Helium-3 Enrichment in Gradual Solar Energetic Particle Events: Evidence for Jet-Supplied Seed Population
R. Bucik, S. T. Hart, M. A. Dayeh, M. I. Desai, G. M. Mason, M. E. Wiedenbeck
TL;DR
This study addresses why $^{3}$He is enriched in gradual solar energetic particle (GSEP) events by analyzing high-energy ($25$--$50$ MeV) protons observed by SOHO that coincide with $^{3}$He-rich periods from ACE. Using a timing-based refinement and EUV imaging of solar sources, it demonstrates that jet-like activity in active regions supplies a fresh $^{3}$He-rich seed population, which is then re-accelerated by CME-driven shocks, producing the observed enrichments in a cleaned sample of 15 events. The work finds a strong link between jet activity and extreme $^{3}$He/$^{4}$He values, and a positive correlation between $^{3}$He/$^{4}$He and Fe/O that is most pronounced for jet-associated events, supporting a jet-seed plus shock-reacceleration scenario. It also identifies that a substantial fraction (~40%) of apparent $^{3}$He enhancements arise from overlap with impulsive SEP activity, underscoring the mixture of seed sources and the importance of carefully separating ISEP and GSEP contributions for interpretation and modeling.
Abstract
Enhancements in 3He abundance, a characteristic feature of impulsive solar energetic particle (ISEP) events, are also frequently observed in gradual SEP (GSEP) events. Understanding the origin of this enrichment is crucial for identifying the mechanisms behind SEP generation. We investigate the origin of 3He enrichment in high-energy (25-50 MeV) solar proton events observed by SOHO, selecting events that coincide with <1 MeV/nucleon 3He-rich periods detected by ACE during 1997-2021. The identified 3He enhancements include cases where material from independent impulsive (3He-rich) SEP events is mixed with GSEP proton populations. Two high-energy proton events exhibit elemental composition and solar source characteristics consistent with ISEPs. Extreme-ultraviolet imaging from SDO and STEREO reveals narrow, jet-like eruptions in the parent active regions of about 60% of the remaining events. Notably, the highest 3He/4He ratios occur when coronal jets are present, consistent with fresh, jet-driven injection of suprathermal 3He that is subsequently re-accelerated during the event. Correspondingly, jet-associated events show fewer pre-event (residual) 3He counts, indicating that enrichment in these cases does not primarily come from remnant material. We find a positive correlation between 3He/4He and Fe/O, strongest in jet-associated events, consistent with a common jet-supplied seed population re-accelerated by the CME shock.
