On the 10-micron silicate feature in Active Galactic Nuclei
Robert Nikutta (1), Moshe Elitzur (1), Mark Lacy (2) ((1) Department, of Physics, Astronomy, University of Kentucky, (2) Spitzer Science Center,, Caltech)

TL;DR
This paper explains the varied 10-micron silicate features in AGN using clumpy dust models, revealing insights into dust geometry, obscuration, and radiative transfer effects that account for observed emission and absorption behaviors.
Contribution
It introduces a comprehensive clumpy dust radiative transfer model that explains the diverse silicate features in AGN spectra, including emission in type 2 sources and shifted peaks.
Findings
First type 2 quasar with silicate emission modeled successfully.
Standard dust models can explain shifted emission peaks.
Silicate features are never deeply absorbed in the models.
Abstract
The 10-micron silicate feature observed with Spitzer in active galactic nuclei (AGN) reveals some puzzling behavior. It (1) has been detected in emission in type 2 sources, (2) shows broad, flat-topped emission peaks shifted toward long wavelengths in several type 1 sources, and (3) is not seen in deep absorption in any source observed so far. We solve all three puzzles with our clumpy dust radiative transfer formalism. (1) We present the spectral energy distribution (SED) of SST1721+6012, the first type 2 quasar observed to show a clear 10-mic silicate feature in emission. We constructed a large database of clumpy torus models and performed extensive fitting of the observed SED, constraining several of the torus parameters. We find that the source bolometric luminosity is ~3*10^12 L_sun. Our modeling suggests that <35% of objects with tori sharing characteristics and geometry similar…
Peer Reviews
No public reviews on file for this paper yet. If you reviewed it on a platform where reviews are public (OpenReview, ICLR, NeurIPS, ICML), you can paste yours below so the community can read it here.
Videos
No videos yet. Explain this paper in a talk, walkthrough, or lecture? Add one.
