The 32S+40,48Ca systems at 17AMeV have been characterized both for fusion and for peripheral events thanks to the GARFIELD setup, which covers a wide angular range and has high granularity; moreover, isotopic identification for forward emitted ions up to Z around 15 is obtained. The main evidences reported here concern pre-equilibrium emission, which was put into evidence in fusion-evaporation events, and isospin diffusion observed studying the average N/Z of the Quasi-Projectile as a function of the target isospin.
First results on the 32S+40,48Ca reactions at 17.7AMeV studied with GARFIELD setup at LNL / Piantelli, S., Valdre', S., Barlini, S., Casini, G., Colonna, M., Baiocco, G., Bini, M., Bruno, M., Camaiani, A., Cicerchia, M., Cinausero, M., D'Agostino, M., Degerlier, M., Fabris, D., Gramegna, F., Kravchuck, V.L., Mabiala, J., Marchi, T., Morelli, L., Olmi, A., et al.. - In: IL NUOVO CIMENTO C. - ISSN 2037-4909. - ELETTRONICO. - 39:(2016), pp. 0-0. (IWM-EC 2016 ) [10.1393/ncc/i2016-16396-4].
First results on the 32S+40,48Ca reactions at 17.7AMeV studied with GARFIELD setup at LNL
Piantelli, S.;Valdre, S.;Barlini, S.;Casini, G.;Bini, M.;CAMAIANI, ALBERTO;Olmi, A.;OTTANELLI, PIETRO;Pasquali, G.;Pastore, G.
2016
Abstract
The 32S+40,48Ca systems at 17AMeV have been characterized both for fusion and for peripheral events thanks to the GARFIELD setup, which covers a wide angular range and has high granularity; moreover, isotopic identification for forward emitted ions up to Z around 15 is obtained. The main evidences reported here concern pre-equilibrium emission, which was put into evidence in fusion-evaporation events, and isospin diffusion observed studying the average N/Z of the Quasi-Projectile as a function of the target isospin.
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