A study of the interacting binary V 393 Scorpii

TL;DR

This study provides detailed spectroscopic analysis of V 393 Sco, revealing its stellar parameters, circumstellar environment, and mass transfer dynamics, with implications for understanding interacting binary systems.

Contribution

It offers new high-resolution spectroscopic data and a comprehensive analysis of V 393 Sco's physical properties and mass loss mechanisms, improving understanding of its long cycle variability.

Findings

Determined stellar temperatures and distance with spectral energy distribution fitting.

Identified orbital modulation of He I line indicating a pseudo-photosphere and equatorial mass loss.

Estimated mass ratio and mass function, supporting equatorial mass loss as the variability cause.

Abstract

We present high resolution J-band spectroscopy of V 393 Sco obtained with the CRIRES at the ESO Paranal Observatory along with a discussion of archival IUE spectra and published broad band magnitudes. The best fit to the spectral energy distribution outside eclipse gives $T_{1}$= 19000 $\pm$ 500 $K$ for the gainer, $T_{2}$= 7250 $\pm$ 300 $K$ for the donor, $E(B-V)$= 0.13 $\pm$ 0.02 mag. and a distance of $d$= 523 $\pm$ 60 pc, although circumstellar material was not considered in the fit. We argue that V 393 Sco is not a member of the open cluster M7. The shape of the He I 1083 nm line shows orbital modulations that can be interpreted in terms of an optically thick pseudo-photosphere mimicking a hot B-type star and relatively large equatorial mass loss through the Lagrangian L3 point during long cycle minimum. IUE spectra show several (usually asymmetric) absorption lines from highly ionized metals and a narrow L$\alpha$ emission core on a broad absorption profile. The overall behavior of these lines suggests the existence of a wind at intermediate latitudes. From the analysis of the radial velocities we find $M_{2}/M_{1}$= 0.24 $\pm$ 0.02 and a mass function of $f$= 4.76 $\pm$ 0.24 M$\odot$. Our observations favor equatorial mass loss rather than high latitude outflows as the cause for the long variability.