Accretion of a giant planet onto a white dwarf
Boris T. Gaensicke, Matthias R. Schreiber, Odette Toloza, Nicola P., Gentile Fusillo, Detlev Koester, Christopher J. Manser

TL;DR
This paper reports the discovery of a giant planet orbiting a hot white dwarf, with evidence of accretion from a unique circumstellar gaseous disc likely originating from planetary material, suggesting planetary survival and interaction in post-main-sequence systems.
Contribution
It provides the first spectroscopic evidence of a giant planet around a white dwarf actively accreting from a circumstellar disc with an unusual composition, indicating planetary survival and dynamical interactions.
Findings
Detection of a gaseous disc with planetary-like composition.
Evidence for a giant planet undergoing evaporation near the white dwarf.
Estimated occurrence rate of close-orbit giant planets around white dwarfs is ~10^-4.
Abstract
The detection of a dust disc around G29-38 and transits from debris orbiting WD1145+017 confirmed that the photospheric trace metals found in many white dwarfs arise from the accretion of tidally disrupted planetesimals. The composition of these planetesimals is similar to that of rocky bodies in the inner solar system. Gravitationally scattering planetesimals towards the white dwarf requires the presence of more massive bodies, yet no planet has so far been detected at a white dwarf. Here we report optical spectroscopy of a K hot white dwarf that is accreting from a circumstellar gaseous disc composed of hydrogen, oxygen, and sulphur at a rate of . The composition of this disc is unlike all other known planetary debris around white dwarfs, but resembles predictions for the makeup of deeper atmospheric layers of icy giant planets,…
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