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Nuclear ground-state masses and deformations: FRDM(2012)

机译:核基态质量和形变:FRDM(2012)

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摘要

We tabulate the atomic mass excesses and binding energies, ground-state shell-plus-pairing corrections, ground-state microscopic corrections, and nuclear ground-state deformations of 9318 nuclei ranging from O-16 to A = 339. The calculations are based on the finite-range droplet macroscopic and the folded-Yukawa single-particle microscopic nuclear-structure models, which are completely specified. Relative to our FRDM(1992) mass table in Moller 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 macroscopic-model parameter, the density-symmetry coefficient L, 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 ground-state masses.
机译:我们将原子质量过量和结合能,基态壳加配对校正,基态微观校正以及从O-16到A = 339的9318核的核基态变形制成表格。这些计算基于完整描述了有限范围液滴宏观和折叠式Yukawa单粒子微观核结构模型。相对于Moller等人的FRDM(1992)质量表。 (1995年),在相同的模型中获得的结果,但由于计算机能力的限制,对变形的处理得到了显着改善,并且早期需要的近似值较少。现在,模型执行得越准确,实验质量数据库越广泛,越准确,我们就可以确定另一个宏观模型参数,密度对称系数L,该参数在先前的计算中没有变化,但设置为零。因为我们现在意识到FRDM对于裂变中发生的某些高度变形的形状是不准确的,因为某些影响是根据球体周围的摄动得出的,所以我们仅将其宏观参数调整为基态质量。

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