Abstract

A new semiempirical atomic mass formula is presented. Special emphasis has been put on a theoretical basis for the microscopic (shell-correction) part, which is added to the macroscopic droplet-model expression. The latter includes the response to the surface diffuseness. The shell function, which is simple and analytic, is derived by bunching the average single-particle spectrum of nuclei with correct size according to the magic numbers. Shell effects from the inner shells are taken care of. In addition, ideas of changing magicities along neutron (proton) magic isotone (isotope) chains, and of damping of the off-Fermi-energy-shell contributions are introduced. These may be important for reliable extrapolations to very neutron-rich (or neutron-deficient) regions of the nuclear chart. The final mass formula is a fairly simple analytic expression. In the preliminary fit with 50 free parameters, presented here, 1312 experimentally known atomic masses are reproduced with a rms error, [ ∑ 1312 (M exp−M cal) 2 (1312−50 ] 1 2 of 670 keV. Comparisons with experimental data are presented in figures for the isobaric mass parabolas, masses, radii, and quadrupole moments. Atomic mass predictions for some 8000 nuclei with Z = 3 to 114 and N = 3 to 184, with S n (or S 2 n ) > 0 and with S p > −2 MeV are presented in the main table of this issue. The simple FORTRAN-IV program (mass excess in MeV as a function of Z and A) is available from the authors on request.

Full Text
Paper version not known

Talk to us

Join us for a 30 min session where you can share your feedback and ask us any queries you have

Schedule a call

Disclaimer: All third-party content on this website/platform is and will remain the property of their respective owners and is provided on "as is" basis without any warranties, express or implied. Use of third-party content does not indicate any affiliation, sponsorship with or endorsement by them. Any references to third-party content is to identify the corresponding services and shall be considered fair use under The CopyrightLaw.