Heavy metals in a light white dwarf: Abundances of the metal-rich, extremely low-mass GALEX J1717+6757
J. J. Hermes, B. T. Gaensicke, D. Koester, M. C. P. Bours, D. M., Townsley, J. Farihi, T. R. Marsh, Stuart Littlefair, V. S. Dhillon, A., Gianninas, E. Breedt, and R. Raddi

TL;DR
This study analyzes the atmospheric metal abundances of a low-mass white dwarf using ultraviolet spectroscopy, revealing complex processes like radiative levitation and ruling out ongoing accretion as the source of metals.
Contribution
First detailed abundance analysis of a low-mass white dwarf with far-ultraviolet spectroscopy, highlighting the roles of radiative levitation and other mechanisms in metal presence.
Findings
Metals detected include Ca, Fe, Ti, P at near-solar levels.
Diffusion timescales for metals are less than 20 years.
Radiative levitation supports some metals but not all, suggesting additional processes.
Abstract
Using the Hubble Space Telescope, we detail the first abundance analysis enabled by far-ultraviolet spectroscopy of a low-mass (~0.19 Msun) white dwarf (WD), GALEX J1717+6757, which is in a 5.9-hr binary with a fainter, more-massive companion. We see absorption from nine metals, including roughly solar abundances of Ca, Fe, Ti, and P. We detect a significantly sub-solar abundance of C, and put upper limits on N and O that are also markedly sub-solar. Updated diffusion calculations indicate that all metals should settle out of the atmosphere of this 14,900 K, log(g) = 5.67 WD in the absence of radiative forces in less than 20 yr, orders of magnitude faster than the cooling age of hundreds of Myr. We demonstrate that ongoing accretion of rocky material that is often the cause of atmospheric metals in isolated, more massive WDs is unlikely to explain the observed abundances in GALEX…
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