We have analysed the line-profile variations of some of the absorption
lines in the spectra of the primary of
Ori, focussing
on lines that are least affected by blending. We have tried to
analyse some HeI lines (4387, 5015, and 5047 Å), but found that
the relatively strong, broad and moving profile of the secondary leads
to inaccuracies in the analysis. These lines show orbital-phase
dependent normalization errors, leading to Fourier spectra dominated
by the orbital frequency and its first eleven (or so) harmonics. We
found that for the absorption lines of heavier elements we had to
prewhiten the data with the orbital frequency and its first four
harmonics, in order to diminish the effects of the orbit. By doing so,
however, we lose the ability to study line-profile variations of the
primary that have frequencies similar to that of the orbit. The
spectra and periodograms we discuss below all have these five
frequencies removed.
In Fig. 1 we display the line-profile variations of the 4552 Å SiIII line in different stages of the analysis. One can clearly see a moving bump pattern remeniscent of that of non-radial pulsations. After shifting the spectra to the velocity frame relative to the primary, it is evident that the bump pattern is not constant. The distance between consecutive bumps varies; beating of two similar moving-bump patterns seems present. This indicates that probably more modes than just one pulsation mode are responsible for the profile variations. The profiles of all other investigated absorption lines show variations very similar to those in the 4552 Å profile.
To study the temporal behaviour of the line-profile variations we have analysed them in the way described by Gies & Kullavanijaya (1988) and Telting & Schrijvers (1997). Figure 4 displays the periodogram resulting from CLEANing the Fourier transform (Roberts et al. 1987) of the signal in each wavelength bin in the profiles of the 4590 and 4596 Å OII lines. We used 400 CLEAN iterations with a gain of 0.2. A double power peak is found at frequency 10.5c/d; the duplicity of this peak explains the apparent beating of the moving-bump pattern. One-day aliasing is still present in the periodogram; the CLEAN algorithm has not been able to fully correct for the window function.
We have tried to resolve the two frequencies responsible for this
double peak by first prewhitening the data with the frequency of the
combined peak (10.5c/d) and then redoing the Fourier analysis, in
order to find the frequency of the lower-amplitude peak of the double
peak. We find this peak to be at 10.73c/d (see
Table 3). Then we prewhitened the original signal with
this frequency, and did a Fourier analysis to recover the frequency of
the higher-amplitude peak of the double peak:
10.48c/d
(Table 3). Note that the HWHM of the main peak of the
window function is 0.083c/d, which means that our frequency
resolution is about 0.17c/d, corresponding to a time base of the
observations of 6 days.
CII | SiIII | SiIII | SiIII | OII | OII | |
4267 | 4552 | 4567 | 4574 | 4590 | 4596 | |
f1 | 10.46 | 10.48 | 10.47 | 10.49 | 10.48 | 10.48 |
![]() ![]() |
3.0 | 3.5 | 3.5 | 4.8 | 3.9 | 4.5 |
f2 | 10.73 | 10.76 | 10.74 | 10.71 | 10.73 | 10.73 |
![]() ![]() |
4.1 | 5.1 | 4.7 | 4.9 | 4.8 | 4.5 |
The amplitude and phase of the variations with the above two
frequencies, as a function of position in the line profiles, give
information about the pulsations that are responsible for these
variations. We have analysed the amplitude and phase diagrams as
obtained from the CLEANed periodogram, as well as those obtained from
multi-sinusoid fits (in this case two sinusoids) to the data in each
wavelength bin. For the multi-sinusoid fits we used the frequencies
as derived from the CLEAN analysis (as listed in Table 3),
and created amplitude and phase diagrams from the fitted amplitudes
and phases (see our forthcoming paper on
Cen,
Schrijvers & Telting, for a further description of this method).
In Fig. 5 we plot the resulting amplitude and phase
diagrams for the SiIII 4574 Å line. As the multi-sinus method
is not affected by one-day aliasing, higher power is found than in the
case of the CLEANed periodogram in which power has leaked to one-day
aliases. From the overplotted phase diagrams we have determined the
blue-to-red phase differences
,
which are a measure of
the degree
of the modes (see Telting & Schrijvers 1997).
The resulting phase differences are listed in Table 3.
We use the linear representation for modes with
from Telting & Schrijvers (1997),
with
expressed in
radians, to derive the degree
of the modes. For this representation the chance of correctly
identifying the modal degree within an interval of
is
about 84%.
In most lines the amplitude of the 10.48c/d frequency was not
detected in the blue wing. For this reason the phase diagram spans
only about 75% of the total line width, which means that the derived
values of
are lower limits for the
value of the
responsible mode.
The amplitude of the 10.73c/d frequency is more symmetrically
distributed over the line profiles. From general line-profile
modelling it has become clear that the phase diagrams run along beyond
of the star, albeit with low corresponding amplitude. As
our dataset does not provide the accuracy to measure the full extent
of the phase diagrams, the derived
values will be lower limits.
Taking the largest values of
from Table 3 we
find
for the 10.48c/d frequency, and
for the
10.73c/d frequency. Given the fact that our determinations are
likely to be lower limits, we estimate the true value for both modes
to be
.
In Fig. 5 one can see that the slope of
the phase diagrams of both frequencies is very similar, which supports
the possibility of both modes having the same degree.
We stress that, because of the limited time base of our data set and the corresponding limiting frequency resolution, the derived phases of the variations at these frequencies might be affected by each other. More data, spanning a longer time base, are needed to confirm our mode identifications.
We did not find significant power at the harmonics of the frequencies derived above, which means that we cannot estimate the m-values of the modes directly from the Fourier analysis (Telting & Schrijvers 1997). It is likely that due to the limited sampling of the variational signal, and the phase smearing during the individual exposures, it has not been possible to detect the harmonic variability in our dataset.
Copyright ESO 2001