Abstract
Fragments from the breakup of 32 MeV/nucleon and projectile nuclei were measured with isotopic resolution using the FAUST detector array. Complete reconstruction of the fragmenting source was performed on an event-by-event basis. Events analyzed in this study were restricted to those with a summed fragment charge equal to the beam in which all fragments were isotopically identified. The change in neutron content of the projectile could be inferred from the complete isotopic reconstruction of the quasiprojectile. The present in the fragmenting source is not equal to the of the initial beam; there has been a shift toward the valley of stability. Additionally, there is now a distribution in the of the fragmenting system. Multineutron transfer from the neutron-rich target was observed for proton-rich projectiles.
- Received 11 June 2001
DOI:https://doi.org/10.1103/PhysRevC.67.064602
©2003 American Physical Society