Seven white dwarfs with circumstellar gas discs I: white dwarf parameters and accreted planetary abundances

Author:

Rogers L K1ORCID,Bonsor A1ORCID,Xu SORCID,Dufour P2,Klein B L3,Buchan A1ORCID,Hodgkin S1,Hardy F2,Kissler-Patig M4ORCID,Melis C5,Weinberger A J6,Zuckerman B3

Affiliation:

1. Institute of Astronomy, University of Cambridge , Madingley Road, Cambridge CB3 0HA , UK

2. Département de Physique, Université de Montréal , C.P. 6128, Succ. Centre-Ville, Montréal, Québec H3C 3J7 , Canada

3. Department of Physics and Astronomy, University of California , Los Angeles, CA 90095-1562 , USA

4. European Space Agency – European Space Astronomy Centre , Camino Bajo del Castillo, s/n., Villanueva de la Canada, E-28692 Madrid , Spain

5. Center for Astrophysics and Space Sciences, University of California , San Diego, CA 92093-0424 , USA

6. Earth and Planets Laboratory, Carnegie Institution for Science , 5241 Broad Branch Rd NW, Washington, DC 20015 , USA

Abstract

ABSTRACT Observations of planetary material polluting the atmospheres of white dwarfs are an important probe of the bulk composition of exoplanetary material. Medium- and high-resolution optical and ultraviolet spectroscopy of seven white dwarfs with known circumstellar dust and gas emission are presented. Detections or meaningful upper limits for photospheric absorption lines are measured for: C, O, Na, S, P, Mg, Al, Si, Ca, Ti, Cr, Fe, and Ni. For 16 white dwarfs with known observable gaseous emission discs (and measured photospheric abundances), there is no evidence that their accretion rates differ, on average, from those without detectable gaseous emission. This suggests that, typically, accretion is not enhanced by gas drag. At the effective temperature range of the white dwarfs in this sample (16 000–25 000 K) the abundance ratios of elements are more consistent than absolute abundances when comparing abundances derived from spectroscopic white dwarf parameters versus photometric white dwarf parameters. Crucially, this highlights that the uncertainties on white dwarf parameters do not prevent white dwarfs from being utilized to study planetary composition. The abundances of oxygen and silicon for the three hydrogen-dominated white dwarfs in the sample with both optical and ultraviolet spectra differ by 0.62 dex depending on if they are derived from the optical or ultraviolet spectra. This optical/ultraviolet discrepancy may be related to differences in the atmospheric depth of line formation; further investigations into the white dwarf atmospheric modelling are needed to understand this discrepancy.

Funder

Royal Society

Science and Technology Facilities Council

National Science Foundation

W. M. Keck Foundation

Publisher

Oxford University Press (OUP)

Subject

Space and Planetary Science,Astronomy and Astrophysics

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