We report on a novel experimental approach for studying the dissipative spreading of collective motion in a meta-stable nuclear system, using, for the first time, highly fissile nuclei with spherical shape. This was achieved by fragmentation of 45 radioactive heavy-ion beams at GSI, Darmstadt. The use of inverse kinematics and a dedicated experimental set-up allowed for the identification in atomic number of both fission fragments. From the width of their charge distributions, a transient time of (3.3±0.7).
10-21 s is deduced for initially spherical nuclei.The problem of escape from a meta-stable state appears in many fields as various as fluid mechanics, chemistry or nuclear physics [1]. An excellent test case for such a process is nuclear fission. Once an excited system has been produced, the collective coordinates start adjusting to the potential-energy landscape, and the distribution of shapes inside the fission saddle develops towards thermo-dynamical quasi-equilibrium. After some time delay, all states in the quasi-bound region are populated according to the available phase space, including those above the fission saddle. Once the system leaves the quasi-bound region, it is driven by the dominating Coulomb force to more elongated shapes and finally separates into two fragments.The ideal scenario for studying the dynamics of the fission process is described in the pioneering theoretical work of Grangé, Weidenmüller and collaborators [2, 3]: They have chosen an initial excited system characterized by a spherical shape. In this case, the probability distribution starts from a configuration where the level density has a local maximum. Under this specific initial condition, the maximum of the probability distribution does not move. The distribution only spreads out under the influence of dissipation due to the fluctuating forces. In contrast, the evolution from saddle to scission is characterized by a strong driving force, and it is the friction force which dominates the dissipation mechanism by slowing down the directed motion towards scission and increasing the saddle-to-scission time relative to its non-viscous limit. Thus, in this ideal scenario starting from the bottom of a spherical potential well, the two stages of the fission process probe selectively the two dissipative phenomena, diffusion and friction, in nuclei [4]. The present work is motivated by the idea to study the time scale of nuclear diffusion. † Present address : Université Lyon I, CNRS/IN2P3, IPNL, Rue Enrico Fermi, 69622 Villeurbanne, France.