurements carried out within
an elliptical aperture of 55
30
.
The smaller size
of aperture was chosen as it should give only the characteristics of
the central source, whereas the larger aperture also covers the
disklike envelope and might even better enclose the emission detected
by IRAS. Figure 2 shows the SED of this source for
the smaller aperture with a grey-body fit to the 100-1300
m flux
densities yielding
K and
.
Our values
of
(central source) and 25 (source and
envelope) are consistent with the Class 0 designation of this source
(Bachiller & Pérez Gutiérrez 1997a).
The reason for the discrepancy in the three maps concerning the
non-detection of the southern outflow within the 450 m waveband,
although it is clearly visible at 850
m and 1300
m, might be
found in the standard deviations listed in Table 2. While
the noise in the 850
m and 1300
m maps is extremely low, the
value at 450
m is only average. Because of this difference,
we analyzed the submillimetre emission in more detail. The IRAS
fluxes were distributed by the already mentioned procedure of adopting
the same flux ratio between the total source and the southern outflow
as measured in the submillimetre regime. A grey-body fit then revealed
that the 450
m flux lies just below the 3
detection limit.
Therefore, the noise argument can easily solve the puzzle.
Another explanation for the relative radiative strength at 850 and
1300 m might have been an extreme contamination by strong molecular
line emission. We therefore compared the 1300
m continuum flux with
the CO (2-1) measurements carried out by Bachiller
& Pérez Gutiérrez (1997b). However, by adopting the equation
![]() |
(2) |
Still the similarity between the spatial CO distribution and our
continuum maps remains obvious, so a closer relationship between the
outflow of CO gas and the dust is very likely and interaction is
almost certain. Umemoto et al. (1992) and Zhang et
al. (2000) obtain a total gas mass of 0.1
,
inferred from 12CO (1-0) observations. If we adapt our continuum
measurements (
S850 = 1.1 Jy,
S1300 = 0.2 Jy) we derive a gas mass
of 2
.
This discrepancy could originate from the column density
of
cm-2 assumed by Umemoto et al. (1992).
On the other hand, our calculations from the modified Planck fit yield
9 1021cm-2. Further properties of the southern outflow derived
from our calculations are a volume density of 4 104cm-3 and
a dust temperature of 27 K which is warmer than the dust of central
protostellar envelope. Although this value should be regarded with caution,
it fits quite well into the interpretation of shock heating (Umemoto et al.
1992), which
is barely detected in low-mass star formation regions. This scenario
was introduced by Clark et al. (1986), who claimed that
collisional heating of the dust by hot gas may be responsible for its
FIR emission. Nevertheless, this source needs further investigation at
mid- and far-infrared wavelengths with high spatial resolution in
order to attain a proper temperature determination.
Figure 1 shows the 450, 850 and 1300 m images of the
IRAS 22134+5834 region. The images display an elongated structure,
with a semi-major axis of 0.22 pc and a semi-minor axis of 0.15 pc,
and an aspect ratio of 3:2. The minor axis of this cloud is closely
aligned with the direction of the CO outflow observed by Dobashi
(1994b).
The peak flux densities and integrated flux densities in a 50
radius circular aperture are listed in Table 1. This size
of aperture was chosen as it enclosed all of the extended flux above
the 3
level. This should be comparable to the IRAS PSC
measurements. Figure 2 shows the SED of this source with
a grey-body fit to the 100-1300
m flux densities yielding
K and
.
We note that our mass
estimate is in good agreement with the 70
found by Dobashi
et al. (1994b). As far as we can tell from the available data,
we estimate that it is most likely a Class I source.
Figure 1 shows the 450, 850 and 1300 m images of
the IRAS 23011+6126 region. In the 850 and 1300
m images we see
evidence of the quadruple outflow observed by Ladd & Hodapp
(1997). The elongation of the central source at the higher
level contours in the north-south direction is coincident with an
outflow detected in molecular hydrogen - as are the 450
m data.
The southern lobe is coincident with HH 377; so again at least part of
the submm/mm emission might originate from dust embedded in the HH object.
The low-level emission seen at 850 and 1300
m to the south-east
(with a hint of very faint emission to the north-west) is coincident
with an outflow detected in CO (see Ladd & Hodapp 1997). The
reason for its absence in the 450
m maps might again be a
combination of a lack of sensitivity and rotational transition
probability, as already shown for L 1157 in Sect. 3.8.
Here again the noise at larger wavelengths is
quite low (see Table 2), whereas its value at 450
m is
extraordinarily high.
The peak flux densities and integrated flux densities in a 30
radius aperture are listed in Table 1. This size of
aperture was chosen as it encloses all of the extended flux from the
central source and the north-south extended structure that is also
seen in the NIR, and which we would also expect to have been detected
by IRAS. However, this aperture size does not cover the area of
the CO outflow. Therefore, the integrated flux measurement at 850
and 1300
m should be fairly reliable and comparable to the IRAS PSC measurements. Figure 2 shows the SED of this
source with a grey-body fit to the 100-1300
m data
yielding
K and
.
From the value
we corroborate earlier results that
IRAS 23011+6126 is a Class 0 source; however, the multiplicity of the
source makes this estimate questionable.
Acknowledgements
The authors wish to thank the staff of the JCMT, and in particular the telescope operators, for their support while these observations were carried out. We also gratefully acknowledge the British Council and the DAAD for financial travel support during the analysis of the data and the writing of this paper.