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A continuum study of the NGC 2024 molecular ridge
We have been studying the properties of dust in NGC 2024 (Orion B) with the JCMT using the UKT14
bolometer. NGC 2024 is a star forming region in the Orion Molecular Cloud complex. It includes a ridge
of dense molecular material containing seven compact sources (FIR cores), initially identified through their
bright mm continuum emission. Some of these cores are associated with molecular outflows and probably
contain protostars, while other cores show no sign of star formation and may be younger objects. The ridge
is therefore an ideal location in which to investigate the effect of star formation on the properties of dust in
the interstellar medium. We have obtained 800 micron and 450 micron continuum maps of the ridge and have
reduced the data using a maximum entropy algorithm written by John Richer (DBMEM).
variations?
Figure 1 shows a spectral index map made from the 450 micron and 800 micron maps. It is striking that the spectral
index is lower at the positions of the FIR cores compared with the surrounding molecular cloud. This may
be explained as follows: if the dust opacity is written in the usual long-wavelength form,
k = k ( / ) , and
the dust is optically thin, the spectral index , (F
 ), can be written as = 2 +
+ , where is a
Rayleigh-Jeans correction factor. An increase in thus indicates an increase in or . The typical
difference in the spectral index between the ridge and the FIR cores is found to be too great to be caused by
only, and we therefore have to conclude that variations in are the most likely cause. In T Tauri disks
is observed to be in the range 0 to 1, which is lower than the theoretical limit for small grains ( = 2). This
has been interpreted as an evolution of the dust properties, perhaps an increase in grain size, in T Tauri
disks compared to the interstellar medium. In the case of NGC 2024 the decreased in the FIR cores might
also suggest an evolution of the dust properties. It is tempting to draw the conclusion that the grain particles
are larger in the denser regions.
Depletion or hot dust?
In Figure 2 the integrated CS(2-1) emission measured using the Owens Valley millimeter array is displayed
in greyscale with 450 micron continuum contours overlayed. There is a good correlation between the 450 micron
dust continuum and the CS(2-1) emission along the ridge, except within 7" of FIR5, where there is bright
continuum but no CS emission. This discrepancy between dust and molecular line emission has been
reported in previous studies, but these new data show the discrepancy to be extremely localised. It has been
suggested that the discrepancy may be caused by depletion of the CS molecules onto cold dust grains in the dense cold condensations. An alternative explanation is that the temperature of the
gas and dust in and near FIR5 is somewhat higher than in the surrounding ridge. Emission from optically
thin dust scales with T(dust), and emission from CS scales with 1/T , if CS is optically thin and
thermalized. At the high densities present here, T(dust) and T are expected to be coupled, so a
higher temperature would cause an increase in dust emission and a decrease in molecular line emission.
High resolution measurements at 50 micron and 100 micron will be essential for determining the spectral energy
distributions, and hence the dust temperatures of the individual FIR cores.

Figure 1: Spectral index map from the 450 micron and 800 micron continuum images. Regions were
blanked in both images if the intensity was less than twice the mean rms noise in either image. The
contours are from the 450 micron continuum map.
With SCUBA it should be possible to observe large regions with a higher sensitivity making it possible to
study variations of dust properties on larger scales.
A. E. Visser(1), J. S. Richer(1), C. J. Chandler(1), J. E. Carlstrom(2) & R. Padman(1)
1. MRAO, Cambridge, UK
2. University of Chicago, USA

Figure 2: The grey scale plot shows integrated CS(2-1) emission (Chandler and Carlstrom, 1996,
ApJ, 466, 338), the contours are 450 micron continuum emission.
Last Modification Date 1996/08/13 - Last Modification Author: gdw
Graeme Watt (gdw)
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