Towards an observationally motivated AGN dusty torus model – I. Dust chemical composition from the modelling of Spitzer spectra

Author:

Reyes-Amador Omar Ulises1ORCID,Fritz Jacopo1ORCID,González-Martín Omaira1ORCID,Srinivasan Sundar1,Baes Maarten2ORCID,Lopez-Rodriguez Enrique3ORCID,Osorio-Clavijo Natalia1ORCID,Victoria-Ceballos Cesar Iván1,Stalevski Marko24,Ramos Almeida C56ORCID

Affiliation:

1. Instituto de Radioastronomía y Astrofísica (IRyA), Universidad Nacional Autónoma de México (UNAM), Antigua Carretera a Pátzcuaro , 8701, Ex-Hda. San José de la Huerta, Morelia, Michoacán, 58089 , México

2. Sterrenkundig Observatorium, Universiteit Gent , Krijgslaan 281 S9, B-9000 Gent , Belgium

3. Kavli Institute for Particle Astrophysics & Cosmology (KIPAC), Stanford University , Stanford, CA 94305 , USA

4. Astronomical Observatory , Volgina 7, 11060 Belgrade , Serbia

5. Instituto de Astrofísica de Canarias, Calle Vía Láctea , s/n, E-38205 La Laguna, Tenerife , Spain

6. Departamento de Astrofísica, Universidad de La Laguna , E-38206 La Laguna, Tenerife , Spain

Abstract

ABSTRACT Spectral energy distribution (SED) fitting is one of the most commonly used techniques to study the dust properties in active galactic nuclei (AGN). Works implementing this technique commonly use radiative transfer models that assume a variety of dust properties. Despite the key role of this aspect, limited effort has been put forward to explore the chemical composition, the role of different optical properties, and the grain size distribution of dust, all of which can have a substantial impact on the theoretical radiative transfer calculations. In this work, we explore the role of the dust chemical composition in the AGN dusty torus through SED fitting to Spitzer/IRS spectra of a sample of 49 nearby AGN with silicate features in emission. We implement a mineralogy model including the popular astronomical silicates and a set of oxides and amorphous silicates with different grain sizes. Wefind that best fits use principally porous alumina, periclase, and olivine. In terms of mass fractions, $\sim 99~{{\ \rm per\ cent}}$ of the dust is composed of dust grains of size $\rm {0.1 \, \mu m}$, with a $\lt 1~{{\ \rm per\ cent}}$ contribution from $\rm {3 \, \mu m}$ grains. Moreover, the astronomical silicates have a very low occurrence in the best fits, suggesting that they are not the most suited dust species to reproduce the silicate features in our sample.

Funder

CONACyT

Horizon 2020

Ministry of Science and Technology

Publisher

Oxford University Press (OUP)

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