Formation of ultra-massive carbon–oxygen white dwarfs from the merger of carbon–oxygen and helium white dwarf pairs. Issue 2 (31st March 2022)

• Record Type: Journal Article
• Authors: Wu, Chengyuan; Xiong, Heran; Wang, Xiaofeng
• Is Part Of: Monthly notices of the Royal Astronomical Society. Volume 512:Issue 2(2022)
• Page Start: 2972
• Page End: 2987
• Publication Date: 2022-03-31
• Subjects: stars: evolution -- binaries: close -- stars: white dwarfs; Astronomy -- Periodicals; Periodicals; 520.5
• DOI: 10.1093/mnras/stac273
• Languages: English
• ISSNs: 0035-8711

Abstract

ABSTRACT: Ultra-massive white dwarfs (UMWDs) with masses larger than 1.05M⊙ are basically believed to harbour oxygen–neon (ONe) cores. Recently, Gaia data have revealed an enhancement of UMWDs on the Hertzsprung–Russell diagram (HRD), which indicates that an extra cooling delay mechanism such as crystallization and elemental sedimentation may exist in UMWDs. Further studies have suggested that some UMWDs should have experienced fairly long cooling delays, implying that they are carbon–oxygen (CO) WDs. However, the formation mechanism of these UMCOWDs is still under debate. In this work, we investigate whether the mergers of massive CO WDs with helium WDs (He WDs) can evolve to UMCOWDs. By employing the stellar evolution code mesa, we construct double WD merger remnants to investigate their final fates. We found that the post-merger evolution of the remnants is similar to R CrB stars. The helium burning of the He shell leads to mass growth of the CO core at a rate of 2.0 × 10 −6 –$5.0\times {10}^{-6}\, {\rm M}_\odot \, \rm {yr}^{-1}$ . The final CO WD mass is influenced by the wind mass-loss rate during the post-merger evolution, and cannot exceed about 1.2M⊙ . Remnants with core masses larger than $1.2\, {\rm M}_\odot$ will experience surface carbon ignition, which may finally end their lives as ONe WDs. The current results imply that at least some UMWDs that experience extra-long cooling delays may stem from the merging of CO WDs and He WDs.