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2900 | 0.60 | 0.13 | 60.0 | 3 | 0.58 |
1300 | 6.97 | 2.24 | 30.0 | 3 | 7.5 |
850 | 30.8 | 6.2 | 15.0 | 1 | 31.3 |
450 | 220.4 | 44.5 | 8.8 | 1 | 220.3 |
100 | 1032.0 | 226.0 | 237.0 | 2 | 852.4 |
60 | 254.9 | 59.5 | 160.0 | 2 | 162.4 |
![]() ![]() ![]() ![]() a single power-law and OH5 dust opacities. Note that the 60 ![]() fluxes are not included in the modelling (see text for details). Refs. - (1) This paper; (2) IRAS Point Source Catalogue; (3) Walker et al. (1990). |
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Figure 1:
SCUBA images at 450 and 850 ![]() ![]() ![]() |
The imaging was made using the jiggle-mapping mode to produce fully
sampled maps. In this mode the SCUBA bolometers instantaneously
under-sample the sky and a 64 point jiggle pattern is carried out by
the telescope to fully sample both the long and short wavelength
arrays. In practice, the 64 point pattern is broken down into four
16-point sub-patterns that spend 1 s integrating on the source at
each gridpoint. After a sub-pattern has been completed the telescope
is nodded and the pattern is repeated again so that sky subtraction
can be made. In all, it takes 128 s to complete one full on/off
source jiggle map. The jiggle mapping mode is the preferred
observational mode for SCUBA when imaging sources smaller than the
chop throw. Usually, a chop throw of 2
is used to ensure
chopping off the arrays. A larger chop throw would result in poor sky
subtraction and loss in image quality.
The data were reduced in a standard way, as described in
Sandell (1997), using the SCUBA reduction package SURF
(Jenness & Lightfoot 1997). The images were calibrated using simultaneous
observations of Uranus retrieved from the JCMT archive. The sky
opacities at 450 m and 850
m were estimated using the
1.3 mm opacity, monitored by the Caltech Submillimeter Observatory
and listed for each individual observation, using the relations in
Archibald et al. (2000). The validity of these relations have been
checked and confirmed using SCUBA sky dips. The total calibration
uncertainty is estimated to be approximately
20%
at 450
m and about
10% at 850
m.
Care was
taken to select data taken during good to excellent submillimetre
conditions. The beam is determined from the Uranus observations and
is dominated by an approximately Gaussian main beam with a deconvolved
FWHM of
and
8
5
9
1 at 850
m and 450
m,
respectively. A substantial error beam is, however, present at these
wavelengths (see below) picking up significant amounts of flux. The
error lobe pick up is estimated to be approximately 15% and 45% at
850
m and 450
m, respectively, and is taken explicitly
into account in the analysis.
The final 450 m and 850
m images are presented in
Fig. 1. All offsets reported are relative to the adopted
position of the protobinary star IRAS 16293-2422
(
,
). The locations of
the two protostars IRAS 16293A (MM1) and IRAS 16293B (MM2) relative to
this position are (-3
,
-1
)
and (-5
,
+3
), respectively. The emission appears to have an overall
spherical symmetry and is centered on the adopted central position
within the pointing accuracy of the telescope. For comparison, the
pointing accuracy of the JCMT is estimated to be about
1.5
in both elevation and azimuth. Also visible is a
second, weak, component apparent near the eastern edge of the SCUBA
maps. This second component, or IRAS 16293E (+77
,
-22
),
which was first identified by its strong ammonia emission, is most
probably also a class 0 protostar (Mizuno et al. 1990; Castets et al. 2001).
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450 | 0.5-0.7 | 220.4 | 72.0 | 0.3 | 8.8 |
850 | 0.12-0.15 | 30.8 | 16.8 | 0.08 | 15.0 |
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Total integrated intensity calculated over full extent of line.
The calibration uncertainty in the intensity scale is estimated to be
15-20%.
Estimated from a Gaussian fit to the observed spectrum. A colon (:)
indicates an uncertain value due to low signal-to-noise or, in the majority of cases,
a significant departure from a Gaussian line profile.
Refs. - (1) JCMT public archive; (2) This paper.
The FWHM of the emission centered on the stellar position is
208
19
4 and 21
9
19
3 at 850
m and 450
m, respectively. The deconvolved envelope
sizes assuming both the beam and brightness distribution to be
described by Gaussian functions are
14
at 850
m
and
19
at 450
m. Thus, only the 450
m
emission appears to be resolved. The observational results are
summarized in Table 2. To compare the observed brightness
distributions with the predictions from a spherically symmetric model,
the SCUBA maps were azimuthally averaged in bins with half the
corresponding beam size in width. Moreover, care was taken to block
out any contribution from IRAS 16293E. The resulting radial brightness
distributions are shown in Fig. 3.
The detected molecular line emission probes the full radial range of the envelope, providing additional constraints on the physical structure of IRAS 16293-2422. Only information on the lowest transitions of the molecules, which occur at millimetre wavelengths and probe the very coldest outer parts, is lacking. The observed line shapes provide valuable information on the velocity structure in the envelope. For example, the single-dish observations of abundant molecules like CO and CS typically show lines with strong self-absorption and some degree of asymmetry. The variation of the line profiles among the CO and CS isotopomers is potentially a sensitive probe of infall models and will be further investigated in Sect. 4.3.
Copyright ESO 2002