论文标题
在核中的同质 - 阿拉穆状态的反转上
On the inversion of isobaric-analogue states in nuclei
论文作者
论文摘要
同源性是原子核中的近似对称性,是由质子和中子相当相似的特性引起的。核内同质蛋白的最明显表现也许是在镜子核中激发态的近乎相同的结构:核数和中子数量倒数的核。等素对称性,因此是镜面对称性,被电磁相互作用和上下夸克质量的差异打破。霍夫(Hoff)和合作者最近的一项研究表明,$^{73} $ sr的基态旋转与镜子的基础旋转不同,$^{73} $ br,由于接地和先开启的状态的反转,仅在$^{73} $ br系统中仅由27 kev隔开。在此简短说明中,我们将这种反演放置在过去半个世纪的实验和理论工作的必要情况下,并表明它与正常行为完全一致,并且对Isospin-MemememeTry breaking breaking没有新的见解。重要的一点是,由于库仑相互作用而引起的同胞破裂效应通常在给定的中等质量核中的水平与水平不等,高达200 keV。任何小于此的分裂水平都可能表现出镜面伙伴中的水平反转,而镜子伙伴没有与适当的核模型分歧,并不会挑战我们的理解。虽然我们注意到核基地状倒置的新颖性,但我们强调,在同义词的背景下,对基态或水平倒置没有什么特别的启发。
Isospin is an approximate symmetry in atomic nuclei, arising from the rather similar properties of protons and neutrons. Perhaps the clearest manifestation of isospin within nuclei is in the near-identical structure of excited states in mirror nuclei: nuclei with inverted numbers of protons and neutrons. Isospin symmetry, and therefore mirror-symmetry, is broken by electromagnetic interactions and the difference in the masses of the up and down quarks. A recent study by Hoff and collaborators presented evidence that the ground-state spin of $^{73}$Sr is different from that of its mirror, $^{73}$Br, due to an inversion of the ground- and first-excited states, separated by only 27 keV in the $^{73}$Br system. In this brief note, we place this inversion within the necessary context of the past half-century of experimental and theoretical work, and show that it is entirely consistent with normal behaviour, and affords no new insight into isospin-symmetry breaking. The essential point is that isospin-breaking effects due to the Coulomb interaction frequently vary from level to level within a given medium-mass nucleus by as much as 200 keV. Any level splitting smaller than this is liable to manifest a level inversion in the mirror partner which, absent disagreement with an appropriate nuclear model, does not challenge our understanding. While we note the novelty of an inversion in nuclear ground states, we emphasize that in the context of isospin there is nothing specifically illuminating about the ground state, or a level inversion.