Production of radioactive $^{22}$Na in core-collapse supernovae: the Ne-E(L) component in presolar grains and its possible consequences on supernova observations
M. Pignatari, S. Amari, P. Hoppe, C. Fryer, S. Jones, A. Psaltis, A. M. Laird, F. Herwig, L. Roberti, T. Siegert, M. Lugaro
TL;DR
The study addresses the Ne-E(L) signature observed in presolar graphites by exploring late H-ingestion in the He shell of core-collapse supernovae as a mechanism to synthesize $^{22}$Na. Through twelve 1D CCSN models, it shows that $^{22}$Na production in the He shell can reach yields up to $3\times10^{-3}\,M_\odot$, with a minimum grain-relevant abundance around $10^{-4}$ in a C-rich mixture, making it plausible to explain Ne-E(L). The work further demonstrates that such $^{22}$Na enhancements can power CCSN light curves at 500–1500 days and produce a detectable $^{22}$Na gamma-ray line at $1274.53$ keV with current or future observatories, while also assessing potential contributions to Galactic positrons. The results connect presolar grain isotopic signatures with observable late-time CCSN phenomena and highlight significant modeling and nuclear-rate uncertainties that require 3D hydrodynamics and further experiments to refine the scenario.
Abstract
Presolar graphite grains carry the isotopic signatures of their parent stars. A significant fraction of presolar graphites shows isotopic abundance anomalies relative to solar for elements such as O, Si, Mg and Ca, which are compatible with nucleosynthesis in core-collapse supernovae (CCSNe). Therefore, they must have condensed from CCSN ejecta before the formation of the Sun. Their most puzzling abundance signature is the $^{22}$Ne-enriched component Ne-E(L), interpreted as the effect of the radioactive decay of $^{22}$Na ($T_{1/2}$ = 2.6 years). Previous works have shown that if H is ingested into the He shell and not fully destroyed before the explosion, the CCSN shock in the He shell material produces large $^{22}$Na amounts. Here we focus on such CCSN models, showing a radioactive $^{26}$Al production compatible with grains measurements, and analyze the conditions of $^{22}$Na nucleosynthesis. In these models, $^{22}$Na is mostly made in the He shell, with a total ejected mass varying between 2.6$\times$10$^{-3}$ M$_{\odot}$ and 1.9$\times$10$^{-6}$ M$_{\odot}$. We show that such $^{22}$Na may already impact the CCSN light curve 500 days after the explosion, and at later stages it can be the main source powering the CCSN light curve for up to a few years before the $^{44}$Ti decay becomes dominant. Based on the CCSN yields above, the 1274.53 keV $γ$-ray flux due to $^{22}$Na decay could be observable for years after the first CCSN light is detected, depending on the distance. This makes CCSNe possible sites to detect a $^{22}$Na $γ$-ray signature consistently with the Ne-E(L) component found in presolar graphites. Finally, we discuss the potential contribution from the $^{22}$Na decay to the galactic positron annihilation rate.
