A rotating white dwarf shows different compositions on its opposite faces
Ilaria Caiazzo, Kevin B. Burdge, Pier-Emmanuel Tremblay, James Fuller,, Lilia Ferrario, Boris T. Gaensicke, J. J. Hermes, Jeremy Heyl, Adela Kawka,, S. R. Kulkarni, Thomas R. Marsh, Przemek Mroz, Thomas A. Prince, Harvey B., Richer, Antonio C. Rodriguez, Jan van Roestel

TL;DR
This paper reports the discovery of a unique white dwarf with opposite faces showing different atmospheric compositions, likely caused by magnetic effects, providing insights into white dwarf spectral evolution.
Contribution
It introduces a new class of magnetic, transitioning white dwarfs with opposite surface compositions, advancing understanding of their spectral evolution mechanisms.
Findings
Discovered a white dwarf with hydrogen on one face and helium on the opposite.
Magnetic fields likely cause surface inhomogeneity in composition.
Suggests a new class of magnetic, transitioning white dwarfs.
Abstract
White dwarfs, the extremely dense remnants left behind by most stars after their death, are characterised by a mass comparable to that of the Sun compressed into the size of an Earth-like planet. In the resulting strong gravity, heavy elements sink toward the centre and the upper layer of the atmosphere contains only the lightest element present, usually hydrogen or helium. Several mechanisms compete with gravitational settling to change a white dwarf's surface composition as it cools, and the fraction of white dwarfs with helium atmospheres is known to increase by a factor ~2.5 below a temperature of about 30,000 K; therefore, some white dwarfs that appear to have hydrogen-dominated atmospheres above 30,000 K are bound to transition to be helium-dominated as they cool below it. Here we report observations of ZTF J203349.8+322901.1, a transitioning white dwarf with two faces: one side…
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