Study of the N14(p, γ)O15 Reaction

Albert E. Evans, Bernard Brown, and Jerry B. Marion
Phys. Rev. 149, 863 – Published 23 September 1966
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Abstract

The reaction N14(p, γ)O15 has been studied using an anticoincidence-shielded scintillation spectrometer. Excitation functions were measured for proton energies of 0.85-1.96 MeV. Resonances were found at bombarding energies of 1.061±0.002, 1.55, 1.739±0.002, and 1800±0.004 MeV, corresponding to the well-known excited states of O15 at 8.283±0.003, 8.75, 8.915±0.003, and 8.972±0.005 MeV. Gamma-ray spectra show that the 8.28-MeV level decays to the ground state (54%), the 5.24-MeV level (43%), and the 6.18-MeV level (2%). In addition, coincidence spectra revealed a 1% branch through the 6.86-MeV level, which level decays to the 5.24-MeV level. No evidence was found for decay of the 8.28-MeV level to a previously reported level at 7.17 MeV. The 8.75-MeV level decays 23 by way of the 5.19-MeV level and 13 by way of the 6.18-MeV level. The 8.915-MeV level decays to the ground state (21%), the 5.19-MeV level (23%), the 6.18-MeV level (30%), and the 6.86-MeV level (26%). The 8.97-MeV level decays 93% to the ground state and 6% to the 5.19-MeV state. Based upon measured transition strengths and the angular distribution of the ground-state gamma rays, the spin of the 8.915-MeV level is established as 32; the 8.972-MeV level is 32 or ½ and the 6.86-MeV level has a spin of either 52 or 32. Off-resonance spectra for Ep near 1.2 MeV indicate direct capture into the 6.79-MeV level, the ground state, and also the 7.55-MeV level. The excitation function of radiation to ground from the bound states of O15 indicate that the broad level of O15 at 9.53 MeV decays almost entirely directly to the ground state or to the ground state and to unbound levels.

  • Received 19 April 1966

DOI:https://doi.org/10.1103/PhysRev.149.863

©1966 American Physical Society

Authors & Affiliations

Albert E. Evans and Bernard Brown

  • U. S. Naval Ordnance Laboratory, Silver Spring, Maryland

Jerry B. Marion*

  • University of Maryland, College Park, Maryland

  • *Research supported in part by the U. S. Atomic Energy Commission.

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Issue

Vol. 149, Iss. 3 — September 1966

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