A hot white dwarf merger remnant revealed by an ultraviolet detection of carbon

TL;DR

This study uses ultraviolet spectroscopy to detect low levels of atmospheric carbon in a white dwarf, revealing it as a merger remnant with a unique envelope structure, thus expanding understanding of white dwarf evolution.

Contribution

First ultraviolet detection of atmospheric carbon in a white dwarf, revealing a merger remnant with a novel envelope structure not seen in single-star evolution.

Findings

Ultraviolet spectrum reveals lower carbon abundance than optical counterparts.

The white dwarf's envelope mass is much lower than expected from single-star evolution.

A thin hydrogen layer atop a semi-convection zone explains the low surface carbon.

Abstract

Atmospheric carbon has been detected in the optical spectra of six hydrogen-rich ultra-massive white dwarfs, revealing large carbon abundances (log C/H > $-$0.5) attributable to the convective dredge-up of internal carbon into thin hydrogen surface layers. These rare white dwarfs likely originate from stellar mergers, making them "smoking guns" for one of the binary evolution channels leading to thermonuclear supernovae. However, optical spectroscopy can uncover only the most carbon-enriched objects, suggesting that many more merger remnants may masquerade as normal pure-hydrogen atmosphere white dwarfs. Here, we report the discovery of atmospheric carbon in a Hubble Space Telescope far-ultraviolet spectrum of WD$\,$0525+526, a long-known hydrogen-rich ultra-massive white dwarf. The carbon abundance (log C/H = $-$4.62) is 4$-$5 dex lower than in the six counterparts and thus detectable only at ultraviolet wavelengths. We find that the total masses of hydrogen and helium in the envelope ($10^{-13.8}$ and $10^{-12.6}$ of the total white dwarf mass) are substantially lower than those expected from single-star evolution, implying that WD$\,$0525+526 is a merger remnant. Our modelling indicates that the low surface carbon abundance arises from an envelope structure in which a thin hydrogen-rich layer floats atop a semi-convection zone$-$a process that has been largely overlooked in white dwarfs. Our study highlights the importance of ultraviolet spectroscopy in identifying and characterising merger remnants.