DI019-0001
Accounting for Short-Lived Radionuclides in the Early Solar System in the Context of a Triggered Star Formation Origin of the Solar System

Monday, 14 December 2020
Poster
Vikram Dwarkadas, University of Chicago, Department of Astronomy and Astrophysics, Chicago, IL, United States, Shamaul Dilmohamed, University of Chicago, Astronomy and Astrophysics, Chicago, IL, United States, Nicolas Dauphas, University of Chicago, Department of the Geophysical Sciences, Chicago, IL, United States and Bradley Meyer, Clemson University, Physics and Astronomy, Clemson, SC, United States
Abstract:
The early Solar System (ESS) was characterized by a value of 26Al that exceeded the Galactic average, while 60Fe in the ESS was about an order of magnitude less than the Galactic value. These results dispute the existence of a supernova near the solar system at the time of formation. An alternative source of 26Al is Wolf-Rayet (W-R) stars. Aluminium-26 is produced in massive stars in the main-sequence phase, and released in the wind in the later W-R phase. No 60Fe is ejected in the wind. Dwarkadas et al. (2017, ApJ, 851, 147) showed that a single W-R star above about 50 solar mass could be sufficient to provide the measured amount of 26Al in the ESS. W-R stars have strong winds that sweep up the surrounding medium to form low density wind bubbles bordered by a dense shell. The 26Al is carried out by dust grains in the wind from the star to the dense shell, where it is released. The solar system is subsequently formed by triggered star formation in the dense shell, due to the combined actions of the wind, shock fronts and the ionization front due to ionizing photons from the hot star. Besides 26Al and 60Fe, many other short-lived radionuclides (SLRs) were present in the ESS, including 10Be, 36Cl, 41Ca, 53Mn, 107Pd, 129I, and 182Hf. Herein we investigate whether this triggered star formation model can account for the abundance of these other SLRs. These SLRs could (1) be produced in the star, carried out in the wind (via dust grains) and injected into the dense shell, (2) be already prevalent in the swept-up dense shell which was formed by sweeping up of the surrounding medium by the supersonic winds, or (3) be due to irradiation, from the supernova following the collapse of the W-R star (if a SN explosion occurs), from the early Sun, or via cosmic-rays. We explore the abundance of each SLR, and show that it can be accounted for using one of the 3 modes described above. 41Ca and 107Pd, being refractory elements, would be transported via dust grains, similar to 26Al in our model. Others would either be already present in the dense shell or can be formed via irradiation. We use abundance information from stellar evolution models calculated by various groups that are available in the literature. We also include abundances obtained using our own models of rotating and non-rotating massive stars, calculated with the publicly available MESA code.