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  5. A new powerful and highly variable disc wind in an AGN-star-forming galaxy, the case of MCG-03-58-007
 

A new powerful and highly variable disc wind in an AGN-star-forming galaxy, the case of MCG-03-58-007

Journal
MONTHLY NOTICES OF THE ROYAL ASTRONOMICAL SOCIETY  
Date Issued
2018
Author(s)
BRAITO, Valentina  
•
Reeves, J. N.
•
Matzeu, G. A.
•
SEVERGNINI, Paola  
•
Ballo, L.
•
CACCIANIGA, Alessandro  
•
CAMPANA, Sergio  
•
CICONE, CLAUDIA
•
DELLA CECA, Roberto  
•
Turner, T. J.
DOI
10.1093/mnras/sty1697
Abstract
We present the discovery of a new candidate for a fast disc wind, in the nearby Seyfert 2 galaxy MCG-03-58-007. This wind is discovered in a deep Suzaku observation that was performed in 2010. Overall the X-ray spectrum of MCG-03-58-007 is highly absorbed by a neutral column density of NH ∼1023 cm-2, in agreement with the optical classification as a type 2 active galactic nucleus. In addition, this observation unveiled the presence of two deep absorption troughs at E = 7.4 ± 0.1 and 8.5 ± 0.2 keV. If associated with blueshifted Fe XXVI, these features can be explained with the presence of two highly ionized (log ξ/erg cm s-1 ∼5.5) and high column density (NH ∼ 5-8 × 1023 cm-2) outflowing absorbers with vout1 ∼ -0.1c and vout2 ∼ -0.2c. The disc wind detected during this observation is most likely launched from within a few hundreds gravitational radii from the central black and has a kinetic output that matches the prescription for significant feedback. The presence of the lower velocity component of the disc wind is independently confirmed by the analysis of a follow-up XMM-Newton and NuSTAR observation. A faster (vout ∼ -0.35c) component of the wind is also seen in this second observation. During this observation we also witnessed an occultation event lasting ∆t ∼ 120 ks, which we ascribe to an increase of the opacity of the disc wind (∆NH ∼ 1.4 × 1024 cm-2). Our interpretation is that the slow zone (vout ∼ -0.1c) of the wind is the most stable but inhomogeneous component, while the faster zones could be associated with two different inner streamlines of the wind.
Volume
479
Issue
3
Start page
3592
Uri
http://hdl.handle.net/20.500.12386/28401
Url
https://academic.oup.com/mnras/article-abstract/479/3/3592/5046490
Issn Identifier
0035-8711
Ads BibCode
2018MNRAS.479.3592B
Rights
open.access
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