Title: Quasimolecular structures and Cold Valleys in Formation and Decay of Heavy Elements
1Quasi-molecular structures and Cold Valleys
in Formation and Decay of Heavy Elements
Serban Misicu, NIPNE-HH, Bucharest
,
,
Walter Greiner, Institut für Theoretische Physik,
Frankfurt am Main
Kemer, 30 September 2003
Quasi-molecular pockets in the heavy-ion
potential Cluster Decay of actindes and
superheavies Orientation windows in fusion and
fission
2Heavy-Ion Potential
Double folding potential with g.s. 1-body
densities
3Heavy-Ion Potential
Double folding potential with g.s. 1-body
densities
Ground state one-body nuclear densities
4Heavy-Ion Potential
Double folding potential with g.s. 1-body
densities
Ground state one-body nuclear densities
M3YCoulomb effective N-N forces
5Heavy-Ion Potential
Double folding potential with g.s. 1-body
densities
Ground state one-body nuclear densities
M3YCoulomb effective N-N forces
6Heavy-Ion Potential
Double folding potential with g.s. 1-body
densities
Ground state one-body nuclear densities
M3YCoulomb effective N-N forces
7Heavy-Ion Potential
Double folding potential with g.s. 1-body
densities
Ground state one-body nuclear densities
M3YCoulomb effective N-N forces
8Heavy-Ion Potential
Double folding potential with g.s. 1-body
densities
Ground state one-body nuclear densities
M3YCoulomb effective N-N forces
Repulsive Core
9Orientation
10Orientation
11Orientation
Fixed Fission(Molecular) Axis
12Touching Configurations
(i) Pole-Pole(nose-to-nose)
13Touching Configurations
(i) Pole-Pole(nose-to-nose)
(ii) Pole-Equator(nose-to-bely)
14Touching Configurations
(i) Pole-Pole(nose-to-nose)
(ii) Pole-Equator(nose-to-bely)
(iii) Equator-Equator(belly-to-bely)
15Touching Configurations
(i) Pole-Pole(nose-to-nose)
(ii) Pole-Equator(nose-to-bely)
(iii) Equator-Equator(belly-to-bely)
(iv) Equator-Equator Twisted(crossed bellies)
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17Driving Potential
- mass asymmetry
- charge asymmetry
Cold valleys
18Cluster Radioactivity
- The residual nuclei are found in the ground state
or in a low-lying excited state. - Emitters - preactinides and actinides.
Daughters - nuclei around 208Pb.
Clusters from C up to Si. - Decay Rates
19Cluster Radioactivity
- The residual nuclei are found in the ground state
or in a low-lying excited state. - Emitters - preactinides and actinides.
Daughters - nuclei around 208Pb.
Clusters from C up to Si. - Decay Rates
20Cluster Radioactivity
- The residual nuclei are found in the ground state
or in a low-lying excited state. - Emitters - preactinides and actinides.
Daughters - nuclei around 208Pb.
Clusters from C up to Si. - Decay Rates
21Spectroscopic Factors(Cluster Preformation
Probabilities)
Blendowske-Walliser Empirical Law
Semimicroscopic Algebraic Cluster Model
22 Life-time in CR and SF
23Cold Valley in Cluster Radioactivity
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28Cluster Radioactivity in the Superheavy Island ?
29Cold Fission of 252Cf
- Fragments are emitted in their ground-states(no
neutron emission) - Low spins at scission
- High mass yields for light fragments in the range
93 114 (heavy fragments in the range 138
157(Gönnenwein-1996)
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33Kalinin, 2001
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42Capture Reactions with 48Ca Projectiles
FLNR-Dubna
43Capture Cross Sections
44 Coupling with Rotational Band States
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48Barrier Distribution
49Effect of various Orientations
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51Conclusions
- Cold valleys explain qualitatively the occurrence
of cluster radioactivity in actinides - Cold valleys explain the yields of neutronless
spontaneous fission of 252Cf if hexadecupole
deformations are taken into account and fragments
are oriented pole-pole - Cold valleys predicted in the past the best
targets to be used with 48Ca projectiles in the
synthesis reactions leading to superheavy
elements - Cold valleys seem to be a tool to explain the
mass distribution of quasi-fission products in
the synthesis of elements with Z112, 114 and 116
using the equator-equator orientation for
projectile and target