New 26 P(p, γ) 27 S Thermonuclear Reaction Rate and Its Astrophysical Implications in the rp-process
Abstract Accurate nuclear reaction rates for 26 P( p , γ ) 27 S are pivotal for a comprehensive understanding of the rp -process nucleosynthesis path in the region of proton-rich sulfur and phosphorus isotopes. However, large uncertainties still exist in the current rate of 26 P( p , γ ) 27 S because of the lack of nuclear mass and energy level structure information for 27 S. We reevaluate this reaction rate using the experimentally constrained 27 S mass, together with the shell model predicted level structure. It is found that the 26 P( p , γ ) 27 S reaction rate is dominated by a direct capture reaction mechanism despite the presence of three resonances at E = 1.104, 1.597, and 1.777 MeV above the proton threshold in 27 S. 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 new 27 S mass. The influence of new rates of forward and reverse reaction in the abundances of isotopes produced in the rp -process is explored by postprocessing nucleosynthesis calculations. The final abundance ratio of 27 S/ 26 P obtained using the new rates is only 10% of that from the old rate. The abundance flow calculations show that the reaction path 26 P( p , γ ) 27 S( β + , ν ) 27 P is not as important as previously thought for producing 27 P. The adoption of the new reaction rates for 26 P( p , γ ) 27 S only reduces the final production of aluminum by 7.1% and has no discernible impact on the yield of other elements.
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