White Dwarf Merger Remnants with Cooling Delays on the Q Branch Lack Strong Magnetism
Lou Baya Ould Rouis, J. J. Hermes, Joseph A. Guidry, Sihao Cheng, Mukremin Kilic, Olivier Vincent, Pierre Bergeron, Simon Blouin, Adam Moss, Isaac D. Lopez, Gracyn Jewett
TL;DR
This study targets the Gaia-identified Q branch of ultra-massive white dwarfs, where long cooling delays may reveal merger histories or alternative evolution. By constructing a spectroscopically complete 100 pc sample and separating objects into a kinematically delayed (merger-like) subset and a young subset, the authors use atmospheric composition, magnetism, and rotation as diagnostic probes, complemented by 26 new spectra and a comparison to canonical-mass WDs. They find that the most delayed WDs show no strong magnetism and a high fraction of carbon-dominated atmospheres, while the younger Q branch remnants can be magnetized but with an overall distinct distribution from field, single-star WDs; pulsations are detected in two DAQ WDs, potentially extending the DAV instability strip for thin-H layers. These results imply that Q branch cooling delays may stem from multiple channels, including merger remnants with little or dissipated magnetism, or alternative formation pathways, with significant implications for cosmological age dating and our understanding of WD evolution.
Abstract
A population of anomalous ultra-massive white dwarfs discovered with Gaia, often referred to as the Q branch, show high (multi-Gyr) cooling delays produced by exotic physical mechanisms. They are believed to be the products of stellar mergers, but the exact origin and formation channel remain unclear. We obtained a spectroscopically complete, volume-limited sample of the Q branch region within 100 pc, and found significant differences in atmospheric composition and rotation rates as a function of tangential velocity. In particular, we discover that stellar remnants with the longest cooling delays do not show strong magnetism nor detectable short-period rotational variability, as opposed to what is generally believed for double-degenerate mergers. This indicates that either these white dwarfs arise from a formation channel with no strong magnetism induced, or that the magnetism produced from the merger dissipates over the cooling delay timescales. Our follow-up photometry has also discovered pulsations in the second and third hydrogen-dominated DAQ white dwarfs, one hotter than 15,500 K, possibly extending the boundaries of the DAV instability strip for white dwarfs with thin hydrogen layers.
