A&A 368, L13-L16 (2001)
DOI: 10.1051/0004-6361:20010209
B. Lefloch1 - J. Cernicharo2 - D. Cesarsky3 - K. Demyk4 - L. F. Rodriguez5
1 -
Laboratoire d'Astrophysique de l'Observatoire de Grenoble, BP 53, 38041 Grenoble Cedex, France
2 -
Consejo Superior de Investigaciones Científicas, Instituto de Estructura de la Materia,
Serrano 123,
28006 Madrid, Spain
3 -
Max-Planck Institut für Extraterrestrische Physik, 85741 Garching, Germany
4 -
Institut d'Astrophysique Spatiale, Bât. 121, Université Paris XI, 91405 Orsay Cedex, France
5 -
Instituto de Astronomía, UNAM, Campus Morelia, A.P. 3-72, Morelia, Mich. 58089, México
Received 8 December 2000 / Accepted 21 January 2001
Abstract
We report on mid-IR observations of the central region in the Trifid
nebula, carried out with ISOCAM in several broad-band infrared
filters and in the low resolution spectroscopic mode provided by the
circular variable filter.
Analysis of the emission indicates the presence of
a hot dust component (500 to 1000 K) and a warm dust component at lower
temperatures (150-200 K) around several members of the cluster
exciting the H II region, and other stars undetected at optical
wavelengths. Complementary VLA observations suggest that the mid-IR emission
could arise from a dust cocoon or a circumstellar disk, evaporated
under the ionization of the central source and the exciting star of the
nebula. In several sources the
silicate band is seen in
emission. One young stellar source shows indications of
crystalline silicates in the circumstellar dust.
Key words: (ISM:) dust, extinction - (ISM:) H II regions - ISM: individual: Trifid - stars: formation
The Trifid nebula is a nice example of a small H II region
in an early stage of evolution. It is located at a distance of
(Lynds et al. 1985) and has an estimated dynamical age
of
(Lefloch & Cernicharo 2000). Because of its youth and
its small size, it provides
us with a comprehensive picture of the early stages of massive
star-forming regions like Orion. Indeed, previous observations at
millimeter wavelengths have shown that the protostellar cores
surrounding the H II region have physical
properties similar to the cores observed in Orion. These protostellar
cores show good evidence that their birth was induced in the expansion
of the H II region (Lefloch & Cernicharo 2000).
The Trifid is excited by the star HD 164492A, classified as O7 V by
Lynds et al. (1985). Five other stars (HD 164492B-F)
were identified within
(
)
of HD 164492A,
suggesting that the formation of a cluster accompanied the birth of the
ionizing star. The spectral types
determined for some of the sources indicate they are of intermediate mass
(Kohoutek 1997).
Here we report on mid-infrared ISOCAM observations of the central region
in the H II region.
These observations bring more insight of the star formation which accompanied
the birth of the ionizing star. In particular, they reveal the lower
mass star formation, embedded in the low-density ionized gas of the
H II region.
We find that many sources are surrounded by dense material,
possibly in the form of disks photoevaporated by the ionizing radiation
of the Trifid, similar to those found close to the Trapezium stars in Orion.
Several images of the Trifid were obtained with ISOCAM onboard ISO
(Cesarsky et al. 1996) in the LW4 filter centered on the PAH band at
(
)
at
resolution,
in the LW7 filter centered on the
silicate band at
(
)
at
resolution and in the LW10 filter
(
,
)
at
resolution. The final maps are shown in Fig. 1.
Several maps of the Trifid were obtained with the Circular Variable Filter
(CVF) between 5 and
,
with a spectral resolution
.
Each map has a size of
pixels
with an angular size of
per pixel.
Superposed to the extended emission from the dust lanes, we detect in the central LW4 image several point-like sources (IRS 1 to IRS 5) near the stellar cluster (see Fig. 1d) and two more remote sources (IRS 6-7), apparent in Figs. 1c-e. The pointlike sources appear with the highest contrast in the LW4 filter; by comparison, IRS 4 and IRS 5 are hardly visible in the LW7 and LW10 band. Except for the bright sources IRS 1-2 and IRS 6, the emission of the individual sources in the LW7 filter can hardly be separated from the extended emission of the dust lanes.
The maximum of emission (source IRS 1-2) peaks approximately
Southwest of HD 164492A and coincides with the members of the
central cluster HD 164492C-D. They are optically visible (Fig. 1a)
and were classified as B6 V (Gahm et al. 1983) and Be LkH
(Herbig 1957) respectively.
In the LW4 filter, the flux distribution is
marginally resolved and indicates a size of
3
for the
emitting region. The angular resolution of the infrared observations
does not allow to distinguish the respective contributions of components C
and D. However, a Gaussian fit to the CVF data gives a size
of
for the emitting region.
This size is very close to the projected distance between
components C and D (
4000 AU, Sect. 2.3)
and suggests that both sources are contributing to the
infrared flux; we identify IRS 1 (IRS 2) with component C (D) of the
stellar cluster. All the other infrared sources are unresolved in our
images.
![]() |
Figure 1:
a) Optical image
of the
![]() ![]() ![]() ![]() ![]() ![]() ![]() ![]() ![]() |
Open with DEXTER |
The spectra of IRS 1-2, IRS 3 and IRS 6 between 5 and
were
obtained from the CVF data after subtracting the emission of a
nearby
pixel2 area used as a reference.
The observed emission was fitted with a Gaussian function convolved
with the Point Spread Function of the instrument.
The IRS 1-2 spectrum is shown in Fig. 1f. It does not exhibit
any narrow emission, apart from a weak Ne II line at
.
Remarkably, the
silicate band at
is detected in emission
whereas it is seen in absorption in the
dust lanes (not shown here).
We model the dust emission as a black-body law modified by a dust
opacity
.
The
continuum emission is satisfactorily fitted by two
components
at temperatures
K and
K respectively (Fig. 1f).
We adopted
for the size of the "cold'' component, as determined
from the VLA observations (see below). The lack of constraints on the size
of the hot component makes the amount of material difficult to quantify
(especially the hot component). We derive typical hydrogen column densities
for the component at 200 K.
The IRS 3 and IRS 6 spectra taken with the CVF display properties similar to
IRS 1-2 (not shown). The continuum emission can be accounted for by the
same simple model: one hot layer at
700-1000 K and a warm
component at
150-300 K.
The shape of the silicate band around
(Fig. 1g)
can help constrain the composition of the dust.
The blue wing of the band (8-10
m)
is well reproduced with amorphous pyroxene grains
containing FeO inclusions (we assume spherical grains of
size
and the optical constants are taken from Henning et al. 1999).
Comparison with
laboratory transmission spectra of submicronic grains obtained at the IAS
suggests that the broad shoulder longward of
is probably due to
crystalline silicates; it is well fitted with pure forsterite grains
(Fig. 1g). We note that other crystalline silicates, such as pyroxenes,
could also be present and account for the red shoulder. However,
observations of other bands longward of
,
like the
forsterite band or the
pyroxene
band are necessary to confirm our identification and search for other disk
components, like crystalline pyroxenes.
We observed the continuum radiation of the central region
at 3.6 cm using the Very Large Array in its highest angular resolution
configuration in 1998 March 13.
The field was centered at
(Eq. 2000), so that
all the infrared sources but IRS6 lie within the field.
We used 1328+307 as absolute amplitude calibrator and 1748-253 as the
phase calibrator. A bootstrapped flux density of
Jy was
obtained for 1748-253. The observations were made in both circular
polarizations with an effective bandwidth of 100 MHz.
The rms noise in the map is
Jy beam-1; the beam size (HPFW) is
and the position angle is
.
The map reveals the presence of two radio
sources that coincide respectively with components C and D of the stellar
cluster. We do not detect any emission from any other
ISOCAM source, nor component B of the cluster, for which
Yusef-Zadeh et al. (2000) report a 3.6 cm flux of 0.66 mJy, much higher
than our
limit of
.
It appears unlikely that this emission arises from a circumstellar
disk, as suggested by these authors;
we propose that component B
is a time variable gyrosynchrotron emitter, that may exhibit circular
polarization in high-sensitivity radio-observations.
The emission from components C and D is compact and forms a close
double, separated by
.
The flux densities at 3.6 cm were
(for C) and
(for D). Both sources appear
unresolved with an angular size smaller than
0.2
.
No linear or circular polarization was found in the sources
to an upper limit of
4% for the degree of polarization.
The lack of polarization is consistent with a
free-free interpretation for the observed emission. To obtain the spectral
indices of both objets we undertook additional
VLA observations at 2-cm in the C configuration during 1998 November 21.
We used 0134+329 as absolute amplitude calibrator and 1741-312 as the
phase calibrator, with a bootstrapped flux density of
Jy.
The flux densities at 2-cm were
mJy
(for C) and
mJy (for D), that combined with the
3.6-cm measurements imply spectral indices of
and
,
for C and D, respectively. These flat spectral indices
in the centimeter range are characteristic of optically thin free-free
emission.
The measured fluxes are in rough agreement with similar observations
at a lower angular resolution (
0.5
)
by
Yusef-Zadeh et al. (2000).
From the observed emissivities and adopting a transverse size of
for the emitting region, we estimate a density of
and a total mass of
for the ionized gas around C and D.
The color excesses measured by Kohoutek et al. (1997)
towards the central stellar cluster (0.3-0.4)
indicate very low hydrogen column densities
.
Hence, there
is no large-scale gas reservoir which could slow down the expansion
of the ionized gas detected around components C and D. The ionized gas
must expand
on the sonic timescale
,
with
as the radius of the region observed and
.
This timescale is so short compared to the age of the
nebula that the free-free emission has to be sustained through the
ionization of some "fresh'' neutral material.
The mid-infrared data provide direct evidence for some neutral
material around components C and D.
Therefore, we propose that the emission observed at the VLA and in the
infrared originates from a reservoir of dense circumstellar material
exposed to the ionizing radiation of HD 164492A,
similar to the photo-evaporated disks detected in Orion
(Churchwell et al. 1987; O'Dell et al. 1993).
Following the same approach as Churchwell et al. (1987), we estimate an
ionizing flux
at the ionization front and
a mass-loss rate
.
It implies the mass of warm material detected in the infrared
(
)
would have completely evaporated on a
timescale of
,
whereas the nebula is
old.
The total circumstellar mass is probably much higher than the mass
of material detected and the bulk of disk material corresponds
to a colder component which emits at longer wavelengths.
We also note that the mass of the photo-evaporated disks
discovered in the Orion nebula are 100 times larger than
the masses estimated here (Störzer & Hollenbach 1999).
The similarity between the mass of the ionized gas and the mid-infrared
material suggests that we are detecting the emission of the
photon-dominated region at the surface of the circumstellar disks.
Interestingly, the column density of warm gas derived from the CVF data
is in good agreement with the model of Johnstone et al. (1998)
for the warm PDR gas at the surface of a photo-evaporated disk.
The only two infrared sources detected at the VLA are classified as
massive or intermediate-mass objects; this suggests
that all the infrared sources detected with ISOCAM have also
low- or intermediate masses. This would naturally explain why
neither IRS 3 nor IRS 4 were detected at the VLA, though
at similar apparent distances to the ionizing
source. However, we cannot exclude that we are misled by
a projection effect and that the true distance to the
exciting star is much larger.
Apart from IRS 1-2, IRS 3 and IRS 6 exhibit the silicate band at
in emission although both lay behind the Western dust lane of the
nebula. It means that the dust temperature of the circumstellar reservoir
must be at least
200 K.
Since IRS 3 is very close to HD 164492A and is also detected in the
optical
line, one cannot exclude that the circumstellar
dust is externally heated by the exciting star.
Interestingly, this is not the case for other sources like IRS 5. This is
probably because these sources are still embedded in their cocoon,
and the outer heating is not sufficient to compete with the inner continuum
source.
Only very few examples of crystalline silicates in protostellar disks
have been reported so far (Malfait et al. 1998, 1999). The mechanism
responsible for the crystallization of silicates is unclear (Molster et al. 1999). Our observations in the Trifid nebula show that many young stellar
sources are removing their parental cocoon, leaving their dense
circumstellar disk exposed to the ionizing radiation of the exciting
stars. In some sources we find a dust component at
temperatures comparable to the glass temperature of silicates (103 K).
We speculate that dust annealing in the PDR of the photoionized disks could
contribute and maybe account for the crystalline component detected
in IRS 1-2 (see e.g. Gail 1998).
Complementary observations of IRS 1-2 with upcoming infrared instruments like
SIRTF are necessary to confirm the presence of crystalline silicates,
characterize their physical properties, and to constrain the possibility
of such a scenario.
Acknowledgements
We acknowledge Spanish DGES for this supporting research under grants PB96-0883 and ESP98-1351E. LFR is grateful to CONACyT, México, for its support This research made use of SIMBAD.