2020/03/31 by Tobias Fischer, Meng-Ru Wu, Benjamin Wehmeyer +5
Physics and Astronomy · #Astronomy #Astrophysics #Condensed matter physics #Core (optical fiber) #Gamma-ray bursts and supernovae #Hadron #Neutrino Physics Research #Nuclear physics #Particle physics #Phase transition #Physics #Pulsars and Gravitational Waves Research #Supernova #astro-ph.HE
paper · pdf · doi:10.3847/1538-4357/ab86b0
published as Astrophys. J. 894 (2020) 9 · 17 pages, 7 figures, The Astrophysical Journal, Volume 894, Issue 1, id.9
openalex publication_date 2020/04/30 · arxiv created 2020/05/07 · arxiv updated 2020/06/04 · openalex created_date 2025/10/10 · openalex updated_date 2026/08/06
Abstract Supernova explosions of massive stars are one of the primary sites for the production of the elements in the universe. Up to now, stars with zero-age main-sequence masses in the range of 35–50 M ⊙ had mostly represented the failed supernova explosion branch. In contrast, it has been demonstrated recently that the appearance of exotic phases of hot and dense matter, associated with a sufficiently strong phase transition from nuclear matter to the quark-gluon plasma at high baryon density, can trigger supernova explosions of such massive supergiant stars. Here, we present the first results obtained from an extensive nucleosynthesis analysis for material being ejected from the surface of the newly born proto-neutron stars of such supernova explosions. These ejecta contain an early neutron-rich component and a late-time high-entropy neutrino-driven wind. The nucleosynthesis robustly overcomes the production of nuclei associated with the second r -process peak, at nuclear mass number A ≃ 130, and proceeds beyond the formation of the third peak ( A ≃ 195) to the actinides. These yields may account for metal-poor star observations concerning r -process elements such as strontium and europium in the Galaxy at low metallicity, while the actinide yields suggests that this source may be a candidate contributing to the abundances of radioactive 244 Pu measured in deep-sea sediments on Earth.