2018
DOI: 10.1093/mnras/sty1700
|View full text |Cite
|
Sign up to set email alerts
|

Polluted white dwarfs: constraints on the origin and geology of exoplanetary material

Abstract: White dwarfs that have accreted rocky planetary bodies provide unique insights regarding the bulk composition of exoplanetary material. The analysis presented here uses observed white dwarf atmospheric abundances to constrain both where in the planetary system the pollutant bodies originated, and the geological and collisional history of the pollutant bodies. At least one, but possibly up to nine, of the 17 systems analysed have accreted a body dominated by either core-like or mantle-like material. The approxi… Show more

Help me understand this report
View preprint versions

Search citation statements

Order By: Relevance

Paper Sections

Select...
2
1
1
1

Citation Types

5
144
0

Year Published

2020
2020
2025
2025

Publication Types

Select...
6
2

Relationship

2
6

Authors

Journals

citations
Cited by 124 publications
(149 citation statements)
references
References 83 publications
5
144
0
Order By: Relevance
“…We verify that neutral atomic Fe is the dominant Fe species using equilibrium chemistry calculations computed with the HSC Chemistry software (version 8) (e.g. Pasek et al 2005;Bond et al 2010;Elser et al 2012;Madhusudhan 2012;Moriarty et al 2014;Harrison et al 2018). These calculations assume solar elemental abundances (Asplund et al 2009) and include the same species as Harrison et al (2018) plus gaseous, solid, neutral and ionic molecules and atomic forms of Fe, Ti, V, Cr and Mg. Figure 4 shows the equilibrium abundances of several neutral gaseous Fe species between 1000-3000 K at a pressure of 1 mbar nominally corresponding to the optical photosphere.…”
Section: Model Spectramentioning
confidence: 99%
See 1 more Smart Citation
“…We verify that neutral atomic Fe is the dominant Fe species using equilibrium chemistry calculations computed with the HSC Chemistry software (version 8) (e.g. Pasek et al 2005;Bond et al 2010;Elser et al 2012;Madhusudhan 2012;Moriarty et al 2014;Harrison et al 2018). These calculations assume solar elemental abundances (Asplund et al 2009) and include the same species as Harrison et al (2018) plus gaseous, solid, neutral and ionic molecules and atomic forms of Fe, Ti, V, Cr and Mg. Figure 4 shows the equilibrium abundances of several neutral gaseous Fe species between 1000-3000 K at a pressure of 1 mbar nominally corresponding to the optical photosphere.…”
Section: Model Spectramentioning
confidence: 99%
“…Pasek et al 2005;Bond et al 2010;Elser et al 2012;Madhusudhan 2012;Moriarty et al 2014;Harrison et al 2018). These calculations assume solar elemental abundances (Asplund et al 2009) and include the same species as Harrison et al (2018) plus gaseous, solid, neutral and ionic molecules and atomic forms of Fe, Ti, V, Cr and Mg. Figure 4 shows the equilibrium abundances of several neutral gaseous Fe species between 1000-3000 K at a pressure of 1 mbar nominally corresponding to the optical photosphere. At the equilibrium temperature of WASP-121 b (∼2400 K), neutral atomic Fe is the dominant form of Fe and should therefore be the most easily detected (also see Kitzmann et al 2018;Lothringer et al 2018).…”
Section: Model Spectramentioning
confidence: 99%
“…Establishing a compositional link between crater ejecta and metals found in white dwarfs is another important extension of these results. If observational distinctions between detections of the bulk remains of an exo-asteroid versus the crustal material of an exo-planet can be enhanced (Harrison et al 2018;Hollands et al 2018;Bonsor et al 2020), then understanding the mass and dynamical pathways of impact ejecta would become more important. Tracing the chemistry and dynamics back to planetary system formation along the early main sequence phase (Harrison et al 2018;Bonsor et al 2020) has the potential to link planetary architecture with instabilities, bombardments and observed accretion rates.…”
Section: Discussionmentioning
confidence: 99%
“…Some white dwarfs contain at least ten different observable exoplanetary metals (e.g. Dufour et al 2012;Melis & Dufour 2017;Swan et al 2019;Xu et al 2019), and about two dozen white dwarfs currently host at least five metals (Harrison et al 2018;Hollands et al 2018). In each case, because of spectroscopic limitations, we obtain only a partial snapshot of the bulk chemical composition of progenitor exoplanetary material.…”
Section: Fates Of Planetary Systemsmentioning
confidence: 99%
“…Some bodies also show evidence for differentiation, posing questions about collisional processing (e.g. Hollands et al 2018;Harrison et al 2018).…”
Section: Introductionmentioning
confidence: 99%