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首页> 外文期刊>Advances in space research >Spin-isospin transitions in chromium isotopes within the quasiparticle random phase approximation
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Spin-isospin transitions in chromium isotopes within the quasiparticle random phase approximation

机译:准粒子随机相近似内铬同位素的自旋-同旋旋跃迁

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摘要

Beta decay and electron capture on isotopes of chromium are advocated to play a key role in the stellar evolution process. In this paper we endeavor to study charge-changing transitions for 24 isotopes of chromium (~(42-65)Cr). These include neutron-rich and neutron-deficient isotopes of chromium. Three different models from the QRPA genre, namely the pn-QRPA, the Pyatov method (PM) and the Schematic model (SM), were selected to calculate and study the Gamow-Teller (GT) transitions in chromium isotopes. The SM was employed separately in the particle-particle (pp) and pp + particle-hole (ph) channels. To study the effect of deformation, the SM was first used assuming the nuclei to be spherical and later to be deformed. The PM was used both in pp and pp + ph channels but only for the case of spherical nuclei. The pn-QRPA calculation was done by considering both pp and ph forces and taking deformation of nucleus into consideration. A recent study proved this version of pn-QRPA to be the best for calculation of GT strength distributions amongst the QRPA models. The pn-QRPA model calculated GT distributions had low-lying centroids and small widths as compared to other QRPA models. Our calculation results were also compared with other theoretical models and measurements wherever available. Our results are in decent agreement with previous measurements and shell model calculations.
机译:提倡β衰变和铬同位素上的电子俘获在恒星演化过程中起关键作用。在本文中,我们努力研究24种铬(〜(42-65)Cr)的电荷变化跃迁。这些包括富中子和缺乏中子的铬同位素。选择了QRPA类型的三种不同模型,即pn-QRPA,Pyatov方法(PM)和示意图模型(SM),以计算和研究铬同位素中的Gamow-Teller(GT)跃迁。 SM分别用于颗粒-颗粒(pp)和pp +颗粒-孔(ph)通道中。为了研究变形的影响,首先使用SM假定原子核为球形,然后假定其变形。 PM用于pp和pp + ph通道,但仅用于球形核。 pn-QRPA的计算是通过同时考虑pp和ph力并考虑原子核的变形来进行的。最近的研究证明,此版本的pn-QRPA是计算QRPA模型中GT强度分布的最佳方法。与其他QRPA模型相比,pn-QRPA模型计算出的GT分布具有较低的质心和较小的宽度。我们还将计算结果与其他可用的理论模型和测量结果进行了比较。我们的结果与以前的测量和壳模型计算非常吻合。

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