Nuclear groundstate masses and deformations: FRDM(2012)
Here, we tabulate the atomic mass excesses and binding energies, groundstate shellpluspairing corrections, groundstate microscopic corrections, and nuclear groundstate deformations of 9318 nuclei ranging from ^{16}O to A=339. The calculations are based on the finiterange droplet macroscopic and the foldedYukawa singleparticle microscopic nuclearstructure models, which are completely specified. Relative to our FRDM(1992) mass table in Möller et al. (1995), the results are obtained in the same model, but with considerably improved treatment of deformation and fewer of the approximations that were necessary earlier, due to limitations in computer power. The more accurate execution of the model and the more extensive and more accurate experimental mass data base now available allow us to determine one additional macroscopicmodel parameter, the densitysymmetry coefficient LL, which was not varied in the previous calculation, but set to zero. Because we now realize that the FRDM is inaccurate for some highly deformed shapes occurring in fission, because some effects are derived in terms of perturbations around a sphere, we only adjust its macroscopic parameters to groundstate masses.
 Authors:

^{[1]};
^{[1]};
^{[2]};
^{[3]}
 Los Alamos National Lab. (LANL), Los Alamos, NM (United States)
 Kyoto Univ., Kyoto (Japan)
 RIKEN Nishina Center, Wako (Japan); Center for Mathematics and Physics Univ. of Aizu, Fukushima (Japan)
 Publication Date:
 Report Number(s):
 LAUR1526310
Journal ID: ISSN 0092640X; PII: S0092640X1600005X
 Grant/Contract Number:
 FG0206ER41407; 25287065; AC5206NA25396
 Type:
 Accepted Manuscript
 Journal Name:
 Atomic Data and Nuclear Data Tables
 Additional Journal Information:
 Journal Volume: 109110; Journal Issue: C; Journal ID: ISSN 0092640X
 Publisher:
 Elsevier
 Research Org:
 Los Alamos National Lab. (LANL), Los Alamos, NM (United States)
 Sponsoring Org:
 USDOE
 Country of Publication:
 United States
 Language:
 English
 Subject:
 73 NUCLEAR PHYSICS AND RADIATION PHYSICS; nuclear masses; fissionbarrier heights; groundstate deformations
 OSTI Identifier:
 1248866
 Alternate Identifier(s):
 OSTI ID: 1325396
Moller, P., Sierk, A. J., Ichikawa, T., and Sagawa, H.. Nuclear groundstate masses and deformations: FRDM(2012). United States: N. p.,
Web. doi:10.1016/j.adt.2015.10.002.
Moller, P., Sierk, A. J., Ichikawa, T., & Sagawa, H.. Nuclear groundstate masses and deformations: FRDM(2012). United States. doi:10.1016/j.adt.2015.10.002.
Moller, P., Sierk, A. J., Ichikawa, T., and Sagawa, H.. 2016.
"Nuclear groundstate masses and deformations: FRDM(2012)". United States.
doi:10.1016/j.adt.2015.10.002. https://www.osti.gov/servlets/purl/1248866.
@article{osti_1248866,
title = {Nuclear groundstate masses and deformations: FRDM(2012)},
author = {Moller, P. and Sierk, A. J. and Ichikawa, T. and Sagawa, H.},
abstractNote = {Here, we tabulate the atomic mass excesses and binding energies, groundstate shellpluspairing corrections, groundstate microscopic corrections, and nuclear groundstate deformations of 9318 nuclei ranging from 16O to A=339. The calculations are based on the finiterange droplet macroscopic and the foldedYukawa singleparticle microscopic nuclearstructure models, which are completely specified. Relative to our FRDM(1992) mass table in Möller et al. (1995), the results are obtained in the same model, but with considerably improved treatment of deformation and fewer of the approximations that were necessary earlier, due to limitations in computer power. The more accurate execution of the model and the more extensive and more accurate experimental mass data base now available allow us to determine one additional macroscopicmodel parameter, the densitysymmetry coefficient LL, which was not varied in the previous calculation, but set to zero. Because we now realize that the FRDM is inaccurate for some highly deformed shapes occurring in fission, because some effects are derived in terms of perturbations around a sphere, we only adjust its macroscopic parameters to groundstate masses.},
doi = {10.1016/j.adt.2015.10.002},
journal = {Atomic Data and Nuclear Data Tables},
number = C,
volume = 109110,
place = {United States},
year = {2016},
month = {3}
}