A&A 372, L41-L44 (2001)
DOI: 10.1051/0004-6361:20010543
F. Motte
1
- P. André
2 - D. Ward-Thompson
3 - S. Bontemps
4
1 - Max-Planck-Institut für Radioastronomie, Auf dem Hügel
69, 53121 Bonn, Germany
2 - CEA/DSM/DAPNIA, Service d'Astrophysique, CE Saclay, 91191
Gif-sur-Yvette Cedex, France
3 - Department of Physics & Astronomy, University of Cardiff,
PO Box 913, Cardiff, UK
4 - Observatoire de Bordeaux, BP 89, 33270 Floirac, France
Received 18 January 2001 / Accepted 11 April 2001
Abstract
We report the results of a submillimeter dust continuum
survey of the protoclusters NGC 2068 and NGC 2071 in Orion B carried
out at m and
m with SCUBA on JCMT. The mapped
region is
in size (
4 pc
2 pc) and consists of filamentary dense cores which
break up into small-scale (
5000 AU) fragments, including 70
starless condensations and 5 circumstellar envelopes/disks. The
starless condensations, seen on the same spatial scales as
protostellar envelopes, are likely to be gravitationally bound and
pre-stellar in nature. Their mass spectrum, ranging from
0.3
to
5
,
is reminiscent of the stellar
initial mass function (IMF). Their mass-size relation suggests that
they originate from gravitationally-driven fragmentation. We thus
argue that pre-collapse cloud fragmentation plays a major role in
shaping the IMF.
Key words: ISM: clouds - ISM: structure - dust - stars: formation - stars: initial mass function - submillimeter
The question of the origin of the stellar initial mass function (IMF), crucial for both star formation and Galactic evolution, remains a matter of debate (e.g. Larson 1999; Elmegreen 2001). Numerous molecular line studies of cloud structure have established that the mass spectrum of observed clumps is significantly shallower than the IMF (see, e.g., Williams et al. 2000 and references therein). The reason for this difference is presumably that most of the clumps detected in CO surveys are not gravitationally bound and reflect more the characteristics of the low-density outer parts of clouds than the initial conditions of protostellar collapse (cf. Kramer et al. 1998).
The recent advent of sensitive bolometer arrays on large
(sub)millimeter radiotelescopes has made possible extensive surveys of
nearby star-forming clouds for young protostars and their pre-stellar
precursors (see, e.g., review by André et al. 2000). Using the
MPIfR bolometer array on the IRAM 30 m telescope, Motte et al. (1998
- hereafter MAN98) could identify a total of 58 small-scale
(
AU), gravitationally-bound starless condensations in
their 1.3 mm continuum mosaic of the
Ophiuchi central cloud.
Remarkably, the mass distribution of these pre-stellar condensations,
which spanned the range
0.05 to
3
,
mimicked the
shape of the stellar IMF. It followed approximately the Salpeter
power-law IMF,
,
above
0.5
,
and flattened out to
at low masses. Interestingly, the position of the break
point at
0.5
was comparable to the typical Jeans mass in
the dense DCO+ cores of
Ophiuchi (cf. Loren et al. 1990).
The results of MAN98 have been essentially confirmed by a
m
survey of the same region with SCUBA (Johnstone et al. 2000).
In a related 3 mm interferometric study with OVRO, Testi & Sargent
(1998) identified 26 compact starless condensations between 0.5
and
10
in the Serpens main cloud core. They measured a
mass spectrum, again close to
the Salpeter IMF.
These recent results are very promising as they support the view that the IMF is at least partly determined by fragmentation at the pre-stellar stage of star formation. However, they are still limited by small-number statistics and need to be confirmed in other star-forming clouds.
In this Letter, we report on a wide-field submillimeter continuum
survey of the NGC 2068/2071 region in the Orion B cloud complex.
Orion B, also called L 1630, is the nearest giant molecular cloud
forming high-mass stars (see review by Launhardt & Lada 2001) in the
vicinity of the Sun (
pc). This complex contains five
active regions where rich clusters of young stellar objects (YSOs) are
currently forming within CS dense cores (Lada et al. 1991a,b). The
two northernmost protoclusters, associated with the reflection nebulae
NGC 2068 and NGC 2071, provide good targets to explore the mass
spectrum of pre-stellar condensations over a broad mass range.
We used the Submillimetre Common User Bolometer Array (SCUBA -
Holland et al. 1999) on the James Clerk Maxwell Telescope
(JCMT) on 1998
December 15 and 16 to carry out a submillimeter continuum mapping of
NGC 2068 and NGC 2071. Five sub-fields were imaged simultaneously at
m and
m in the standard scan-map mode to produce
two mosaics of a
32
field (see
Fig. 1). Each sub-field was covered twelve times using
three different chop throws in both right ascension and declination.
Pointing and calibration checks were made on HL Tau at regular
intervals. The zenith atmospheric optical depth was measured to be
0.25 at
m and
1.4 at
m. The FWHM beam size as measured on Uranus was
13
at
m and
at
m. The mosaics were reduced
with a SURF script from R. Tilanus using the "Emerson 2'' restoration
algorithm (Emerson 1995).
With a spatial extent of 3.7 pc 2.1 pc, our mosaics cover
of the region mapped in CS(2-1) by Lada et al. (1991a -
hereafter LBS) around NGC 2068/2071. In the submm continuum, the CS
dense cores of LBS have a filamentary appearance, with typical
dimensions
0.08
pc (aspect ratio
0.15),
and are highly fragmented. Within these extended filaments, a total of
82 condensations with lengthscales characteristic of YSO circumstellar
structures (see Table 1, only available in electronic form at
http://www.edpsciences.org and at
http://cdsweb.u-strasbg.fr/cgi-bin/qcat?J/A+A/ 372/L41,
and Fig. 2) were
identified using a multiresolution wavelet analysis (cf. Starck et al. 1998; MAN98; Motte & André 2001). The outer sizes of the
condensations were estimated from their radial intensity profiles at
m. The ambient background observed on larger lengthscales
was then subtracted to allow a proper derivation of the integrated
flux densities of the condensations (see MAN98). Unlike the
filaments, the (resolved) condensations are roughly circular (mean
aspect ratio
0.6) with an average deconvolved FWHM
diameter of
13
(i.e.
5000 AU).
Our m mosaic (e.g. Fig. 2) mainly traces
optically thin thermal dust emission from cold, dense structures in
the cloud. The map contours should thus primarily reflect the column
density distribution of dust and gas. The condensation masses were
estimated from the integrated
m fluxes (cf. MAN98), adopting
recommended values for the dust opacity per unit mass column density
(of dust and gas):
for protostellar envelopes and
for starless condensations (cf. Henning et al. 1995). The dust temperature
was taken to be
20-40 K and 15 K, respectively, in agreement with published
temperatures (Harju et al. 1993; Gibb & Little 2000). Under these
assumptions, our 5
column density sensitivity is
cm-2. The
condensations
have masses ranging from
0.3
to
5
(
9
for NGC 2071-IRS), with a factor
2 absolute
uncertainty. The average density
of
the condensations is
while that of
the filaments is
.
The m emission of seven condensations identified in the
vicinity of the luminous embedded infrared source NGC 2071-IRS
(e.g. Harvey et al. 1979) may not arise only from dust. NGC 2071-IRS
(called LBS8-MM18 in Table 1) drives a prominent bipolar flow
(e.g. Chernin & Masson 1992), which is responsible for a
northeast-southwest ridge of broad-band
m emission. The
spectral index observed between
m and
m in this
ridge is atypical:
(where
)
instead of
as measured for the extended emission
outside the ridge. Based on the CO(3-2) and HCO+(4-3) maps of
Chernin & Masson (1992) and Girart et al. (1999), we estimate that
line emission may contribute up to
of the SCUBA
m
emission in the outflow region. We are, however, confident that the
75 other condensations represent genuine dust continuum sources. Many
of them are detected at both
m and
m
(cf. Figs. 1 and 2).
Among the 75 dust condensations of Sect. 2, four are associated with
both point-like mid-IR sources detected by ISOCAM (in the ISO core
programme - e.g. Olofsson et al. 2000) and near-IR sources
(e.g. Strom et al. 1976). These four objects most likely correspond
to circumstellar envelopes and/or disks around embedded YSOs. In
addition, the condensation called LBS17-MM9 in Table 1 coincides with
the Class 0 outflow driving source LBS17-H of Gibb & Little (2000).
The remaining 70 condensations appear to be truly starless. Several
of them are seen in absorption by ISOCAM against the diffuse, ambient
mid-IR background (Bontemps et al. in prep.), which is reminiscent of
isolated pre-stellar cores (Bacmann et al. 2000).
Six submillimeter condensations (5 starless sources plus the Class 0
envelope LBS17-H) have been mapped in high-density molecular tracers
with good (
20
)
angular resolution (e.g. Gibb et al. 1995). Comparing the virial masses estimated by Gibb et al. from
HCO+(3-2) observations with the masses derived here from the submm
continuum, we find
.
This
suggests that the condensations are close to virial equilibrium,
although more extensive spectroscopic observations in an optically
thin line tracer would be required to draw definitive conclusions.
Figure 3 shows the cumulative mass spectrum (N(>m)vs. m) of the 70 starless condensations identified in
NGC 2068/2071. The mass spectrum for the 30 condensations of the
NGC 2068 sub-region (cf. Fig. 2) is very similar in shape. The
best-fit power-law is
above
,
which is close to the Salpeter IMF,
.
A
flattening of the mass distribution to
is
apparent below
in Fig. 3. The break point
is, however, close to our completeness limit at
(
detection level for the largest condensations with
- see Fig. 4). Altogether, the derived
mass spectrum is in good agreement with the IMF of field stars which,
in cumulative form, scales roughly as a
at
low masses (
)
and steepens to
for
(e.g. Scalo 1998).
By contrast, this mass spectrum is much steeper than the
power-law measured by LBS and Kramer et al. (1996)
in their CS and CO studies of Orion B. The latter is rejected by a
Kolmogorov-Smirnov test at the
confidence level.
![]() |
Figure 3:
Cumulative mass distribution of the 70 pre-stellar condensations of
NGC 2068/2071. The dotted and dashed lines are power-laws
corresponding to the mass spectrum of CO clumps (Kramer et al. 1996)
and to the IMF of Salpeter (1955), respectively. The error bars
correspond to ![]() |
Figure 4 compares the mass-size relations derived for the
(sub)mm continuum condensations of the NGC 2068/2071 and Oph
protoclusters (from this paper and MAN98, respectively) with those
found for CO clumps in various clouds (e.g. Heithausen et al. 1998).
It can be seen that the (sub)mm continuum condensations are more than
one order of magnitude denser than typical CO clumps. The mass-size
relation of the submillimeter condensations spans only one decade in
size and is much flatter than that of CO clumps: a formal fitting
analysis gives
as
opposed to
.
Although
the observed correlations may be partly affected by size-dependent
detection thresholds (cf. Fig. 4), it is worth pointing out
that they are suggestive of a change from a turbulence-dominated to a
gravity-dominated regime. Indeed, while the Larson law
is consistent with the fractal, turbulent nature of molecular
clouds (e.g. Elmegreen & Falgarone 1996), a linear correlation (
)
is expected for a sample of self-gravitating isothermal
Bonnor-Ebert condensations assuming a uniform temperature and a range
of external pressures (cf. Bonnor 1956 and Fig. 4). Most CO
clumps are transient structures associated with low density contrasts
and probably arise from hierarchical fragmentation driven by
turbulence (e.g. Elmegreen & Falgarone 1996). The starless
condensations identified here are much more centrally concentrated and
clearly require the additional effects of self-gravity. Their
properties (e.g. Figs. 3 and 4) make them
excellent candidates for being the immediate progenitors of accreting
(Class 0/Class I) protostars.
The results of Sect. 3 suggest that the 70 starless condensations
identified in the NGC 2068/2071 protoclusters are about to form stars
on a one-to-one (or perhaps one-to-two) basis, with a high
(
50%) efficiency roughly independent of mass. They confirm the
findings of MAN98 and Testi & Sargent (1998) in
Ophiuchi and
Serpens. There is now a growing body of evidence that the
fragmentation of dense (
10
)
cores into
compact, self-gravitating condensations determines the IMF of star
clusters in the low- to intermediate-mass range (
). A
plausible scenario, supported by some numerical simulations of cluster
formation (Klessen & Burkert 2000;
Padoan et al. 2001), could be the
following. First, cloud turbulence generates a field of density
fluctuations, a fraction of them corresponding to self-gravitating
fragments. Second, these fragments (or "kernels'') decouple from
their turbulent environment (e.g. Myers 1998) and collapse to
protostars after little interaction with their surroundings.
The fact that none of the NGC 2068/2071 pre-stellar condensations is
found more massive than
is statistically consistent with a
Salpeter-like mass distribution, given the relatively small number of
objects. A more extensive submillimeter mapping of the Orion B
complex should be done to improve the statistics and search for
starless condensations of higher mass. However, massive stars may not
form from the collapse of single condensations but from the merging of
several pre-/proto-stellar condensations of low to intermediate mass.
In the collision scenario of Bonnell et al. (1998), the cluster
crossing time must be short enough to allow individual condensations
to collide and coalesce with one another. Follow-up dynamical studies
of the NGC 2068/2071 condensations in dense molecular tracers could
help decide whether they have the potential to form massive stars with
.
Acknowledgements
We would like to thank Jason Kirk for his participation during the observing run.
Condensation | Coordinates |
![]() |
FWHM (3) | M (4) |
![]() |
Comments | |
Name |
![]() |
![]() |
[mJy] | [AU![]() |
[![]() |
(5) | |
LBS18-MM1 | 05:46:28.2 | 00:19:29 | ![]() |
![]() |
3.80 | 3.0 | |
LBS18-MM2 | 05:46:28.5 | 00:21:41 | 550 |
![]() |
1.40 | 4.0 | |
LBS18-MM3 | 05:46:29.5 | 00:20:16 | 790 |
![]() |
2.00 | 3.0 | |
LBS18-MM4 | 05:46:30.0 | 00:19:52 | 250 |
![]() |
0.65 | 3.0 | |
LBS15-MM4 | 05:46:37.7 | 00:27:04 | 150 |
![]() |
0.40 | 3.0 | |
LBS8-MM1 | 05:46:55.0 | 00:23:25 | 500 |
![]() |
1.25 | 3.5 | |
LBS8-MM2 | 05:46:57.1 | 00:20:10 | 490 |
![]() |
1.25 | 3.0 | |
LBS8-MM3 | 05:46:57.1 | 00:23:56 | 320 |
![]() |
0.80 | 3.5 | |
LBS8-MM4 | 05:46:58.2 | 00:20:12 | 210 |
![]() |
0.55 | 3.0 | |
LBS8-MM5 | 05:46:58.4 | 00:24:34 | 150 |
![]() |
0.40 | 3.5 | |
LBS8-MM6 | 05:46:59.8 | 00:20:26 | 160 |
![]() |
<0.40 | 3.0 | line contamination of
![]() |
LBS8-MM7 | 05:47:00.3 | 00:20:35 | 180 |
![]() |
<0.45 | 3.0 | line contamination of
![]() |
LBS8-MM8 | 05:47:01.0 | 00:26:19 | ![]() |
![]() |
5.30 | 3.0 | |
LBS8-MM9 | 05:47:01.1 | 00:20:37 | 130 | unresolved | <0.35 | 3.0 | line contamination of
![]() |
LBS8-MM10 | 05:47:01.7 | 00:18:03 | ![]() |
![]() |
2.85 | 3.5 | |
LBS8-MM11 | 05:47:02.0 | 00:20:45 | 250 |
![]() |
<0.65 | 3.0 | line contamination of
![]() |
LBS8-MM12 | 05:47:02.7 | 00:22:55 | 270 |
![]() |
0.70 | 3.5 | |
LBS8-MM13 | 05:47:03.2 | 00:19:40 | 110 | unresolved | 0.30 | 4.0 | |
LBS8-MM14 | 05:47:03.3 | 00:22:35 | 400 |
![]() |
1.00 | 3.5 | |
LBS8-MM15 | 05:47:03.6 | 00:19:54 | 110 | unresolved | 0.30 | 4.0 | |
LBS8-MM16 | 05:47:03.6 | 00:20:08 | 210 |
![]() |
0.55 | 4.0 | |
LBS8-MM17 | 05:47:04.2 | 00:20:23 | 140 | unresolved | 0.35 | 4.0 | |
LBS8-MM18 | 05:47:04.7 | 00:21:45 | ![]() |
![]() |
9.20 | 3.5 | NGC2071-IRS envelope,
![]() |
LBS8-MM19 | 05:47:06.4 | 00:22:36 | 540 |
![]() |
<1.35 | 3.0 | line contamination of
![]() |
LBS8-MM20 | 05:47:07.5 | 00:22:46 | 210 |
![]() |
<0.55 | 2.5 | line contamination of
![]() |
LBS8-MM21 | 05:47:07.9 | 00:25:07 | 210 |
![]() |
0.55 | - | |
LBS8-MM22 | 05:47:08.2 | 00:22:52 | 220 | unresolved | <0.55 | 2.5 | line contamination of
![]() |
LBS8-MM23 | 05:47:10.4 | 00:21:15 | ![]() |
![]() |
1.10 | 3.5 | SSV37 envelope,
![]() |
LBS8-MM24 | 05:47:10.7 | 00:22:29 | 110 | unresolved | 0.30 | 3.5 | |
LBS8-MM25 | 05:47:11.9 | 00:22:45 | 150 | unresolved | 0.40 | 3.5 | |
LBS8-MM26 | 05:47:12.4 | 00:23:27 | 150 |
![]() |
0.40 | 3.0 | |
LBS8-MM27 | 05:47:12.6 | 00:22:23 | 530 |
![]() |
1.35 | 3.0 | |
LBS6-MM1 | 05:47:14.3 | 00:21:30 | 125 | unresolved | 0.30 | 3.0 | |
LBS6-MM2 | 05:47:16.0 | 00:21:24 | ![]() |
![]() |
2.65 | - | |
LBS6-MM3 | 05:47:17.2 | 00:21:27 | 150 | unresolved | 0.40 | - | |
LBS6-MM4 | 05:47:24.9 | 00:20:59 | ![]() |
![]() |
4.20 | 3.0 | |
LBS6-MM5 | 05:47:25.1 | 00:18:49 | 410 |
![]() |
1.05 | 3.0 | |
LBS6-MM6 | 05:47:26.2 | 00:19:56 | 540 |
![]() |
1.35 | 3.0 | |
LBS6-MM7 | 05:47:26.5 | 00:20:45 | 320 |
![]() |
0.80 | 3.0 | |
LBS6-MM8 | 05:47:29.8 | 00:20:39 | 330 |
![]() |
0.85 | 3.5 | |
LBS5-MM1 | 05:47:32.5 | 00:20:24 | 610 |
![]() |
1.55 | 3.5 | |
LBS5-MM2 | 05:47:35.1 | 00:20:21 | 260 |
![]() |
0.65 | 3.5 | |
LBS5-MM3 | 05:47:36.9 | 00:20:07 | 760 |
![]() |
0.60 | 3.5 | 05450+0019 envelope,
![]() |
LBS16-MM1 | 05:46:36.3 | 00:05:49 | 500 |
![]() |
1.25 | 3.5 | |
LBS11-MM1 | 05:46:45.3 | 00:07:31 | 540 |
![]() |
1.35 | 3.5 | |
LBS11-MM2 | 05:46:46.1 | 00:07:09 | 580 |
![]() |
1.45 | 3.5 | |
LBS11-MM3 | 05:46:47.3 | 00:07:27 | 420 |
![]() |
1.05 | 3.5 | |
LBS7-MM1 | 05:47:04.9 | 00:14:59 | ![]() |
![]() |
2.55 | 3.5 | |
LBS7-MM2 | 05:47:05.2 | 00:13:21 | 200 |
![]() |
0.50 | - | |
LBS7-MM3 | 05:47:06.7 | 00:12:35 | ![]() |
![]() |
3.00 | 3.0 | |
LBS7-MM4 | 05:47:15.3 | 00:18:42 | 300 |
![]() |
0.75 | 3.5 |
Condensation | Coordinates |
![]() |
FWHM (3) | M (4) |
![]() |
Comments | |
Name |
![]() |
![]() |
[mJy] | [AU![]() |
[![]() |
(5) | |
LBS17-MM1 | 05:46:24.3 | -00:00:06 | 460 |
![]() |
1.15 | 4.0 | |
LBS17-MM2 | 05:46:24.5 | -00:00:22 | 160 | unresolved | 0.40 | 4.0 | |
LBS17-MM3 | 05:46:24.6 | 00:00:13 | 300 |
![]() |
0.75 | 4.0 | |
LBS17-MM4 | 05:46:26.8 | 00:01:07 | ![]() |
![]() |
3.25 | 3.5 | |
LBS17-MM5 | 05:46:27.6 | 00:01:31 | 300 |
![]() |
0.75 | 3.5 | |
LBS17-MM6 | 05:46:27.9 | -00:00:52 | ![]() |
![]() |
4.30 | 3.5 | |
LBS17-MM7 | 05:46:28.1 | -00:01:39 | 760 |
![]() |
1.90 | 3.5 | |
LBS17-MM8 | 05:46:30.1 | -00:01:07 | 340 |
![]() |
0.85 | 3.5 | |
LBS17-MM9 | 05:46:31.0 | -00:02:35 | ![]() |
![]() |
3.00 | 3.0 | LBS17-H envelope,
![]() |
LBS17-MM10 | 05:46:32.3 | -00:00:40 | 330 |
![]() |
0.85 | 4.0 | |
LBS17-MM11 | 05:46:32.9 | -00:00:23 | 125 | unresolved | 0.30 | 4.0 | |
LBS17-MM12 | 05:46:33.4 | -00:00:12 | 180 | unresolved | 0.45 | 4.0 | |
LBS17-MM13 | 05:46:33.5 | -00:00:02 | 160 | unresolved | 0.40 | 4.0 | |
LBS10-MM1 |
05:46:34.9 | 00:00:32 | 250 | unresolved | 0.65 | 4.0 | |
LBS10-MM2 | 05:46:35.8 | 00:00:33 | 260 |
![]() |
0.65 | 3.5 | |
LBS10-MM3 | 05:46:37.7 | 00:00:34 | 990 |
![]() |
2.50 | 3.5 | |
LBS10-MM4 | 05:46:39.1 | 00:00:33 | 120 | unresolved | 0.30 | 4.0 | |
LBS10-MM5 | 05:46:39.4 | 00:01:11 | 940 |
![]() |
2.35 | 3.5 | |
LBS10-MM6 | 05:46:40.5 | 00:00:34 | 360 |
![]() |
0.90 | 4.0 | |
LBS10-MM7 | 05:46:43.0 | 00:00:47 | ![]() |
![]() |
3.50 | 4.0 | |
LBS10-MM8 | 05:46:45.1 | 00:00:18 | 230 |
![]() |
0.60 | 4.0 | |
LBS10-MM9 | 05:46:47.4 | 00:00:25 | ![]() |
![]() |
1.35 | 3.5 | 05442-0000 envelope,
![]() |
LBS10-MM10 | 05:46:48.4 | 00:01:31 | 410 |
![]() |
1.05 | 4.0 | |
LBS10-MM11 | 05:46:48.9 | 00:01:22 | 370 |
![]() |
0.95 | 4.0 | |
LBS10-MM12 | 05:46:49.7 | 00:00:20 | 165 | unresolved | 0.40 | 4.0 | |
LBS10-MM13 | 05:46:49.7 | 00:02:04 | 540 |
![]() |
1.35 | 4.0 | |
LBS10-MM14 | 05:46:50.7 | 00:02:07 | 440 |
![]() |
1.10 | 3.5 | |
LBS10-MM15 | 05:46:51.4 | 00:00:00 | 150 | unresolved | 0.40 | 4.0 | |
LBS10-MM16 | 05:46:52.8 | 00:01:48 | 150 | unresolved | 0.40 | 4.0 | |
LBS10-MM17 | 05:46:54.2 | -00:00:24 | 310 |
![]() |
0.80 | 3.5 | |
LBS10S-MM1 | 05:46:43.1 | -00:01:42 | 230 |
![]() |
0.60 | 4.5 |