Astronomy and Astrophysics – Astrophysics
Scientific paper
1998-03-17
Astronomy and Astrophysics
Astrophysics
Accepted for publication in ApJ. LaTeX, 30 pages (including 8 figs and 2 tables)
Scientific paper
10.1086/306109
This paper discusses the properties of scattering--dominated active galactic nuclei (AGN). We define these to be AGN for which the direct line-of-sight to the continuum source is obscured by Compton-thick material. The aim is to construct, for the first time, a model consistent with X-ray line luminosities, line ratios and various luminosity indicators. The ASCA spectra of six such sources show several X-ray lines that can be reliably measured, mostly due to highly ionized magnesium, silicon sulphur and iron. These enable us to investigate the physical conditions of the scattering material. The sources show evidence of He-like and H-like iron lines that are likely to be produced in hot (T approx 10^6 K) photoionized gas. By measuring the EW of the lines, and by constructing a diagnostic line-ratio diagram, we demonstrate that the silicon and magnesium lines are produced by the same gas emitting the highly ionized iron lines. The properties of this gas are rather different from the properties of warm absorbers in type I AGN. Neutral 6.4 keV iron lines are also detected, originating in a different component which can be either Compton-thin or Compton-thick. The best measured iron lines suggest an enhancement of n_{Fe}/n_H by a factor approx 2 compared to solar, in both the hot and cool Compton-thin components. We further show that in four of the sources, the Fe Kalpha(6.4keV)/Hbeta (lambda 4861Ang) line ratio is consistent with that predicted for typical narrow line region clouds, and the reddening corrected Hbeta is known, provided the column density is larger than approx 10^{22.5}/cm^2, alpha_{ox} is smaller than 1.3. For some sources, this is a viable alternative to the commonly assumed Compton thick medium as the origin of the 6.4 keV iron line.
George Ian Michael
Netzer Hagai
Turner Tracey Jane
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