We have analyzed the large-scale 21 cm- HI emission in a
field around the nebula NGC2359, and found a large expanding bubble
roughly centered at the nebula and its exciting star, the Wolf-Rayet HD56925.
The systemic velocity of the bubble is
64 km s-1 and it is expanding at
12 km s-1. At an assumed distance of 5 kpc, the bubble has a size of
pc and a HI mass between 700 and 2400
.
By simple estimates of
energetics, ages and stellar wind parameters, we think that this feature is a
wind-blown bubble produced by the O-progenitor of the WR star. The presence of
a nearly spatially-coincident IRAS shell reinforces our hypothesis.
We have also mapped the CO J=
and
emission adjacent to NGC2359 and
found three CO components in this region. Two of these components, with radial
velocities of 34 (component A1) and 67 (component A2) km s-1, have
narrow profiles (up to 2 km s-1) and do not show any morphological or kinematical
effects which indicate the disturbance by the nebula or the WR star. However,
the third component (the component B, emitting at 54 km s-1), clearly bounds
NGC2359 at its southern and eastern border. The profiles are broad, with
linewidths of 4-5.5 km s-1. A velocity gradient of a few km s-1 is noted
towards the south and south-eastern interface with the nebula. A weak
"bridge'' in velocity of small angular extension seems to connect this
component with the component B2 at the southern part.
We have observed the 13CO J=
line at a few points in the region
where the component B is detected. We have found a striking variation of the
12CO/13CO ratio both in position and in velocity. This ratio seems
to decrease near the peak of the CO emission, for velocities higher
than 53 km s-1. This particular emiting region is not resolved by the beam,
and is probably 0.2 pc wide.
From the observational data, we have estimated the physical conditions for each CO component using the LVG approximation. The highest excitation temperature and density are found in the component B. It is remarkable that high temperatures (up to 80K) are derived for the CO emission projected onto the HII region.
In view of the kinematics, the morphology and the physical properties of the CO, we think that the component A2 was shocked and accelerated by the expanding bubble to reach the radial velocities of the component B. The shock front is still acting at the southern part of the region. The origin of such shock might be related to the WR phase of HD56925 or, more probably, to previous episodes of RSG of LBV. From the 12CO/13CO ratio we infer the presence of a thin layer of dense gas which represent the more recently shocked material. Our data, however, cannot resolve spatially the region where a thin layer of shocked material is expected. CO observations with better resolution and sensitivity is needed to disclose the main features of the region.
Copyright ESO 2001