The spectral evolution of white dwarfs: where do we stand?
Antoine B\'edard

TL;DR
This review summarizes current observational and theoretical understanding of white dwarf spectral evolution, highlighting complex atmospheric composition changes and the mechanisms driving these variations over their cooling history.
Contribution
It provides a comprehensive synthesis of recent observational data and models of element transport, clarifying the processes behind spectral evolution in white dwarfs.
Findings
White dwarf atmospheres show complex composition changes over cooling.
Models of element transport partially explain observed spectral variations.
Open questions remain about the mechanisms driving spectral evolution.
Abstract
White dwarfs are the dense, burnt-out remnants of the vast majority of stars, condemned to cool over billions of years as they steadily radiate away their residual thermal energy. To first order, their atmosphere is expected to be made purely of hydrogen due to the efficient gravitational settling of heavier elements. However, observations reveal a much more complex situation, as the surface of a white dwarf (1) can be dominated by helium rather than hydrogen, (2) can be polluted by trace chemical species, and (3) can undergo significant composition changes with time. This indicates that various mechanisms of element transport effectively compete against gravitational settling in the stellar envelope. This phenomenon is known as the spectral evolution of white dwarfs and has important implications for Galactic, stellar, and planetary astrophysics. This invited review provides a…
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