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

机译:核地基质量和变形:FRDm(2012)

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摘要

We tabulate the atomic mass excesses and binding energies, ground-stateshell-plus-pairing corrections, ground-state microscopic corrections, andnuclear ground-state deformations of 9318 nuclei ranging from $^{16}$O to$A=339$. The calculations are based on the finite-range droplet macroscopicmodel and the folded-Yukawa single-particle microscopic model. Relative to ourFRDM(1992) mass table in {\sc Atomic Data and Nuclear Data Tables} [{\bf 59}185 (1995)], the results are obtained in the same model, but with considerablyimproved treatment of deformation and fewer of the approximations that werenecessary earlier, due to limitations in computer power. The more accurateexecution of the model and the more extensive and more accurate experimentalmass data base now available allows us to determine one additionalmacroscopic-model parameter, the density-symmetry coefficient $L$, which wasnot varied in the previous calculation, but set to zero. Because we now realizethat the FRDM is inaccurate for some highly deformed shapes occurring infission, because some effects are derived in terms of perturbations around asphere, we only adjust its macroscopic parameters to ground-state masses. Thevalues of ten constants are determined directly from an optimization to fitground-state masses of 2149 nuclei ranging from $^{16}$O to $^{265}_{106}$Sgand $^{264}_{108}$Hs. The error of the mass model is 0.5595~MeV. We alsoprovide masses in the FRLDM, which in the more accurate treatments now has anerror of 0.6618 MeV. But in contrast to the FRDM, it is suitable for studies offission and has been extensively so applied elsewhere, with FRLDM(2002)constants. The FRLDM(2012) fits 31 fission barrier heights from $^{70}$Se to$^{252}$Cf with a root-mean-square deviation of 1.052 MeV.
机译:我们将9318原子核的原子质量过剩和结合能,基态-壳对配对校正,基态微观校正和核基态变形列表化,范围从$ ^ {16} $ O到$ A = 339 $。该计算基于有限范围的液滴宏观模型和折叠的Yukawa单颗粒微观模型。相对于{\ sc原子数据和核数据表} [{\ bf 59} 185(1995)]中的FRDM(1992)质量表,可以在同一模型中获得结果,但是对变形的处理得到了显着改善,并且变形量较少。由于计算机功能的限制,因此需要较早的近似值。该模型的执行更加精确,并且现在可获得更广泛,更准确的实验质量数据库,这使我们能够确定一个附加的宏观模型参数,即密度对称系数$ L $,该参数在先前的计算中未发生变化,但设置为零。因为我们现在意识到FRDM对于某些高度变形的形状发生的扩散是不准确的,因为某些影响是根据非球面周围的扰动得出的,所以我们仅将其宏观参数调整为基态质量。十个常数的值直接从优化到2149个原子核的基态质量确定,范围从$ ^ {16} $ O到$ ^ {265} _ {106} $ Sgand $ ^ {264} _ {108} $ Hs 。质量模型的误差为0.5595〜MeV。我们还在FRLDM中提供质量,以更精确的处理方法现在的误差为0.6618 MeV。但是与FRDM相比,它适合于研究问题,并且已与FRLDM(2002)常数一起广泛应用于其他地方。 FRLDM(2012)拟合了31个裂变屏障高度,从$ ^ {70} $ Se到$ ^ {252} $ Cf,均方根偏差为1.052 MeV。

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