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Beta-decay half-life of the rp-process waiting-point nuclide molybdenum-84.

机译:rp-过程等待点核钼钼84的Beta衰变半衰期。

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84Mo is an even-even N = Z nucleus lying on the proton drip line that is thought to be created during explosive hydrogen burning in Type I X-ray bursts in the astrophysical rapid proton capture (rp) process. 84Mo is an important waiting point in the rp-process reaction sequence, determining mass abundance at and procession beyond A = 84 for stable isotopes on the proton-rich side of the valley of stability [1]. A previous experiment established the half-life of 84Mo to be 3.7+1.0-0.8 s [2]. However, treatment of the background and the poor statistics accumulated during that study left questions about the statistical and systematic errors in the measurement. The half-life of 84Mo has been re-measured using a concerted setup of the NSCL beta Counting System (BCS) [3] and 16 detectors from the Segmented Germanium Array (SeGA) [4]. The BCS relies on a highly-segmented Si detector to correlate implantations and subsequent beta decays on an event-by-event basis. The correlation method employed to deduce half-lives and other properties of the beta decay required that the average time between implantations be larger than the half-life of the nuclide under study. Consequently, the overall implantation rate into this detector must be carefully controlled, without negatively affecting the typically low rate of the desired isotope. The recently constructed Radio Frequency Fragment Separator (RFFS) [5] at NSCL was used to purify 84Mo based on relative time-of-flight differences between the beam species of interest, isotonic contaminants, and contaminants due to the overlap of low momentum tails of high-yield beam species. A half-life of 2.2(2) s was deduced for 84Mo, based on a sample of 1037 implantations, more than 30 times larger than the previous study. The new half-life reduced the uncertainty in the amount of 84Mo formed in the rp process, and the consequent amount of 84Sr, to less than a factor 2. Implications of the new half-life on theoretical treatments of nuclear level density near A = 84 along N = Z will also be discussed. The performance capabilities of the RFFS in rejecting unwanted isotopes associated with the production of 84 Mo will be reported as well.
机译:84Mo是位于质子滴线上的偶数N = Z核,据认为是在天体物理快速质子捕获(rp)过程中在I型X射线爆发的爆炸性氢燃烧中产生的。 84Mo是rp过程反应序列中的重要等待点,它决定了稳定谷富质子侧稳定同位素的A = 84处的质量丰度和超过A = 84的丰度[1]。先前的实验确定84Mo的半衰期为3.7 + 1.0-0.8 s [2]。但是,对背景的处理以及在该研究期间积累的统计数据不佳,使人们对测量中的统计和系统误差产生了疑问。 84Mo的半衰期已通过协调设置的NSCL beta计数系统(BCS)[3]和分段锗阵列(SeGA)的16个检测器[4]进行了重新测量。 BCS依靠高度细分的Si检测器来逐事件关联注入和随后的β衰变。用于推导β衰变的半衰期和其他特性的相关方法要求植入之间的平均时间大于所研究核素的半衰期。因此,必须小心控制该检测器的总体注入速率,而又不会对所需同位素的通常较低速率产生负面影响。 NSCL最近构造的射频碎片分离器(RFFS)[5]用于根据感兴趣的光束种类,等渗污染物和由于低动量尾部重叠而产生的污染物之间的相对飞行时间差来纯化84Mo。高产束种。基于1037次植入的样本,得出84Mo的半衰期为2.2(2)s,是先前研究的30倍以上。新的半衰期将rp过程中形成的84Mo量的不确定性以及随之而来的84Sr的不确定性降低到小于2倍。新的半衰期对A =附近的核能级密度理论处理的意义还将讨论沿着N = Z的84。还将报告RFFS抑制与84 Mo产生相关的有害同位素的性能。

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