Journal
MONTHLY NOTICES OF THE ROYAL ASTRONOMICAL SOCIETY
Volume 525, Issue 2, Pages 2366-2379Publisher
OXFORD UNIV PRESS
DOI: 10.1093/mnras/stad2386
Keywords
accretion, accretion discs; stars: neutron; X-rays: binaries; X-rays: individual: 4U 1820-30; ISM: jets and outflows
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This paper presents the results of a multiwavelength observational campaign on the neutron star low-mass X-ray binary 4U 1820-30, showing that the X-ray flux modulation is mainly caused by changes in the size of the region providing seed photons for the Comptonization spectrum.
The accretion flow/jet correlation in neutron star (NS) low-mass X-ray binaries (LMXBs) is far less understood when compared to black hole (BH) LMXBs. In this paper we will present the results of a dense multiwavelength observational campaign on the NS LMXB 4U 1820-30, including X-ray (NICER, NuSTAR, and AstroSat) and quasi-simultaneous radio (ATCA) observations in 2022. 4U 1820-30 shows a peculiar 170 d super-orbital accretion modulation, during which the system evolves between 'modes' of high and low X-ray flux. During our monitoring, the source did not show any transition to a full hard state. X-ray spectra were well described using a disc blackbody, a Comptonization spectrum along with a Fe K emission line at similar to 6.6 keV. Our results show that the observed X-ray flux modulation is almost entirely produced by changes in the size of the region providing seed photons for the Comptonization spectrum. This region is large (similar to 15 km) in the high mode and likely coincides with the whole boundary layer, while it shrinks significantly (less than or similar to 10 km) in low mode. The electron temperature of the corona and the observed rms variability in the hard X-rays also exhibit a slight increase in low mode. As the source moves from high to low mode, the radio emission due to the jet becomes similar to 5 fainter. These radio changes appear not to be strongly connected to the hard-to-soft transitions as in BH systems, while they seem to be connected mostly to variations observed in the boundary layer.
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