Equilibrium, Isoscaling and Nuclear Isotope Thermometry Related to 1 Gev Proton Induced Reactions

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dc.creatorAndronenko, M. N.
dc.creatorAndronenko, L. N.
dc.creatorNeubert, W.
dc.creatorSeliverstov, D. M.
dc.date2001-12-27
dc.date.accessioned2026-07-07T05:36:52Z
dc.date.available2026-07-07T05:36:52Z
dc.descriptionYields of isotopically separated light fragments and residual nuclei produced in p(1GeV)+A collisions have been analyzed. For both fragmentation and spallation reactions isotopic scaling, i.e. factorization of the isotope ratios, was observed. A generalized isoscaling for arbitrary combinations of two systems has been demonstrated. The average isotopic temperature about 4 MeV for fragmentation process was found.
dc.description9 pages, 13 figures
dc.identifierhttps://arxiv.org/abs/nucl-ex/0112014
dc.identifierhttp://arxiv.org/abs/nucl-ex/0112014
dc.identifier.urihttp://salesiana.dossiersoluciones.com/handle/123456789/81134
dc.subjectNuclear Experiment
dc.titleEquilibrium, Isoscaling and Nuclear Isotope Thermometry Related to 1 Gev Proton Induced Reactions
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