Predictions from $s$-process AGB models of the isotopic variations of zirconium and neodymium for comparison to bulk meteorites
Maria Lugaro, Giulia C. Cinquegrana, Balázs Szányi, James M. Ball, Borbála Cseh, Mattias Ek, Amanda I. Karakas, Maria Schönbächler, John C. Lattanzio
TL;DR
This study tests whether s-process isotopic variations observed in bulk meteorites, notably the larger Zr than Nd anomalies, can be reproduced by AGB star models of metallicity higher than solar. Using 68 Monash-based post-processing AGB models with varied convective overshoot and $^{13}$C-pocket sizes, the authors translate surface abundances into diluted $\varepsilon$ values for $^{96}$Zr/$^{90}$Zr and $^{148}$Nd/$^{144}$Nd, and compare their ratio $\varepsilon^{96}$Zr/$\varepsilon^{148}$Nd to meteoritic data. They find that the observed Zr–Nd contrast is best matched by super-solar metallicity AGB stars with strong third-dredge-up overshoot and/or small $M_{\rm mixed}$, suggesting that the presolar material contributing to the Solar System came from an old, high-metallicity stellar population. This work supports a scenario where bulk meteoritic s-process signatures originate from specific AGB progenitors rather than requiring multiple dust carriers, with implications for Galactic chemical evolution and the early Solar System’s stellar environment. Future work will refine neutron-source rates and cross sections, extend the analysis to other isotopes and meteorite components, and probe the impact of varying metallicities and stellar masses on broader s-process signatures.
Abstract
Bulk meteoritic data show isotopic variability of $slow$-neutron-capture ($s$-process) origin in a several elements heavier than Fe. One peculiar feature is that the lighter $s$-process elements (e.g., Zr and Mo) present larger anomalies than the heavier $s$-process elements (e.g., Nd and W). To address this observation, we compared Zr and Nd data to model predictions of the s-process abundances at the surface of low-mass asymptotic giant branch (AGB) stars of initial metallicity from solar to twice solar. We found that the relative magnitude of the isotopic variability between these two elements can be matched by models of AGB stars of super-solar metallicity. The match is favoured by stronger convective overshoot, leading to a deeper dredge-up of the H-rich envelope into the He-rich region, and/or a smaller (~ half than standard) mass of the region rich in the $^{13}$C nuclei that produce free neutrons via the $^{13}$C($α$,n)$^{16}$O reaction. We conclude that nucleosynthesis in AGB stars can match the difference in the magnitude of the bulk meteoritic variations in Zr and Nd, provided that super-solar metallicity stars are the original site of these signatures. The AGB stars that produced such variations could have belonged to the current population of old, super-solar metallicity stars seen in the galactic solar neighbourhood.
