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Astron. Astrophys. 342, 756-762 (1999) 3. NLTE calculationsSimultaneous solution of the radiative transfer and statistical
equilibrium equations has been realized using MULTI-code (Carlsson,
1986) in the approximation of complete frequency redistribution for
all the lines. Taking into account that this code was initially
exploited for rather cool stars, it was modified with the aim to apply
it for early-type stars' analysis. In particular, we have added the
opacity sources from ATLAS9 program (Kurucz, 1992). It enabled us to
calculate more precisely a continuum opacity. At the same time, a
possibility to take into account an absorption in the great number of
spectral lines (especially within the region of the near-UV) allowed
to calculate much accurately an intensity distribution in the region
900-1500 Å, that plays a key role in the determination of the
radiative rates of Atmosphere model was selected from the grid calculated with the help of ALTLAS9 (Kurucz, 1992). From the spectrum of program star we have selected N ii lines that are formed due to transitions between different levels and situated in the different spectral regions (Table 1). Such a choice gives a guarantee that an accordance between calculated line profiles and observed ones results from the sufficiently complete description of the nitrogen atom model. 3.1. Parameters of the nitrogen atomWe employed the model of nitrogen atom consisting of 109 levels: 3
ground levels of N i, 93 levels of N ii with
Table 2. Energy levels included in nitrogen atom model Within the described system of the nitrogen atom levels we
considered the radiative transitions between the first 43 levels of N
ii, 5 N iii levels and ground level of N iv. Only transitions having
Photoionization cross-sections were mainly taken from the Opacity
Project (Yan et al., 1987) keeping a detailed structure of their
frequency dependence, including resonances. For some important
Oscillator strengths were selected from the extensive compilative
catalogue by Hirata & Horaguchi (1995), from survey of the lines
which are formed as transitions from the ground level by Verner et
al., (1994) and from 23 CD-ROM by Kurucz (1994). Some information was
obtained through the Opacity Project. As we ignored a multiple
structure of all the levels, the oscillator strengths for each
averaged transition were calculated as
Table 3. Linearized transitions Table 4. Fixed transitions After the combined solution of radiative transfer and statistical equilibrium equations, the averaged levels have been splitted with respect to multiplet structure, then level populations were redistributed proportionally to the statistical weights of the corresponding sublevels and finally the lines of the interest were studied. A certain problem is linked with a correct accounting of the line
broadening due to a quadratic Stark effect. Some estimates of the
broadening constants were taken from Kuruczs CD-ROM 23. For the rest
transitions we used a classic expression for radiative broadening
constant and Stark broadening constant was adopted to be equal to
Together with the broadening constants, we have also taken into account the microturbulence parameter. It is important to note that all the broadening mechanisms were included in both the statistical equilibrium and line formation calculations. Collisional ionization was described using Seaton's formula (Seaton, 1962): were where with collisional force of 1. ![]() ![]() ![]() ![]() © European Southern Observatory (ESO) 1999 Online publication: February 23, 1999 ![]() |