X-ray Variability of VHE FSRQs
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IISER Mohali
Abstract
Flat Spectrum Radio Quasars (FSRQs) are a class of Active Galactic Nuclei (AGNs) that
come under the category of Blazars along with BL Lacs. They have relativistic jets aligned
at very small angles (< 15 0 ) to the line of sight. Despite being strong gamma-ray emitters
in the MeV-GeV range, these are not frequently detected at Very High Energy (VHE, E >
100GeV). Usually, high-frequency peaked BL Lacs are found emitting VHE. Out of a total
of 651 FSRQ detected in the Fermi gamma-ray observatory, 9 of them have been found to
emit in VHE. The project studied the properties of the 9 FSRQs in the X-ray region. The
Blazars have a characteristic double-humped Spectral Energy Distribution (SED), with the
first peak (optical/UV) attributed to Synchrotron emission and the second peak (gamma
ray) to inverse Compton scattering. In this leptonic scenario, both peaks are correlated.
X-ray emission can have contributions from the high-energy tail of the synchrotron peak
and thus is related to the VHE emission. X-ray emissions in FSRQs are due to Synchrotron
Self Compton (SSC) in general.
The temporal and spectral behaviour of the source was studied using the light curves and
SEDs during VHE and non-VHE times in the X-ray regime. The data was taken from the
XRT Telescope of the Neils Geherel Swift Observatory. HEASoft version 6.30.1 package
was used for the analysis. The light curve showed variability, and VHE emissions were
found at both low and high flux states. The SEDs were fitted to the power law model. It
showed a rising trend for all sources except for PKS 1441+25, which showed completely
opposite behaviour plausibly due to more synchrotron components. The SED showed a
similar trend during VHE and non-VHE times. There was no peculiarity for the 9 sources
during VHE emissions in terms of temporal flux variability, flux states, spectral index, and
spectral shape compared to these behaviour during non-VHE times, indicating the VHE to
be likely due to the high brightness of the source.
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