Spectroscopic observations of RR Tel were obtained using the 3.9m
telescope at the Anglo-Australian Observatory on July 22 1996. The University
College London Echelle Spectrograph was employed with the 31linesmm-1
grating and 700mm camera, along with the Tek CCD as a detector. The result
was a high resolution, high signal-to-noise (S/N) spectrum of RR Tel
over the near-UV, optical and near-IR regions, 3100 - 9800Å. The
resolution was
/![]()
50000, a factor of 2
greater than for the previous data from the Cerro Tololo Inter-American
Observatory (CTIO) (McKenna et al. [1997]), and the S/N was
20pixel-1 in the continuum, similar to the CTIO observations.
This allowed a greater dynamic range than with earlier observations, and
enabled us to measure reliable line intensities for much weaker features than
was previously possible. A section of our high resolution data is shown in
Fig.1.
In order to absolutely flux-calibrate our data, it was necessary to obtain low
resolution spectra of RR Tel. These were obtained on August 2 1996
with the Australian National University 2.3m telescope and double beam
spectrograph, which gave a resolution of
2Å pixel-1.
However, this instrumental setup only gave useful data for wavelengths in the
range 3490![]()
![]()
5530Å. Line fluxes for
wavelengths outside this range were derived from the HeII recombination
line spectrum (see Sect. 4). The low resolution spectrum is shown in
Fig.2, where, due to seeing of
2
, the accuracy
of the flux calibration is estimated at
10%.
![]() |
Figure 2: The flux-calibrated low resolution optical spectrum of RR Tel, where the flux is in units of 10-11 ergscm-2 s-1Å-1 |
![]() |
All CCD images were reduced using the Image Reduction and Analysis Facility (IRAF) version 2.3 implemented at the Queen's University, Belfast STARLINK node. Standard procedures were followed in the reduction of the images to one dimensional spectra. Low resolution spectra were optimally extracted and flux-calibrated using standards from AAO lists. The densely-packed échelle spectra were extracted using cosmic ray rejection algorithms for sky regions only, as cosmic ray hits in the spectra themselves could be confused with real emission features. Multiple high resolution échelle images enabled us to median filter the extracted spectra to subsequently eliminate cosmic rays. Once reduced to one dimensional spectra, the data were input to the user-friendly spectrum analysis program DIPSO (Howarth et al. [1996]) for further analysis.
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