4.7 Article

The OmegaWhite Survey for short-period variable stars - IV. Discovery of the warm DQ white dwarf OWJ175358.85-310728.9

Journal

MONTHLY NOTICES OF THE ROYAL ASTRONOMICAL SOCIETY
Volume 470, Issue 1, Pages 732-741

Publisher

OXFORD UNIV PRESS
DOI: 10.1093/mnras/stx741

Keywords

stars: carbon; stars: evolution; stars: individual: OW J175358.85-310728.9; stars: magnetic field; stars: rotation; white dwarfs

Funding

  1. Erasmus Mundus Programme SAPIENT
  2. National Research Foundation of South Africa (NRF)
  3. Nederlandse Organisatie voor Wetenschappelijk Onderzoek (the Dutch Organisation for Science Research), Radboud University
  4. University of Cape Town
  5. NSERC (Canada)
  6. Northern Ireland Executive
  7. ESO Telescopes at the La Silla Paranal Observatory [093.D-0753(A), 177.D-3023]
  8. Southern African Large Telescope (SALT) [2016-1-SCI-015]
  9. NWO/NRF

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We present the discovery and follow-up observations of the second known variable warm DQ white dwarf OWJ175358.85-310728.9 (OWJ1753-3107). OWJ1753-3107 is the brightest of any of the currently known warm or hot DQ and was discovered in the Omega White Survey as exhibiting optical variations on a period of 35.5452 (2) min, with no evidence for other periods in its light curves. This period has remained constant over the last 2 yr and a single-period sinusoidal model provides a good fit for all follow-up light curves. The spectrum consists of a very blue continuum with strong absorption lines of neutral and ionized carbon, a broad He I lambda 4471 line and possibly weaker hydrogen lines. The CI lines are Zeeman split, and indicate the presence of a strong magnetic field. Using spectral Paschen-Back model descriptions, we determine that OWJ1753-3107 exhibits the following physical parameters: T-eff = 15 430 K, log (g) = 9.0, log (N(C)/N(He))=-1.2 and the mean magnetic field strength is B-z = 2.1 MG. This relatively low temperature and carbon abundance (compared to the expected properties of hot DQs) is similar to that seen in the other warm DQ SDSS J1036+6522. Although OW J1753-3107 appears to be a twin of SDSS J1036+ 6522, it exhibits a modulation on a period slightly longer than the dominant period in SDSS J1036+ 6522 and has a higher carbon abundance. The source of variations is uncertain, but they are believed to originate from the rotation of the magnetic white dwarf.

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