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Reaction-Mechanism Study in the 1f2p Shell of (O16, C12) Four-Nucleon-Transfer Reaction

P. Bonche and B. Giraud

A. Cunsolo*, M. -C. Lemaire, M. C. Mermaz, and J. -L. Québert

  • Service de Physique Théorique, Centre d'Etudes Nucléaires de Saclay, France

  • Service de Physique Nucléaire à Basse Energie, Centre d'Etudes Nucléaires de Saclay, France

  • *Visiting scientist on Contract No. BI-II/12766 with the Centre d'Etudes Nucléaires de Saclay and the Centro Siciliano di Fisica Nucleare e Struttura della Materia, Catania. On leave from the Istituto di Fisica Nucleare and the Istituto Nazionale di Fisica Nucleare, Universita di Catania, Italy.
  • Permanent address: Laboratoire de Physique Nucléaire, Université de Bordeaux, France.

Phys. Rev. C 6, 577 – Published 1 August, 1972

DOI: https://doi.org/10.1103/PhysRevC.6.577

Abstract

The (O16, C12) four-nucleon-transfer reaction has been performed on a Fe54 target using the 46-MeV O16 beam of the FN tandem Van de Graaff at Saclay. The study of the reaction Fe54 (O16, C12)Ni58 shows that the four-nucleon transfer occurs via a direct surface reaction, well described by the quasielastic process formalism due to Frahn and Venter, which is based on the diffractional model. The transfer-reaction cross sections are peaked at the grazing angle where the elastic scattering begins to deviate from the pure Rutherford law. A distorted-wave Born-approximation investigation of nuclear properties of levels reached by (O16, C12) four-nucleon transfer has been performed using the SETILL code based on the generator-coordinate framework. The Q-value dependence of the cross section, as well as the configuration mixing effects, has been estimated. The cases of other 1f2p-shell nuclei have been also investigated.

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