# A New Generation of Cool White Dwarf Atmosphere Models. III. WD   J2356$-$209: Accretion of a Planetesimal with an Unusual Composition

**Authors:** S. Blouin, P. Dufour, N.F. Allard, S. Salim, R.M. Rich, L.V.E., Koopmans

arXiv: 1902.03219 · 2019-03-06

## TL;DR

This study uses advanced atmosphere models to analyze the peculiar white dwarf WD J2356$-$209, revealing an unprecedented sodium-to-calcium ratio and insights into the composition of the accreted planetesimal, which is unlike typical chondritic material.

## Contribution

The paper introduces improved high-density atmosphere models to accurately analyze the spectrum of WD J2356$-$209, revealing its unique chemical composition and accretion history.

## Key findings

- Highest Na/Ca ratio ever observed in a white dwarf
- Accreted planetesimal likely had a mass of at least 10^21 g
- Planetesimal composition incompatible with chondrites

## Abstract

WD J2356$-$209 is a cool metal-polluted white dwarf whose visible spectrum is dominated by a strong and broad sodium feature. Although discovered nearly two decades ago, no detailed and realistic analysis of this star had yet been realized. In the absence of atmosphere models taking into account the nonideal high-density effects arising at the photosphere of WD J2356$-$209, the origin of its unique spectrum had remained nebulous. We use the cool white dwarf atmosphere code presented in the first paper of this series to finally reveal the secrets of this peculiar object and details about the planetesimal that polluted its atmosphere. Thanks to the improved input physics of our models, we find a solution that is in excellent agreement with the photometric observations and the visible spectrum. Our solution reveals that the photosphere of WD J2356$-$209 has a number density ratio of $\log\,{\rm Na/Ca}= 1.0 \pm 0.2$, which is the highest ever found in a white dwarf. Since we do not know how long ago the accretion episode stopped (if it has), we cannot precisely determine the composition nor the mass of the accreted planetesimal. Nevertheless, all scenarios considered indicate that its composition is incompatible with that of chondrite-like material and that its mass was at least $10^{21}\,{\rm g}$.

## Full text

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## Figures

8 figures with captions in the complete paper: https://tomesphere.com/paper/1902.03219/full.md

## References

84 references — full list in the complete paper: https://tomesphere.com/paper/1902.03219/full.md

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Source: https://tomesphere.com/paper/1902.03219