Astron. Astrophys. 324, L5-L8 (1997)
4. Results
In order to optimize the resolution, we choose the J band
and a number stars to estimate the local
density. The extinction is characterized at each point by the mean
distance to the 20 nearest stars. In the J band the resulting
spatial resolution is for low extinction
( ) and for
. In the I band we find more than
and the band is not
sensitive enough. The final result is the extinction map presented in
Fig. 3 with the IRAS 100 emission
isocontours in which a warm contribution has been subtracted
(see below). This map in false colours results from the recombination
of the 4 wavelet planes.
![[FIGURE]](img49.gif) |
Fig. 3. Extinction map derived from J band stellar counts and cold IRAS 100 emission isocontours at 20, 25, 30, 35 MJy.sr-1 (see text)
|
The standard deviation of the map is
magnitude. The resolution for high extinction allows to clearly
identify 4 distinct maxima greater than 7 which were not resolved by
the Schmidt plate analysis. The maximum is .
There is no evidence of saturation. Using the relation between visual
extinction and column density (Savage and
Mathis, 1979) we derive the mass M of the cloud for
:
where is the angular size in square radian,
d the distance to the cloud, and µ the mean
particle mass. To calculate µ we consider a gas composed
of of hydrogen (H2 +HI) and
of helium. The mass cannot be estimated in a
straightforward way for because the slow
variation of the extinction and the lower sensitivity in the J
band induce important consequences on the value of the solid angle
which delineates the absorbing region, but the
larger uncertainty on the mass determination comes from the distance
estimate.
The extinction map that we have drawn out and the 100
map of IRAS have a comparable spatial
resolution. It is therefore tempting to cross-correlate the 2 maps to
derive some properties of the dust grains. According to Laureijs et
al. (1991) the IRAS 100 flux consists of a
cold and a warm components which can be split off into
two components using the 60/100 colour
temperature. Following Boulanger et al. (1997), the cold contribution
can be written:
![[EQUATION]](img60.gif)
Fig. 3 shows that our extinction map and the cold 100
emission are in very good agreement. Note that
the two areas with no IRAS contour ( ) are due to
the presence of peculiar objects such as the Infrared Nebula
(Schwartz & Henize, 1983) and very young stellar objects with
outflows (Jones et al., 1985). This excellent correlation suggests
that the J extinction and the cold 100
emission have the same origin, a result in agreement with the
Désert at al. (1990) dust model which shows that the 100
emission and the near infrared extinction are
both caused by big grains. The warm component contribute strongly to
emission, but not much to the extinction. A
plot of the cold IRAS emission versus visual
extinction is presented in Fig. 4.
![[FIGURE]](img64.gif) |
Fig. 4. Variation of cold IRAS emission with visual extinction. Each point corresponds to a position on the map spaced of in both directions
|
© European Southern Observatory (ESO) 1997
Online publication: May 26, 1998
helpdesk.link@springer.de  |