Abstract
Planetary material accreted by white dwarfs provides critical insights regarding the composition of planetary material . The analysis of polluted white dwarfs suggests that rocky planetary material similar in composition to bulk Earth is common, and that differentiation and collisions play a key role in planetary systems. Infrared observations track the accretion of dusty planetary material in disks that share many similarities with Saturn’s rings, as well as proto-planetary disks. Planetary material arrives close to the star, scattered inwards from an outer planetary systems that has survived the star’s evolution. White dwarf planetary systems provide key observational constraints that enable us to study the evolution of planetary systems under extreme conditions.
Notes
- 1.
Out of all the dusty white dwarfs, eight of them display double peaked emission lines from a circumstellar gas disk . Some of the gas lines also change on yearly timescale (e.g. Gänsicke et al. 2006). However, the detailed discussion about these systems is beyond the scope of this review.
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We thank Bruce Gary and Saul Rappaport for updating Fig. 8.7 for this chapter.
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Bonsor, A., Xu, S. (2017). White Dwarf Planetary Systems: Insights Regarding the Fate of Planetary Systems. In: Pessah, M., Gressel, O. (eds) Formation, Evolution, and Dynamics of Young Solar Systems. Astrophysics and Space Science Library, vol 445. Springer, Cham. https://doi.org/10.1007/978-3-319-60609-5_8
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