The spectra toward Orion IRc2, Peak 1 and Peak 2 from 12.0-16.5 m were
made with the ISO-SWS grating. IRc2 was observed on September 6 1997
(revolution 660) using the SWS06 observing mode centered at
(1950
,
(1950
,
which is about 1
S
and 3
W of the IRc2 position listed by Gezari
(1992).
The Peak 1 spectrum was taken at the position
(1950
,
(1950
in the SWS01 speed 4 observing mode, on
October 3, 1997 (revolution 687).
Finally, on February 25 1998 (revolution 833) the spectrum toward Peak 2 was
taken using the SWS01 speed 4 observing mode at the position
(1950
,
(1950
,
1
E of the
position listed by Beckwith et al. (1978). The beam size in this
wavelength range is 14
,
and
was oriented
7
and
11
in NW-SE direction for IRc2
and Peak 2 respectively. These two beams do not overlap; however, the
infrared source BN falls within the IRc2 beam (see sketch of region in
Fig. 1). The Peak 1 beam, which has the same size and is
orientated
6
in NE-SW direction, partially overlaps with the IRc2
beam, but does not contain the BN object at the observed wavelength range.
Data reduction was done within the ISO-SWS Interactive Analysis System
SIA using the ISO Off-line Processing (OLP version 10) software
modules and calibration
files (see Lahuis et al. 1998 and Wieprecht et al.
2001 for a description
of the SIA system and its relation to the ISO OLP system). For the
SWS01 observations the Standard Processed Data (SPD) were re-derived to
create spectra at full
grating resolution with some loss in signal to noise. This software
has been developed at the Dutch ISO Data Analysis Centre (DIDAC) and is based
on the OLP software and calibration. It will become available within
SIA and OSIA for general use. Instrumental fringes have been minimized when applying the
Instrumental Spectral Response Function (RSRF) by RSRF matching to allow for
offsets in the wavelength calibration and differences in resolution between
the data and the RSRF. The remaining fringe residuals after the RSRF
calibration were removed using a robust iterative sine fitting method based
on an approximated Fabry-Pérot
model (see Lahuis & van Dishoeck 2000 and
Kester et al. 2001). All spectra have been rebinned to a
spectral resolving power
of 3500, twice the instrumental resolution. The final spectra have a
typical S/N ratio on the continuum of 50-100.
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Figure 2:
Comparison of the 13.5-14.3 ![]() ![]() ![]() |
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Copyright ESO 2003