Nuclear masses, deformations and shell effects

Physics – Nuclear Physics – Nuclear Theory

Scientific paper

Rate now

  [ 0.00 ] – not rated yet Voters 0   Comments 0

Details

10 pages, 8 tables, Proc. of the XXXIV Nuclear Physics Symposium, January 4-7 2011, Cocoyoc, Morelos, Mexico. IOP Journal of P

Scientific paper

We show that the Liquid Drop Model is best suited to describe the masses of prolate deformed nuclei than of spherical nuclei. To this end three Liquid Drop Mass formulas are employed to describe nuclear masses of eight sets of nuclei with similar quadrupole deformations. It is shown that they are able to fit the measured masses of prolate deformed nuclei with an RMS smaller than 750 keV, while for the spherical nuclei the RMS is, in the three cases, larger than 2000 keV. The RMS of the best fit of the masses of semi-magic nuclei is also larger than 2000 keV. The parameters of the three models are studied, showing that the surface symmetry term is the one which varies the most from one group of nuclei to another. In one model, isospin dependent terms are also found to exhibit strong changes. The inclusion of shell effects allows for better fits, which continue to be better in the prolate deformed nuclei region

No associations

LandOfFree

Say what you really think

Search LandOfFree.com for scientists and scientific papers. Rate them and share your experience with other people.

Rating

Nuclear masses, deformations and shell effects does not yet have a rating. At this time, there are no reviews or comments for this scientific paper.

If you have personal experience with Nuclear masses, deformations and shell effects, we encourage you to share that experience with our LandOfFree.com community. Your opinion is very important and Nuclear masses, deformations and shell effects will most certainly appreciate the feedback.

Rate now

     

Profile ID: LFWR-SCP-O-662878

  Search
All data on this website is collected from public sources. Our data reflects the most accurate information available at the time of publication.