Icy Exomoons Evidenced by Spallogenic Nuclides in Polluted White Dwarfs
Alexandra E. Doyle, Steven J. Desch, Edward D. Young

TL;DR
This paper provides evidence that excess beryllium in polluted white dwarfs results from accreted icy exomoons formed in giant planet rings, highlighting a new method to detect such moons through spallogenic nuclide analysis.
Contribution
It introduces a novel explanation for Be excess in white dwarfs as originating from icy exomoons formed via energetic proton irradiation in planetary rings.
Findings
Excess Be in white dwarf GALEX J2339-0424 is due to spallation in icy exomoons.
Proton irradiation in planetary rings can produce high Be/O ratios in accreted material.
Predicted excesses in Li and B could also indicate icy exomoons.
Abstract
We present evidence that excesses in Be in polluted white dwarfs (WDs) are the result of accretion of icy exomoons that formed in the radiation belts of giant exoplanets. Here we use excess Be in the white dwarf GALEX J2339-0424 as an example. We constrain the parent body abundances of rock-forming elements in GALEX J2339-0424 and show that the overabundance of beryllium in this WD cannot be accounted for by differences in diffusive fluxes through the WD outer envelope nor by chemical fractionations during typical rock-forming processes. We argue instead that the Be was produced by energetic proton irradiation of ice mixed with rock. We demonstrate that the MeV proton fluence required to form the high Be/O ratio in the accreted parent body is consistent with irradiation of ice in the rings of a giant planet within its radiation belt, followed by accretion of the ices to form a moon that…
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Taxonomy
TopicsStellar, planetary, and galactic studies · Astro and Planetary Science · Astrophysics and Star Formation Studies
