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r-Process Radioisotopes from Near-Earth Supernovae and Kilonovae
The astrophysical sites where r -process elements are synthesized remain mysterious: it is clear that neutron star mergers (kilonovae (KNe)) contribute, and some classes of core-collapse supernovae (SNe) are also possible sources of at least the lighter r -process species. The discovery of 60 Fe on...
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Published in: | The Astrophysical journal 2021-12, Vol.923 (2), p.219 |
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Main Authors: | , , , , , , , , |
Format: | Article |
Language: | English |
Subjects: | |
Citations: | Items that this one cites Items that cite this one |
Online Access: | Get full text |
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Summary: | The astrophysical sites where
r
-process elements are synthesized remain mysterious: it is clear that neutron star mergers (kilonovae (KNe)) contribute, and some classes of core-collapse supernovae (SNe) are also possible sources of at least the lighter
r
-process species. The discovery of
60
Fe on the Earth and Moon implies that one or more astrophysical explosions have occurred near the Earth within the last few million years, probably SNe. Intriguingly,
244
Pu has now been detected, mostly overlapping with
60
Fe pulses. However, the
244
Pu flux may extend to before 12 Myr ago, pointing to a different origin. Motivated by these observations and difficulties for
r
-process nucleosynthesis in SN models, we propose that ejecta from a KN enriched the giant molecular cloud that gave rise to the Local Bubble, where the Sun resides. Accelerator mass spectrometry (AMS) measurements of
244
Pu and searches for other live isotopes could probe the origins of the
r
-process and the history of the solar neighborhood, including triggers for mass extinctions, e.g., that at the end of the Devonian epoch, motivating the calculations of the abundances of live
r
-process radioisotopes produced in SNe and KNe that we present here. Given the presence of
244
Pu, other
r
-process species such as
93
Zr,
107
Pd,
129
I,
135
Cs,
182
Hf,
236
U,
237
Np, and
247
Cm should be present. Their abundances and well-resolved time histories could distinguish between the SN and KN scenarios, and we discuss prospects for their detection in deep-ocean deposits and the lunar regolith. We show that AMS
129
I measurements in Fe–Mn crusts already constrain a possible nearby KN scenario. |
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ISSN: | 0004-637X 1538-4357 |
DOI: | 10.3847/1538-4357/ac2d90 |