Phase-resolved optical and X-ray spectroscopy of low-mass X-ray binary X1822-371

TL;DR

This study combines optical and X-ray phase-resolved spectroscopy to analyze the accretion disc structure and outflows in the high-inclination low-mass X-ray binary X1822-371, revealing a thick disc rim and isotropic outflows.

Contribution

It presents a comprehensive multi-wavelength analysis of X1822-371, introducing a model with a thick disc rim and outflowing matter, supported by Doppler tomography and spectral fitting.

Findings

Accretion disc has a thick rim at stream impact site.

Evidence of isotropic outflow from the impact region.

Optical emission lines originate above the disc plane.

Abstract

(Abridged) X1822-371 is the prototypical accretion disc corona X-ray source, a low-mass X-ray binary viewed at very high inclination, thereby allowing the disc structure and extended disc coronal regions to be visible. We study the structure of the accretion disc in X1822-371 by modelling the phase-resolved spectra both in optical and X-ray regime. We analyse high time resolution optical ESO/VLT spectra of X1822-371 to study the variability in the emission line profiles. In addition, we use data from XMM-Newton space observatory to study phase-resolved as well as high resolution X-ray spectra. We apply the Doppler tomography technique to reconstruct a map of the optical emission distribution in the system. We fit multi-component models to the X-ray spectra. We find that our results from both the optical and X-ray analysis can be explained with a model where the accretion disc has a thick rim in the region where the accretion stream impacts the disc. The behaviour of the H_beta line complex implies that some of the accreting matter creates an outburst around the accretion stream impact location and that the resulting outflow of matter moves both away from the accretion disc and towards the centre of the disc. Such behaviour can be explained by an almost isotropic outflow of matter from the accretion stream impact region. The optical emission lines of HeII 4686 and 5411 show double peaked profiles, typical for an accretion disc at high inclination. However, their velocities are slower than expected for an accretion disc in a system like X1822-371. This, combined with the fact that the HeII emission lines do not get eclipsed during the partial eclipse in the continuum, suggests that the line emission does not originate in the orbital plane and is more likely to come from above the accretion disc, for example the accretion disc wind.