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SDSSJ084539.17+225728.0: the first DBZ white dwarf with a metal-rich gaseous debris disc

  • Gaensicke, B. T.
  • Koester, D.
  • Marsh, T. R.
  • Rebassa-Mansergas, A.
  • Southworth, J.
Published Article
Publication Date
Sep 15, 2008
Submission Date
Sep 15, 2008
DOI: 10.1111/j.1745-3933.2008.00565.x
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We report the discovery of a third white dwarf hosting a gaseous debris disc, SDSSJ084539.17+225728.0. The typical double-peaked CaII 8498,8542,8662A emission lines can be modelled in terms of a Keplerian gas disc with a radial extent from ~0.5Rsun to ~1.0. The effective temperature of SDSS0845+2257, Teff=18600+-500K, is comparable to the two other white dwarfs with gaseous discs, SDSS1043+0855 and SDSS1228+1040, and hence substantially hotter than the bulk of white dwarfs where dusty debris discs were identified through the presence of infrared excess flux. This may suggest that the conditions to produce emission lines from debris discs in the optical wavelength range are only met for a relatively narrow range in Teff. The observed asymmetry in the line profiles indicates a substantial eccentricity in the disc. Two spectra obtained four years apart reveal a significant change in the shapes and equivalent widths of the line profiles, implying that the circumstellar disc evolves on relatively short time scales. In contrast to SDSS1043+0855 and SDSS1228+1040, SDSS0845+2257 has a helium-dominated atmosphere. We detect photospheric absorption lines of He, Ca, Mg, and Si in the Sloan Digital Sky Survey spectrum, and hence classify SDSS0845+2257 as DBZ white dwarf. The abundances for the three metals determined from model atmosphere fits are Ca/He~1.3x10^-7, Mg/He~6.0x10^-6, and Si/He~8.0x10^-6. From the non-detection of Halpha we derive H/He<3x10^-5, which implies that the hydrogen-to-metal abundance ratio of the circumstellar material is >~1000 times lower than in the Sun. This lends strong support to the hypothesis that the gaseous and dusty debris discs found around roughly a dozen white dwarfs originate from the disruption of rocky planetary material.

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