资源环境科技发展态势分析平台

The detection¹ of a dust disk around the white dwarf star G29-38 and transits from debris orbiting the white dwarf WD 1145+017 (ref. ²) confirmed that the photospheric trace metals found in many white dwarfs³ arise from the accretion of tidally disrupted planetesimals⁴. The composition of these planetesimals is similar to that of rocky bodies in the inner Solar System⁵. Gravitational scattering of planetesimals towards the white dwarf requires the presence of more massive bodies⁶, yet no planet has so far been detected at a white dwarf. Here we report optical spectroscopy of a hot (about 27,750 kelvin) white dwarf, WD聽J091405.30+191412.25, that is accreting from a circumstellar gaseous disk composed of hydrogen, oxygen and sulfur at a rate of about 3.3聽脳聽10⁹ grams per second. The composition of this disk is unlike all other known planetary debris around white dwarfs⁷, but resembles predictions for the makeup of deeper atmospheric layers of icy giant planets, with H₂O and H₂S being major constituents. A giant planet orbiting a hot white dwarf with a semi-major axis of around 15 solar radii will undergo substantial evaporation with expected mass loss rates comparable to the accretion rate that we observe onto the white dwarf. The orbit of the planet is most probably the result of gravitational interactions, indicating the presence of additional planets in the system. We infer an occurrence rate of approximately 1 in 10,000 for spectroscopically detectable giant planets in close orbits around white dwarfs.