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ESO Press Photo 26a/03
28 August 2003
For immediate release
Infrared Halo Frames a Newborn Star
Summary: Observations with the VLT of a
star-forming cloud have revealed, for the first time, a ring of
infrared light around a nascent star. The images also show the
presence of jets that emanate from the young object and collide with
the surrounding cloud.
The DC303.8-14.2 globule
A small and dark interstellar cloud with the
rather cryptic name of DC303.8-14.2 is located in the inner part of
the Milky Way galaxy. It is seen in the southern constellation
Chamaeleon and consists of dust and gas. Astronomers classify it as
a typical example of a "globule".
As many other globules, this cloud is also giving
birth to a star. Some years ago, observations in the infrared
spectral region with the ESA IRAS satellite observatory detected the
signature of a nascent star at its centre. Subsequent observations
with the Swedish ESO Submillimetre
Telescope (SEST) at La Silla (Chile) were carried
out by Finnish astronomer Kimmo Lehtinen. He revealed that
DC303.8-14.2 is collapsing under its own gravity, a process which
will ultimately result in the birth of a new star from the gas and
dust in this cloud.
Additional SEST observations of the millimetre
emission of carbon monoxide (CO) molecules demonstrated a strong
outflow from the nascent star. A small part of the gas that falls
inward onto the central object is re-injected into the surrounding
via this outward-bound "bipolar stream".
The structure of DC303.8-14.2
The left panel in PR Photo 26a/03 shows the
DC303.8-14.2 globule as it looks in red light. This image was
obtained at wavelength 700 nm and has been reproduced from the
Digitized Sky Survey (DSS) [1].
It covers a sky region of 20 x 20 arcmin2, or about 50%
of the area of the full moon. The dust particles in the cloud
reflect the light from stars, causing the cloud to appear brighter
than the adjacent sky.
The brightness distribution over the cloud depends
mostly on three factors connected to the dust. The first is the
distribution of dust grains in the cloud, the way the dust density
changes with the distance from the centre of the cloud. The second
is the relative amount of light that is reflected by the dust
particles. The third indicates the dominant direction in which the
dust particles scatter light; this is dependent on the geometry of
the grains and their preferred spatial alignment. Accurate
observations of the brightness distribution over the surface of a
globule allow an investigation of these properties and thus to learn
more about the structure and composition of the cloud.
From the image obtained in red light (left panel in PR
Photo 26a/03) it appears, somewhat surprisingly, that the brightest
area of DC303.8-14.2 is not where there is most dust. Instead, it
takes the form of a bright ring around the centre. This rim
corresponds to a region where the intensity of the light from stars
behind the cloud is reduced by a moderate factor of 3 to 5 when
passing through the cloud and where the light-scattering efficiency
of the dust grains in the cloud is the highest.
Observing with ISAAC on the VLT
In order to study the structure of DC303.8-14.2
in more detail, Kimmo Lehtinen and his team of Finnish and
Danish astronomers [2]
used the near-infrared imaging capabilities of the ISAAC multi-mode
instrument on the 8.2-m VLT ANTU telescope at
the ESO Paranal Observatory (Chile).
Under good observing conditions, they obtained a mosaic image of
this cloud in several near-IR wavelength bands, including the J-
(centered at wavelength 1.25 µm), H- (1.65) and Ks-bands (2.17).
These exposures were combined to produce images of DC303.8-14.2, two
of which are shown in PR Photo 26a/03 (middle and right panels).
The middle image shows the central part of the globule
in the H-band. A bright rim is clearly detected - this is the
first time such a ring is seen in infrared light around a
globule.
This rim has a smaller size in infrared than in
visible light. This is because the absorption of infrared light by
dust particles is smaller than the absorption of visible light. More
dust is then needed to produce the same amount of scattering and to
show a rim in infrared light. The infrared rim will therefore show
up in an area where the dust density is higher, i.e. closer to the
centre of the cloud, than the visible-light rim.
Similar rings were also detected in the J- and
Ks-band images and, as expected, of different sizes. Thus the mere
observation of the size (and shape) of a bright rim already provides
information about the internal structure of the cloud. In the case
of DC303.8-14.2, a detailed evaluation shows that the dust density
of the centre is so high that any visible light from the nascent
star in there would be dimmed at least 1000 times before it emerges
from the cloud.
Getting a bonus: Jets from a young star
As an unexpected and welcome bonus, the astronomers
also detected several jet- and knot-like structures in the Ks-band
image (right panel in PR Photo 26a/03), near the IRAS source. The
area shown represents the innermost region of the cloud (65 x 50
arcsec2, or just 1/500 of the area of the DSS image to
the left).
Several knot-like structures on a line like a string
of beads are clearly seen. They are most probably regions where the
gas ejected by the young stellar object rams into the surrounding
medium, creating zones of compressed and hot molecular hydrogen.
Such structures are known by astronomers as "Herbig-Haro objects",
cf. ESO
PR 17/99.
More information
A general description of the methods used to study and
model surface brightness observations of small dark clouds in given
in a basic paper by Kimmo Lehtinen and Kalevi Mattila in the
research journal Astronomy & Astrophysics (Vol. 309, p. 570
1996). The results presented here will be published in a forthcoming
paper in Astronomy & Astrophysics.
Notes
[1]: The Digitized Sky Survey was
produced at the Space Telescope Science Institute under U.S.
Government grant NAG W-2166. The images of these surveys are based
on photographic data obtained using the Oschin Schmidt Telescope on
Palomar Mountain and the UK Schmidt Telescope. The plates were
processed into the present compressed digital form with the
permission of these institutions.
[2]: The team is
composed of Kimmo Lehtinen, Kalevi Mattila from the Observatory of
the University of Helsinki (Finland), Petri Väisänen from ESO/Chile
and Jens Knude from the Observatory of the University of Copenhagen
(Denmark). P. Väisänen is also affiliated with the University of
Helsinki.
Contact
Kimmo Lehtinen Observatory, University of
Helsinki Finland Phone: +358-0-19122909 email: kimmo.lehtinen@helsinki.fi |