Orbitally modulated dust formation by the WC7+O5 colliding-wind binary WR140

TL;DR

This study uses high-resolution infrared imaging and photometry to analyze dust formation and distribution in the colliding-wind binary WR140, revealing the dynamics and timing of dust features related to the binary's orbit.

Contribution

First detailed multi-epoch infrared imaging and photometry of WR140, linking dust features to binary orbit and wind-collision region dynamics.

Findings

Dust features move with constant proper motions

Dust formation episodes correlate with binary orbital phases

Dust distribution is asymmetric and influenced by wind collision geometry

Abstract

We present high-resolution infrared (2--18 micron) images of the archetypal periodic dust-making Wolf-Rayet binary system WR140 (HD 193793) taken between 2001 and 2005, and multi-colour (J -- [19.5]) photometry observed between 1989 and 2001. The images resolve the dust cloud formed by WR140 in 2001, allowing us to track its expansion and cooling, while the photometry allows tracking the average temperature and total mass of the dust. The combination of the two datasets constrains the optical properties of the dust. The most persistent dust features, two concentrations at the ends of a `bar' of emission to the south of the star, were observed to move with constant proper motions of 324+/-8 and 243+/-7 mas/y. Longer wavelength (4.68-micron and 12.5-micron) images shows dust emission from the corresponding features from the previous (1993) periastron passage and dust-formation episode. A third persistent dust concentration to the east of the binary (the `arm') was found to have a proper motion ~ 320 mas/y. Extrapolation of the motions of the concentrations back to the binary suggests that the eastern `arm' began expansion 4--5 months earlier than those in the southern `bar', consistent with the projected rotation of the binary axis and wind-collision region (WCR) on the sky. Comparison of model dust images and the observations constrain the intervals when the WCR was producing sufficiently compressed wind for dust nucleation in the WCR, and suggests that the distribution of this material was not uniform about the axis of the WCR, but more abundant in the following edge in the orbital plane.