Modelling the distributions of white dwarf atmospheric pollution: a low Mg abundance for accreted planetesimals?
Samuel G. D. Turner, Mark C. Wyatt

TL;DR
This study models the pollution of white dwarf atmospheres by accreted planetesimals, revealing a significant Mg depletion in the material, and challenges the single-body assumption in pollution analysis.
Contribution
It introduces a stochastic model for planetesimal accretion, showing the need for Mg depletion to fit observed data and predicting variability timescales in atmospheric pollution.
Findings
Single-body assumption invalid in >20% of cases
Good fit with core, mantle, crust fractions from logit-normal distributions
Mg depletion factor of 4 needed, possibly due to stellar heating effects
Abstract
The accretion of planetesimals onto white dwarf atmospheres allows determination of the composition of this polluting material. This composition is usually inferred from observed pollution levels by assuming it originated from a single body. This paper instead uses a stochastic model wherein polluting planetesimals are chosen randomly from a mass distribution, finding that the single body assumption is invalid in >20% of cases. Planetesimal compositions are modelled assuming parent bodies that differentiated into core, mantle and crust components. Atmospheric levels of Ca, Mg and Fe in the model are compared to a sample of 230 DZ white dwarfs for which such pollution is measured. A good fit is obtained when each planetesimal has its core, mantle and crust fractions chosen independently from logit-normal distributions which lead to average mass fractions of ,…
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