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Underground study of the O17(p,γ)F18 reaction relevant for explosive hydrogen burning

A. Di Leva1,2,*, D. A. Scott3, A. Caciolli4,5, A. Formicola6,†, F. Strieder7, M. Aliotta3, M. Anders8, D. Bemmerer8, C. Broggini4 et al. (LUNA Collaboration)

C. Broggini4, P. Corvisiero9,10, Z. Elekes8, Zs. Fülöp11, G. Gervino12, A. Guglielmetti13,14, C. Gustavino15, Gy. Gyürky11, G. Imbriani1,2, J. José16, M. Junker6, M. Laubenstein6, R. Menegazzo4, E. Napolitani17, P. Prati9,10, V. Rigato5, V. Roca1,2, E. Somorjai11, C. Salvo6,10, O. Straniero2,18, T. Szücs11, F. Terrasi2,19, and D. Trezzi13,14 (LUNA Collaboration)

  • 1Dipartimento di Fisica, Università di Napoli “Federico II,” Napoli, Italy
  • 2INFN, Sezione di Napoli, Napoli, Italy
  • 3SUPA, School of Physics and Astronomy, University of Edinburgh, Edinburgh EH9 3JZ, UK
  • 4INFN, Sezione di Padova, 35131 Padova, Italy
  • 5INFN, Laboratori Nazionali di Legnaro, Padova, Italy
  • 6INFN, Laboratori Nazionali del Gran Sasso, Assergi, Italy
  • 7Institut für Experimentalphysik, Ruhr-Universität Bochum, Bochum, Germany
  • 8Helmholtz-Zentrum Dresden-Rossendorf, Dresden, Germany
  • 9Dipartimento di Fisica, Università di Genova, Genova, Italy
  • 10INFN Sezione di Genova, Genova, Italy
  • 11MTA Atomki, Debrecen, Hungary
  • 12Dipartimento di Fisica Sperimentale, Università degli Studi di Torino, and INFN, Sezione di Torino, Torino, Italy
  • 13Università degli Studi di Milano, Milano, Italy
  • 14INFN, Sezione di Milano, Milano, Italy
  • 15INFN, Roma La Sapienza, Italy
  • 16Departament de Física i Enginyeria Nuclear, EUETIB, Universitat Politécnica de Catalunya, and Institut d'Estudis Espacials de Catalunya, Barcelona, Spain
  • 17CNR-IMM MATIS at Dipartimento di Fisica e Astronomia, Università di Padova, Padova, Italy
  • 18Osservatorio Astronomico di Collurania, Teramo, Italy
  • 19Seconda Università di Napoli, Caserta, Italy

  • *Corresponding author: antonino.dileva@unina.it
  • Corresponding author: alba.formicola@lngs.infn.it

Phys. Rev. C 89, 015803 – Published 21 January, 2014Erratum Phys. Rev. C 90, 019902 (2014)

DOI: https://doi.org/10.1103/PhysRevC.89.015803

Abstract

Background: The O17(p,γ)F18 reaction affects the production of key isotopes (e.g., F18 and O18) in the explosive hydrogen burning that powers classical novae. Under these explosive conditions, the reaction rate is dominated by contributions from a narrow resonance at Ec.m.=183keV and by the combined contributions of direct capture and low-energy tails of broad resonances. At present, the astrophysical reaction rate is not well constrained because of the lack of data in the energy region appropriate to classical novae.

Purpose: This study aims at the measurement of the O17(p,γ)F18 reaction cross section in order to determine its reaction rate in the temperature region appropriate to explosive hydrogen burning in novae.

Method: The O17(p,γ)F18 reaction cross section was measured using both the prompt detection of the emitted γ rays and an activation technique. Measurements were carried out at the Laboratory for Underground Nuclear Astrophysics (Gran Sasso, Italy) where the strongly reduced cosmic-ray-induced background allows for improved sensitivity compared to previous studies.

Results: The O17(p,γ)F18 reaction cross section was measured in the range Ec.m.=160 to 370keV. The strength of the Ec.m.=183keV resonance, ωγ=1.67±0.12μeV, was determined with unprecedented precision. The total S factor was obtained through a combined fit of prompt γ-ray and activation results. An overall global fit including other existing data sets was also carried out and a recommended astrophysical reaction rate is presented.

Conclusions: The reaction rate uncertainty attained in this work is now below the required precision for nova models. We verified, following a full set of hydrodynamic nova models, that the abundances of oxygen and fluorine isotopes obtained with the present reaction rate are determined with 10% precision and put firmer constraints on observational signatures of novae events.

Erratum

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