Finite-temperature Hartree-Fock-Bogoliubov calculations in rare earth nuclei

Journal Article · Sat Nov 01 04:00:00 EST 1986 · Phys. Rev. C; (United States)

DOI:https://doi.org/10.1103/PhysRevC.34.1942· OSTI ID:7166299

Goodman, A L

The temperature dependence of deformations and pair gaps is calculated for /sup 148/Sm, /sup 170/Er, and /sup 186,188/Os. Increasing the temperature induces a variety of shape phase transitions: prolate and oblate to spherical, triaxial to oblate, and spherical to prolate. Heating also produces the superfluid to normal phase transition.

• Research Organization: Department of Physics and Quantum Theory Group, Tulane University, New Orleans, Louisiana 70118
• OSTI ID: 7166299
• Journal Information: Phys. Rev. C; (United States), Journal Name: Phys. Rev. C; (United States) Vol. 34:5; ISSN PRVCA
• Country of Publication: United States
• Language: English

Related Subjects

653001 -- Nuclear Theory-- Nuclear Structure
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653001* -- Nuclear Theory-- Nuclear Structure
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73 NUCLEAR PHYSICS AND RADIATION PHYSICS
BARYONS
DAYS LIVING RADIOISOTOPES
DEFORMATION
DIPOLE MOMENTS
ELEMENTARY PARTICLES
ERBIUM 170
ERBIUM ISOTOPES
EVEN-EVEN NUCLEI
FERMIONS
GIANT RESONANCE
HADRONS
HAMILTONIANS
HARTREE-FOCK-BOGOLYUBOV THEORY
HEAVY NUCLEI
INTERMEDIATE MASS NUCLEI
ISOMERIC TRANSITION ISOTOPES
ISOTOPES
MATHEMATICAL OPERATORS
NEUTRONS
NUCLEAR DEFORMATION
NUCLEAR PROPERTIES
NUCLEAR RADII
NUCLEAR STRUCTURE
NUCLEI
NUCLEONS
OSMIUM 186
OSMIUM 188
OSMIUM ISOTOPES
PHASE TRANSFORMATIONS
PROTONS
QUANTUM OPERATORS
RADIOISOTOPES
RARE EARTH ISOTOPES
RARE EARTH NUCLEI
RESONANCE
SAMARIUM 148
SAMARIUM ISOTOPES
STABLE ISOTOPES
TEMPERATURE DEPENDENCE