![]() |
| Parameter | Value | |
| Photon Index |
0.68 |
|
| IP.L.6 |
0.0406 |
|
| E17 | Fe I |
6.377 |
| I18 | 21 |
|
| E29 | Fe XV |
6.68 |
| I210 | 13 |
|
| E311 | Fe XVI |
6.97 |
| I312 | 13 |
|
| Ebroad13 | Comptonized iron line? |
6.33 |
|
|
Gaussian width in keV |
0.44 |
| Ibroad14 | 47 |
![]() |
![]() |
This model gave a significantly
better fit to the observation-averaged spectrum than the model of
Ebisawa et al. (1996) in which
was fixed at 1.0.
It is convenient to refer to the three continuum components as the
medium, hard, and
soft components, respectively, and identify them with the subscripts m,
h, and s. To the medium component were added narrow
lines at 1.85, 2.01, and 2.64 keV, corresponding to emission from Si XII,
Si XIV, and S XVI, respectively. To the hard component was added a 6.4 keV
narrow line with centroid energy 6.4 keV. This is due to fluorescence of
iron in low ionization stages.
This fit yielded an unacceptably high
.
The poor fit is due to the presence of residuals
around 6 keV. Allowing the 6.4 keV line to have a finite width improved
the fit but it was still unacceptable. When a broad Gaussian with centroid
energy
6.3 keV was added to the hard component an acceptable fit
was obtained as shown in Figure 3.4. This component may be
due to Comptonization of the 6.4 keV iron line. The best fit spectral
parameters are shown in Table 3.
![]() |
| Parameter | Value | |
| Photon Index |
1.29 |
|
| Imedium15 |
0.0354 |
|
| I6.6716 | Fe XV |
3.79 |
| I6.9717 | Fe XVI | 3.6 |
| I1.8518 | Si XII |
14.8 |
| I2.0119 | Si XIV | 8.9 |
| I2.6420 | S XVI |
4.13 |
| NHmedium | ( 1022 cm-2) |
3.25 |
| Ihard21 |
0.0219 |
|
| I6.422 | Fe I | 12 |
| Ebroad | Gaussian centroid energy in keV |
6.34 |
|
|
Gaussian width in keV |
0.78 |
| Ibroad24 |
28.2 |
|
| NHhard | (1022 cm-2) |
25.1 |
| Isoft25 |
0.027 |
In order to examine the iron line equivalent widths the GIS data were fitted with the energy range restricted to 5-8 keV. The continuum model was a power law with iron K-edge absorption. The iron line complex was modeled by three narrow lines with centroid energies fixed at 6.4, 6.67, and 6.97 keV. This model fitted a spectrum extracted from all the GIS high bitrate data well. Pulse-phase averaged spectra were extracted from 24 time intervals. The edge energy and the power law index were fixed at the observation-average value. This yielded acceptable fits to the 24 spectra. The 6.4 keV iron line equivalent width is plotted versus orbital phase in Figure 3.4.
![]() |
Because of the limitations of counting statistics, pulse-phase resolved
spectroscopy of these 24 intervals was not feasible. Thus, the observation
was divided into five intervals. These are denoted
``eclipse egress'', ``pre-flare non-eclipse'',
``flare'', ``post-flare non-eclipse'', and
``pre-eclipse'' phases. The corresponding orbital phase intervals
were
= 0.12 - 0.26,
= 0.18 - 0.38,
= 0.38 - 0.42,
= 0.44 - 0.64, and
= 0.66 - 0.8, respectively. These
spectra were fitted to the continuum model of equation 7.2.
The three iron lines were included in the fit.
The 6.36 keV broad feature was not required. However, allowing the 6.4 keV
line's width to vary improved the fit. The ratio of the 6.4 keV line to the
hard power power law intensity and the ratio of the 6.67 and 6.97 keV recombination
lines were fixed.
Also,
was fixed at
the observation-average value. Clear variations in the continuum spectra are
apparent in figures 3.4 and 3.4.