THE EFFECTS OF FE-II NON-LTE ON NOVA ATMOSPHERES AND SPECTRA

Citation
Ph. Hauschildt et al., THE EFFECTS OF FE-II NON-LTE ON NOVA ATMOSPHERES AND SPECTRA, The Astrophysical journal, 462(1), 1996, pp. 386-403
Citations number
22
Categorie Soggetti
Astronomy & Astrophysics
Journal title
ISSN journal
0004637X
Volume
462
Issue
1
Year of publication
1996
Part
1
Pages
386 - 403
Database
ISI
SICI code
0004-637X(1996)462:1<386:TEOFNO>2.0.ZU;2-B
Abstract
The atmospheres of novae at early times in their outbursts are very ex tended, expanding shells with low densities. Models of these atmospher es show that non-LTE effects are very important and must be included i n realistic calculations. We have, therefore, been improving our atmos pheric studies by increasing the number of ions treated in non-LTE. On e of the most important ions is Fe II, which has a complex structure a nd numerous lines in the observable spectrum. In this paper we investi gate non-LTE effects for Fe II for a wide variety of parameters. We us e a detailed Fe Ir model atom with 617 level and 13,675 primary lines, treated using a rate-operator formalism. We show that the radiative t ransfer equation in nova atmospheres must be treated with sophisticate d numerical methods and that simple approximations, such as the Sobole v method, cannot be used because of the large number of overlapping li nes in the comoving frame.Our results show that the formation of the F e II lines is strongly affected by non-LTE effects. For low effective temperatures, T-eff < 20,000 K, the optical Fe II lines are most influ enced by non-LTE effects, while for higher T-eff the UV lines of Fe II are very strongly affected by non-LTE. The departure coefficients are such that Fe II tends to be overionized in non-LTE when compared to L TE. Therefore, Fe II non-LTE must be included with sophisticated radia tive transfer in nova atmosphere models in order to analyze observed n ova spectra reliably. Finally, we show that the number of wavelength p oints required for the Fe II non-LTE model atmosphere calculations can be reduced from 90,000 to about 30,000 without changing the results i f we choose a sufficiently dense UV wavelength grid.