Long-Term Lithium Abundance Signatures following Planetary Engulfment
Jason Sevilla, Aida Behmard, Jim Fuller

TL;DR
This study models how planetary engulfment affects stellar lithium levels over time, revealing signatures that depend on star mass and can last from hundreds of millions to billions of years.
Contribution
It provides detailed predictions of lithium abundance signatures post-engulfment using stellar evolution models across various star masses.
Findings
Lithium is rapidly depleted in low-mass stars within hundreds of Myrs.
Significant lithium enrichment can persist for Gyrs in G-type stars.
Engulfment signatures are consistent with observed lithium-rich stars.
Abstract
Planetary engulfment events can occur while host stars are on the main sequence. The addition of rocky planetary material during engulfment will lead to refractory abundance enhancements in the host star photosphere, but the level of enrichment and its duration will depend on mixing processes that occur within the stellar interior, such as convection, diffusion, and thermohaline mixing. We examine engulfment signatures by modeling the evolution of photospheric lithium abundances. Because lithium can be burned before or after the engulfment event, it produces unique signatures that vary with time and host star type. Using MESA stellar models, we quantify the strength and duration of these signatures following the engulfment of a 1, 10, or 100 planetary companion with bulk Earth composition, for solar-metallicity host stars with masses ranging from 0.51.4 . We…
Peer Reviews
No public reviews on file for this paper yet. If you reviewed it on a platform where reviews are public (OpenReview, ICLR, NeurIPS, ICML), you can paste yours below so the community can read it here.
Videos
No videos yet. Explain this paper in a talk, walkthrough, or lecture? Add one.
Taxonomy
TopicsStellar, planetary, and galactic studies · Astro and Planetary Science · Astronomy and Astrophysical Research
