New region of nuclear deformation with N approx. = Z approx. = 40
Conference
·
OSTI ID:6594246
A technique has been developed for assigning the isotopic origin of gamma rays emitted following compound nuclear reactions. A survey has been made of the region with N approx. = Z approx. = 40 and bands of states have been observed in 13 previously unstudied nuclei. Our data indicate this region contains some of the most deformed nuclei known, and that the size of deformation is very sensitive to N,Z and angular momentum J.
- Research Organization:
- Manchester Univ. (UK); Liverpool Univ. (UK); Science Research Council, Daresbury (UK). Daresbury Lab.; Brookhaven National Lab., Upton, NY (USA)
- DOE Contract Number:
- AC02-76CH00016
- OSTI ID:
- 6594246
- Report Number(s):
- BNL-32162; CONF-821143-1; ON: DE83003943
- Country of Publication:
- United States
- Language:
- English
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Related Subjects
651623* -- Nuclear Properties & Reactions
A=59-89
Experimental-- Energy Levels & Transitions-- (-1987)
73 NUCLEAR PHYSICS AND RADIATION PHYSICS
ALKALI METAL ISOTOPES
ALKALINE EARTH ISOTOPES
ANGULAR MOMENTUM
CHARGED-PARTICLE REACTIONS
COMPOUND NUCLEI
COMPOUND-NUCLEUS REACTIONS
DEFORMATION
DEFORMED NUCLEI
ENERGY LEVELS
GAMMA SPECTROSCOPY
HEAVY ION REACTIONS
INTERMEDIATE MASS NUCLEI
ISOTOPES
KRYPTON ISOTOPES
NEUTRON-DEFICIENT ISOTOPES
NIOBIUM ISOTOPES
NUCLEAR DEFORMATION
NUCLEAR REACTIONS
NUCLEI
RADIOISOTOPES
RUBIDIUM ISOTOPES
SPECTROSCOPY
STRONTIUM ISOTOPES
YTTRIUM ISOTOPES
ZIRCONIUM ISOTOPES
A=59-89
Experimental-- Energy Levels & Transitions-- (-1987)
73 NUCLEAR PHYSICS AND RADIATION PHYSICS
ALKALI METAL ISOTOPES
ALKALINE EARTH ISOTOPES
ANGULAR MOMENTUM
CHARGED-PARTICLE REACTIONS
COMPOUND NUCLEI
COMPOUND-NUCLEUS REACTIONS
DEFORMATION
DEFORMED NUCLEI
ENERGY LEVELS
GAMMA SPECTROSCOPY
HEAVY ION REACTIONS
INTERMEDIATE MASS NUCLEI
ISOTOPES
KRYPTON ISOTOPES
NEUTRON-DEFICIENT ISOTOPES
NIOBIUM ISOTOPES
NUCLEAR DEFORMATION
NUCLEAR REACTIONS
NUCLEI
RADIOISOTOPES
RUBIDIUM ISOTOPES
SPECTROSCOPY
STRONTIUM ISOTOPES
YTTRIUM ISOTOPES
ZIRCONIUM ISOTOPES