Prevalence of short-lived radioactive isotopes across exoplanetary systems inferred from polluted white dwarfs
Alfred Curry, Amy Bonsor, Tim Lichtenberg, Oliver Shorttle

TL;DR
This study uses white dwarf pollution data to estimate how common short-lived radioactive isotopes like 26Al are in exoplanetary systems, suggesting such enrichment is widespread and not due to rare events.
Contribution
It introduces a quantitative method to infer the prevalence of short-lived radionuclide enrichment in exoplanetary systems from white dwarf observations, indicating widespread enrichment.
Findings
A significant fraction of exo-planetesimals formed iron cores.
Most exoplanetary systems likely have high short-lived radioisotope abundances.
Enrichment is probably common, not due to rare stellar events.
Abstract
In the Solar System short-lived radioisotopes, such as 26Al, played a crucial role during the formation planetary bodies by providing a significant additional source of heat. Notably, this led to early and large-scale melting and iron core formation in planetesimals and their loss of volatile elements, such as hydrogen and carbon. In the context exoplanetary systems, therefore, the prevalence of short-lived radioisotopes is key to interpreting the observed bulk volatile budget and atmospheric diversity among low-mass exoplanets. White dwarfs that have accreted planetary material provide a unique means to infer the frequency of iron core formation in extrasolar planetesimals, and hence the ubiquity of planetary systems forming with high short-lived radioisotope abundances. Here, we devise a quantitative method to infer the fraction of planetary systems enriched with shortlived…
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