Abstract
The S()Cl reaction is important for constraining predictions of certain isotopic abundances in oxygen-neon novae. Models currently predict as much as 150 times the solar abundance of S in oxygen-neon nova ejecta. This overproduction factor may vary by orders of magnitude due to uncertainties in the S()Cl reaction rate at nova peak temperatures. Depending on this rate, S could potentially be used as a diagnostic tool for classifying certain types of presolar grains. Better knowledge of the S()Cl rate would also aid in interpreting nova observations over the S-Ca mass region and contribute to the firm establishment of the maximum endpoint of nova nucleosynthesis. Additionally, the total S elemental abundance which is affected by this reaction has been proposed as a thermometer to study the peak temperatures of novae. Previously, the S()Cl reaction rate had only been studied directly down to resonance energies of 432 keV. However, for nova peak temperatures of GK there are seven known states in Cl both below the 432-keV resonance and within the Gamow window that could play a dominant role. Direct measurements of the resonance strengths of these states were performed using the DRAGON (Detector of Recoils And Gammas of Nuclear reactions) recoil separator at TRIUMF. Additionally two new states within this energy region are reported. Several hydrodynamic simulations have been performed, using all available experimental information for the S()Cl rate, to explore the impact of the remaining uncertainty in this rate on nucleosynthesis in nova explosions. These calculations give a range of 20–150 for the expected S overproduction factor, and a range of 100–450 for the S/S ratio expected in ONe novae.
1 More- Received 6 June 2013
DOI:https://doi.org/10.1103/PhysRevC.88.045801
©2013 American Physical Society