Reevaluation of the $^{14}$O($\alpha$,p)$^{17}$F Resonant Reaction Rate
J.J. He, H.W. Wang, J. Hu, S.W. Xu

TL;DR
This paper reevaluates the $^{14}$O($$,p)$^{17}$F reaction rate, correcting previous state assignments, which significantly alters the reaction rate calculations and impacts astrophysical models.
Contribution
The study corrects the spin-parity assignment of key nuclear states, leading to revised reaction rates for astrophysical modeling.
Findings
The 6.286-MeV state is the dominant 1$^-$ resonance affecting reaction rates.
Revised reaction rates are about 1/6 of previous estimates at 0.4 GK.
Revised reaction rates are approximately 2.4 times larger than previous estimates at 2 GK.
Abstract
The reaction rates of the key stellar reaction of O(,p)F have been reevaluated. It is thought that the previous 1 assignment for the 6.15-MeV state is incorrect by a careful reanalysis of the previous experimental data [J. G\'{o}mez del Campo {\it et al.}, Phys. Rev. Lett. {\bf 86}, 43 (2001)]. Most probably, the 6.286-MeV state is the key 1 state and the 6.15-MeV state is a 2 one, and hence the resonance at =6.286 MeV (=1) actually dominates the reaction rates in the temperature region of astrophysical interests. The newly calculated reaction rates for the O(,p)F reaction are quite different from the previous ones, for instance, it's only about 1/6 of the previous value around 0.4 GK, while it's about 2.4 times larger than the previous value around 2 GK. The astrophysical implications have been briefly discussed…
Peer Reviews
No public reviews on file for this paper yet. If you reviewed it on a platform where reviews are public (OpenReview, ICLR, NeurIPS, ICML), you can paste yours below so the community can read it here.
Videos
No videos yet. Explain this paper in a talk, walkthrough, or lecture? Add one.
Taxonomy
TopicsAdvanced Data Storage Technologies · Atmospheric Ozone and Climate · Advanced Chemical Physics Studies
