Formation of ultra-massive carbon-oxygen white dwarfs from the merger of carbon-oxygen and helium white dwarf pairs
Chengyuan Wu, Heran Xiong, Xiaofeng Wang

TL;DR
This study explores how mergers of carbon-oxygen and helium white dwarfs can produce ultra-massive white dwarfs, potentially explaining observed long cooling delays and the formation of oxygen-neon cores.
Contribution
It demonstrates through stellar evolution modeling that CO and He WD mergers can lead to UMWDs with diverse core compositions, including ONe cores, clarifying their formation pathways.
Findings
Post-merger remnants resemble R CrB stars.
CO core mass can grow up to about 1.2 solar masses.
Remnants with core mass >1.2 Msun may ignite surface carbon.
Abstract
Ultra-massive white dwarfs (UMWDs) with masses larger than 1.05Msun are basically believed to harbour oxygen-neon (ONe) cores. Recently, Gaia data reveals an enhancement of UMWDs on Hertzsprung-Russell diagram (HRD), which indicates that extra cooling delay mechanism such as crystallization and elemental sedimentation may exist in the UMWDs. Further studies suggested that a portion of UMWDs should have experienced pretty 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 investigated whether the merges of massive CO WDs with helium WDs (He WDs) can evolve to UMCOWDs. By employing 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 are similar to R CrB stars. The helium burning…
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