![]() | ![]() |
Astron. Astrophys. 332, 1055-1063 (1998) 4. DiscussionThe NIR emission of the region around the IRAS 20126+4104
source shows three main condensations (A, B and C, see figure 2),
which are approximately aligned with the The detailed analysis of the IR spectra carried out above shows that the situation is probably somewhat more complex. Our images and spectra show that the NW IR lobe is composed of two E-W elongated emission line condensations (B and C, see figure 2), with a star at the E end of each condensation. This morphology is somewhat curious, and might suggest a possible association of the two stars with condensations B and C. We also find that the observed H2 line ratios indicate
that the excitation of the rotational-vibrational levels has a strong
fluorescent component. Particularly interesting is the stratification
of the line ratios along condensation C (see figure 2), which shows a
1-0 S(1)/2-1 S(1) line ratio indicating fluorescence towards
the E end of the condensation (i. e., close to the position of
the star), and a line ratio indicating collisional excitation towards
the Western end of the condensation. The weighted mean ortho/para
ratio for all the condensations, However, it is unclear whether or not these observations indicate
an association of condensations B and C with the stars embedded at
their Eastern tips. If such an association does exist, the emission of
these condensations might partly be associated with radiative
excitations by a UV continuum and/or Lyman- To summarize, from our IR spectra we find partial evidence that the
H2 emission of condensations B and C (NW of
IRAS 20126+4104) is associated with the stars embedded at the
Eastern end of these condensations. On the other hand, these
condensations also coincide spatially with the blue lobe of the
The nature of the IR emission might be clarified with future, high spectral resolution spectroscopy. The resulting kinematic information would help to resolve the present, somewhat complex scenario. ![]() ![]() ![]() ![]() © European Southern Observatory (ESO) 1998 Online publication: March 30, 1998 ![]() |