The GAPS Programme with HARPS-N at TNG. X. Differential abundances in the XO-2 planet hosting binary

TL;DR

This study performs a high-precision differential abundance analysis of the XO-2 binary stars, revealing subtle chemical differences possibly linked to planetary formation and evolution, with implications for understanding planet-star chemical interactions.

Contribution

It provides the first detailed differential abundance comparison of the XO-2 binary, highlighting chemical signatures associated with planetary presence and potential material accretion.

Findings

XO-2N shows higher elemental abundances than XO-2S by about 0.07 dex.

Abundance differences correlate with condensation temperature, suggesting planet-related chemical processes.

The results imply possible ingestion or depletion of heavy elements related to planetary formation.

Abstract

Binary stars hosting exoplanets are a unique laboratory where chemical tagging can be performed to measure with high accuracy the elemental abundances of both stellar components, with the aim to investigate the formation of planets and their subsequent evolution. Here, we present a high-precision differential abundance analysis of the XO-2 wide stellar binary based on high resolution HARPS-N@TNG spectra. Both components are very similar K-dwarfs and host planets. Since they formed presumably within the same molecular cloud, we expect they should possess the same initial elemental abundances. We investigate if the presence of planets can cause some chemical imprints in the stellar atmospheric abundances. We measure abundances of 25 elements for both stars with a range of condensation temperature $T_{\rm C}=40-1741$ K, achieving typical precisions of $\sim 0.07$ dex. The North component shows abundances in all elements higher by $+0.067 \pm 0.032$ dex on average, with a mean difference of +0.078 dex for elements with $T_{\rm C} > 800$ K. The significance of the XO-2N abundance difference relative to XO-2S is at the $2\sigma$ level for almost all elements. We discuss the possibility that this result could be interpreted as the signature of the ingestion of material by XO-2N or depletion in XO-2S due to locking of heavy elements by the planetary companions. We estimate a mass of several tens of $M_{\oplus}$ in heavy elements. The difference in abundances between XO-2N and XO-2S shows a positive correlation with the condensation temperatures of the elements, with a slope of $(4.7 \pm 0.9) \times 10^{-5}$ dex K$^{-1}$, which could mean that both components have not formed terrestrial planets, but that first experienced the accretion of rocky core interior to the subsequent giant planets.