Accurate nuclear reaction rates for26P(
- Award ID(s):
- 1927130
- PAR ID:
- 10543443
- Publisher / Repository:
- AAP
- Date Published:
- Journal Name:
- Astronomy & Astrophysics
- Volume:
- 677
- ISSN:
- 0004-6361
- Page Range / eLocation ID:
- A139
- Format(s):
- Medium: X
- Sponsoring Org:
- National Science Foundation
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New 26 P(p, γ) 27 S Thermonuclear Reaction Rate and Its Astrophysical Implications in the rp-process
Abstract p ,γ )27S are pivotal for a comprehensive understanding of therp -process nucleosynthesis path in the region of proton-rich sulfur and phosphorus isotopes. However, large uncertainties still exist in the current rate of26P(p ,γ )27S because of the lack of nuclear mass and energy level structure information for27S. We reevaluate this reaction rate using the experimentally constrained27S mass, together with the shell model predicted level structure. It is found that the26P(p ,γ )27S reaction rate is dominated by a direct capture reaction mechanism despite the presence of three resonances atE = 1.104, 1.597, and 1.777 MeV above the proton threshold in27S. The new rate is overall smaller than the other previous rates from the Hauser–Feshbach statistical model by at least 1 order of magnitude in the temperature range of X-ray burst interest. In addition, we consistently update the photodisintegration rate using the new27S mass. The influence of new rates of forward and reverse reaction in the abundances of isotopes produced in therp -process is explored by postprocessing nucleosynthesis calculations. The final abundance ratio of27S/26P obtained using the new rates is only 10% of that from the old rate. The abundance flow calculations show that the reaction path26P(p ,γ )27S(β +,ν )27P is not as important as previously thought for producing27P. The adoption of the new reaction rates for26P(p ,γ )27S only reduces the final production of aluminum by 7.1% and has no discernible impact on the yield of other elements. -
Context. An accurate28P(p ,γ )29S reaction rate is crucial to defining the nucleosynthesis products of explosive hydrogen burning in ONe novae. Using the recently released nuclear mass of29S, together with a shell model and a direct capture calculation, we reanalyzed the28P(p ,γ )29S thermonuclear reaction rate and its astrophysical implication.Aims. We focus on improving the astrophysical rate for28P(p ,γ )29S based on the newest nuclear mass data. Our goal is to explore the impact of the new rate and associated uncertainties on the nova nucleosynthesis.Methods. We evaluated this reaction rate via the sum of the isolated resonance contribution instead of the previously used Hauser-Feshbach statistical model. The corresponding rate uncertainty at different energies was derived using a Monte Carlo method. Nova nucleosynthesis is computed with the 1D hydrodynamic code SHIVA.Results. The contribution from the capture on the first excited state at 105.64 keV in28P is taken into account for the first time. We find that the capture rate on the first excited state in28P is up to more than 12 times larger than the ground-state capture rate in the temperature region of 2.5 × 107K to 4 × 108K, resulting in the total28P(p ,γ )29S reaction rate being enhanced by a factor of up to 1.4 at ~1 × 109K. In addition, the rate uncertainty has been quantified for the first time. It is found that the new rate is smaller than the previous statistical model rates, but it still agrees with them within uncertainties for nova temperatures. The statistical model appears to be roughly valid for the rate estimation of this reaction in the nova nucleosynthesis scenario. Using the 1D hydrodynamic code SHIVA, we performed the nucleosynthesis calculations in a nova explosion to investigate the impact of the new rates of28P(p ,γ )29S. Our calculations show that the nova abundance pattern is only marginally affected if we use our new rates with respect to the same simulations but statistical model rates. Finally, the isotopes whose abundance is most influenced by the present28P(p ,γ )29S uncertainty are28Si,33,34S,35,37Cl, and36Ar, with relative abundance changes at the level of only 3% to 4%. -
Abstract The observation of
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