The observations were carried out at the Swedish-ESO Submillimetre
Telescope (SEST) in two runs: February 1993 and May 2000. During the
first session we mapped B68 in the
CO
and C
O
lines at 110.2 and 109.8 GHz, respectively.
The map grid
spacing was 20
in the cloud centre and 40
in the
outer parts. The receiver used during these earlier observations was a
3 mm Schottky mixer dual channel receiver. By using two mixers tuned
to the same frequency we observed orthogonal polarizations
simultaneously. The system temperature,
,
reduced to
outside of the atmosphere, ranged from 300 to 400 K. In the mapping
the observing time per position was typically 2 min, which
resulted in an rms noise level of about 0.1 K. During the second
period in May 2000 we mapped the cloud in C
O
and C
O
at 109.8 and 219.6 GHz simultaneously with 3 and
1.3 mm SIS receivers. The grid spacing was
.
The system
temperatures at the two frequencies were around 160 and 260 K, and the
observing time per position was typically
1 min. The rms noise
level attained was typically 0.06 K at 3 mm and 0.1 K at 1.3 mm.
The half-power beam width (HPBW) of the antenna is 47
at 110 GHz
and 25
at 220 GHz. The pointing and focus were checked at
3-4 hour intervals towards circumstellar
SiO
maser line
sources, and the pointing accuracy was typically found to be
3
.
The map was centred on
RA 17
19
34.
6,
Dec -23
46
34
(1950.0).
All observations were performed in the frequency switching mode. The
two mixers used at the same time were connected to a 2000 channel
acousto-optical spectrometer which was split in two bands of 43 MHz
each. The AOS channel width corresponds to 0.12
at 2.7 mm
and 0.06
at 1.37 mm. Further details of the SEST are
available at http://www.ls.eso.org/lasilla/Telescopes/SEST.
Calibration was done by the chopper wheel method. To convert the
observed antenna temperatures,
,
to the radiation
temperatures,
,
the former were divided by the assumed
source-beam coupling efficiences,
,
where
is the beam solid
angle of the antenna and
the normalised beam pattern. For
we adopted the main beam efficiences of the telescope
interpolated to the frequencies used, i.e. 0.71 and 0.61 at 110 and
220 GHz, respectively. Our numerical estimates for
were in fact close to these values when the source was assumed to be
disk-like with a radius of 100
.
Line area maps of the C
O transitions are presented in
Fig. 1. Characteristic for the C
O
line
intensity distribution is a steep rise at the edge and a plateau at
the centre of the globule. The C
O
line area looks patchy
with maxima at the eastern edge of the globule and the prominent
"nose'' (cmp. Fig. 3) in the southeast.
Copyright ESO 2002