Unusual Abundances from Planetary System Material Polluting the White Dwarf G238-44
Ted M Johnson, Beth L. Klein, D. Koester, Carl Melis, B. Zuckerman, M., Jura

TL;DR
This study analyzes the atmospheric composition of white dwarf G238-44, revealing unusual elemental abundances and evidence of accretion from multiple planetary bodies, including rocky and icy objects, indicating a highly perturbed exoplanetary system.
Contribution
It presents the first detection of nitrogen in a white dwarf polluted by planetary material and models the accreted material as a mix of rocky and icy bodies, revealing complex planetary system dynamics.
Findings
Detection of ten heavy elements, including nitrogen, in G238-44's atmosphere.
Stable accretion over 24 years suggests a continuous circumstellar reservoir.
Evidence for a mix of iron-rich and icy planetary material.
Abstract
Ultraviolet and optical spectra of the hydrogen-dominated atmosphere white dwarf star G238-44 obtained with FUSE, Keck/HIRES, HST/COS, and HST/STIS reveal ten elements heavier than helium: C, N, O, Mg, Al, Si, P, S, Ca, and Fe. G238-44 is only the third white dwarf with nitrogen detected in its atmosphere from polluting planetary system material. Keck/HIRES data taken on eleven nights over 24 years show no evidence for variation in the equivalent width of measured absorption lines, suggesting stable and continuous accretion from a circumstellar reservoir. From measured abundances and limits on other elements we find an anomalous abundance pattern and evidence for the presence of metallic iron. If the pollution is from a single parent body, then it would have no known counterpart within the solar system. If we allow for two distinct parent bodies, then we can reproduce the observed…
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Taxonomy
TopicsAstro and Planetary Science · Stellar, planetary, and galactic studies · Astronomy and Astrophysical Research
